基于树轮资料重建石羊河上游历史时期气候与径流量变化
|
摘要
石羊河流域面临日益恶化的生态环境问题,已成为制约区域经济持续发展的重要因素。过短的气候、水文观测资料,不足于理解气候变化的潜在范围,区域极端事件以及在全球日益变暖的气候背景下区域气候、径流如何响应。树木年轮具有定年准确、连续性好、分辨率高、对环境变化敏感性强等优势,已在全球气候变化研究中被广泛应用。本文以石羊河上游为研究区,建立树轮网络,以树轮的宽度、灰度和密度参数作为研究对象,系统的分析树轮年表的变化特点及其环境意义,建立石羊河上游高分辨率的气候、径流序列,分析其演变规律,并对气候、径流变化的机制、机理进行探讨,为水资源变化研究提供丰富的数据资料,对建立合理的水资源分配制度、水资源的可持续管理以及未来水资源发展趋势预报,发挥至关重要的作用。主要的研究内容和结果为：
1.在石羊河上游合理的采点布局,建立由21个样点组成的树轮网络,获取树轮的宽度、密度和灰度参数,经准确的交叉定年,建立多种参数的树轮年表。年表的变化型一致,石羊河上游树木生长有着共同的限制因子,记录了区域气候信息。对于轮印较清晰的树种,可用图像分析方法代替传统的宽度量测方法,提高工作效率。
2.宽度年表与上年9月到当年4月降水、1-8月温度以及上年9月到当年8月的帕尔默干旱指数(PDSI)相关性最显著。用DendroClim2002软件中的渐变和滑动时段分析方法分析树木生长一气候要素关系随时间的微妙变化,宽度年表与温度、降水相关关系的时间稳定性差,在80年代前后相关性的强度发生改变,此后树木生长对温度的敏感性降低；而PDSI对树木生长的限制作用强烈,稳定性好,持续性强,上年9月到当年8月的水分条件是石羊河上游树木生长的限制性因子。
3.最大密度年表更多地反映温度,特别是夏季温度变化信息,同样最大灰度年表也与夏季温度关系密切,而最小灰度对夏半年(1～8月)温度的响应更为强烈,可用最小灰度这种易获取的相对密度值代替最大绝对密度值,节约实验时间和成本,使树轮分析工作变得简单、有效。温度和水分条件对最大灰度和最小灰度的影响呈反向关系。用最小灰度年表对夏半年最大温度进行重建效果更佳。
4.利用嵌套回归和线性回归模型重建了石羊河上游的干旱变化序列,该区的干湿变化和树轮宽度指数与太阳活动的一致性较好。虽然近几十年祁连山不同地区的干湿变化呈现出差异性,但在较长的时间尺度上,祁连山地区的干湿变化还是一致的。此外,亚洲季风西北边缘区干湿序列的年代际变化也具有同步性。
5.选择最小灰度年表和线性回归对石羊河上游夏半年最大温度进行重建,与祁连山中、西部温度变化具有一致性,表明该区树木年轮指示的气候变化具有一定的区域代表性。石羊河上游气候的年代际变化以冷湿和暖干组合占优势,20世纪20、30、60和90年代的暖干期,20世纪初、40和50年代的冷湿期,在一定程度上可以表征冷龙岭冰川的进退。周期分析显示,该区的干旱序列和温度序列均包含35、4.14和2.6年的周期,该区的气候变化与ENSO和太平洋年代际涛动(PDO)关系密切,但是在20世纪初北极涛动(AO)对该区温度的影响更为强烈。
6.上年9月至当年8月的水分条件是形成年轮一径流量良好相关性的物理气候学基础。采用不同的回归模型,分别对各支流径流量进行重建,探讨了径流量在不同时间尺度上的变化规律。各支流补给来源较稳定,年际变化不大,平水年出现概率最高,极端丰、枯水年出现的概率基本相同。径流的丰枯变化对应于气候的冷湿、暖干变化,其中水分条件对径流变化的影响较温度更为强烈。
In the past few years, many serious ecological problems caused by the shortage of water resources, such as discontinuous surface runoff, dried lakes, lowered groundwater level, and deteriorated water quality had emerged in the Shiyang River Basin. But hydrologic observation data were short and clearly insufficient for understanding the extremes, and how hydrological variability may be changing in a warming world. And few high-resolution and long researches had been carried out in this region yet. Compared with most of palaeoclimatological proxies, tree-ring showed advantages in its relative high-resolution and annual time-series for calibrating the relationships between climate and proxy, and it had been well established as records of past climate and streaflow changes. The upstream of the Shiyang River was chosen as the focuses of this study. We present some of the first hydrometeorological reconstructions for this region using a tree-ring chronology network from Picea crassifolia using multiple sites across Lenglongling Mountain, and extended available instrumental observations by more than one century. The results should contribute to sustainable water management solutions in the face of increasing water scarcity and growing conflicts over water use for the Shiyang River Basin and to the methodology of incorporating tree-ring data in the assessment of the probability of hydrologic drought.
Twenty-one sampling sites were selected in the upstream of the Shiyang River, and a total of 805 increment cores were extracted with standard increment borers. Cores were cross-dated by visual growth pattern matching, statistical tests in the software package TSAP and skeleton in the WinDENDRO, possible dating errors were re-checked using the quality control software COFECHA. Finally, thirty-four new tree-ring width chronologies, four maximum density chronologies, thirty-four minimum gray chronologies, and twelve maximum gray chronologies were developed in study area.
Width chronologies were significant related to precipitation from previous September to current April, mean temperature from January to August, and mean PDSI (Palmer Drought Severity Index) from previous September to current August. Correlation and stability analyses calculated by the program of DendroClim2002 showed that regional moisture conditions were the main environmental factor limiting tree growth at Lenglongling Mountain and PDSI as a predictand for drought reconstructions was much more appropriate than any climatic variable. Two maximum density standardized chronologies were significant negative related to maximum temperature from January to August, minimum gray chronologies were significant positive related to maximum temperature from January to August, and maximum gray chronologies were negative related to summer temperature.
Drought fluctuations in the upstream of the Shiyang River were reconstructed using nest and linear regressions. PDSI reconstructions successfully captured both high-frequency (three extreme drought events and two significant humid events) and low-frequency (three obvious descendent periods and two ascendant periods) variations of local moisture availability. By comparing our reconstruction with other available drought reconstructions, the results indicated that good consistency in multi-decadal-scale moisture variations in Qilian Mountains and similar regional moisture variations and analogous modes of climate forcing on tree growth in the northwest margin of the Asian monsoon. Mean maximum temperature from January to August in the upstream of the Shiyang River was reconstructed based on minimum gray chronologies. During 1920s,1930s,1960s and 1990s, the climate was warm and dry. The dominant periodicities of drought and temperature reconstructions were 35,4.14 and 2.6-years obtained by multi-taper method of spectrum analysis. Climate change in study area was closely related to surface sea temperature variations in Pacific.
To understand the hydrologic response of the radial growth of Picea crassifolia, correlation analyses of tree-ring chronologies with precipitation and runoff were conducted. The results showed that chronologies were significantly and strongly related to total runoff from September of the previous year to August of the growing year (RSA), chronologies also had significant and positive relationships with total precipitation from September of the previous year to August of the growing year (PSA), and the correlation coefficients between RSA and PSA were significant and positive. Therefore, precipitation played a role of bridge and tie between tree-rings and runoff. Then, annual runoff series of Jinta, Zamu and Huangyang Rivers were reconstructed according to multiple linear stepwise regression models, and runoff series of Xiying River were reconstructed utilizing principal components extraction and stepwise regression, and all models were tested by the methods of leave-one-out and cross-verification. There was a notable correlation between four runoff series, with a correlation coefficient of 0.52. Four series had the same change tendency, and contained four severe dry periods (during 1880-1892,1925-1935,1960-1967, and 1997-2002) and three significant wet periods (occurred in 1894-1923,1935-1959, and 1967-1986). The dominant periods calculated by MTM spectrum analysis were 2-4 and 35 years at different significant levels.
1.在石羊河上游合理的采点布局,建立由21个样点组成的树轮网络,获取树轮的宽度、密度和灰度参数,经准确的交叉定年,建立多种参数的树轮年表。年表的变化型一致,石羊河上游树木生长有着共同的限制因子,记录了区域气候信息。对于轮印较清晰的树种,可用图像分析方法代替传统的宽度量测方法,提高工作效率。
2.宽度年表与上年9月到当年4月降水、1-8月温度以及上年9月到当年8月的帕尔默干旱指数(PDSI)相关性最显著。用DendroClim2002软件中的渐变和滑动时段分析方法分析树木生长一气候要素关系随时间的微妙变化,宽度年表与温度、降水相关关系的时间稳定性差,在80年代前后相关性的强度发生改变,此后树木生长对温度的敏感性降低；而PDSI对树木生长的限制作用强烈,稳定性好,持续性强,上年9月到当年8月的水分条件是石羊河上游树木生长的限制性因子。
3.最大密度年表更多地反映温度,特别是夏季温度变化信息,同样最大灰度年表也与夏季温度关系密切,而最小灰度对夏半年(1～8月)温度的响应更为强烈,可用最小灰度这种易获取的相对密度值代替最大绝对密度值,节约实验时间和成本,使树轮分析工作变得简单、有效。温度和水分条件对最大灰度和最小灰度的影响呈反向关系。用最小灰度年表对夏半年最大温度进行重建效果更佳。
4.利用嵌套回归和线性回归模型重建了石羊河上游的干旱变化序列,该区的干湿变化和树轮宽度指数与太阳活动的一致性较好。虽然近几十年祁连山不同地区的干湿变化呈现出差异性,但在较长的时间尺度上,祁连山地区的干湿变化还是一致的。此外,亚洲季风西北边缘区干湿序列的年代际变化也具有同步性。
5.选择最小灰度年表和线性回归对石羊河上游夏半年最大温度进行重建,与祁连山中、西部温度变化具有一致性,表明该区树木年轮指示的气候变化具有一定的区域代表性。石羊河上游气候的年代际变化以冷湿和暖干组合占优势,20世纪20、30、60和90年代的暖干期,20世纪初、40和50年代的冷湿期,在一定程度上可以表征冷龙岭冰川的进退。周期分析显示,该区的干旱序列和温度序列均包含35、4.14和2.6年的周期,该区的气候变化与ENSO和太平洋年代际涛动(PDO)关系密切,但是在20世纪初北极涛动(AO)对该区温度的影响更为强烈。
6.上年9月至当年8月的水分条件是形成年轮一径流量良好相关性的物理气候学基础。采用不同的回归模型,分别对各支流径流量进行重建,探讨了径流量在不同时间尺度上的变化规律。各支流补给来源较稳定,年际变化不大,平水年出现概率最高,极端丰、枯水年出现的概率基本相同。径流的丰枯变化对应于气候的冷湿、暖干变化,其中水分条件对径流变化的影响较温度更为强烈。
In the past few years, many serious ecological problems caused by the shortage of water resources, such as discontinuous surface runoff, dried lakes, lowered groundwater level, and deteriorated water quality had emerged in the Shiyang River Basin. But hydrologic observation data were short and clearly insufficient for understanding the extremes, and how hydrological variability may be changing in a warming world. And few high-resolution and long researches had been carried out in this region yet. Compared with most of palaeoclimatological proxies, tree-ring showed advantages in its relative high-resolution and annual time-series for calibrating the relationships between climate and proxy, and it had been well established as records of past climate and streaflow changes. The upstream of the Shiyang River was chosen as the focuses of this study. We present some of the first hydrometeorological reconstructions for this region using a tree-ring chronology network from Picea crassifolia using multiple sites across Lenglongling Mountain, and extended available instrumental observations by more than one century. The results should contribute to sustainable water management solutions in the face of increasing water scarcity and growing conflicts over water use for the Shiyang River Basin and to the methodology of incorporating tree-ring data in the assessment of the probability of hydrologic drought.
Twenty-one sampling sites were selected in the upstream of the Shiyang River, and a total of 805 increment cores were extracted with standard increment borers. Cores were cross-dated by visual growth pattern matching, statistical tests in the software package TSAP and skeleton in the WinDENDRO, possible dating errors were re-checked using the quality control software COFECHA. Finally, thirty-four new tree-ring width chronologies, four maximum density chronologies, thirty-four minimum gray chronologies, and twelve maximum gray chronologies were developed in study area.
Width chronologies were significant related to precipitation from previous September to current April, mean temperature from January to August, and mean PDSI (Palmer Drought Severity Index) from previous September to current August. Correlation and stability analyses calculated by the program of DendroClim2002 showed that regional moisture conditions were the main environmental factor limiting tree growth at Lenglongling Mountain and PDSI as a predictand for drought reconstructions was much more appropriate than any climatic variable. Two maximum density standardized chronologies were significant negative related to maximum temperature from January to August, minimum gray chronologies were significant positive related to maximum temperature from January to August, and maximum gray chronologies were negative related to summer temperature.
Drought fluctuations in the upstream of the Shiyang River were reconstructed using nest and linear regressions. PDSI reconstructions successfully captured both high-frequency (three extreme drought events and two significant humid events) and low-frequency (three obvious descendent periods and two ascendant periods) variations of local moisture availability. By comparing our reconstruction with other available drought reconstructions, the results indicated that good consistency in multi-decadal-scale moisture variations in Qilian Mountains and similar regional moisture variations and analogous modes of climate forcing on tree growth in the northwest margin of the Asian monsoon. Mean maximum temperature from January to August in the upstream of the Shiyang River was reconstructed based on minimum gray chronologies. During 1920s,1930s,1960s and 1990s, the climate was warm and dry. The dominant periodicities of drought and temperature reconstructions were 35,4.14 and 2.6-years obtained by multi-taper method of spectrum analysis. Climate change in study area was closely related to surface sea temperature variations in Pacific.
To understand the hydrologic response of the radial growth of Picea crassifolia, correlation analyses of tree-ring chronologies with precipitation and runoff were conducted. The results showed that chronologies were significantly and strongly related to total runoff from September of the previous year to August of the growing year (RSA), chronologies also had significant and positive relationships with total precipitation from September of the previous year to August of the growing year (PSA), and the correlation coefficients between RSA and PSA were significant and positive. Therefore, precipitation played a role of bridge and tie between tree-rings and runoff. Then, annual runoff series of Jinta, Zamu and Huangyang Rivers were reconstructed according to multiple linear stepwise regression models, and runoff series of Xiying River were reconstructed utilizing principal components extraction and stepwise regression, and all models were tested by the methods of leave-one-out and cross-verification. There was a notable correlation between four runoff series, with a correlation coefficient of 0.52. Four series had the same change tendency, and contained four severe dry periods (during 1880-1892,1925-1935,1960-1967, and 1997-2002) and three significant wet periods (occurred in 1894-1923,1935-1959, and 1967-1986). The dominant periods calculated by MTM spectrum analysis were 2-4 and 35 years at different significant levels.
引文
Akkemik U, D'Arrigo R, Cherubini P, et al. Tree-ring reconstructions of precipitation and streamflow for north-western Turkey [J]. International Journal of Climatology, 2008,28:173-183.
Anderson RL, Byrne R, Dawson T. Stable isotope evidence for a foggy climate on Santa Cruz Island, California at -?6,600 cal. yr. B.P[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2008,262:176-181.
Bar A, Pape R, Brauning A et al. Growth-ring variations of dwarf shrubs reflect regional climate signals in alpine environments rather than topoclimatic differences[J]. Journal of Biogeography,2008,35:625-636.
Bale RJ, Robertson I, Leavitt SW, et al. Temporal stability in bristlecone pine tree-ring stable oxygen isotope chronologies over the last two centuries[J]. The Holocene,2010,20:3-6.
Biondi F. Evolutionary and moving response functions in dendroclimatology[J]. Dendrochronologia,1997,15:139-150.
Biondi F. Are cliamte-tree growth relationships changing in north-central Idaho? [J] Arctic, Antarctic, and Alpine Research,2000,32:111-116.
Biondi F, Estrada IG. Tree-Ring Evidence for the 1913 Eruption of Volcan de Fuego de Colima, Mexico[J]. Quaternary Research,2003,59:293-299.
Biondi F, Waikul K. DENDROCLIM2002:a C++ program for statistical calibration of climate signals in tree-ring chronologies [J]. Computer Geoscience,2004,30:303-311.
Black BA, Copenheaver CA, Frank DC, et al. Multi-proxy reconstructions of northeastern Pacific sea surface temperature data from trees and Pacific geoduck[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2009,278:40-47.
Boswijk G, Fowler A, Lorrey A, et al. Extension of the New Zealand kauri (Agathis australis) chronology to 1724 BC[J]. The Holocene,2006,16:188-199.
Briffa KR, Jones PD, Bartholin TS, et al. Fennoscandian summers from AD 500:temperature changes on short and long timescales[J]. Climate Dynamics,1992a,7:111-119.
Briffa KR, Jones PD, Schweingruber FH. Summer temperature patterns over Europe:A reconstruction from 1750 A.D. based on maximum latewood density indices of conifers[J]. Quaternary Research,1988,30:36-52.
Briffa KR, Jones PD, Schweingruber FH. Tree-ring density reconstructions of summer temperature patterns across western North America since 1600[J]. Journal of Climate, 1992b,5:735-754.
Briffa KR, Jones PD, Schweingruber FH, et al. Influence of volcanic eruptions on Northern Hemisphere summer temperature over the past 600 years[J]. Nature,1998,393:450-455.
Brito-Castillo L, Diaz-Castro S, Salinas-Zavala CA, et al. Reconstruction of long-term winter streamflow in the Gulf of California continental watershed[J]. Journal of Hydrology, 2003,278:39-50.
Buntgen U, Brazdil R,Frank D, et al. Three centuries of Slovakian drought dynamics[J]. Climate Dynamics,2009.35:315-329.
Biintgen U, Esper J, Frank DC, et al. A 1052-year tree-ring proxy for Alpine summer temperatures [J]. Climate Dynamics,2005a,25:141-153.
Buntgen U, Esper J, Frank DC, et al. The effect of power transformation on RCS-evidence from three millennial-length alpine chronologies. In:Gartner et al. (Eds.) Proceedings volume. International conference tree rings in archaeology, climatology and ecology, Birmensdorf, Switzerland. Environment 53, Julich,2005b,141-149.
Biintgen U, Frank D, Wilson R, et al. Testing for tree-ring divergence in the European Alps[J]. Global Change Biology,2008,14:1-11.
Cai QF,Liu Y. January to August temperature variability since 1776 inferred from tree-ring width of Pinus tabulaeformis in Helan Mountain[J]. Journal of Geographical Sciences, 2007,17:293-303.
Cai Q F, Liu Y, Song H, et al. Tree-ring-based reconstruction of the April to September mean temperature since 1826 AD for north-central Shaanxi Province, China[J]. Science in China Series D:Earth Sciences,2008,51:1099-1106.
Camarero JJ, Guerrero-Campo G, Gutierrez E. Tree-ring growth and structure of Pinus uncinata and Pinus sylvestris in the central Spanish Pyrenees[J]. Arctic and Alpine Research, 1998,30:1-10.
Campbell R, McCarroll D, Loader NJ, et al. Blue intensity in Pinus sylvestris tree-rings, developing a new palaeoclimate proxy[J]. The Holocene,2007,17:821-828.
Campbell R, McCarroll D, Robertson I, et al. Blue Intensity in Pinus sylvestris tree rings:A manual for a new palaeoclimate proxy[J]. tree-ring research,2011,67:127-134.
Carson EC, Munroe JS. Tree-ring based streamfiow reconstruction for Ashley Creek, northeastern Utah:implications for palaeohydrology of the southern Uinta Mountains[J]. The Holocene,2005,15:602-611.
Case RA, MacDonald GM. A Dendroclimatic Reconstruction of Annual Precipitation on the Western Canadian Prairies since A.D.1505 from Pinus flexilis James[J]. Quaternary Research, 1995,44:267-275.
Case RA, MacDonald GM. Tree ring reconstructions of streamflow for three Canadian Prairie Rivers[J]. Journal of the American Water Resources Association,2003,39:703-716.
Charles CD, Hunter DE, Fairbanks RG. Interaction between the ENSO and the Asian monsoon in a coral record of tropical climate[J]. Science,1997,277:925-928.
Chen J, Wang LL, Zhu HF, et al. Reconstructing mean maximum temperature of growing season from the maximum density of the Schrenk Spruce in Yili, Xinjiang, China[J]. Chinese Science Bulletin,2009,54:2300-2308.
Chinga-Carrasco G. Microscopy and computerized image analysis of wood pulp fibres multiscale structures. In:Mendez-Vilas A, Diaz J (Eds.), Microscopy:Science, Technology, Applications and Education. Microscopy Book Series. Formatex,2011,2182-2189.
Cleaveland MK. a 963-year reconstrucion of summer (JJA) stream flow in the white river,from tree-rings[J]. The Holocene,2000,10:33-41.
Cook ER, D' Arrigo RD, Mann ME. A well-verified, multiproxy reconstruction of the winter North Atlantic Oscillation Index since A.D.1400[J]. Journal of Climate, 2002a,15:1754-1764.
Cook ER, Esper J, D' Arrigo RD. Extra-tropical Northern Hemisphere land temperature variability over the past 1000 years[J]. Quaternary Science Reviews,2004,23:2063-2074.
Cook ER, Kairiukstis A. Methods of Dendrochronology:Applications in the Environmental Sciences[M]. Dordrecht:Kluwer Academic Press,1990.
Cook ER, Keith R, Briffa PDJ. Spatial regression methods in dendroclimatology:A review and comparison of two techniques[J]. International Journal of Climatology,1994,14:379-402.
Cook ER, Meko DM, Stahle DW, et al. Drought reconstructions for the continental United States[J]. Journal of Climate,1999,12:1145-1162.
Cook ER, Palmer JG, D'Arrigo RD. Evidence for a 'Medieval Warm Period' in a 1100 year tree-ring reconstruction of past austral summer temperatures in New Zealand[J]. Geophysical Research Letters,2002b,29:1667-1770.
Cook ER, Seager R, Cane MA, et al. North American drought:Reconstructions, causes, and consequences[J]. Earth-Science Reviews,2007,81:93-134.
Cook ER, Woodhouse CA, Eakin M. Long-Term Aridity Changes in the Western United States[J]. Science,2006,306:1015-1018.
Cropper JP. Tree-ring skeleton plotting by computer[J]. Tree-ring bulletin,1979,39:47-54.
Cruz-Munoz AR, Rodriguez-Fernandez L, Calva-Vazquez G, et al. Effects due to Popocatepetl volcano eruptions on the elemental concentrations in tree growth rings[J]. X-Ray Spectrometry,2008,37:163-168.
Cullen LE, Grierson PF.Multi-decadal scale variability in autumn-winter rainfall in south-western Australia since 1655 AD as reconstructed from tree rings of Callitris columellaris[J]. Climate Dynamics,2009,33:433-444.
D'Arrigo R, Abram N, Ummenhofer C, et al. Reconstructed streamflow for Citarum River, Java, Indonesia:linkages to tropical climate dynamics[J]. Climate Dynamics,2010,36:451-462.
D'Arrigo R, Allan R, Wilson R, et al. Pacific and Indian Ocean climate signals in a tree-ring record of Java monsoon drought[J].International Journal of Climatology, 2008a,28:1889-1901.
D'Arrigo, Cook ER, Wilson RJ, et al. On the variability of ENSO over the past six centuries[J]. Geophysical Research Letters,2005a,32:L03711.
D'arrigo RD, Jacoby GC. Northern north American tree-ring evidence for regional temperature changes after major volcanic events[J]. Climatic Change,1999,41:1-15.
D'Arrigo R, Jacoby G, Frank D, et al.1738 years of Mongolian temperature variability inferred from a tree-ring width chronology of siberian pine[J]. Geophysical Research Letters, 2001,28:543-546.
D'Arrigo R, Mashig E, Frank D, et al. Temperature variability over the past millennium inferred from Northwestern Alaska tree rings[J]. Climate Dynamics,2005b,24:227-236.
D'Arrigo R,Wilson R. El Nino and Indian Ocean influences on Indonesian drought:implications for forecasting rainfall and crop productivity[J]. International Journal of Climatology, 2008b,28:611-616.
D'Arrigo R, Wilson R, Liepert B, et al. On the'Divergence Problem'in Northern Forests:A review of the tree-ring evidence and possible causes[J]. Global and Planetary Change, 2008c,60:289-305.
D'Arrigo R, Wilson R, Jacoby G. On the long-term context for late twentieth century warming[J]. Journal of Geophysical Research.2006a,111:D03103.
D'Arrigo R, Wilson R, Palmer J, et al. Monsoon drought over Java, Indonesia, during the past two centuries[J]. Geophysical Research Letters,2006b,33:L04709.
D'Arrigo R, Wilson R, Palmer J, et al. The reconstructed Indonesian warm pool sea surface temperatures from tree rings and corals:Linkages to Asian monsoon drought and El Nino-Southern Oscillation[J]. Paleoceanography,2006c,21:1-13.
D'arrigo R, Wilson R, Tudhope A. The impact of volcanic forcing on tropical temperatures during the past four centuries[J]. Nature Geoscience,2009,2:51-56.
D'Arrigo R, Wilson R. On the Asian expression of the PDO[J]. International Journal of Climatology,2006d,26:1607-1617.
Dai A. Characteristics and trends in various forms of the Palmer Drought Severity Index (PDSI) during 1900-2008[J]. Journal of Geophysical Research,2011a,116:D12115.
Dai A. Drought under global warming:Areview[J]. Climate Change,2011b,2:45-65.
Dai A, Trenberth KE, Qian T. A global dataset of Palmer Drought Severity Index for 1870-2002: relationship with soil moisture and effects of surface warming[J]. Journal of Hydrometeorology,2004,5:1117-1130.
Davi NK, Jacoby GC, D'Arrigo RD, et al. A tree-ring-based drought index reconstruction for far-western Mongolia:1565-2004[J]. International Journal of Climatology,2008,29: 1508-1514.
Davi NK, Jacoby GC, Wiles GC. Boreal temperature variability inferred from maximum latewood density and tree-ring width data, Wrangell Mountain region, Alaska[J]. Quaternary Research,2003,60:252-262.
Eronen M, Briffa KR, Lindholm M, et al. The supra-long Scots pine tree-ring record for Finnish Lapland:Part 1, chronology construction and initial inferences [J]. The Holocene, 2002,12:673-680.
Esper J, Frank D. Divergence pitfalls in tree-ring research[J]. Climatic Change, 2009,94:261-266.
Esper J, Frank D, Buntgen U, et al. Long-term drought severity variations in Morocco [J]. Geophysical Research Letters,2007,34:L17702.
Esper J, Cook ER, Schweingruber FH. Low-Frequency Signals in Long Tree-Ring Chronologies for Reconstructing Past Temperature Variability [J]. Science,2002,295:2250-2253
Esper J, Cook ER, Krusic PJ, et al. Tests of the RCS method for preserving low-frequency variability in long tree-ring chronologies[J]. tree-ring research,2003,59:81-98.
Fan ZX, Brauning A, Cao KF. Annual temperature reconstruction in the central Hengduan Mountains, China, as deduced from tree rings[J]. Dendrochronologia,2008a,26:97-107.
Fan ZX, Brauning A, Cao KF, et al. Tree-ring based drought reconstruction in the central Hengduan Mountains region (China) since A.D.1655[J]. International Journal of Climatology, 2008b,28:1879-1887.
Fan ZX, Brauning A, Tian QH, et al. Tree ring recorded May-August temperature variations since A.D.1585 in the Gaoligong Mountains, southeastern Tibetan Plateau[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2010,296:94-102.
Fan ZX, Brauning A, Yang B, et al. Tree ring density-based summer temperature reconstruction for the central Hengduan Mountains in southern China[J]. Global and Planetary Change, 2009.65:1-11.
Fang KY, Gao XH. Chen FH. et al. Drought variations in the eastern part of northwest China over the past two centuries:evidence from tree rings[J]. Climate Research,2009,38:129-135.
Fang KY, Gou XH, Chen FH, et al. Tree-ring based drought reconstruction for the Guiqing Mountain (China):linkages to the Indian and Pacific Oceans[J]. International Journal of Climatology,2010a,30:1137-1145.
Fang KY, Gou XH, Chen FH, et al. Reconstructed droughts for the southeastern Tibetan Plateau over the past 568 years and its linkages to the Pacific and Atlantic Ocean climate variability[J]. Climate Dynamics,2010b,35:577-585.
Feng S, Hu Q. Variations in the teleconnection of ENSO and summer rainfall in northern China: a role of the Indian summer monsoon[J]. Journal of Climate,2004,17:4871-4881.
Frank D, Esper J. Temperature reconstructions and comparisons with instrumental data from a tree-ring network for the European Alps[J]. International Journal of Climatology, 2005,25:1437-1454.
Fritts HC. Tree ring and climate[M], London:Academic Press,1976.
Fowler AM, Boswijk G, Gergisb J, et al. ENSO history recorded in Agathis australis (kauri) tree rings. Part A:kauri's potential as an ENSO proxy[J]. International Journal of Climatology, 2008,28:1-20.
Gagen M, Zorita E, McCarroll D, et al. Cloud response to summer temperatures in Fennoscandia over the last thousand years[J]. Geophysical Research Letters,2011,338:L05701.
Gao SY, Lu RJ, Qiang MR, et al. Reconstruction of precipitation in the last 140 years from tree ring at south margin of the Tengger Desert, China[J]. Chinese Science Bulletin, 2005,50:2487-2492.
Gedalof Z, Peterson DL, Mantua NJ. Columbia River flow and drought since 1750[J]. Journal of the American Water Resourses Association,2004,60:1579-1592.
George SS, Nielsen E. Hydroclimatic change in southern Manitoba since A.D.1409 inferred from tree rings [J]. Quaternary Research,2002,58:103-111.
Gindl W, Grabner M, Wimmer R. The influence of temperature on latewood lignin content in treeline Norway spruce compared with maximum density and ring width[J].Trees, 2000.14:409-414.
Glueck MF, Stockton CW. Reconstruction of the North Atlantic Oscillation,1429-1983[J]. International Journal of Climatology,2001,21:1453-1465.
Gou XH, Chen FH, Cook ER, et al. Streamflow variations of the Yellow River over the past 593 years in western China reconstructed from tree rings[J]. Water Resources Research, 2007,43:W06434.
Gou XH, Chen FH, Yang MX, et al. Climatic response of thick leaf spruce(Picea crassifolia) tree-ring width at different elevations over Qilian Mountains, northwestern China[J]. Journal of Arid Environments,2005,61:513-524.
Graumlich LJ. A 1000-Year Record of Temperature and Precipitation in the Sierra Nevada[J]. Quaternary Research,1993,39:249-255.
Graumlich LJ, Pisaric MJ, Waggoner LA. Upper Yellowstone River flow and teleconnections with Pacific basin climate variability during the past three centuries[J]. Climatic Change, 2003,59:245-262.
Grudd H. Briffa KR. Karlen W, et al. A 7400-year tree-ring chronology in northern Swedish Lapland--natural climatic variability expressed on annual to millennial timescales[J]. The Holocene,2002,12:657-665.
Grudd H. Tornetrask tree-ring width and density AD 500-2004:a test of climatic sensitivity and a new 1500-year reconstruction of north Fennoscandian summers[J]. Climate Dynamics, 2008,31:843-857.
Guilderson TP, Schrag DP. Abrupt shift in subsurface temperature in the tropical Pacific associated with changes in El Nino[J]. Science,1998,281:240-243.
Gunnarson BE. Temporal distribution pattern of subfossil pines in central Sweden:perspective on Holocene humidity fluctuations[J]. Holocene,2008,18:569-577.
Heinrich I, Weidner K, Helle G, et al. Hydroclimatic variation in Far North Queensland since 1860 inferred from tree rings[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2008,270:116-127.
Helama S, Lindholm M, Timonen M, et al. The supra-long Scots pine tree-ring record for Finnish Lapland:Part 2, interannual to centennial variability in summer temperatures for 7500 years[J]. The Holocene,2002,12:681-687.
Holmes JA, Cook ER, Yang B. Climate change over the past 2000 years in Western China[J]. Quaternary International,2009,194:91-107.
Hughes M K,张光威,刘季花.根据树轮密度和宽度对公元1600年以来中国中北部降雨量的初步重建[J].海洋地质动态,1995：17-19.
Hughes MK, Brown PM. Drought frequency in central California since 101 B.C. recorded in giant sequoia tree rings[J]. Climate Dynamics,1992,6:161-167.
Hughes MK, Graumlich, LJ. Multimillennial dendroclimatic studies from the western United States. In:Jones PD, Bradley RS, Jouzel J (Eds.), Climatic Variations and Forcing Mechanisms of the Last 2000 Years[M]. Springer-Verlag, Berlin,1996,109-124.
Hurrell JW, Trenberth KE. Sea surface temperature analyses:multiple problems and their implications for climate analysis, modeling, and reanalysis[J]. Bulletin of the American Meteological Society,1999,80:2661-2678.
Jacoby GC, Lovelius NV, Shumilov 01, et al. Long-term temperature trends and tree growth in the Taymir Region of northern Siberia[J]. Quaternary Research,2000,53:312-318.
Jagels, R, Telewski FW. Computer-aided image analysis of tree rings. In:E.R. Cook & L.A. Kairiukstis (eds.), Methods of dendrochronology:Applications in the environmental sciences[M]. Kluwer Academic Publishers, Dordrecht,1990,76-93.
Kirdyanov AV, Vaganov EA, Hughes MK. Separating the climatic signal from tree-ring width and maximum latewood density records[J]. Trees,2007,21:37-44.
Knight TA, Meko DM, Baisan CH. A bimillennial-length tree-ring reconstruction of precipitation for the Tavaputs Plateau, Northeastern Utah[J]. Quaternary Research,2010,73:107-117.
Koretsune S, Fukuda K, Chang Z. Effective rainfall seasons for interannual variation in δ13C and tree-ring width[J]. Journal of Forest Research,2009,14:88-94.
Lan YC, Lin S, Hu XL, et al. Effect of ENSO cycle on the temperature precipitation and runoff in Qilian Mountainous area, northwestern China[J]. Journal of Desert Research, 2009,29:352-258.
Lan YC, Kang ES, Zhang JS. et al. Trends and characteristics on mountainous runoff in Hexi inland arid region[J]. Journal of Desert Research,2002,22:135-141.
Lara A, Urrutia R, Villalba R, et al. The potential use of tree-rings to reconstruct streamflow and estuarine salinity in the Valdivian Rainforest eco-region, Chile[J]. Dendrochronologia, 2005,22:155-161.
Lara A, Villalba R. A 3620-year temperature record from Fitzroya cupressoides tree rings in southern South America[J]. Science,1993,260:1104-1106.
Lara A, Villalba R, Urrutia R. A 400-year tree-ring record of the Puelo River summer-fall streamflow in the Valdivian Rainforest eco-region, Chile[J]. climate Change, 2008,86:331-356.
Lees JM, Park J. Multiple-taper spectral analysis:A stand-alone C-subroutine. Computers & Geosciences,1995,21:199-236.
Li JB, Chen FH, Cook. ER, et al. Drought reconstruction for North Central China from tree rings: the value of the Palmer drought severity index[J]. International Journal of Climatology, 2007,27:903-909.
Li ZS, Shi CM, Liu YB, et al. Summer mean temperature variation from 1710-2005 inferred from tree-ring data of the Baimang Snow Mountains, northwestern Yunnan, China[J]. Climate Research,2011a,47(3):207-218.
Li ZS, Zhang QB, Ma KP. Tree-ring reconstruction of summer temperature for A.D.1475-2003 in the central Hengduan Mountains, Northwestern Yunnan, China[J]. Climatic Change,2011b. DOI:10.1007/s 10584-011-0111-z.
Liang EY, Liu XH, Yuan YJ, et al. The 1920S drought recorded by tree rings and historical documents in the semi-arid and arid areas of Northern China[J]. Climatic Change, 2006,79:403-432.
Liang EY, Shao XM, Hu YX, et al. A dendroclimatic study of relic picea meyeri in Inner Mongolian Steppe[J]. Acta Botanica Sinica,2001,43:288-294.
Liang E, Shao X, Kong Z, et al. The extreme drought in the 1920s and its effect on tree growth deduced from tree ring analysis:a case study in North China[J]. Annals of forest science, 2003,60:145-152.
Liang EY, Shao XM, Liu XH. Annual precipitation variation inferred from tree rings since A.D. 1770 for the western Qilian Mts., northern Tibetan Plateau[J]. Tree-ring research, 2009a,65:95-104.
Liang EY, Shao XM, Liu HY, et al. Tree-ring based PDSI reconstruction since AD 1842 in the Ortindag Sand Land, east Inner Mongolia[J]. Chinese Science Bulletin,2007,52:2715-2721.
Liang EY, Shao XM, Xu Y. Tree-ring evidence of recent abnormal warming on the southest Tibetan Plateau[J]. Theoretical and Applied Climatology,2009b,98:9-18.
Liang EY, Eckstein D, Liu HY. Assessing the recent grassland greening trend in a long-term context based on tree-ring analysis:A case study in North China[J]. Ecological Indicators, 2009c,9:1280-1283.
Liang Y, Yu HJ, Xu XY, et al. Exploratory Precipitation in North-Central China during the Past Four Centuries[J]. Acta Geologica Sinica,2010,84:223-229.
Lindeberg J. X-ray based tree ring analyses[D]. Umea:Swedish University,2004.
Liu Y, An Z, Linderholm HW, et al. Annual temperatures during the last 2485 years in the mid-eastern Tibetan Plateau inferred from tree rings[J]. Science in China Series D:Earth Sciences,2009a,52:348-359.
Liu Y, Bao G, Song HM, et al. Precipitation reconstruction from Hailar pine (Pinus sylvestris var. mongolica) tree rings in the Hailar region, Inner Mongolia, China back to 1865 AD[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2009b,282:81-87.
Liu Y, Cai QF, Park W-K, et al. Tree-ring precipitation records from Baiyinaobao, Inner Mongolia since A.D.1838[J]. Chinese Science Bulletin,2003,48:1140-1145.
Liu Y, Cai QF, Liu WG, et al. Monsoon precipitation variation recorded by tree-ring [delta] 180 in arid Northwest China since AD 1878[J]. Chemical Geology,2008,252:56-61.
Liu Y, Linderholm HW, Song H, et al. Temperature variations recorded in tree rings from the southern and northern slopes of the central Qinling Mountains, central China[J]. Boreas, 2009c,38:285-291.
Liu Y, Ma LM, Leavitt SW, et al. A prepliminary seasonal precipitation reconstruction from tree-ring stable carbon isotopes at Mt.Helan, China, since AD 1804[J]. Global and Planetary Change,2004,41:229-239.
Liu PX, Peng JF,Chen FH. Hydrological response of Populus euphratica Olve. radial growth in Ejinaa Banner, Inner Mongolia[J]. Journal of Integrative Plant Biology,2007a,49:150-156.
Liu XH, Qin DH, Shao XM, et al. Temperature variations recovered from tree-rings in the middle Qilian Mountain over the last millennium[J]. Science in China Series D:Earth Sciences,2005,48:521-529.
Liu XH, Shao XM, Zhao LJ, et al. Dendroclimatic temperature record derived from tree-ring width and stable carbon isotope chronologies in the middle Qilian Mountains, China[J]. Arctic, Antarctic, and Alpine Research,2007b,39:651-657.
Liu Y, Sun JY, Song HM, et al. Tree-ring hydrologic reconstructions for the Heihe River watershed, western China since AD 1430 [J]. Water Research,2010,44:2781-2792.
Liu Y, Sun JY, Yang YK, et al. Tree-ring-derived precipitation records from inner Mongolia, China, Since A.D.1627[J]. Tree-Ring Research,2007c,63:3-14.
Liu WH, Gou XH, Yang MX, et al. Drought reconstruction in the Qilian Mountains over the last two centuries and its implications for large-scale moisture patterns[J]. Advances In Atmospheric Sciences,2009d,26:621-629.
Mantua NJ, Hare SR, Zhang Y, et al. A Pacific interdecadal climate oscillation with impacts on salmon production[J]. Bulletin of the American Meteorological Society,1997,78:1069-1079.
Martinez-Meier A, Sanchez L, Pastorino M, et al. What is hot in tree rings? The wood density of surviving Douglas-firs to the 2003 drought and heat wave[J]. Forest Ecology and Management,2008,256:837-843.
McCarroll D, Pettigrew E, Luckman A, et al. Blue reflectance provides a surrogate for latewood density of high-latitude pine tree rings[J]. Arctic, Antarctic and Alpine Research, 2002,34:450-453.
Meko DM, Cook ER, Stahle DW, et al. Spatial patterns of tree-growth anomalies in the United States and southeastern Canada[J]. Journal of Climate,1993,6:1773-1786.
Meko DM, Therrell MD, Baisan CH, et al. Sacramento river flow reconstructed to A.D.869 from tree rings[J]. Journal of the American Water Resourses Association,2001,37:1029-1039.
Meko DM, Woodhouse CA. Tree-ring footprint of joint hydrologic drought in Sacramento and Upper Colorado river basins, western USA[J]. Journal of Hydrology,2005,308:196-213.
Moell MK. Donaldson LA. Comparison of segmentation methods for digital image analysis of confocal microscope images to measure tracheid cell dimensions[J].IAWA Journal, 2001,22:267-288.
Nicault A, Alleaume S, Brewer S, et al. Mediterranean drought fluctuation during the last 500 years based on tree-ring data [J]. Climate Dynamics,2008,31:227-245.
Nicolussi K, Kaufmann M, Melvin TM, et al. A 9111 year long conifer tree-ring chronology for the European Alps:a base for environmental and climatic investigations[J]. The Holocene, 2009,19:909-920.
Nitta T, Yanmada S. Recent warming of the tropical sea surface temperature and its relationship to northern hemisphere circulation[J]. Journal of the Meteorological Society of Japan, 1989,67:375-383.
Ogurtsov MG, Kocharov GE, Lindholm M, et al. Evidence of solar variation in tree-ring-based climate reconstructions[J]. Solar Physics,2002,205:403-417.
Ogurtsov MG, Helama S, Eronen M, et al. Centennial-to-millennial fluctuations in July temperatures in North Finland as recorded by timberline tree rings of Scots pine[J]. Quaternary Research,2005,63:182-188.
Park WK, Telewski FW. Measuring maximum latewood density by image analysis at the cellular level[J]. Wood and Fiber Science,1993,25:326-332.
Palmer WC. Meteorological drought. Weather Bureau Research Paper 45. U.S. Department of Commerce:Washington, DC,1965,58.
Pederson N, Jacoby GC, D'arrigo RD, et al Hydrometeorological reconstructions for northeastern Mongolia derived from tree rings:1651-1995 [J]. Journal of Climate, 2001,14:872-881.
Pilcher JR, Baillie MGL, Schmidt B, et al. A 7,272-year tree-ring chronology for western Europe[J]. Nature,1984,312:150-152.
Polge H. Fifteen years of wood radiation densitometry[J]. Wood Science Technology, 1978,12:187-196.
Popa 1, Kern Zn. Long-term summer temperature reconstruction inferred from tree-ring records[J]. Climate Dynamics,2009,32:1107-1117.
Qin C, Yang B, Burchardt I, et al. Intensified pluvial conditions during the twentieth century in the inland Heihe River Basin in arid northwestern China over the past millennium[J]. Global and Planetary Change,2010,72:192-200.
Qian WH, Ding T, Hu HR, Lin X, Qin AM. An overview of dry-wet climate variability among monsoon-westerly region and the monsoon northernmost marginal active zone in China[J]. Advances in Atmospheric Science,2009,26:600-641.
Ram S, Borgaonkar HP,Sikder AB. Tree-ring analysis of teak (Tectona grandis L.F.) in central India and its relationship with rainfall and moisture index[J]. Journal of Earth System Science, 2008,117:637-645.
Ram S, Borgaonkar HP,Sikder AB. Varying strength of the relationship between tree-rings and summer month moisture index (April-September) over Central India:A case study [J]. Quaternary International,2010,212:70-75.
Raspopov OM, Dergachev VA, Kolstrom T. Periodicity of climate conditions and solar variability derived from dendrochronological and other palaeoclimatic data in high latitudes. Palaeogeography. Palaeoclimatology. Palaeoecology,2004.209:127-139.
Reynolds RW, Smith TM. Improved global sea surface temperature analyses using optimum interpolation[J]. Journal of Climate,1994,7:929-948.
Rigozo NR, Nordemann DJR, Echer E, et al. An interactive method for digital tree-ring width measurement[J]. Geofisica Internacional,2004,43:281-285.
Rigozo NR, Nordemann DJR, Echer E, et al. Solar variability effects studied by tree-ring data wavelet analysis[J]. Advances in Space Research,2002,29:1985-1988.
Rinn F. High frequency wood density scanning[R].7th International Conference on Dendrochronology (1CD), Beijing, China,2006.
Roig FA, Le-Quesne C, Boninsegna JA, et al.. Climate variability 50,000 years ago in mid-latitude Chile as reconstructed from tree rings[J]. Nature,2001,410:567-570.
Sano M, Furuta F, Kobayashi O, et al. Temperature variations since the mid-18th century for western Nepal, as reconstructed from tree-ring width and density of Abies spectabilis[J]. Dendrochronologia,2005,23:83-92.
Sano M, Buckley BM, Sweda T. Tree-ring based hydroclimate reconstruction over northern Vietnam from Fokienia hodginsii:eighteenth century mega-drought and tropical Pacific influence[J]. Climate Dynamics,2009,33:331-340.
Schinker MG, Hansen N, Spiecker H. High-freqency densitometry-a new method for the rapid evaluation of wood density variations [J]. IAWA Journal,2003,24:231-239.
Selvaraj K, Chen CTA, Lou JY. Holocene East Asian monsoon variability:links to solar and tropical Pacific forcing[J]. Geophysical Research Letters,2007,34:L01703.
Shao XM, Xu Y, Yin ZY, et al. Climatic implications of a 3585-year tree-ring width chronology from the northeastern Qinghai[J]. Quaternary Science Reviews,2010,29:2111-2122.
Sheppard PR, Graumlich LJ, Conkey LE. Reflected-light image analysis of conifer tree rings for reconstructing climate[J]. The Holocene,1996,6:62-68.
Shi YF, Shen YP, Kaag ES, et al. Recent and Future Climate Change in Northwest China[J]. Climatic Change,2007,80:379-393.
Singh J, Park WK.Yadav RR. Tree-ring-based hydrological records for western Himalaya, India, since a.d.1560[J]. Climate Dynamics,2006,26:295-303.
Spiecker H, Schinker M, Hansen J, et al. Cell structure in tree rings:novel methods for preparation and image analysis of large cross sections[J]. IAWA Journal,2000,21:361-373.
Tan LC, Cai YJ, Yi L, An ZS, Ai L. Precipitation variations of Longxi, northeast margin of Tibetan Plateau since AD 960 and their relationship with solar activity [J]. Climate of the Past, 2008,4:19-28.
Thetford RD, D'Arrigo RD, Jacoby GC. An image analysis system for determining densitometric and ring-width time series[J]. Canadian Journal of Forest Research,1991,21:1544-1549.
Tian QH, Gou XH, Zhang Y, et al. May-June mean temperature reconstruction over the past 300 years based on tree rings on the Qilian Mountains of the northeastern Tibetan Plateau[J]. IAWA Journal,2009,30:421-434.
Tian QH, Gou XH, Zhang Y, et al. Tree-ring based drought reconstruction (A.D.1855-2001) for the qilian mountains, northwestern china[J]. Tree-ring research,2007,63:27-36.
Till C, Guiot J. Reconstruction of precipitation in Morocco since 1100 A.D. based on cedrus atlantica tree-ring widths[J]. Quaternary Research,1990,33:337-351.
Timilsena J, Piechota TC, Hidalgo H, et al. Five hundred years of hydrological drought in the upper Colorado River Basin[J]. Journal of the American Water Resources Association, 2007,43:798-812.
Torrence C, Webster PJ. Interdecadal changes in the ENSO-Monsoon system. Journal of Climate, 1999,12:2679-2690.
Touchan R, Akkemik U, Hughes MK, et al. May-June precipitation reconstruction of southwestern Anatolia, Turkey during the last 900 years from tree rings[J]. Quaternary Research,2007,68:196-202.
Touchan R, Meko DM, Aloui A. Precipitation reconstruction for Northwestern Tunisia from tree rings[J]. Journal of Arid Environments,2008,72:1887-1896.
Trenberth KE. The definition of El Nino[J]. Bulletin of the American Meteorological Society, 1997,78:2771-2777.
Trenberth KE, Stepaniak DK. Indices of El Nino evolution[J]. Journal of Climate, 2001,14:1697-1701.
Tuovinen M, McCarroll D, Grudd H. Spatial and temporal stability of the climatic signal in northern Fennoscandian pine tree-ring width and maximum density[J].Boreas,2008,38:1-12.
Twine TE, Kucharik CJ, Foley JA. Effects of El Nino-Southern Oscillation on the climate, water balance, and streamflow of the Mississippi River Basin[J]. Journal of Climate, 2005,18:4840-4861.
Vaganov EA, Hughes MK, Kirdyanov AV, et al. Influence of snowfall and melt timing on tree growth in Subarctic Eurasia[J]. Nature,1999,400:149-151.
Vieira J, Campelo F, Nabais C. Age-dependent responses of tree-ring growth and intra-annual density fluctuations of Pinus pinaster to Mediterranean climate[J]. Trees,2009,23:257-265.
Wang B, Wu R, Fu X. Pacific-east Asian teleconnection:how does ENSO affect East Asian Climate? Journal of Climate,2000,13:1517-1536.
Wang LL, Duan JP, Chen J, et al. Temperature reconstruction from tree-ring maximum density of Balfour spruce in eastern Tibet, China[J]. International Journal of Climatology, 2010,30:972-979.
Wang XC, Zhang QB, Ma KP, et al. A tree-ring record of 500-year dry-wet changes in nothern Tibet, China[J]. The Holocene,2008,18:579-588.
Wang YJ, Cheng H, Edwards RL, et al. The Holocene Asian monsoon:links to solar changes and north Atlantic climate[J]. Science,2005,308:854-857.
Wang YX, Liu GY, Zhang XG, et al. The relationships between tree rings of Qilianshan juniper and climatic change and glacial activity during the past 1000 years in China. [J]. Chinese Science Bulletin,1983,28:1647-1647.
Watson TA, Barnett FA, Gray ST, et al. Reconstructed streamflows for the headwaters of the Wind River, Wyoming, United States[J]. Journal of the American Water Resources Association,2009,45:224-236.
Westermann J, Zerbe S, Eckstein D. Age structure and growth of degraded populus euphratica floodplain forests in north-west China and perspectives for their recovery[J]. Journal of Integrative Plant Biology,2008,50(5):536-546.
Wilmking M, Juday GP, Barder VA, et al. Recent climate warming forces constrasting growth response of white spruce at treeline in Alask through temperature thresholds[J]. Global Change Biology,2004,10:1724-1736.
Wilmking M, Myers-Smith I. Changing climate sensitivity of black spruce (Picea mariana Mill.) in a peatland-forest landscape in Interior Alaska[J]. Dendrochronologia,2008,25:167-175.
Wilson R, D'Arrigo R, Buckley B, et al. A matter of divergence:tracking recent warming at hemispheric scales using tree ring data[J]. Journal of Geophysical Research, 2007,112:D17103.
Woodcock DW. Climate sensitivity of wood-anatomical features in a ring-porous oak (Quercusmacrocarpa)[J]. Canadian Journal of Forest Research,1989,19:639-644.
Woodhouse CA. A tree-ring reconstruction of streamflow for the Colorado front range[J]. Journal of the American Water Resourses Association,2001,27:561-568.
Woodhouse CA, Lukas JJ. Multi-century tree-ring reconstructions of Colorado streamflow for water resource planning[J]. Climate Change,2006,78:293-315.
Yadav RR, Braeuning A, Singh J. Tree ring inferred summer temperature variations over the last millennium in western Himalaya, India[J]. Climate Dynamics,2010,36:1545-1554.
Yang B, Brauning A, Liu JJ, et al. Temperature changes on the Tibetan Plateau during the past 600 years inferred from ice cores and tree rings[J]. Global and Planetary Change, 2009a,69:71-78.
Yang B, Brauning A, Shi YF. Late Holocene temperature fluctuations on the Tibetan Plateau[J]. Quaternary Science Reviews,2003,22:2335-2344.
Yang B, Kang X, Brauning A, et al. A 622-Year regional temperature history of southeast Tibet derived from tree rings[J]. The Holocene,2009b,20:181-190.
Yang B, Kang XC, Shi YF. Decadal climaticvariations indicated by Dulan tree ring and comparison with other proxy data in China of the last 2000 years[J]. Chinese Geographical Science,2000,10:193-201.
Yanosky TM, Robinove CJ. Digital image measurement of the area and anatomical structure of tree-rings[J]. Canadian Journal of Botany,1986,64:2896-2902.
Yin ZY, Shao XM, Qin NS, et al. Reconstruction of a 1436-year soil moisture and vegetation water use history based on tree-ring widths from Qilian junipers in northeastern Qaidam Basin, northwestern China[J]. International Journal of Climatology,2008,28:37-53.
Yuan YJ, Shao XM, Wei WS, et al. The potential to reconstruct Manasi River streamflow in the Northern Tien Shan mountains, NW China[J]. Tree-ring Research,2007,63:81-93.
Zhang QB, Cheng GD, Yao TD, et al. A 2,326-year tree-ring record of climate variability on the northeastern Qinghai-Tibetan Plateau[J]. Geophysical Research Letters,2003,30:1739-1742.
Zhang Y, Tian QH, Gou XH, et al. Annual precipitation reconstruction since AD 775 based on tree rings from the Qilian Mountains, northwestern China[J]. International Journal of Climatology,2011,31:371-381.
Zhang YX, Wilmking M, Gou XH. Changing relationships between tree growth and climate in Northwest China[J]. Plant Ecology,2009,201:39-50.
Zheng JY, Wang WC, Ge QS, Man ZM, Zhang PY. Precipitation variability and extreme events in eastern China during the past 1500 years. Terrestrial Atmospheric and Oceanic Sciences, 2006,17:579-592.
Zhu HF, Shao XM, Yin ZY, et al. August temperature variability in the southeastern Tibetan Plateau since AD 1385 inferred from tree rings[J]. Palaeogeography, Palaeoclimatology, Palaeuecology.2011.305:84-92.
Zhu HF, Zheng Y, Shao X, et al. Millennial temperature reconstruction based on tree-ring widths of Qilian juniper from Wulan, Qinghai Province, China[J]. Chinese Science Bulletin, 2008,53:3914-3920.
曹泊,潘保田,高红山,等1972-2007年祁连山东段冷龙岭现代冰川变化研究[J].冰川冻土,2010,32(2)：242-248.
曹艳艳,郭品文,王群.ENSO与北半球冬季大气环流异常的年代际关系[J].南京气象学院学报,2007,30(6)：792-798.
蔡秋芳,刘禹,包光,等树轮记录的吕梁山地区公元1836年以来5-7月平均气温变化[J].科学通报,2010,55(20)：2033-2039.
蔡秋芳,刘禹,宋慧明,等树轮记录的陕西中-北部地区1826年以来4-9月温度变化[J].中国科学D辑：地球科学,2008,38(8)：971-977.
蔡秋芳,刘禹,杨银科,等陕西黄龙树轮年表的建立及其2-3月降水记录[J].海洋地质与第四纪地质,2005,25(2)：133-139.
蔡秋芳.贺兰山油松生长对三种不同水分指数的响应及1-7月Walter指数重建[J].海洋地质与第四纪地质,2009,29(6)：131-136.
曹受金,曹福祥,祁承经.湖南通道马尾松树轮宽度与气候因子的关系[J].中南林业科技大学学报,2010,30(12)：66-69.
陈宝君,钱君龙,濮培民,等.ENSO对天目山柳杉树轮同位素的影响[J].海洋地质与第四纪地质,2002,22(4)：53-58.
陈峰,陆守曾,杨珉Bootstrap估计及其应用[J].中国卫生统计,1997,14(5)：5-7.
陈峰,袁玉江,魏文寿,等.利用树轮图像灰度重建南天山北坡西部初夏温度序列[J].中国沙漠,2008,28(5)：842-847.
陈峰,袁玉江,魏文寿,等用西伯利亚落叶松年轮最大密度重建和布克赛尔5-8月份平均最高温度[J].生态学报,2010a,30(17)：4652-4658.
陈峰,袁玉江,魏文寿,等福建沙县马尾松树轮宽度与夏季亚洲-太平洋涛动指数的关系[J].第四纪研究,2011,31(1)：96-103.
陈峰,袁玉江,魏文寿,等树轮记录的甘肃山丹近224年降水变化[J].地理与地理信息科学,2010b,26(5)：82-86.
陈峰,袁玉江,魏文寿,等树轮记录的伊犁地区近354年帕尔默干旱指数变化[J].高原气象,2011,30(2)：355-362.
陈峰,袁玉江,魏文寿,等.特克斯河流域近236a降水变化及其趋势预测[J].山地学报,2010c,28(5)：545-551.
陈拓,陈发虎,安黎哲,等不同海拔祁连园柏树轮和叶片813C值的变化[J].冰川冻土,2004,26(6)：767-771.
陈月娟,周任君,简俊.东亚夏季风环流与ENSO循环的关系[J].高原气象,2002,21(6)：536-545.
崔宇,袁玉江,金海龙,等乌鲁木齐河源467年春季降水的重建与分析[J].干旱区地理,2007,30(04)：496-500.
邓自旺,钱君龙,屠其璞,等.环境因素对天目山柳杉树轮δ13C方位分布的影响[J].植物生态学报,2003,27(1)：93-98.
丁小俊.利用树轮资料的EOF迭代方案重建中东亚干旱半干旱区1500年来气温变化的初步研究[D].兰州：兰州大学,2007.
丁永建,叶佰生,刘时银.祁连山中部地区40a来气候变化及其对径流的影响[J].冰川冻土,2000,22(3)：193-199.
段建平.基于树轮的海螺沟冰川区气候及冰川变化研究[D].北京：中科院研究生院,2010a.
段建平,王丽丽,李论,等树轮最大密度记录的贡嘎山区公元1837年以来的温度变化[J].科学通报,2010b,55(11)：1036-1042.
范敏杰,袁玉江,魏文寿,等用树木年轮重建伊犁南天山北坡西部的降水量序列[J].干早区地理,2007,30(02)：268-273.
方克艳.近400年来西北地区气候变化的树轮记录研究[D].兰州：兰州大学,2010.
高琳琳,勾晓华,邓洋,等.树轮气候学中分异现象的研究进展[J].冰川冻土,2011,33(2)：453-460.
高尚玉,鲁瑞洁,强明瑞,等140年来腾格里沙漠南缘树木年轮记录的降水量变化[J].科学通报,2006,51(3)：326-331.
勾晓华,陈发虎,李金豹,等祁连山东部地区高分辨率气候记录研究[J].兰州大学学报(自然科学版),2002,38(1)：105-110.
勾晓华,陈发虎,王亚军,等利用树轮宽度重建近280 a来祁连山东部地区的春季降水[J].冰川冻土,2001,23(3)：292-296.
勾晓华,陈发虎,杨梅学,等祁连山中部地区树轮宽度年表特征随海拔高度的变化[J].生态学报,2004,24(1)：172-176.
勾晓华,陈发虎,杨梅学,等.青藏高原东北部树木年轮记录揭示的最高最低温的非对称变化[J].中国科学(D辑：地球科学),2007,37(11)：1480-1492.
勾晓华,邓洋,陈发虎,等.黄河上游过去1234年流量的树轮重建与变化特征分析[J].科学通报,2010,55(33)：3236-3243.
勾晓华,邵雪梅,王亚军,等祁连山东部地区树木年轮年表的建立[J].中国沙漠,1999,19(4)：364-367.
勾晓华,杨梅学,彭剑峰,等树轮记录的阿尼玛卿山区过去830年夏半年最高温变化[J].第四纪研究,2006,26(6)：991-998.
勾晓华.黄河源区树木年轮记录研究[D].兰州：兰州大学,2004.
何海.使用WinDENDRO测量树轮宽度及交叉定年方法[J].重庆师范大学学报(自然科学版),2005,22(4)：39-44.
何吉成,王丽丽,邵雪梅.漠河樟子松树轮指数与标准化植被指数的关系研究[J].第四纪研究,2005,25(2)：252-257.
何吉成,邵雪梅.德令哈地区树轮宽度指数与草地植被指数的关系[J].科学通报,2006,51(9)：1083-1090.
侯迎,王乃昂,李钢,等利用树轮资料重建1751-2005年崆峒山地区夏季温度变化[J].气候变化研究进展,2007,3(3)：172-176.
侯迎,王乃昂,张学敏,等高频光密度测量法在崆峒山树轮年表建立中的应用[J].干旱区地理,2010,33(02)：236-242.
胡良温,杨改河,李轶冰,等利用祁连圆柏年轮资料重建江河源区东北部600余年气候研究[J].西北农林科技大学学报(自然科学版),2006,34(5)：107-113.
黄磊,邵雪梅.青海德令哈地区近400年来的降水量变化与太阳活动[J].第四纪研究,2005,25(2)：184-192.
黄玉霞,王宝鉴,张强,等气候变化和人类活动对石羊河流域水资影响评价[J].高原气象,2008,27(4)：866-872.
贾文雄,何元庆,李宗省,等祁连山区气候变化的区域差异特征及突变分析[J].地理学报,2008,63(3)：257-269
江善虎,任立良,雍斌,等利用树木年轮重建马鞍山地区7-9月降水量序列[J].河海大学学报(自然科学版),2010,38(1)：31-35.
蒋全荣,郑定英,余志豪.副热带高压季节性移动与海温场的联系[J].大气科学,1997,21(2)：199-204.
金祖辉,陶诗言.ENSO循环与中国东部地区夏季和冬季降水关系的研究[J].大气科学,1999,23(6)：664-672.
康尔泗,程国栋,等中国西北干旱区冰雪水资源与出山径流[M].北京：科学出版社,2002.
康玲玲,王云璋,马燕,等黄河花园口站近523年天然径流量序列重建[J].水资源与水工程学报,2008,19(6)：10-13.
康兴成,Graumlich LJ, Sheppard P.青海都兰地区1835年来的气候变化—来自树轮资料[J].第四纪研究,1997a,17(1)：70-75.
康兴成,Graumlich LJ, Sheppard P青海都兰地区1835a年轮序列的建立和初步分析[J].科学通报,1997b,42(10)：1089-1091.
康兴成,程国栋,陈发虎,等祁连山中部公元904年以来树木年轮记录的旱涝变化[J].冰川冻土,2003,25(5)：518-525.
康兴成,程国栋,康尔泗,等利用树轮资料重建黑河近千年来出山口径流量[J].中国科学D辑,2002,32(8)：675-685.
康兴成,张其花,Graumlich LJ,等青海都兰过去2000年来的气候重建及其变迁[J].地球科学进展,2000,15(2)：215-221.
蓝永超,丁永建,沈永平等河西内陆河流域出山径流对气候转型的响应[J].冰川冻土,2003,25(2)：188-192.
蓝永超,康尔泗,仵彦卿等气候变化对河西内陆干旱区出山径流的影响[J].冰川冻上,2001a,23(3)：276-282.
蓝永超,康尔泗,张济世,等近50年来ENSO与祁连山区气温降水和出山径流的对应关系[J].水科学进展,2002,13(2)：141-145.
蓝永超,仵彦卿,康尔泗,等祁连山北麓出山径流对气候变化的响应[J].兰州大学学报(自然科学版),2001b,37(4)：125-132.
李峰,何金海.北太平洋海温异常与东亚夏季风相互作用的年代际变化[J].热带气象学报,2002,16(3)：261-271.
李江风,袁玉江,马慧明,等.伊犁地区历史径流深度场的重建[J].自然资源学报,1994,9(1)：67-76.
李江风,袁玉江,由希尧,等树木年轮水文学研究与应用[M].北京：科学出版社,2000.
李江风,袁玉江,由希尧.乌鲁木齐河山区流域360年径流量的重建[J].第四纪研究,1997,17(2)：131-138.
李江风,袁玉江,马慧明,等.用树木年轮重建伊犁地区的年径流量场[J].水文,1996(1)：30-35.
李金豹.利用树木年轮重建新疆地区近300年来的气候变化[D].兰州：兰州大学,2003.
李强,刘禹,蔡秋芳,等.山西宁武地区1686年以来年降水重建[J].第四纪研究,200626(6)：999-1006.
李洋.石羊河流域水循环要素变化特征研究[D].杨凌：西北农林科技大学,2008.
李颖.完全耦合的海气环流模式中ENSO和亚洲季风的相互作用[D]北京：中国科学院研究生院,2006.
李宗善,刘国华,傅伯杰,等川西卧龙国家级自然保护区树木生长对气候响应的时间稳定性评估[J].植物生态学报,2010,34(9)：1045-1057.
李宗善,刘国华,张齐兵.利用树木年轮宽度资料重建川西卧龙地区过去159年夏季温度的变化[J].植物生态学报,2010,34(6)：628-641.
梁尔源.中国北方干旱、半干旱区树轮网络的建立及其气候事件研究[D].北京：中科院地理科学与资源研究所,2004.
梁尔源,邵雪梅,刘鸿雁,等树轮所记录的公元1842年以来内蒙古东部浑善达克沙地PDSI的变化[J].科学通报,2007,52(14)：1694-1699.
刘洪滨,刘洪滨,邵雪梅.采用秦岭冷杉年轮宽度重建陕西镇安1755年以来的初春温度[J].气象学报,2000,58(02)：223-233.
刘洪滨,邵雪梅,黄磊.中国陕西关中及周边地区近500年来初夏干燥指数序列的重建[J].第四纪研究,2002,22(3)：220-229.
刘洪滨,邵雪梅.秦岭南坡佛坪1789年以来1-4月平均温度重建[J].应用气象学报,2003,14(2)：188-196.
刘洪滨,吴祥定,邵雪梅.采用树轮图像分析方法研究历史时期气候变化的可行性[J].地理研究,1996,15(2)：44-51.
刘录三,邵雪梅,梁尔源,等祁连山中部祁连圆柏生长与更新方式的树轮记录[J].地理研究,2006,25(1)：53-61.
刘普幸.额济纳旗胡杨径向生长的水文气候因子研究[D].兰州：兰州大学,2007a.
刘普幸,陈发虎,靳立亚,等基于胡杨年轮重建黑河下游近100年春季径流量[J].干旱区地理,2007b,30(5)：696-700.
刘晓宏,秦大河,邵雪梅,等祁连山中部过去近千年温度变化的树轮记录[J].中国科学D辑,2004,34(1)：89-95.
刘晓宏,秦大河,邵雪梅,等.西藏林芝地区近350a来降水变化及突变分析[J].冰川冻土,2003,25(4)：375-379.
刘义花,汪青春,马占良,等.利用多条树轮重建黑河上游地区540年径流量[J].干旱区资源与环境,2009,23(3)：93-97.
刘屹岷,吴国雄.副热带高压研究回顾及对几个基本问题的再认识[J].气象学报,2000,58(4)：500-512.
刘永强,丁一汇.ENSO事件对我国季节降水和温度的影响[J].大气科学,1995,19(2)：200-208.
刘禹,Shishov V,史江峰,等内蒙古西部贺兰山和东部白音敖包未来20年降水趋势预测[J].科学通报,2004a,49(3)：270-274.
刘禹,Won-Kyu P,蔡秋芳,等公元1840年以来东亚夏季风降水变化——以中国和韩国的树轮记录为例[J].中国科学D辑,2003a,33(6)：543-549.
刘禹,安芷生,Linderholm HW,等青藏高原中东部过去2485年以来温度变化的树轮记录[J].中国科学D辑：地球科学,2009c,39(2)：166-176.
刘禹,安芷生,马海州,等.青海都兰地区公元850年以来树轮记录的降水变化及其与北半球气温的联系[J].中国科学(D辑：地球科学),2006a,36(5)：461-471.
刘禹,蔡秋芳,Park WK,等内蒙古锡林浩特白音敖包1838年以来树轮降水记录[J].科学通报,2003b,48(9)：952-957.
刘禹,蔡秋芳,马利民等.树轮降水记录及东亚夏季风强弱变化——以内蒙古包头地区为例[J].地学前缘,2001,8(1)：91-97.
刘禹,刘娜,宋慧明,等以树轮宽度重建秦岭中段分水岭地区1-7月平均气温[J].气候变化研究进展,2009a,5(5)：260-265.
刘禹,马利民.树轮宽度对近376年呼和浩特季节降水的重建[J].科学通报,1999,44(18)：1986-1992.
刘禹,马利民,蔡秋芳,等依据陕西秦岭镇安树木年轮重建3—4月份气温序列[J].自然科学进展,2001,11(2)：157-162.
刘禹,马利民,蔡秋芳,等采用树轮稳定碳同位素重建贺兰山1890年以来夏季(6-8月)气温[J].中国科学(D辑),2002,32(8)：667-674.
刘禹,史江峰,Shishov V,等以树轮晚材宽度重建公元1726年以来贺兰山北部5～7月降水量[J].科学通报,2004b,49(3)：265-269.
刘禹,田沁花,宋慧明,等以树轮宽度重建公元1558年以来华山5-6月平均温度及20世纪中后期升温[J].第四纪研究,2009b,29(5)：888-895.
刘禹,田华,宋慧明,等油松年轮记录的河北围场公元1884年以来5-6月平均温度[J].第四纪研究,2009d,29(5)：896-904.
刘禹,王雷,史江峰,等利用贺兰山北部树轮资料重建过去270年以来6-8月平均干燥指数[J].第四纪研究,2005,25(5)：540-544.
刘禹,杨银科,蔡秋芳,等以树木年轮宽度资料重建湟水河过去248年来6-7月份河流径流量[J].干旱区资源与环境,2006b,20(6)：69-73.
刘禹,吴祥定,邵雪梅,等.树轮密度、稳定C同位素对过去近100a陕西黄陵季节气温与降水的恢复[J].中国科学：D辑,1997,27(3)：271-276.
鲁瑞洁,夏虹.腾格里沙漠南缘油松树轮宽度变化及其对气候因子的响应[J].中国沙漠,2006,26(3)：399-402.
罗连升,杨修群.从有效位能来分析El Ninno的年代际变化[J].气象科学,2003,23(1)：1-11.
吕军,江志红,张静,等天目山树轮碳同位素与周边地区旱涝变化关系的研究[J].南京气象学院学报,2008,31(03)：389-394.
吕军,屠其璞,钱君龙,等天目山柳杉树轮813C对华东地区降水序列的重建[J].南京气象学院学报,2001,24(3)：350-355.
马宏伟,王乃昂.近50年石羊河出山口径流对气候变化的响应[J].干旱区资源与环境,2010,24(1)：113-117.
马龙,刘延玺,翼鸿兰,等科尔沁沙地1826年以来榆树树轮宽度年表的建立及降水重建[J].第四纪研究,2011,31(2)：360-369.
马柱国,邵丽娟.中国北方近百年干湿变化与太平洋年代际振荡的关系[J].大气科学,2006,30(3)：464-474.
马柱国.华北干旱化趋势及转折性变化与太平洋年代际振荡的关系[J].科学通报,2007,52(10)：1199-1206.
慕巧珍,王绍武,朱锦红,等近百年夏季西太平洋副热带高压的变化[J].大气科学,2001,25(6)：787-797.
潘娅婷,袁玉江,喻树龙,等采用树轮图像分析法重建过去气候变化[J].干旱区研究,2007,24(2)：255-260.
钱君龙,邓自旺,屠其璞,等天目山柳杉树轮δD年序列及其气候含义[J].中国科学：D辑,2001,31(5)：372-376.
秦宁生,靳立亚.时兴台,等利用树轮资料重建通天河流域518年径流量[J].地理学报,2004,59(4)：550-556.
邵雪梅,黄磊,刘洪滨,等.树轮记录的青海德令哈地区千年降水变化[J].中国科学D辑,2004,34(2)：145-153.
邵雪梅,梁尔源,黄磊,等柴达木盆地东北部过去1437a的降水变化重建[J].气候变化研究进展,2006,2(3)：122-126.
邵雪梅,王树芝,徐岩,等柴达木盆地东北部3500年树轮定年年表的初步建立[J].第四纪研究,2007,27(4)：477-485.
沈吉,陈毅风.南京地区近二十年来雪松树轮的稳定碳同位素与气候重建[J].植物资源与环境学报,2000,9(3)：34-37.
沈长泗,陈金敏,张志华.采用树木年轮资料重建山东沂山地区200多年来的湿润指数[J].地理研究,1998,17(2)：150-156.
沈永平,刘时银,甄丽丽,等祁连山北坡流域冰川物质平衡波动及其对河西水资源的影响[J].冰川冻土,2001,23(3)：244-250.
施雅风,沈永平,胡汝骥.西北气候由暖干向暖湿转型的信号、影响和前景初步探讨[J].冰川冻土,2002,24(3)：219-226.
施雅风,沈永平,李栋梁,等中国西北气候由暖干向暖湿转型的特征和趋势探讨[J].第四纪研究,2003,23(2)：152-164.
时兴合,秦宁生,邵雪梅,等青海湖流域圆柏年轮指示的近千年降水变化[J].湖泊科学,2009,21(4)：579-586.
史江峰,刘禹,蔡秋芳,等油松(Pinus tabulaeformis)树轮宽度与气候因子统计相关的生理机制—以贺兰山地区为例[J].生态学报,2006,26(3)：697-705.
史江峰,刘禹,蔡秋芳,等贺兰山过去196年降水的树轮宽度重建及降水变率[J].海洋地质与第四纪地质,2007,27(1)：95-100.
宋慧明,刘禹,倪万眉,等以树轮宽度重建九寨沟1750年以来冬半年平均最低温度[J].第四纪研究,2007,27(4)：486-491.
孙军艳,刘禹,蔡秋芳,等额济纳233年来胡杨树轮年表的建立及其所记录的气象、水文变化[J].第四纪研究,2006,26(5)：799-807.
孙艳荣,崔海亭,穆治国,等广东现代樟树树轮纤维素的碳同位素与厄尔尼诺事件的关系[J].地球学报,2003,24(6)：505-510.
谭明,邵雪梅,刘晓宏,等.中国近千年石笋-树轮集成温度记录[J].气候变化研究进展,2006,2(3)：113-116.
汤绪,孙国武,钱维宏.亚洲夏季风北边缘研究[M].北京：气象出版社,2007.
唐劲松.浙江天目山柳杉树轮δ13C年序列与气候变化[D].南京：中国科学院南京地理与湖泊研究所,1999.
田沁花,刘禹,蔡秋芳,等油松树轮记录的过去134年伏牛山5-7月平均最高温度[J].地理学报,2009,64(7)：879-887.
田沁花.祁连山中—西部近500年来气候变化的树轮记录[D].兰州：兰州大学,2006.
汪青春,秦宁生,李栋梁,等.利用多条树轮资料重建青海高原近250年年平均气温序列[J].高原气象,2005,24(3)：320-325.
王兵,高鹏,郭浩,等江西大岗山林区樟树年轮对气候变化的响应[J].应用生态学报,2009,20(1)：71-76.
王国荣,罗哲贤,赵东.西北地区3—9月降水量与ENSO的联系[J].南京气象学院学报,2007,30(6)：849-856
王建,赵兴云,钱君龙.天目山柳杉树轮δ13C方位变化及成因探讨[J].地理研究, 2006,25(2)：242-254.
王树芝.青海都兰地区公元前515年以来树木年轮表的建立及应用[J].考古与文物,2004(6)：45-50.
王文志,刘晓宏,陈拓,等基于祁连山树轮宽度指数的区域NDVI重建[J].植物生态学报,2010,34(9)：1033-1044.
王亚军,陈发虎,勾晓华,等利用树木年轮资料重建祁连山中段春季降水的变化[J].地理科学,2001,21(4)：373-377.
王亚军,陈发虎,勾晓华.黑河230a以来3-6月径流的变化[J].冰川冻土,2004,26(2)：202-206.
王亚军,高尚玉,马玉贞,等基于树轮重建的宁夏河东沙地西部公元1899年来年降水量的变化[J].干旱区地理,2010,33(3)：377-384.
王亚军,勾晓华,刘普幸,等甘肃榆中200年来春季气温的变化[J].中国沙漠,2006,26(2)：283-285.
王亚军,马玉贞,鲁瑞洁,等树木年轮记录的祁连山东段公元1895年来的气温变化[J].第四纪研究,2009,29(5)：905-912.
王玉玺.祁连山园柏年轮与我国近千年气候变化和冰川进退的关系[J].科学通报,1982,27(21)：1316-1319.
王越,江志红,张强,等基于Palmer湿润指数的旱涝参数研究[J].南京气象学院学报,2007,30(3)：383-389.
王振宇,李林,江青春,等树轮纪录的500年来青海地区夏半年降水变化特征[J].气候与环境研究,2005,10(2)：250-256.
魏本勇,方修琦.树轮气候学中树木年轮密度分析方法的研究进展[J].古地理学报,2008,10(2)：193-202.
魏文寿,袁玉江,喻树龙,等中国天山山区235a气候变化及降水趋势预测[J].中国沙漠,2008,28(5)：803-808.
武炳义,卞林根,张人禾.冬季北极涛动和北极海冰变化对东亚气候变化的影响[J].极地研究,2004,16(3)：211-220.
吴普,王丽丽,邵雪梅.采用高山松最大密度重建川西高原近百年夏季气温[J].地理学报,2005,60(6)：998-1006.
吴祥定,孙力,湛绪志.利用树木年轮资料重建西藏中部过去气候的初步尝试[J].地理学报,1989,44(3)：334-342.
吴祥定,邵雪梅.中国秦岭地区树木年轮密度对气候响应的初步分析[J].应用气象学报,1994,5(2)：253-256.
吴祥定.树木年轮与气候变化[M].北京：气象出版社,1990.
肖生春,肖洪浪.极端干旱区湖岸柽柳径向生长对水环境演变的响应[J].北京林业大学学报,2006,28(2)：39-45.
肖生春,肖洪浪,司建华,等.干旱区多枝柽柳的生长特性[J].西北植物学报,2005,25(5)：1012-1016.
肖生春,肖洪浪,周茂先,等近百年来西居延海湖泊水位变化的湖岸林树轮记录[J].冰川冻土,2004,26(5)：557-562.
肖支才,高华明,丁通,等自助法在小样本数据均值估计中的应用[J].海军航空工程学院学报,2009.24(5)：563-572.
谢益辉,朱饪Bootstrap方法的历史发展和前沿研究[J].统计与信息论坛, 2008,23(2)：90-96.
徐国保,刘晓宏,陈拓,等新疆哈密八大石森林上限树轮记录的温度变化信息[J].山地学报,2009,27(4)：402-410.
徐瑞珍,周陆生.由斑玛云杉年表重建青海高原东南部夏季降水序列[J].气象,2000,26(1)：3-8.
许武成,马劲松,王文.关于ENSO事件及其对中国气候影响研究的综述[J].气象科学,2005,25(2)：213-220.
杨涛,勾晓华,李颖俊.青藏高原东北部树轮海拔梯度研究的散点图分析应用[J].冰川冻土,2010,32(2)：429-437.
杨小利,杨兴国,马鹏里,等PDSI在甘肃中东部地区的修正和应用[J].地球科学进展,2005,20(9)：1022-1028.
杨修群,郭燕娟,徐桂玉,等年际和年代际气候变化的全球时空特征比较[J].南京大学学报：自然科学版,2002,38(3)：308-317.
杨银科,黄强,刘禹,等.利用树轮资料重建河流径流量研究进展[J].水科学进展,2010,21(3)：430-434.
杨银科,刘禹,蔡秋芳,等以树木年轮宽度资料重建祁连山中部地区过去248年来的降水量[J].海洋地质与第四纪地质,2005,25(3)：113-118.
杨银科,刘禹,史江峰,等树木年轮密度实验方法及其在内蒙古准格尔旗树轮研究中的应用[J].干旱区地理,2006,29(5)：639-645.
尹红.西北地区过去千年降水序列的初步重建及变化特征分析[D].南京：南京信息工程大学,2006.
游泳,郭品文,廖勇,等ENSO与中国东部地区夏季降水相关性年代际变化特征[J].气象科技,2005,33(2)：142-146.
余丹丹,张韧,洪梅,等亚洲夏季风系统成员与西太平洋副高的相关特征分析[J].热带气象学报,2007,23(1)：78-84.
喻树龙,袁玉江,龚原,等奎屯河近379a 9月径流量的重建与特征分析[J].干旱区资源与环境,2008,22(7)：115-119.
喻树龙,袁玉江,何清,等1468-2001年新疆精河5-8月平均气温的重建[J].冰川冻土,2007,29(3)：374-379.
喻树龙,袁玉江,金海龙,等.用树木年轮重建天山北坡中西部7-8月379a的降水量[J].冰川冻土,2005,27(3)：404-410.
袁玉江,李江风,胡汝骥,等用树木年轮重建天山中部近350年来的降水量[J].冰川冻土,2001,23(1)：34-40.
袁玉江,邵雪梅,李江风,等夏干萨特树轮年表中降水信息的探讨与326年降水重建[J].生态学报,2002,22(12)：2048-2053.
袁玉江,邵雪梅,魏文寿,等乌鲁木齐河山区树木年轮一积温关系及≥5.7℃积温的重建[J].生态学报,2005,25(4)：756-762.
袁玉江,叶玮,董光荣.天山西部伊犁地区314a降水的重建与分析[J].冰川冻土,2000,22(2)：121-127.
袁玉江,喻树龙,穆桂金,等天山北坡玛纳斯河355a来年径流量的重建与分析[J].冰川冻土,2005,27(3)：411-417.
袁玉江,李江风.天山乌鲁木齐河源450a冬季温度序列的重建与分析[J].冰川冻土,1999,21(1)：64-70.
臧增亮.ENSO对东亚夏季风和我国夏季降水的影响研究进展[J].解放军理工大学学报(自然科学版),2005,6(4)：394-398.
张寒松,韩士杰,李玉文,等利用树木年轮宽度资料重建长白山地区240年来降水量的变化[J].生态学杂志,2007,26(12)：1924-1929.
张杰,李栋梁.祁连山及黑河流域降雨量的分布特征分析[J].高原气象,2004,23(1)：81-88.
张庆乐,刘卫国,刘禹,等贺兰山地区树轮碳氧同位素与夏季风降水的相关性讨论[J].地球化学,2005,34(1)：51-56.
张瑞波,魏文寿,袁玉江,等.1396-2005年天山南坡阿克苏河流域降水序列重建与分析[J].冰川冻土,2009,31(1)：27-33.
张瑞波,袁玉江,魏文寿,等用树轮灰度重建乌孙山北坡4—5月平均最低气温[J].中国沙漠,2008(5)：848-854.
张瑞波,袁玉江,魏文寿,等西藏东部过去400年秋、冬季平均最低气温的树木年轮分析[J].高原气象,2010,29(2)：359-365.
张同文,王丽丽,袁玉江,等利用树轮宽度资料重建天山中段南坡巴仑台地区过去645年来的降水变化[J].地理科学,2011,31(2)：251-256.
张同文,袁玉江,魏文寿,等阿勒泰柯姆地区树轮宽度年表与灰度年表的建立[J].沙漠与绿洲气象,2007,1(3)：9-14.
张同文,袁玉江,魏文寿,等使用树轮资料重建阿勒泰西部年积雪深度≥0cm日数的长期变化[J].沙漠与绿洲气象,2010,4(3)：6-11.
张小明,魏锋,陆燕.祁连山近45a年降水异常的气候特征[J].干旱气象,2006,24(3)：35-41.
张永香.季风边缘区近200年来的树轮记录研究[D].兰州：兰州大学,2005a.
张永香,勾晓华,胡文东,等树轮记录的贺兰山区近百年来的干旱事件[J].生态学报,2005b,25(8)：2121-2126.
张志华,李骥,Graumlich LJ,等用树轮密度及宽度资料重建新疆吉木萨尔县的季节降水和最高温度[J].气象学报,1998,56(1)：77-86.
张志华,吴祥定.利用树木年轮资料恢复祁连山地区近700年来气候变化[J].科学通报,1997,42(8)：849-851.
张志华,吴祥定,李骥.利用树木年轮资料重建新疆东天山300多年来干旱日数的变化[J].应用气象学报,1996,7(1)：53-60.
张志华,吴祥定.祁连山地区1310年以来湿润指数及其年际变幅的变化与突变分析[J].第四纪研究,1996,15(4)：368-378.
赵兴云.中国东部亚热带地区树轮δ13C年序列及方位变化的环境意义[D].南京：南京师范大学,2006.
赵兴云,王建,钱君龙,等天目山地区树轮δ13C记录的300多年的秋季气候变化[J].山地学报,2005,23(5)：540-549.
赵兴云,王建,商志远,等天目山柳杉树轮813C序列所反映的植物水分利用率对大气CO2浓度变化的生理响应[J].地理科学,2008,28(5)：698-702.
周文盛.根据阿尔泰山南坡树木年轮初步分析额尔齐斯河500年(1582-2081)径流量[J].干旱区地理,1984,7(1)：35-49.
朱海峰.利用树轮宽度网络重建我国东北地区东部温度变化[D].北京：北京师范大学,2006.
朱守森,王强.祁连山区北坡降水的时空分布及近期变化[J].冰川冻土,1996.18(增刊)：296-304.
朱西德,秦宁生,李栋梁,等利用树木年轮重建柴达木地区5-6月地温[J].高原气象,2005,24(3)：331-337.
朱西德,王振宇,李林,等树木年轮指示的柴达木东北缘近千年夏季气温变化[J].地理科学,2007,27(2)：256-260.
朱益民,杨修群.太平洋年代际振荡与中国气候变率的联系[J].气象学报,2003,61(6)：641-654.
卓正大,胡双熙,张先恭,等祁连山地区树木年轮与我国近千年(1059-1975年)的气候变化[J].兰州大学学报,1978,14(2)：145-157.
Anderson RL, Byrne R, Dawson T. Stable isotope evidence for a foggy climate on Santa Cruz Island, California at -?6,600 cal. yr. B.P[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2008,262:176-181.
Bar A, Pape R, Brauning A et al. Growth-ring variations of dwarf shrubs reflect regional climate signals in alpine environments rather than topoclimatic differences[J]. Journal of Biogeography,2008,35:625-636.
Bale RJ, Robertson I, Leavitt SW, et al. Temporal stability in bristlecone pine tree-ring stable oxygen isotope chronologies over the last two centuries[J]. The Holocene,2010,20:3-6.
Biondi F. Evolutionary and moving response functions in dendroclimatology[J]. Dendrochronologia,1997,15:139-150.
Biondi F. Are cliamte-tree growth relationships changing in north-central Idaho? [J] Arctic, Antarctic, and Alpine Research,2000,32:111-116.
Biondi F, Estrada IG. Tree-Ring Evidence for the 1913 Eruption of Volcan de Fuego de Colima, Mexico[J]. Quaternary Research,2003,59:293-299.
Biondi F, Waikul K. DENDROCLIM2002:a C++ program for statistical calibration of climate signals in tree-ring chronologies [J]. Computer Geoscience,2004,30:303-311.
Black BA, Copenheaver CA, Frank DC, et al. Multi-proxy reconstructions of northeastern Pacific sea surface temperature data from trees and Pacific geoduck[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2009,278:40-47.
Boswijk G, Fowler A, Lorrey A, et al. Extension of the New Zealand kauri (Agathis australis) chronology to 1724 BC[J]. The Holocene,2006,16:188-199.
Briffa KR, Jones PD, Bartholin TS, et al. Fennoscandian summers from AD 500:temperature changes on short and long timescales[J]. Climate Dynamics,1992a,7:111-119.
Briffa KR, Jones PD, Schweingruber FH. Summer temperature patterns over Europe:A reconstruction from 1750 A.D. based on maximum latewood density indices of conifers[J]. Quaternary Research,1988,30:36-52.
Briffa KR, Jones PD, Schweingruber FH. Tree-ring density reconstructions of summer temperature patterns across western North America since 1600[J]. Journal of Climate, 1992b,5:735-754.
Briffa KR, Jones PD, Schweingruber FH, et al. Influence of volcanic eruptions on Northern Hemisphere summer temperature over the past 600 years[J]. Nature,1998,393:450-455.
Brito-Castillo L, Diaz-Castro S, Salinas-Zavala CA, et al. Reconstruction of long-term winter streamflow in the Gulf of California continental watershed[J]. Journal of Hydrology, 2003,278:39-50.
Buntgen U, Brazdil R,Frank D, et al. Three centuries of Slovakian drought dynamics[J]. Climate Dynamics,2009.35:315-329.
Biintgen U, Esper J, Frank DC, et al. A 1052-year tree-ring proxy for Alpine summer temperatures [J]. Climate Dynamics,2005a,25:141-153.
Buntgen U, Esper J, Frank DC, et al. The effect of power transformation on RCS-evidence from three millennial-length alpine chronologies. In:Gartner et al. (Eds.) Proceedings volume. International conference tree rings in archaeology, climatology and ecology, Birmensdorf, Switzerland. Environment 53, Julich,2005b,141-149.
Biintgen U, Frank D, Wilson R, et al. Testing for tree-ring divergence in the European Alps[J]. Global Change Biology,2008,14:1-11.
Cai QF,Liu Y. January to August temperature variability since 1776 inferred from tree-ring width of Pinus tabulaeformis in Helan Mountain[J]. Journal of Geographical Sciences, 2007,17:293-303.
Cai Q F, Liu Y, Song H, et al. Tree-ring-based reconstruction of the April to September mean temperature since 1826 AD for north-central Shaanxi Province, China[J]. Science in China Series D:Earth Sciences,2008,51:1099-1106.
Camarero JJ, Guerrero-Campo G, Gutierrez E. Tree-ring growth and structure of Pinus uncinata and Pinus sylvestris in the central Spanish Pyrenees[J]. Arctic and Alpine Research, 1998,30:1-10.
Campbell R, McCarroll D, Loader NJ, et al. Blue intensity in Pinus sylvestris tree-rings, developing a new palaeoclimate proxy[J]. The Holocene,2007,17:821-828.
Campbell R, McCarroll D, Robertson I, et al. Blue Intensity in Pinus sylvestris tree rings:A manual for a new palaeoclimate proxy[J]. tree-ring research,2011,67:127-134.
Carson EC, Munroe JS. Tree-ring based streamfiow reconstruction for Ashley Creek, northeastern Utah:implications for palaeohydrology of the southern Uinta Mountains[J]. The Holocene,2005,15:602-611.
Case RA, MacDonald GM. A Dendroclimatic Reconstruction of Annual Precipitation on the Western Canadian Prairies since A.D.1505 from Pinus flexilis James[J]. Quaternary Research, 1995,44:267-275.
Case RA, MacDonald GM. Tree ring reconstructions of streamflow for three Canadian Prairie Rivers[J]. Journal of the American Water Resources Association,2003,39:703-716.
Charles CD, Hunter DE, Fairbanks RG. Interaction between the ENSO and the Asian monsoon in a coral record of tropical climate[J]. Science,1997,277:925-928.
Chen J, Wang LL, Zhu HF, et al. Reconstructing mean maximum temperature of growing season from the maximum density of the Schrenk Spruce in Yili, Xinjiang, China[J]. Chinese Science Bulletin,2009,54:2300-2308.
Chinga-Carrasco G. Microscopy and computerized image analysis of wood pulp fibres multiscale structures. In:Mendez-Vilas A, Diaz J (Eds.), Microscopy:Science, Technology, Applications and Education. Microscopy Book Series. Formatex,2011,2182-2189.
Cleaveland MK. a 963-year reconstrucion of summer (JJA) stream flow in the white river,from tree-rings[J]. The Holocene,2000,10:33-41.
Cook ER, D' Arrigo RD, Mann ME. A well-verified, multiproxy reconstruction of the winter North Atlantic Oscillation Index since A.D.1400[J]. Journal of Climate, 2002a,15:1754-1764.
Cook ER, Esper J, D' Arrigo RD. Extra-tropical Northern Hemisphere land temperature variability over the past 1000 years[J]. Quaternary Science Reviews,2004,23:2063-2074.
Cook ER, Kairiukstis A. Methods of Dendrochronology:Applications in the Environmental Sciences[M]. Dordrecht:Kluwer Academic Press,1990.
Cook ER, Keith R, Briffa PDJ. Spatial regression methods in dendroclimatology:A review and comparison of two techniques[J]. International Journal of Climatology,1994,14:379-402.
Cook ER, Meko DM, Stahle DW, et al. Drought reconstructions for the continental United States[J]. Journal of Climate,1999,12:1145-1162.
Cook ER, Palmer JG, D'Arrigo RD. Evidence for a 'Medieval Warm Period' in a 1100 year tree-ring reconstruction of past austral summer temperatures in New Zealand[J]. Geophysical Research Letters,2002b,29:1667-1770.
Cook ER, Seager R, Cane MA, et al. North American drought:Reconstructions, causes, and consequences[J]. Earth-Science Reviews,2007,81:93-134.
Cook ER, Woodhouse CA, Eakin M. Long-Term Aridity Changes in the Western United States[J]. Science,2006,306:1015-1018.
Cropper JP. Tree-ring skeleton plotting by computer[J]. Tree-ring bulletin,1979,39:47-54.
Cruz-Munoz AR, Rodriguez-Fernandez L, Calva-Vazquez G, et al. Effects due to Popocatepetl volcano eruptions on the elemental concentrations in tree growth rings[J]. X-Ray Spectrometry,2008,37:163-168.
Cullen LE, Grierson PF.Multi-decadal scale variability in autumn-winter rainfall in south-western Australia since 1655 AD as reconstructed from tree rings of Callitris columellaris[J]. Climate Dynamics,2009,33:433-444.
D'Arrigo R, Abram N, Ummenhofer C, et al. Reconstructed streamflow for Citarum River, Java, Indonesia:linkages to tropical climate dynamics[J]. Climate Dynamics,2010,36:451-462.
D'Arrigo R, Allan R, Wilson R, et al. Pacific and Indian Ocean climate signals in a tree-ring record of Java monsoon drought[J].International Journal of Climatology, 2008a,28:1889-1901.
D'Arrigo, Cook ER, Wilson RJ, et al. On the variability of ENSO over the past six centuries[J]. Geophysical Research Letters,2005a,32:L03711.
D'arrigo RD, Jacoby GC. Northern north American tree-ring evidence for regional temperature changes after major volcanic events[J]. Climatic Change,1999,41:1-15.
D'Arrigo R, Jacoby G, Frank D, et al.1738 years of Mongolian temperature variability inferred from a tree-ring width chronology of siberian pine[J]. Geophysical Research Letters, 2001,28:543-546.
D'Arrigo R, Mashig E, Frank D, et al. Temperature variability over the past millennium inferred from Northwestern Alaska tree rings[J]. Climate Dynamics,2005b,24:227-236.
D'Arrigo R,Wilson R. El Nino and Indian Ocean influences on Indonesian drought:implications for forecasting rainfall and crop productivity[J]. International Journal of Climatology, 2008b,28:611-616.
D'Arrigo R, Wilson R, Liepert B, et al. On the'Divergence Problem'in Northern Forests:A review of the tree-ring evidence and possible causes[J]. Global and Planetary Change, 2008c,60:289-305.
D'Arrigo R, Wilson R, Jacoby G. On the long-term context for late twentieth century warming[J]. Journal of Geophysical Research.2006a,111:D03103.
D'Arrigo R, Wilson R, Palmer J, et al. Monsoon drought over Java, Indonesia, during the past two centuries[J]. Geophysical Research Letters,2006b,33:L04709.
D'Arrigo R, Wilson R, Palmer J, et al. The reconstructed Indonesian warm pool sea surface temperatures from tree rings and corals:Linkages to Asian monsoon drought and El Nino-Southern Oscillation[J]. Paleoceanography,2006c,21:1-13.
D'arrigo R, Wilson R, Tudhope A. The impact of volcanic forcing on tropical temperatures during the past four centuries[J]. Nature Geoscience,2009,2:51-56.
D'Arrigo R, Wilson R. On the Asian expression of the PDO[J]. International Journal of Climatology,2006d,26:1607-1617.
Dai A. Characteristics and trends in various forms of the Palmer Drought Severity Index (PDSI) during 1900-2008[J]. Journal of Geophysical Research,2011a,116:D12115.
Dai A. Drought under global warming:Areview[J]. Climate Change,2011b,2:45-65.
Dai A, Trenberth KE, Qian T. A global dataset of Palmer Drought Severity Index for 1870-2002: relationship with soil moisture and effects of surface warming[J]. Journal of Hydrometeorology,2004,5:1117-1130.
Davi NK, Jacoby GC, D'Arrigo RD, et al. A tree-ring-based drought index reconstruction for far-western Mongolia:1565-2004[J]. International Journal of Climatology,2008,29: 1508-1514.
Davi NK, Jacoby GC, Wiles GC. Boreal temperature variability inferred from maximum latewood density and tree-ring width data, Wrangell Mountain region, Alaska[J]. Quaternary Research,2003,60:252-262.
Eronen M, Briffa KR, Lindholm M, et al. The supra-long Scots pine tree-ring record for Finnish Lapland:Part 1, chronology construction and initial inferences [J]. The Holocene, 2002,12:673-680.
Esper J, Frank D. Divergence pitfalls in tree-ring research[J]. Climatic Change, 2009,94:261-266.
Esper J, Frank D, Buntgen U, et al. Long-term drought severity variations in Morocco [J]. Geophysical Research Letters,2007,34:L17702.
Esper J, Cook ER, Schweingruber FH. Low-Frequency Signals in Long Tree-Ring Chronologies for Reconstructing Past Temperature Variability [J]. Science,2002,295:2250-2253
Esper J, Cook ER, Krusic PJ, et al. Tests of the RCS method for preserving low-frequency variability in long tree-ring chronologies[J]. tree-ring research,2003,59:81-98.
Fan ZX, Brauning A, Cao KF. Annual temperature reconstruction in the central Hengduan Mountains, China, as deduced from tree rings[J]. Dendrochronologia,2008a,26:97-107.
Fan ZX, Brauning A, Cao KF, et al. Tree-ring based drought reconstruction in the central Hengduan Mountains region (China) since A.D.1655[J]. International Journal of Climatology, 2008b,28:1879-1887.
Fan ZX, Brauning A, Tian QH, et al. Tree ring recorded May-August temperature variations since A.D.1585 in the Gaoligong Mountains, southeastern Tibetan Plateau[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2010,296:94-102.
Fan ZX, Brauning A, Yang B, et al. Tree ring density-based summer temperature reconstruction for the central Hengduan Mountains in southern China[J]. Global and Planetary Change, 2009.65:1-11.
Fang KY, Gao XH. Chen FH. et al. Drought variations in the eastern part of northwest China over the past two centuries:evidence from tree rings[J]. Climate Research,2009,38:129-135.
Fang KY, Gou XH, Chen FH, et al. Tree-ring based drought reconstruction for the Guiqing Mountain (China):linkages to the Indian and Pacific Oceans[J]. International Journal of Climatology,2010a,30:1137-1145.
Fang KY, Gou XH, Chen FH, et al. Reconstructed droughts for the southeastern Tibetan Plateau over the past 568 years and its linkages to the Pacific and Atlantic Ocean climate variability[J]. Climate Dynamics,2010b,35:577-585.
Feng S, Hu Q. Variations in the teleconnection of ENSO and summer rainfall in northern China: a role of the Indian summer monsoon[J]. Journal of Climate,2004,17:4871-4881.
Frank D, Esper J. Temperature reconstructions and comparisons with instrumental data from a tree-ring network for the European Alps[J]. International Journal of Climatology, 2005,25:1437-1454.
Fritts HC. Tree ring and climate[M], London:Academic Press,1976.
Fowler AM, Boswijk G, Gergisb J, et al. ENSO history recorded in Agathis australis (kauri) tree rings. Part A:kauri's potential as an ENSO proxy[J]. International Journal of Climatology, 2008,28:1-20.
Gagen M, Zorita E, McCarroll D, et al. Cloud response to summer temperatures in Fennoscandia over the last thousand years[J]. Geophysical Research Letters,2011,338:L05701.
Gao SY, Lu RJ, Qiang MR, et al. Reconstruction of precipitation in the last 140 years from tree ring at south margin of the Tengger Desert, China[J]. Chinese Science Bulletin, 2005,50:2487-2492.
Gedalof Z, Peterson DL, Mantua NJ. Columbia River flow and drought since 1750[J]. Journal of the American Water Resourses Association,2004,60:1579-1592.
George SS, Nielsen E. Hydroclimatic change in southern Manitoba since A.D.1409 inferred from tree rings [J]. Quaternary Research,2002,58:103-111.
Gindl W, Grabner M, Wimmer R. The influence of temperature on latewood lignin content in treeline Norway spruce compared with maximum density and ring width[J].Trees, 2000.14:409-414.
Glueck MF, Stockton CW. Reconstruction of the North Atlantic Oscillation,1429-1983[J]. International Journal of Climatology,2001,21:1453-1465.
Gou XH, Chen FH, Cook ER, et al. Streamflow variations of the Yellow River over the past 593 years in western China reconstructed from tree rings[J]. Water Resources Research, 2007,43:W06434.
Gou XH, Chen FH, Yang MX, et al. Climatic response of thick leaf spruce(Picea crassifolia) tree-ring width at different elevations over Qilian Mountains, northwestern China[J]. Journal of Arid Environments,2005,61:513-524.
Graumlich LJ. A 1000-Year Record of Temperature and Precipitation in the Sierra Nevada[J]. Quaternary Research,1993,39:249-255.
Graumlich LJ, Pisaric MJ, Waggoner LA. Upper Yellowstone River flow and teleconnections with Pacific basin climate variability during the past three centuries[J]. Climatic Change, 2003,59:245-262.
Grudd H. Briffa KR. Karlen W, et al. A 7400-year tree-ring chronology in northern Swedish Lapland--natural climatic variability expressed on annual to millennial timescales[J]. The Holocene,2002,12:657-665.
Grudd H. Tornetrask tree-ring width and density AD 500-2004:a test of climatic sensitivity and a new 1500-year reconstruction of north Fennoscandian summers[J]. Climate Dynamics, 2008,31:843-857.
Guilderson TP, Schrag DP. Abrupt shift in subsurface temperature in the tropical Pacific associated with changes in El Nino[J]. Science,1998,281:240-243.
Gunnarson BE. Temporal distribution pattern of subfossil pines in central Sweden:perspective on Holocene humidity fluctuations[J]. Holocene,2008,18:569-577.
Heinrich I, Weidner K, Helle G, et al. Hydroclimatic variation in Far North Queensland since 1860 inferred from tree rings[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2008,270:116-127.
Helama S, Lindholm M, Timonen M, et al. The supra-long Scots pine tree-ring record for Finnish Lapland:Part 2, interannual to centennial variability in summer temperatures for 7500 years[J]. The Holocene,2002,12:681-687.
Holmes JA, Cook ER, Yang B. Climate change over the past 2000 years in Western China[J]. Quaternary International,2009,194:91-107.
Hughes M K,张光威,刘季花.根据树轮密度和宽度对公元1600年以来中国中北部降雨量的初步重建[J].海洋地质动态,1995：17-19.
Hughes MK, Brown PM. Drought frequency in central California since 101 B.C. recorded in giant sequoia tree rings[J]. Climate Dynamics,1992,6:161-167.
Hughes MK, Graumlich, LJ. Multimillennial dendroclimatic studies from the western United States. In:Jones PD, Bradley RS, Jouzel J (Eds.), Climatic Variations and Forcing Mechanisms of the Last 2000 Years[M]. Springer-Verlag, Berlin,1996,109-124.
Hurrell JW, Trenberth KE. Sea surface temperature analyses:multiple problems and their implications for climate analysis, modeling, and reanalysis[J]. Bulletin of the American Meteological Society,1999,80:2661-2678.
Jacoby GC, Lovelius NV, Shumilov 01, et al. Long-term temperature trends and tree growth in the Taymir Region of northern Siberia[J]. Quaternary Research,2000,53:312-318.
Jagels, R, Telewski FW. Computer-aided image analysis of tree rings. In:E.R. Cook & L.A. Kairiukstis (eds.), Methods of dendrochronology:Applications in the environmental sciences[M]. Kluwer Academic Publishers, Dordrecht,1990,76-93.
Kirdyanov AV, Vaganov EA, Hughes MK. Separating the climatic signal from tree-ring width and maximum latewood density records[J]. Trees,2007,21:37-44.
Knight TA, Meko DM, Baisan CH. A bimillennial-length tree-ring reconstruction of precipitation for the Tavaputs Plateau, Northeastern Utah[J]. Quaternary Research,2010,73:107-117.
Koretsune S, Fukuda K, Chang Z. Effective rainfall seasons for interannual variation in δ13C and tree-ring width[J]. Journal of Forest Research,2009,14:88-94.
Lan YC, Lin S, Hu XL, et al. Effect of ENSO cycle on the temperature precipitation and runoff in Qilian Mountainous area, northwestern China[J]. Journal of Desert Research, 2009,29:352-258.
Lan YC, Kang ES, Zhang JS. et al. Trends and characteristics on mountainous runoff in Hexi inland arid region[J]. Journal of Desert Research,2002,22:135-141.
Lara A, Urrutia R, Villalba R, et al. The potential use of tree-rings to reconstruct streamflow and estuarine salinity in the Valdivian Rainforest eco-region, Chile[J]. Dendrochronologia, 2005,22:155-161.
Lara A, Villalba R. A 3620-year temperature record from Fitzroya cupressoides tree rings in southern South America[J]. Science,1993,260:1104-1106.
Lara A, Villalba R, Urrutia R. A 400-year tree-ring record of the Puelo River summer-fall streamflow in the Valdivian Rainforest eco-region, Chile[J]. climate Change, 2008,86:331-356.
Lees JM, Park J. Multiple-taper spectral analysis:A stand-alone C-subroutine. Computers & Geosciences,1995,21:199-236.
Li JB, Chen FH, Cook. ER, et al. Drought reconstruction for North Central China from tree rings: the value of the Palmer drought severity index[J]. International Journal of Climatology, 2007,27:903-909.
Li ZS, Shi CM, Liu YB, et al. Summer mean temperature variation from 1710-2005 inferred from tree-ring data of the Baimang Snow Mountains, northwestern Yunnan, China[J]. Climate Research,2011a,47(3):207-218.
Li ZS, Zhang QB, Ma KP. Tree-ring reconstruction of summer temperature for A.D.1475-2003 in the central Hengduan Mountains, Northwestern Yunnan, China[J]. Climatic Change,2011b. DOI:10.1007/s 10584-011-0111-z.
Liang EY, Liu XH, Yuan YJ, et al. The 1920S drought recorded by tree rings and historical documents in the semi-arid and arid areas of Northern China[J]. Climatic Change, 2006,79:403-432.
Liang EY, Shao XM, Hu YX, et al. A dendroclimatic study of relic picea meyeri in Inner Mongolian Steppe[J]. Acta Botanica Sinica,2001,43:288-294.
Liang E, Shao X, Kong Z, et al. The extreme drought in the 1920s and its effect on tree growth deduced from tree ring analysis:a case study in North China[J]. Annals of forest science, 2003,60:145-152.
Liang EY, Shao XM, Liu XH. Annual precipitation variation inferred from tree rings since A.D. 1770 for the western Qilian Mts., northern Tibetan Plateau[J]. Tree-ring research, 2009a,65:95-104.
Liang EY, Shao XM, Liu HY, et al. Tree-ring based PDSI reconstruction since AD 1842 in the Ortindag Sand Land, east Inner Mongolia[J]. Chinese Science Bulletin,2007,52:2715-2721.
Liang EY, Shao XM, Xu Y. Tree-ring evidence of recent abnormal warming on the southest Tibetan Plateau[J]. Theoretical and Applied Climatology,2009b,98:9-18.
Liang EY, Eckstein D, Liu HY. Assessing the recent grassland greening trend in a long-term context based on tree-ring analysis:A case study in North China[J]. Ecological Indicators, 2009c,9:1280-1283.
Liang Y, Yu HJ, Xu XY, et al. Exploratory Precipitation in North-Central China during the Past Four Centuries[J]. Acta Geologica Sinica,2010,84:223-229.
Lindeberg J. X-ray based tree ring analyses[D]. Umea:Swedish University,2004.
Liu Y, An Z, Linderholm HW, et al. Annual temperatures during the last 2485 years in the mid-eastern Tibetan Plateau inferred from tree rings[J]. Science in China Series D:Earth Sciences,2009a,52:348-359.
Liu Y, Bao G, Song HM, et al. Precipitation reconstruction from Hailar pine (Pinus sylvestris var. mongolica) tree rings in the Hailar region, Inner Mongolia, China back to 1865 AD[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2009b,282:81-87.
Liu Y, Cai QF, Park W-K, et al. Tree-ring precipitation records from Baiyinaobao, Inner Mongolia since A.D.1838[J]. Chinese Science Bulletin,2003,48:1140-1145.
Liu Y, Cai QF, Liu WG, et al. Monsoon precipitation variation recorded by tree-ring [delta] 180 in arid Northwest China since AD 1878[J]. Chemical Geology,2008,252:56-61.
Liu Y, Linderholm HW, Song H, et al. Temperature variations recorded in tree rings from the southern and northern slopes of the central Qinling Mountains, central China[J]. Boreas, 2009c,38:285-291.
Liu Y, Ma LM, Leavitt SW, et al. A prepliminary seasonal precipitation reconstruction from tree-ring stable carbon isotopes at Mt.Helan, China, since AD 1804[J]. Global and Planetary Change,2004,41:229-239.
Liu PX, Peng JF,Chen FH. Hydrological response of Populus euphratica Olve. radial growth in Ejinaa Banner, Inner Mongolia[J]. Journal of Integrative Plant Biology,2007a,49:150-156.
Liu XH, Qin DH, Shao XM, et al. Temperature variations recovered from tree-rings in the middle Qilian Mountain over the last millennium[J]. Science in China Series D:Earth Sciences,2005,48:521-529.
Liu XH, Shao XM, Zhao LJ, et al. Dendroclimatic temperature record derived from tree-ring width and stable carbon isotope chronologies in the middle Qilian Mountains, China[J]. Arctic, Antarctic, and Alpine Research,2007b,39:651-657.
Liu Y, Sun JY, Song HM, et al. Tree-ring hydrologic reconstructions for the Heihe River watershed, western China since AD 1430 [J]. Water Research,2010,44:2781-2792.
Liu Y, Sun JY, Yang YK, et al. Tree-ring-derived precipitation records from inner Mongolia, China, Since A.D.1627[J]. Tree-Ring Research,2007c,63:3-14.
Liu WH, Gou XH, Yang MX, et al. Drought reconstruction in the Qilian Mountains over the last two centuries and its implications for large-scale moisture patterns[J]. Advances In Atmospheric Sciences,2009d,26:621-629.
Mantua NJ, Hare SR, Zhang Y, et al. A Pacific interdecadal climate oscillation with impacts on salmon production[J]. Bulletin of the American Meteorological Society,1997,78:1069-1079.
Martinez-Meier A, Sanchez L, Pastorino M, et al. What is hot in tree rings? The wood density of surviving Douglas-firs to the 2003 drought and heat wave[J]. Forest Ecology and Management,2008,256:837-843.
McCarroll D, Pettigrew E, Luckman A, et al. Blue reflectance provides a surrogate for latewood density of high-latitude pine tree rings[J]. Arctic, Antarctic and Alpine Research, 2002,34:450-453.
Meko DM, Cook ER, Stahle DW, et al. Spatial patterns of tree-growth anomalies in the United States and southeastern Canada[J]. Journal of Climate,1993,6:1773-1786.
Meko DM, Therrell MD, Baisan CH, et al. Sacramento river flow reconstructed to A.D.869 from tree rings[J]. Journal of the American Water Resourses Association,2001,37:1029-1039.
Meko DM, Woodhouse CA. Tree-ring footprint of joint hydrologic drought in Sacramento and Upper Colorado river basins, western USA[J]. Journal of Hydrology,2005,308:196-213.
Moell MK. Donaldson LA. Comparison of segmentation methods for digital image analysis of confocal microscope images to measure tracheid cell dimensions[J].IAWA Journal, 2001,22:267-288.
Nicault A, Alleaume S, Brewer S, et al. Mediterranean drought fluctuation during the last 500 years based on tree-ring data [J]. Climate Dynamics,2008,31:227-245.
Nicolussi K, Kaufmann M, Melvin TM, et al. A 9111 year long conifer tree-ring chronology for the European Alps:a base for environmental and climatic investigations[J]. The Holocene, 2009,19:909-920.
Nitta T, Yanmada S. Recent warming of the tropical sea surface temperature and its relationship to northern hemisphere circulation[J]. Journal of the Meteorological Society of Japan, 1989,67:375-383.
Ogurtsov MG, Kocharov GE, Lindholm M, et al. Evidence of solar variation in tree-ring-based climate reconstructions[J]. Solar Physics,2002,205:403-417.
Ogurtsov MG, Helama S, Eronen M, et al. Centennial-to-millennial fluctuations in July temperatures in North Finland as recorded by timberline tree rings of Scots pine[J]. Quaternary Research,2005,63:182-188.
Park WK, Telewski FW. Measuring maximum latewood density by image analysis at the cellular level[J]. Wood and Fiber Science,1993,25:326-332.
Palmer WC. Meteorological drought. Weather Bureau Research Paper 45. U.S. Department of Commerce:Washington, DC,1965,58.
Pederson N, Jacoby GC, D'arrigo RD, et al Hydrometeorological reconstructions for northeastern Mongolia derived from tree rings:1651-1995 [J]. Journal of Climate, 2001,14:872-881.
Pilcher JR, Baillie MGL, Schmidt B, et al. A 7,272-year tree-ring chronology for western Europe[J]. Nature,1984,312:150-152.
Polge H. Fifteen years of wood radiation densitometry[J]. Wood Science Technology, 1978,12:187-196.
Popa 1, Kern Zn. Long-term summer temperature reconstruction inferred from tree-ring records[J]. Climate Dynamics,2009,32:1107-1117.
Qin C, Yang B, Burchardt I, et al. Intensified pluvial conditions during the twentieth century in the inland Heihe River Basin in arid northwestern China over the past millennium[J]. Global and Planetary Change,2010,72:192-200.
Qian WH, Ding T, Hu HR, Lin X, Qin AM. An overview of dry-wet climate variability among monsoon-westerly region and the monsoon northernmost marginal active zone in China[J]. Advances in Atmospheric Science,2009,26:600-641.
Ram S, Borgaonkar HP,Sikder AB. Tree-ring analysis of teak (Tectona grandis L.F.) in central India and its relationship with rainfall and moisture index[J]. Journal of Earth System Science, 2008,117:637-645.
Ram S, Borgaonkar HP,Sikder AB. Varying strength of the relationship between tree-rings and summer month moisture index (April-September) over Central India:A case study [J]. Quaternary International,2010,212:70-75.
Raspopov OM, Dergachev VA, Kolstrom T. Periodicity of climate conditions and solar variability derived from dendrochronological and other palaeoclimatic data in high latitudes. Palaeogeography. Palaeoclimatology. Palaeoecology,2004.209:127-139.
Reynolds RW, Smith TM. Improved global sea surface temperature analyses using optimum interpolation[J]. Journal of Climate,1994,7:929-948.
Rigozo NR, Nordemann DJR, Echer E, et al. An interactive method for digital tree-ring width measurement[J]. Geofisica Internacional,2004,43:281-285.
Rigozo NR, Nordemann DJR, Echer E, et al. Solar variability effects studied by tree-ring data wavelet analysis[J]. Advances in Space Research,2002,29:1985-1988.
Rinn F. High frequency wood density scanning[R].7th International Conference on Dendrochronology (1CD), Beijing, China,2006.
Roig FA, Le-Quesne C, Boninsegna JA, et al.. Climate variability 50,000 years ago in mid-latitude Chile as reconstructed from tree rings[J]. Nature,2001,410:567-570.
Sano M, Furuta F, Kobayashi O, et al. Temperature variations since the mid-18th century for western Nepal, as reconstructed from tree-ring width and density of Abies spectabilis[J]. Dendrochronologia,2005,23:83-92.
Sano M, Buckley BM, Sweda T. Tree-ring based hydroclimate reconstruction over northern Vietnam from Fokienia hodginsii:eighteenth century mega-drought and tropical Pacific influence[J]. Climate Dynamics,2009,33:331-340.
Schinker MG, Hansen N, Spiecker H. High-freqency densitometry-a new method for the rapid evaluation of wood density variations [J]. IAWA Journal,2003,24:231-239.
Selvaraj K, Chen CTA, Lou JY. Holocene East Asian monsoon variability:links to solar and tropical Pacific forcing[J]. Geophysical Research Letters,2007,34:L01703.
Shao XM, Xu Y, Yin ZY, et al. Climatic implications of a 3585-year tree-ring width chronology from the northeastern Qinghai[J]. Quaternary Science Reviews,2010,29:2111-2122.
Sheppard PR, Graumlich LJ, Conkey LE. Reflected-light image analysis of conifer tree rings for reconstructing climate[J]. The Holocene,1996,6:62-68.
Shi YF, Shen YP, Kaag ES, et al. Recent and Future Climate Change in Northwest China[J]. Climatic Change,2007,80:379-393.
Singh J, Park WK.Yadav RR. Tree-ring-based hydrological records for western Himalaya, India, since a.d.1560[J]. Climate Dynamics,2006,26:295-303.
Spiecker H, Schinker M, Hansen J, et al. Cell structure in tree rings:novel methods for preparation and image analysis of large cross sections[J]. IAWA Journal,2000,21:361-373.
Tan LC, Cai YJ, Yi L, An ZS, Ai L. Precipitation variations of Longxi, northeast margin of Tibetan Plateau since AD 960 and their relationship with solar activity [J]. Climate of the Past, 2008,4:19-28.
Thetford RD, D'Arrigo RD, Jacoby GC. An image analysis system for determining densitometric and ring-width time series[J]. Canadian Journal of Forest Research,1991,21:1544-1549.
Tian QH, Gou XH, Zhang Y, et al. May-June mean temperature reconstruction over the past 300 years based on tree rings on the Qilian Mountains of the northeastern Tibetan Plateau[J]. IAWA Journal,2009,30:421-434.
Tian QH, Gou XH, Zhang Y, et al. Tree-ring based drought reconstruction (A.D.1855-2001) for the qilian mountains, northwestern china[J]. Tree-ring research,2007,63:27-36.
Till C, Guiot J. Reconstruction of precipitation in Morocco since 1100 A.D. based on cedrus atlantica tree-ring widths[J]. Quaternary Research,1990,33:337-351.
Timilsena J, Piechota TC, Hidalgo H, et al. Five hundred years of hydrological drought in the upper Colorado River Basin[J]. Journal of the American Water Resources Association, 2007,43:798-812.
Torrence C, Webster PJ. Interdecadal changes in the ENSO-Monsoon system. Journal of Climate, 1999,12:2679-2690.
Touchan R, Akkemik U, Hughes MK, et al. May-June precipitation reconstruction of southwestern Anatolia, Turkey during the last 900 years from tree rings[J]. Quaternary Research,2007,68:196-202.
Touchan R, Meko DM, Aloui A. Precipitation reconstruction for Northwestern Tunisia from tree rings[J]. Journal of Arid Environments,2008,72:1887-1896.
Trenberth KE. The definition of El Nino[J]. Bulletin of the American Meteorological Society, 1997,78:2771-2777.
Trenberth KE, Stepaniak DK. Indices of El Nino evolution[J]. Journal of Climate, 2001,14:1697-1701.
Tuovinen M, McCarroll D, Grudd H. Spatial and temporal stability of the climatic signal in northern Fennoscandian pine tree-ring width and maximum density[J].Boreas,2008,38:1-12.
Twine TE, Kucharik CJ, Foley JA. Effects of El Nino-Southern Oscillation on the climate, water balance, and streamflow of the Mississippi River Basin[J]. Journal of Climate, 2005,18:4840-4861.
Vaganov EA, Hughes MK, Kirdyanov AV, et al. Influence of snowfall and melt timing on tree growth in Subarctic Eurasia[J]. Nature,1999,400:149-151.
Vieira J, Campelo F, Nabais C. Age-dependent responses of tree-ring growth and intra-annual density fluctuations of Pinus pinaster to Mediterranean climate[J]. Trees,2009,23:257-265.
Wang B, Wu R, Fu X. Pacific-east Asian teleconnection:how does ENSO affect East Asian Climate? Journal of Climate,2000,13:1517-1536.
Wang LL, Duan JP, Chen J, et al. Temperature reconstruction from tree-ring maximum density of Balfour spruce in eastern Tibet, China[J]. International Journal of Climatology, 2010,30:972-979.
Wang XC, Zhang QB, Ma KP, et al. A tree-ring record of 500-year dry-wet changes in nothern Tibet, China[J]. The Holocene,2008,18:579-588.
Wang YJ, Cheng H, Edwards RL, et al. The Holocene Asian monsoon:links to solar changes and north Atlantic climate[J]. Science,2005,308:854-857.
Wang YX, Liu GY, Zhang XG, et al. The relationships between tree rings of Qilianshan juniper and climatic change and glacial activity during the past 1000 years in China. [J]. Chinese Science Bulletin,1983,28:1647-1647.
Watson TA, Barnett FA, Gray ST, et al. Reconstructed streamflows for the headwaters of the Wind River, Wyoming, United States[J]. Journal of the American Water Resources Association,2009,45:224-236.
Westermann J, Zerbe S, Eckstein D. Age structure and growth of degraded populus euphratica floodplain forests in north-west China and perspectives for their recovery[J]. Journal of Integrative Plant Biology,2008,50(5):536-546.
Wilmking M, Juday GP, Barder VA, et al. Recent climate warming forces constrasting growth response of white spruce at treeline in Alask through temperature thresholds[J]. Global Change Biology,2004,10:1724-1736.
Wilmking M, Myers-Smith I. Changing climate sensitivity of black spruce (Picea mariana Mill.) in a peatland-forest landscape in Interior Alaska[J]. Dendrochronologia,2008,25:167-175.
Wilson R, D'Arrigo R, Buckley B, et al. A matter of divergence:tracking recent warming at hemispheric scales using tree ring data[J]. Journal of Geophysical Research, 2007,112:D17103.
Woodcock DW. Climate sensitivity of wood-anatomical features in a ring-porous oak (Quercusmacrocarpa)[J]. Canadian Journal of Forest Research,1989,19:639-644.
Woodhouse CA. A tree-ring reconstruction of streamflow for the Colorado front range[J]. Journal of the American Water Resourses Association,2001,27:561-568.
Woodhouse CA, Lukas JJ. Multi-century tree-ring reconstructions of Colorado streamflow for water resource planning[J]. Climate Change,2006,78:293-315.
Yadav RR, Braeuning A, Singh J. Tree ring inferred summer temperature variations over the last millennium in western Himalaya, India[J]. Climate Dynamics,2010,36:1545-1554.
Yang B, Brauning A, Liu JJ, et al. Temperature changes on the Tibetan Plateau during the past 600 years inferred from ice cores and tree rings[J]. Global and Planetary Change, 2009a,69:71-78.
Yang B, Brauning A, Shi YF. Late Holocene temperature fluctuations on the Tibetan Plateau[J]. Quaternary Science Reviews,2003,22:2335-2344.
Yang B, Kang X, Brauning A, et al. A 622-Year regional temperature history of southeast Tibet derived from tree rings[J]. The Holocene,2009b,20:181-190.
Yang B, Kang XC, Shi YF. Decadal climaticvariations indicated by Dulan tree ring and comparison with other proxy data in China of the last 2000 years[J]. Chinese Geographical Science,2000,10:193-201.
Yanosky TM, Robinove CJ. Digital image measurement of the area and anatomical structure of tree-rings[J]. Canadian Journal of Botany,1986,64:2896-2902.
Yin ZY, Shao XM, Qin NS, et al. Reconstruction of a 1436-year soil moisture and vegetation water use history based on tree-ring widths from Qilian junipers in northeastern Qaidam Basin, northwestern China[J]. International Journal of Climatology,2008,28:37-53.
Yuan YJ, Shao XM, Wei WS, et al. The potential to reconstruct Manasi River streamflow in the Northern Tien Shan mountains, NW China[J]. Tree-ring Research,2007,63:81-93.
Zhang QB, Cheng GD, Yao TD, et al. A 2,326-year tree-ring record of climate variability on the northeastern Qinghai-Tibetan Plateau[J]. Geophysical Research Letters,2003,30:1739-1742.
Zhang Y, Tian QH, Gou XH, et al. Annual precipitation reconstruction since AD 775 based on tree rings from the Qilian Mountains, northwestern China[J]. International Journal of Climatology,2011,31:371-381.
Zhang YX, Wilmking M, Gou XH. Changing relationships between tree growth and climate in Northwest China[J]. Plant Ecology,2009,201:39-50.
Zheng JY, Wang WC, Ge QS, Man ZM, Zhang PY. Precipitation variability and extreme events in eastern China during the past 1500 years. Terrestrial Atmospheric and Oceanic Sciences, 2006,17:579-592.
Zhu HF, Shao XM, Yin ZY, et al. August temperature variability in the southeastern Tibetan Plateau since AD 1385 inferred from tree rings[J]. Palaeogeography, Palaeoclimatology, Palaeuecology.2011.305:84-92.
Zhu HF, Zheng Y, Shao X, et al. Millennial temperature reconstruction based on tree-ring widths of Qilian juniper from Wulan, Qinghai Province, China[J]. Chinese Science Bulletin, 2008,53:3914-3920.
曹泊,潘保田,高红山,等1972-2007年祁连山东段冷龙岭现代冰川变化研究[J].冰川冻土,2010,32(2)：242-248.
曹艳艳,郭品文,王群.ENSO与北半球冬季大气环流异常的年代际关系[J].南京气象学院学报,2007,30(6)：792-798.
蔡秋芳,刘禹,包光,等树轮记录的吕梁山地区公元1836年以来5-7月平均气温变化[J].科学通报,2010,55(20)：2033-2039.
蔡秋芳,刘禹,宋慧明,等树轮记录的陕西中-北部地区1826年以来4-9月温度变化[J].中国科学D辑：地球科学,2008,38(8)：971-977.
蔡秋芳,刘禹,杨银科,等陕西黄龙树轮年表的建立及其2-3月降水记录[J].海洋地质与第四纪地质,2005,25(2)：133-139.
蔡秋芳.贺兰山油松生长对三种不同水分指数的响应及1-7月Walter指数重建[J].海洋地质与第四纪地质,2009,29(6)：131-136.
曹受金,曹福祥,祁承经.湖南通道马尾松树轮宽度与气候因子的关系[J].中南林业科技大学学报,2010,30(12)：66-69.
陈宝君,钱君龙,濮培民,等.ENSO对天目山柳杉树轮同位素的影响[J].海洋地质与第四纪地质,2002,22(4)：53-58.
陈峰,陆守曾,杨珉Bootstrap估计及其应用[J].中国卫生统计,1997,14(5)：5-7.
陈峰,袁玉江,魏文寿,等.利用树轮图像灰度重建南天山北坡西部初夏温度序列[J].中国沙漠,2008,28(5)：842-847.
陈峰,袁玉江,魏文寿,等用西伯利亚落叶松年轮最大密度重建和布克赛尔5-8月份平均最高温度[J].生态学报,2010a,30(17)：4652-4658.
陈峰,袁玉江,魏文寿,等福建沙县马尾松树轮宽度与夏季亚洲-太平洋涛动指数的关系[J].第四纪研究,2011,31(1)：96-103.
陈峰,袁玉江,魏文寿,等树轮记录的甘肃山丹近224年降水变化[J].地理与地理信息科学,2010b,26(5)：82-86.
陈峰,袁玉江,魏文寿,等树轮记录的伊犁地区近354年帕尔默干旱指数变化[J].高原气象,2011,30(2)：355-362.
陈峰,袁玉江,魏文寿,等.特克斯河流域近236a降水变化及其趋势预测[J].山地学报,2010c,28(5)：545-551.
陈拓,陈发虎,安黎哲,等不同海拔祁连园柏树轮和叶片813C值的变化[J].冰川冻土,2004,26(6)：767-771.
陈月娟,周任君,简俊.东亚夏季风环流与ENSO循环的关系[J].高原气象,2002,21(6)：536-545.
崔宇,袁玉江,金海龙,等乌鲁木齐河源467年春季降水的重建与分析[J].干旱区地理,2007,30(04)：496-500.
邓自旺,钱君龙,屠其璞,等.环境因素对天目山柳杉树轮δ13C方位分布的影响[J].植物生态学报,2003,27(1)：93-98.
丁小俊.利用树轮资料的EOF迭代方案重建中东亚干旱半干旱区1500年来气温变化的初步研究[D].兰州：兰州大学,2007.
丁永建,叶佰生,刘时银.祁连山中部地区40a来气候变化及其对径流的影响[J].冰川冻土,2000,22(3)：193-199.
段建平.基于树轮的海螺沟冰川区气候及冰川变化研究[D].北京：中科院研究生院,2010a.
段建平,王丽丽,李论,等树轮最大密度记录的贡嘎山区公元1837年以来的温度变化[J].科学通报,2010b,55(11)：1036-1042.
范敏杰,袁玉江,魏文寿,等用树木年轮重建伊犁南天山北坡西部的降水量序列[J].干早区地理,2007,30(02)：268-273.
方克艳.近400年来西北地区气候变化的树轮记录研究[D].兰州：兰州大学,2010.
高琳琳,勾晓华,邓洋,等.树轮气候学中分异现象的研究进展[J].冰川冻土,2011,33(2)：453-460.
高尚玉,鲁瑞洁,强明瑞,等140年来腾格里沙漠南缘树木年轮记录的降水量变化[J].科学通报,2006,51(3)：326-331.
勾晓华,陈发虎,李金豹,等祁连山东部地区高分辨率气候记录研究[J].兰州大学学报(自然科学版),2002,38(1)：105-110.
勾晓华,陈发虎,王亚军,等利用树轮宽度重建近280 a来祁连山东部地区的春季降水[J].冰川冻土,2001,23(3)：292-296.
勾晓华,陈发虎,杨梅学,等祁连山中部地区树轮宽度年表特征随海拔高度的变化[J].生态学报,2004,24(1)：172-176.
勾晓华,陈发虎,杨梅学,等.青藏高原东北部树木年轮记录揭示的最高最低温的非对称变化[J].中国科学(D辑：地球科学),2007,37(11)：1480-1492.
勾晓华,邓洋,陈发虎,等.黄河上游过去1234年流量的树轮重建与变化特征分析[J].科学通报,2010,55(33)：3236-3243.
勾晓华,邵雪梅,王亚军,等祁连山东部地区树木年轮年表的建立[J].中国沙漠,1999,19(4)：364-367.
勾晓华,杨梅学,彭剑峰,等树轮记录的阿尼玛卿山区过去830年夏半年最高温变化[J].第四纪研究,2006,26(6)：991-998.
勾晓华.黄河源区树木年轮记录研究[D].兰州：兰州大学,2004.
何海.使用WinDENDRO测量树轮宽度及交叉定年方法[J].重庆师范大学学报(自然科学版),2005,22(4)：39-44.
何吉成,王丽丽,邵雪梅.漠河樟子松树轮指数与标准化植被指数的关系研究[J].第四纪研究,2005,25(2)：252-257.
何吉成,邵雪梅.德令哈地区树轮宽度指数与草地植被指数的关系[J].科学通报,2006,51(9)：1083-1090.
侯迎,王乃昂,李钢,等利用树轮资料重建1751-2005年崆峒山地区夏季温度变化[J].气候变化研究进展,2007,3(3)：172-176.
侯迎,王乃昂,张学敏,等高频光密度测量法在崆峒山树轮年表建立中的应用[J].干旱区地理,2010,33(02)：236-242.
胡良温,杨改河,李轶冰,等利用祁连圆柏年轮资料重建江河源区东北部600余年气候研究[J].西北农林科技大学学报(自然科学版),2006,34(5)：107-113.
黄磊,邵雪梅.青海德令哈地区近400年来的降水量变化与太阳活动[J].第四纪研究,2005,25(2)：184-192.
黄玉霞,王宝鉴,张强,等气候变化和人类活动对石羊河流域水资影响评价[J].高原气象,2008,27(4)：866-872.
贾文雄,何元庆,李宗省,等祁连山区气候变化的区域差异特征及突变分析[J].地理学报,2008,63(3)：257-269
江善虎,任立良,雍斌,等利用树木年轮重建马鞍山地区7-9月降水量序列[J].河海大学学报(自然科学版),2010,38(1)：31-35.
蒋全荣,郑定英,余志豪.副热带高压季节性移动与海温场的联系[J].大气科学,1997,21(2)：199-204.
金祖辉,陶诗言.ENSO循环与中国东部地区夏季和冬季降水关系的研究[J].大气科学,1999,23(6)：664-672.
康尔泗,程国栋,等中国西北干旱区冰雪水资源与出山径流[M].北京：科学出版社,2002.
康玲玲,王云璋,马燕,等黄河花园口站近523年天然径流量序列重建[J].水资源与水工程学报,2008,19(6)：10-13.
康兴成,Graumlich LJ, Sheppard P.青海都兰地区1835年来的气候变化—来自树轮资料[J].第四纪研究,1997a,17(1)：70-75.
康兴成,Graumlich LJ, Sheppard P青海都兰地区1835a年轮序列的建立和初步分析[J].科学通报,1997b,42(10)：1089-1091.
康兴成,程国栋,陈发虎,等祁连山中部公元904年以来树木年轮记录的旱涝变化[J].冰川冻土,2003,25(5)：518-525.
康兴成,程国栋,康尔泗,等利用树轮资料重建黑河近千年来出山口径流量[J].中国科学D辑,2002,32(8)：675-685.
康兴成,张其花,Graumlich LJ,等青海都兰过去2000年来的气候重建及其变迁[J].地球科学进展,2000,15(2)：215-221.
蓝永超,丁永建,沈永平等河西内陆河流域出山径流对气候转型的响应[J].冰川冻土,2003,25(2)：188-192.
蓝永超,康尔泗,仵彦卿等气候变化对河西内陆干旱区出山径流的影响[J].冰川冻上,2001a,23(3)：276-282.
蓝永超,康尔泗,张济世,等近50年来ENSO与祁连山区气温降水和出山径流的对应关系[J].水科学进展,2002,13(2)：141-145.
蓝永超,仵彦卿,康尔泗,等祁连山北麓出山径流对气候变化的响应[J].兰州大学学报(自然科学版),2001b,37(4)：125-132.
李峰,何金海.北太平洋海温异常与东亚夏季风相互作用的年代际变化[J].热带气象学报,2002,16(3)：261-271.
李江风,袁玉江,马慧明,等.伊犁地区历史径流深度场的重建[J].自然资源学报,1994,9(1)：67-76.
李江风,袁玉江,由希尧,等树木年轮水文学研究与应用[M].北京：科学出版社,2000.
李江风,袁玉江,由希尧.乌鲁木齐河山区流域360年径流量的重建[J].第四纪研究,1997,17(2)：131-138.
李江风,袁玉江,马慧明,等.用树木年轮重建伊犁地区的年径流量场[J].水文,1996(1)：30-35.
李金豹.利用树木年轮重建新疆地区近300年来的气候变化[D].兰州：兰州大学,2003.
李强,刘禹,蔡秋芳,等.山西宁武地区1686年以来年降水重建[J].第四纪研究,200626(6)：999-1006.
李洋.石羊河流域水循环要素变化特征研究[D].杨凌：西北农林科技大学,2008.
李颖.完全耦合的海气环流模式中ENSO和亚洲季风的相互作用[D]北京：中国科学院研究生院,2006.
李宗善,刘国华,傅伯杰,等川西卧龙国家级自然保护区树木生长对气候响应的时间稳定性评估[J].植物生态学报,2010,34(9)：1045-1057.
李宗善,刘国华,张齐兵.利用树木年轮宽度资料重建川西卧龙地区过去159年夏季温度的变化[J].植物生态学报,2010,34(6)：628-641.
梁尔源.中国北方干旱、半干旱区树轮网络的建立及其气候事件研究[D].北京：中科院地理科学与资源研究所,2004.
梁尔源,邵雪梅,刘鸿雁,等树轮所记录的公元1842年以来内蒙古东部浑善达克沙地PDSI的变化[J].科学通报,2007,52(14)：1694-1699.
刘洪滨,刘洪滨,邵雪梅.采用秦岭冷杉年轮宽度重建陕西镇安1755年以来的初春温度[J].气象学报,2000,58(02)：223-233.
刘洪滨,邵雪梅,黄磊.中国陕西关中及周边地区近500年来初夏干燥指数序列的重建[J].第四纪研究,2002,22(3)：220-229.
刘洪滨,邵雪梅.秦岭南坡佛坪1789年以来1-4月平均温度重建[J].应用气象学报,2003,14(2)：188-196.
刘洪滨,吴祥定,邵雪梅.采用树轮图像分析方法研究历史时期气候变化的可行性[J].地理研究,1996,15(2)：44-51.
刘录三,邵雪梅,梁尔源,等祁连山中部祁连圆柏生长与更新方式的树轮记录[J].地理研究,2006,25(1)：53-61.
刘普幸.额济纳旗胡杨径向生长的水文气候因子研究[D].兰州：兰州大学,2007a.
刘普幸,陈发虎,靳立亚,等基于胡杨年轮重建黑河下游近100年春季径流量[J].干旱区地理,2007b,30(5)：696-700.
刘晓宏,秦大河,邵雪梅,等祁连山中部过去近千年温度变化的树轮记录[J].中国科学D辑,2004,34(1)：89-95.
刘晓宏,秦大河,邵雪梅,等.西藏林芝地区近350a来降水变化及突变分析[J].冰川冻土,2003,25(4)：375-379.
刘义花,汪青春,马占良,等.利用多条树轮重建黑河上游地区540年径流量[J].干旱区资源与环境,2009,23(3)：93-97.
刘屹岷,吴国雄.副热带高压研究回顾及对几个基本问题的再认识[J].气象学报,2000,58(4)：500-512.
刘永强,丁一汇.ENSO事件对我国季节降水和温度的影响[J].大气科学,1995,19(2)：200-208.
刘禹,Shishov V,史江峰,等内蒙古西部贺兰山和东部白音敖包未来20年降水趋势预测[J].科学通报,2004a,49(3)：270-274.
刘禹,Won-Kyu P,蔡秋芳,等公元1840年以来东亚夏季风降水变化——以中国和韩国的树轮记录为例[J].中国科学D辑,2003a,33(6)：543-549.
刘禹,安芷生,Linderholm HW,等青藏高原中东部过去2485年以来温度变化的树轮记录[J].中国科学D辑：地球科学,2009c,39(2)：166-176.
刘禹,安芷生,马海州,等.青海都兰地区公元850年以来树轮记录的降水变化及其与北半球气温的联系[J].中国科学(D辑：地球科学),2006a,36(5)：461-471.
刘禹,蔡秋芳,Park WK,等内蒙古锡林浩特白音敖包1838年以来树轮降水记录[J].科学通报,2003b,48(9)：952-957.
刘禹,蔡秋芳,马利民等.树轮降水记录及东亚夏季风强弱变化——以内蒙古包头地区为例[J].地学前缘,2001,8(1)：91-97.
刘禹,刘娜,宋慧明,等以树轮宽度重建秦岭中段分水岭地区1-7月平均气温[J].气候变化研究进展,2009a,5(5)：260-265.
刘禹,马利民.树轮宽度对近376年呼和浩特季节降水的重建[J].科学通报,1999,44(18)：1986-1992.
刘禹,马利民,蔡秋芳,等依据陕西秦岭镇安树木年轮重建3—4月份气温序列[J].自然科学进展,2001,11(2)：157-162.
刘禹,马利民,蔡秋芳,等采用树轮稳定碳同位素重建贺兰山1890年以来夏季(6-8月)气温[J].中国科学(D辑),2002,32(8)：667-674.
刘禹,史江峰,Shishov V,等以树轮晚材宽度重建公元1726年以来贺兰山北部5～7月降水量[J].科学通报,2004b,49(3)：265-269.
刘禹,田沁花,宋慧明,等以树轮宽度重建公元1558年以来华山5-6月平均温度及20世纪中后期升温[J].第四纪研究,2009b,29(5)：888-895.
刘禹,田华,宋慧明,等油松年轮记录的河北围场公元1884年以来5-6月平均温度[J].第四纪研究,2009d,29(5)：896-904.
刘禹,王雷,史江峰,等利用贺兰山北部树轮资料重建过去270年以来6-8月平均干燥指数[J].第四纪研究,2005,25(5)：540-544.
刘禹,杨银科,蔡秋芳,等以树木年轮宽度资料重建湟水河过去248年来6-7月份河流径流量[J].干旱区资源与环境,2006b,20(6)：69-73.
刘禹,吴祥定,邵雪梅,等.树轮密度、稳定C同位素对过去近100a陕西黄陵季节气温与降水的恢复[J].中国科学：D辑,1997,27(3)：271-276.
鲁瑞洁,夏虹.腾格里沙漠南缘油松树轮宽度变化及其对气候因子的响应[J].中国沙漠,2006,26(3)：399-402.
罗连升,杨修群.从有效位能来分析El Ninno的年代际变化[J].气象科学,2003,23(1)：1-11.
吕军,江志红,张静,等天目山树轮碳同位素与周边地区旱涝变化关系的研究[J].南京气象学院学报,2008,31(03)：389-394.
吕军,屠其璞,钱君龙,等天目山柳杉树轮813C对华东地区降水序列的重建[J].南京气象学院学报,2001,24(3)：350-355.
马宏伟,王乃昂.近50年石羊河出山口径流对气候变化的响应[J].干旱区资源与环境,2010,24(1)：113-117.
马龙,刘延玺,翼鸿兰,等科尔沁沙地1826年以来榆树树轮宽度年表的建立及降水重建[J].第四纪研究,2011,31(2)：360-369.
马柱国,邵丽娟.中国北方近百年干湿变化与太平洋年代际振荡的关系[J].大气科学,2006,30(3)：464-474.
马柱国.华北干旱化趋势及转折性变化与太平洋年代际振荡的关系[J].科学通报,2007,52(10)：1199-1206.
慕巧珍,王绍武,朱锦红,等近百年夏季西太平洋副热带高压的变化[J].大气科学,2001,25(6)：787-797.
潘娅婷,袁玉江,喻树龙,等采用树轮图像分析法重建过去气候变化[J].干旱区研究,2007,24(2)：255-260.
钱君龙,邓自旺,屠其璞,等天目山柳杉树轮δD年序列及其气候含义[J].中国科学：D辑,2001,31(5)：372-376.
秦宁生,靳立亚.时兴台,等利用树轮资料重建通天河流域518年径流量[J].地理学报,2004,59(4)：550-556.
邵雪梅,黄磊,刘洪滨,等.树轮记录的青海德令哈地区千年降水变化[J].中国科学D辑,2004,34(2)：145-153.
邵雪梅,梁尔源,黄磊,等柴达木盆地东北部过去1437a的降水变化重建[J].气候变化研究进展,2006,2(3)：122-126.
邵雪梅,王树芝,徐岩,等柴达木盆地东北部3500年树轮定年年表的初步建立[J].第四纪研究,2007,27(4)：477-485.
沈吉,陈毅风.南京地区近二十年来雪松树轮的稳定碳同位素与气候重建[J].植物资源与环境学报,2000,9(3)：34-37.
沈长泗,陈金敏,张志华.采用树木年轮资料重建山东沂山地区200多年来的湿润指数[J].地理研究,1998,17(2)：150-156.
沈永平,刘时银,甄丽丽,等祁连山北坡流域冰川物质平衡波动及其对河西水资源的影响[J].冰川冻土,2001,23(3)：244-250.
施雅风,沈永平,胡汝骥.西北气候由暖干向暖湿转型的信号、影响和前景初步探讨[J].冰川冻土,2002,24(3)：219-226.
施雅风,沈永平,李栋梁,等中国西北气候由暖干向暖湿转型的特征和趋势探讨[J].第四纪研究,2003,23(2)：152-164.
时兴合,秦宁生,邵雪梅,等青海湖流域圆柏年轮指示的近千年降水变化[J].湖泊科学,2009,21(4)：579-586.
史江峰,刘禹,蔡秋芳,等油松(Pinus tabulaeformis)树轮宽度与气候因子统计相关的生理机制—以贺兰山地区为例[J].生态学报,2006,26(3)：697-705.
史江峰,刘禹,蔡秋芳,等贺兰山过去196年降水的树轮宽度重建及降水变率[J].海洋地质与第四纪地质,2007,27(1)：95-100.
宋慧明,刘禹,倪万眉,等以树轮宽度重建九寨沟1750年以来冬半年平均最低温度[J].第四纪研究,2007,27(4)：486-491.
孙军艳,刘禹,蔡秋芳,等额济纳233年来胡杨树轮年表的建立及其所记录的气象、水文变化[J].第四纪研究,2006,26(5)：799-807.
孙艳荣,崔海亭,穆治国,等广东现代樟树树轮纤维素的碳同位素与厄尔尼诺事件的关系[J].地球学报,2003,24(6)：505-510.
谭明,邵雪梅,刘晓宏,等.中国近千年石笋-树轮集成温度记录[J].气候变化研究进展,2006,2(3)：113-116.
汤绪,孙国武,钱维宏.亚洲夏季风北边缘研究[M].北京：气象出版社,2007.
唐劲松.浙江天目山柳杉树轮δ13C年序列与气候变化[D].南京：中国科学院南京地理与湖泊研究所,1999.
田沁花,刘禹,蔡秋芳,等油松树轮记录的过去134年伏牛山5-7月平均最高温度[J].地理学报,2009,64(7)：879-887.
田沁花.祁连山中—西部近500年来气候变化的树轮记录[D].兰州：兰州大学,2006.
汪青春,秦宁生,李栋梁,等.利用多条树轮资料重建青海高原近250年年平均气温序列[J].高原气象,2005,24(3)：320-325.
王兵,高鹏,郭浩,等江西大岗山林区樟树年轮对气候变化的响应[J].应用生态学报,2009,20(1)：71-76.
王国荣,罗哲贤,赵东.西北地区3—9月降水量与ENSO的联系[J].南京气象学院学报,2007,30(6)：849-856
王建,赵兴云,钱君龙.天目山柳杉树轮δ13C方位变化及成因探讨[J].地理研究, 2006,25(2)：242-254.
王树芝.青海都兰地区公元前515年以来树木年轮表的建立及应用[J].考古与文物,2004(6)：45-50.
王文志,刘晓宏,陈拓,等基于祁连山树轮宽度指数的区域NDVI重建[J].植物生态学报,2010,34(9)：1033-1044.
王亚军,陈发虎,勾晓华,等利用树木年轮资料重建祁连山中段春季降水的变化[J].地理科学,2001,21(4)：373-377.
王亚军,陈发虎,勾晓华.黑河230a以来3-6月径流的变化[J].冰川冻土,2004,26(2)：202-206.
王亚军,高尚玉,马玉贞,等基于树轮重建的宁夏河东沙地西部公元1899年来年降水量的变化[J].干旱区地理,2010,33(3)：377-384.
王亚军,勾晓华,刘普幸,等甘肃榆中200年来春季气温的变化[J].中国沙漠,2006,26(2)：283-285.
王亚军,马玉贞,鲁瑞洁,等树木年轮记录的祁连山东段公元1895年来的气温变化[J].第四纪研究,2009,29(5)：905-912.
王玉玺.祁连山园柏年轮与我国近千年气候变化和冰川进退的关系[J].科学通报,1982,27(21)：1316-1319.
王越,江志红,张强,等基于Palmer湿润指数的旱涝参数研究[J].南京气象学院学报,2007,30(3)：383-389.
王振宇,李林,江青春,等树轮纪录的500年来青海地区夏半年降水变化特征[J].气候与环境研究,2005,10(2)：250-256.
魏本勇,方修琦.树轮气候学中树木年轮密度分析方法的研究进展[J].古地理学报,2008,10(2)：193-202.
魏文寿,袁玉江,喻树龙,等中国天山山区235a气候变化及降水趋势预测[J].中国沙漠,2008,28(5)：803-808.
武炳义,卞林根,张人禾.冬季北极涛动和北极海冰变化对东亚气候变化的影响[J].极地研究,2004,16(3)：211-220.
吴普,王丽丽,邵雪梅.采用高山松最大密度重建川西高原近百年夏季气温[J].地理学报,2005,60(6)：998-1006.
吴祥定,孙力,湛绪志.利用树木年轮资料重建西藏中部过去气候的初步尝试[J].地理学报,1989,44(3)：334-342.
吴祥定,邵雪梅.中国秦岭地区树木年轮密度对气候响应的初步分析[J].应用气象学报,1994,5(2)：253-256.
吴祥定.树木年轮与气候变化[M].北京：气象出版社,1990.
肖生春,肖洪浪.极端干旱区湖岸柽柳径向生长对水环境演变的响应[J].北京林业大学学报,2006,28(2)：39-45.
肖生春,肖洪浪,司建华,等.干旱区多枝柽柳的生长特性[J].西北植物学报,2005,25(5)：1012-1016.
肖生春,肖洪浪,周茂先,等近百年来西居延海湖泊水位变化的湖岸林树轮记录[J].冰川冻土,2004,26(5)：557-562.
肖支才,高华明,丁通,等自助法在小样本数据均值估计中的应用[J].海军航空工程学院学报,2009.24(5)：563-572.
谢益辉,朱饪Bootstrap方法的历史发展和前沿研究[J].统计与信息论坛, 2008,23(2)：90-96.
徐国保,刘晓宏,陈拓,等新疆哈密八大石森林上限树轮记录的温度变化信息[J].山地学报,2009,27(4)：402-410.
徐瑞珍,周陆生.由斑玛云杉年表重建青海高原东南部夏季降水序列[J].气象,2000,26(1)：3-8.
许武成,马劲松,王文.关于ENSO事件及其对中国气候影响研究的综述[J].气象科学,2005,25(2)：213-220.
杨涛,勾晓华,李颖俊.青藏高原东北部树轮海拔梯度研究的散点图分析应用[J].冰川冻土,2010,32(2)：429-437.
杨小利,杨兴国,马鹏里,等PDSI在甘肃中东部地区的修正和应用[J].地球科学进展,2005,20(9)：1022-1028.
杨修群,郭燕娟,徐桂玉,等年际和年代际气候变化的全球时空特征比较[J].南京大学学报：自然科学版,2002,38(3)：308-317.
杨银科,黄强,刘禹,等.利用树轮资料重建河流径流量研究进展[J].水科学进展,2010,21(3)：430-434.
杨银科,刘禹,蔡秋芳,等以树木年轮宽度资料重建祁连山中部地区过去248年来的降水量[J].海洋地质与第四纪地质,2005,25(3)：113-118.
杨银科,刘禹,史江峰,等树木年轮密度实验方法及其在内蒙古准格尔旗树轮研究中的应用[J].干旱区地理,2006,29(5)：639-645.
尹红.西北地区过去千年降水序列的初步重建及变化特征分析[D].南京：南京信息工程大学,2006.
游泳,郭品文,廖勇,等ENSO与中国东部地区夏季降水相关性年代际变化特征[J].气象科技,2005,33(2)：142-146.
余丹丹,张韧,洪梅,等亚洲夏季风系统成员与西太平洋副高的相关特征分析[J].热带气象学报,2007,23(1)：78-84.
喻树龙,袁玉江,龚原,等奎屯河近379a 9月径流量的重建与特征分析[J].干旱区资源与环境,2008,22(7)：115-119.
喻树龙,袁玉江,何清,等1468-2001年新疆精河5-8月平均气温的重建[J].冰川冻土,2007,29(3)：374-379.
喻树龙,袁玉江,金海龙,等.用树木年轮重建天山北坡中西部7-8月379a的降水量[J].冰川冻土,2005,27(3)：404-410.
袁玉江,李江风,胡汝骥,等用树木年轮重建天山中部近350年来的降水量[J].冰川冻土,2001,23(1)：34-40.
袁玉江,邵雪梅,李江风,等夏干萨特树轮年表中降水信息的探讨与326年降水重建[J].生态学报,2002,22(12)：2048-2053.
袁玉江,邵雪梅,魏文寿,等乌鲁木齐河山区树木年轮一积温关系及≥5.7℃积温的重建[J].生态学报,2005,25(4)：756-762.
袁玉江,叶玮,董光荣.天山西部伊犁地区314a降水的重建与分析[J].冰川冻土,2000,22(2)：121-127.
袁玉江,喻树龙,穆桂金,等天山北坡玛纳斯河355a来年径流量的重建与分析[J].冰川冻土,2005,27(3)：411-417.
袁玉江,李江风.天山乌鲁木齐河源450a冬季温度序列的重建与分析[J].冰川冻土,1999,21(1)：64-70.
臧增亮.ENSO对东亚夏季风和我国夏季降水的影响研究进展[J].解放军理工大学学报(自然科学版),2005,6(4)：394-398.
张寒松,韩士杰,李玉文,等利用树木年轮宽度资料重建长白山地区240年来降水量的变化[J].生态学杂志,2007,26(12)：1924-1929.
张杰,李栋梁.祁连山及黑河流域降雨量的分布特征分析[J].高原气象,2004,23(1)：81-88.
张庆乐,刘卫国,刘禹,等贺兰山地区树轮碳氧同位素与夏季风降水的相关性讨论[J].地球化学,2005,34(1)：51-56.
张瑞波,魏文寿,袁玉江,等.1396-2005年天山南坡阿克苏河流域降水序列重建与分析[J].冰川冻土,2009,31(1)：27-33.
张瑞波,袁玉江,魏文寿,等用树轮灰度重建乌孙山北坡4—5月平均最低气温[J].中国沙漠,2008(5)：848-854.
张瑞波,袁玉江,魏文寿,等西藏东部过去400年秋、冬季平均最低气温的树木年轮分析[J].高原气象,2010,29(2)：359-365.
张同文,王丽丽,袁玉江,等利用树轮宽度资料重建天山中段南坡巴仑台地区过去645年来的降水变化[J].地理科学,2011,31(2)：251-256.
张同文,袁玉江,魏文寿,等阿勒泰柯姆地区树轮宽度年表与灰度年表的建立[J].沙漠与绿洲气象,2007,1(3)：9-14.
张同文,袁玉江,魏文寿,等使用树轮资料重建阿勒泰西部年积雪深度≥0cm日数的长期变化[J].沙漠与绿洲气象,2010,4(3)：6-11.
张小明,魏锋,陆燕.祁连山近45a年降水异常的气候特征[J].干旱气象,2006,24(3)：35-41.
张永香.季风边缘区近200年来的树轮记录研究[D].兰州：兰州大学,2005a.
张永香,勾晓华,胡文东,等树轮记录的贺兰山区近百年来的干旱事件[J].生态学报,2005b,25(8)：2121-2126.
张志华,李骥,Graumlich LJ,等用树轮密度及宽度资料重建新疆吉木萨尔县的季节降水和最高温度[J].气象学报,1998,56(1)：77-86.
张志华,吴祥定.利用树木年轮资料恢复祁连山地区近700年来气候变化[J].科学通报,1997,42(8)：849-851.
张志华,吴祥定,李骥.利用树木年轮资料重建新疆东天山300多年来干旱日数的变化[J].应用气象学报,1996,7(1)：53-60.
张志华,吴祥定.祁连山地区1310年以来湿润指数及其年际变幅的变化与突变分析[J].第四纪研究,1996,15(4)：368-378.
赵兴云.中国东部亚热带地区树轮δ13C年序列及方位变化的环境意义[D].南京：南京师范大学,2006.
赵兴云,王建,钱君龙,等天目山地区树轮δ13C记录的300多年的秋季气候变化[J].山地学报,2005,23(5)：540-549.
赵兴云,王建,商志远,等天目山柳杉树轮813C序列所反映的植物水分利用率对大气CO2浓度变化的生理响应[J].地理科学,2008,28(5)：698-702.
周文盛.根据阿尔泰山南坡树木年轮初步分析额尔齐斯河500年(1582-2081)径流量[J].干旱区地理,1984,7(1)：35-49.
朱海峰.利用树轮宽度网络重建我国东北地区东部温度变化[D].北京：北京师范大学,2006.
朱守森,王强.祁连山区北坡降水的时空分布及近期变化[J].冰川冻土,1996.18(增刊)：296-304.
朱西德,秦宁生,李栋梁,等利用树木年轮重建柴达木地区5-6月地温[J].高原气象,2005,24(3)：331-337.
朱西德,王振宇,李林,等树木年轮指示的柴达木东北缘近千年夏季气温变化[J].地理科学,2007,27(2)：256-260.
朱益民,杨修群.太平洋年代际振荡与中国气候变率的联系[J].气象学报,2003,61(6)：641-654.
卓正大,胡双熙,张先恭,等祁连山地区树木年轮与我国近千年(1059-1975年)的气候变化[J].兰州大学学报,1978,14(2)：145-157.