阿拉善荒漠及周边山区树木年轮学研究进展
|
摘要
阿拉善荒漠地处西风带、高原季风和东亚夏季风尾闾和交汇影响区,不仅是我国气候变化的敏感区,还是我国主要的沙尘源区和运移通道。通过总结分析阿拉善荒漠及周边地区的树木年轮学研究成果,综述了阿拉善荒漠绿洲区河/湖岸林、荒漠灌木、周边山地针叶林等乔灌木树种日-季-年尺度径向生长的主要气候限制因子、年轮记录的过去百余年来气候变化特征及其驱动机制。今后该区域树木年轮研究应更加注重未来气候发展趋势预测,并拓展更多研究树种及树轮指标,将荒漠区乔灌木年轮研究、荒漠周边山地树木年轮研究和荒漠演变过程三者有机地结合起来,为更加全面、深入了解阿拉善荒漠化驱动机制和治理决策制定提供科学依据。
The Alxa desert is located in the tail and interaction area of the westerly,plateau monsoon and East Asian summer monsoon. It is not only a sensitive area of climate change in China,but also the main sandstorm source region and migration channel in China. By summarizing and analyzing the research results of dendrochronology in the Alxa desert and its surrounding areas,this paper reviewed the main climatic limiting factors for radial growth on the day-season-year scale of desert riparian forests,lakeshore forests,desert shrubs and surrounding mountainous coniferous forests and characteristics of climate change recorded by the tree rings over the hundreds of years and its driving mechanisms. In the future,the study of dendrochronology in the region should pay more attention to predict the future climate development trends and expand more tree species and tree-ring indicators. The study of the tree and shrub rings in the desert area,the study of tree rings around the desert and the process of desert evolution should be organically combined,which may provide scientific basis for more comprehensive and in-depth understanding of the driving mechanism of desertification and decision-making in Alxa Desert.
The Alxa desert is located in the tail and interaction area of the westerly,plateau monsoon and East Asian summer monsoon. It is not only a sensitive area of climate change in China,but also the main sandstorm source region and migration channel in China. By summarizing and analyzing the research results of dendrochronology in the Alxa desert and its surrounding areas,this paper reviewed the main climatic limiting factors for radial growth on the day-season-year scale of desert riparian forests,lakeshore forests,desert shrubs and surrounding mountainous coniferous forests and characteristics of climate change recorded by the tree rings over the hundreds of years and its driving mechanisms. In the future,the study of dendrochronology in the region should pay more attention to predict the future climate development trends and expand more tree species and tree-ring indicators. The study of the tree and shrub rings in the desert area,the study of tree rings around the desert and the process of desert evolution should be organically combined,which may provide scientific basis for more comprehensive and in-depth understanding of the driving mechanism of desertification and decision-making in Alxa Desert.
引文
Briffa K R,Schweingruber F H,Jones P D,et al,1998.Reduced sensitivity of recent tree-growth to temperature at high northern latitudes[J].Nature,391(6668):678-682.
Cai Q F,Liu Y,2007.January to August temperature variability since1776 inferred from tree-ring width of Pinus tabulaeformis in Helan Mountain[J].Journal of Geographical Sciences,17(3):293-303.DOI:10.1007/s11442-007-0293-5.
Chen F,Yuan Y J,Wei W S,et al,2012.Tree-ring-based reconstruction of precipitation in the Changling Mountains,China,since A.D.1691[J].Int J Biometeorol,56(4):765-74.DOI:10.1007/s00484-011-0431-8.
Cook E R,Meko D M,Stahle D W,et al,1999.Drought reconstructions for the continental United States[J].Journal of Climate,12(4):1145-1162.
Gou X H,Gao L L,Deng Y,et al,2015.An 850-year tree-ring-based reconstruction of drought history in the western Qilian Mountains of northwestern China[J].International Journal of Climatology,35(11):3308-3319.
Liang E Y,Liu W W,Ren P,et al,2015.The alpine dwarf shrub Cassiope fastigiata in the Himalayas:does it reflect site-specific climatic signals in its annual growth rings?[J].Trees,29(1):79-86.
Liu X H,Zhang X W,Zhao L J,et al,2017.Tree ringδ18O reveals no long-term change of atmospheric water demand since 1800 in the northern Great Hinggan Mountains,China[J].Journal of Geophysical Research Atmospheres,122(13):6697-6712.
Liu Y,Cai Q F,Liu W G,et al,2008.Monsoon precipitation variation recorded by tree-ringδ18O in arid Northwest China since AD 1878[J].Chemical Geology,252(1-2):56-61.DOI:10.1016/j.chemg eo.2008.01.024.
Liu Y,Cai Q F,Shi J F,et al,2005.Seasonal precipitation in the south-central Helan Mountain region,China,reconstructed from tree-ring width for the past 224 years[J].Canadian Journal of Forest Research,35(10):2403-2412.
Liu Y,Lei Y,Sun B,et al,2013.Annual precipitation variability inferred from tree-ring width chronologies in the Changling-Shoulu region,China,during AD 1853-2007[J].Dendrochronologia,31(4):290-296.DOI:10.1016/j.dendro.2013.02.001.
Liu Y,Ma L M,Cai Q F,et al,2002.Reconstruction of summer temperature(June-August)at Mt.Helan,China,from tree-ring stable carbon isotope values since AD 1890[J].Sciencein China(Earth Sciences),45(12):1127-1136.DOI:10.1360/02yd9109.
Liu Y,Shi J F,Shishov V,et al,2004.Reconstruction of May-July precipitation in the north Helan Mountain,Inner Mongolia since A.D.1726 from tree-ring late-wood widths[J].Chinese Science Bulletin,49(4):405-409,doi:10.1007/bf02900325.
Liu Y,Sun C F,Li Q,et al,2016.A Picea crassifolia Tree-Ring WidthBased Temperature Reconstruction for the Mt.Dongda Region,Northwest China,and Its Relationship to Large-Scale Climate Forcing[J].Plos One,11(8).DOI:10.1371/journal.pone.0160963.
Peng X M,Xiao S C,Cheng G D,et al,2015.Human activity impacts on the stem radial growth of Populus euphratica riparian forests in China’s Ejina Oasis,using tree-ring analysis[J].Trees,31(2):379-392.DOI:10.1007/s00468-015-1287-z.
Peng X M,Xiao S C,Xiao H L,2013.Preliminary dendrochronological studies on Populus euphratica in the lower reaches of the Heihe River basin in northwest China[J].Dendrochronologia,31(3):242-249.
Peng X M,Xiao S C,Cheng G D,et al,2017.Microcoring and dendrometer-detected intra-annual wood formation of Populus euphratica in the Ejina Oasis,northwestern China[J].Sciences In Cold And Arid Regions,9(1):54-66.DOI:10.3724/SP.J.1226.2017.00054.
Rydval M,Loader N J,Gunnarson B E,et al,2017.Reconstructing 800years of summer temperatures in Scotland from tree rings[J].Climate Dynamics,49(9-10):2951-2974.DOI:10.1007/s00382-016-3478-8.
Si J H,Feng Q,Cao S K,et al,2014.Water use sources of desert riparian Populus euphratica forests[J].Environmental Monitoring&Assessment,186(9):5469-77.DOI:10.1007/s10661-014-3796-4.
Wang J L,Yang B,Qin C,et al,2014.Tree-ring inferred annual mean temperature variations on the southeastern Tibetan Plateau during the last millennium and their relationships with the Atlantic Multidecadal Oscillation[J].Climate Dynamics,43(3-4):627-640.DOI:10.1007/s00382-013-1802-0.
Xiao S C,Xiao H L,Si J H,et al,2005.Lake level changes recorded by tree rings of lakeshore shrubs:a case study at the Lake West-Juyan,Inner Mongolia,China[J].Journal of Integrative Plant Biology,47(11):1303-1314.
Xiao S C,Xiao H L,Peng X M,et al,2014a.Daily and seasonal stem radial activity of Populus euphratica and its association with hydroclimatic factors in the lower reaches of China’s Heihe River basin[J].Environmental Earth Sciences,72(2):609-621.DOI:10.1007/s12665-013-2982-y.
Xiao S C,Peng X M,Tian Q Y,2015a.Climatic and human drivers of recent lake-level change in East Juyan Lake,China[J].Regional Environmental Change,16(4):1063-1073.DOI:10.1007/s10113-01 5-0822-1.
Xiao S C,Xiao H L,2007a.Radial growth of Tamarix ramosissima responds to changes in the water regime in an extremely arid region of northwestern China[J].Environmental Geology,53(3):543-551.DOI:10.1007/s00254-007-0666-1.
Xiao S C,Xiao H L,Kobayashi O,et al,2007b.Dendroclimatological Investigations of Sea Buckthorn(Hippophae rhamnoides)and Reconstruction of the Equilibrium Line Altitude of the July First Glacier in the Western Qilian Mountains,Northwestern China[J].TreeRing Research,63(1):15-26.
Xiao S C,Xiao H L,Peng X M,et al,2014b.Intra-annual stem diameter growth of Tamarix ramosissima and association with hydroclimatic factors in the lower reaches of China’s Heihe River[J].Journal of Arid Land,6(4):498-510.DOI:10.1007/s40333-013-0248-x.
Xiao S C,Xiao H L,Peng X M,et al,2015b.Dendroecological assessment of Korshinsk peashrub(Caragana korshinskii Kom.)from the perspective of interactions among growth,climate,and topography in the western Loess Plateau,China[J].Dendrochronologia,33:61-68.DOI:10.1016/j.d endro.2015.01.001.
Xiao S C,Xiao H L,Dong Z B,et al,2012.Dry/wet variation recorded by shrub tree-rings in the central Badain Jaran Desert of northwestern China[J].Journal of Arid Environments,87:85-94.DOI:10.1016/j.jaridenv.2012.06.013.
Zhang Q B,Li Z S,Liu P X,et al,2012.On the vulnerability of oasis forest to changing environmental conditions:perspectives from tree rings[J].Landscape Ecology,27(3):343-353.DOI:10.1007/s1098 0-011-9685-0.
Zhang Q B,Evans M N,Lyu L,2015.Moisture dipole over the Tibetan Plateau during the past five and a half centuries[J].Nat Commun,6:8062.DOI:10.1038/ncomms9062.
蔡秋芳,2009.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,29(6):131-136.DOI:10.3724/SP.J.1140.2 009.06131.
陈峰,魏文寿,袁玉江,等,2013.基于多点树轮序列的1768-2006年甘肃降水量变化[J].中国沙漠,33(5):1520-1526.DOI:10.7522/j.issn.1000-694X.2013.00218.
陈峰,袁玉江,魏文寿,等,2010a.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,26(5):82-86.
陈峰,袁玉江,魏文寿,等,2010b.树轮记录的贺兰山北部5-7月PDSI变化[J].气候变化研究进展,6(5):344-348.
陈峰,袁玉江,魏文寿,等,2011.树轮记录的贺兰山北部近208年5-7月温度变化[J].应用气象学报,22(4):463-471.
陈婕,黄伟,靳立亚,等,2018.东亚夏季风的气候北界指标及其年际变化研究[J].中国科学(地球科学),48(1):93-101.DOI:10.1360/N072017-00150.
丁爱军,肖生春,彭小梅,等,2018.霸王(Sarcozygium xanthoxylon)灌木年轮记录的1902-2015年阿拉善荒漠中部气候干湿变化[J].中国沙漠,38(2):1-9.DOI:10.7522/j.issn.1000-694X.2017.0010 0.
杜方红,李伟,云敏瑞,等,2006.额济纳绿洲生态环境的百年演变[J].环境保护,(10):73-77.DOI:10.14026/j.cnki.0253-9705.2006.10.020.
范子昂,魏文寿,陈峰,等,2012.树轮记录的腾格里沙漠东缘1775-2005年降水变化[J].中国沙漠,32(4):996-1002.
高尚玉,鲁瑞洁,强明瑞,等,2006.140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,51(3):326-331.
黄荣凤,张国盛,王林和,等,2004.影响毛乌素沙地臭柏年轮宽度变化的主要气候因子分析[J].干旱区资源与环境,18(6):164-169.DOI:10.13448/j.cnki.jal re.2004.06.032.
黄荣辉,徐予红,周连童,1999.我国夏季降水的年代际变化及华北干旱化趋势[J].高原气象,18(4):465-476.
黄玉霞,王宝鉴,王研峰,等,2017.甘肃省夏季暴雨日数特征及其与大气环流关系[J].高原气象,36(1):183-194.DOI:10.7522/j.issn.1000-0534.2015.00118.
雷光炳,2009.寿鹿山自然保护区青海云杉梢斑螟的观测与防治[J].甘肃林业(3):37-38.
李栋梁,邵鹏程,王慧,等,2013.中国东亚副热带夏季风北边缘带研究进展[J].高原气象,32(1):305-314.DOI:1000-0534(2013)01-0305-10.
李栋梁,张茜,姚慧茹,等,2016.北印度夏季风与中国河套及邻近地区盛夏降水的联系[J].高原气象,35(6):1512-1523.DOI:10.7522/j.issn.1000-0534.2016.00075.
李钢,闫海枫,王科,等,2018.东大山植物资源多样性分析[J].林业科技通讯(7):23-26.
李钢铁,史晴,任改莲,等,1995.确定梭梭年龄的初步探讨[J].内蒙古林学院学报,17(2):52-55.
李森,李凡,孙武,等,2004.黑河下游额济纳绿洲现代荒漠化过程及其驱动机制[J].地理科学,24(1):61-67.DOI:10.13249/j.cnki.sgs.200 4.01.011.
李媛媛,秦宁生,时兴合,等,2015.近714年扎曲河流域径流量的重建和变化特征[J].高原气象,34(4):1065-1073.DOI:10.7522/j.issn.1000-0534.2014.00018.
刘普幸,陈发虎,勾晓华,等,2005.额济纳旗近100 a来胡杨年表的建立与响应分析[J].中国沙漠,25(5):764-768.
刘禹,Shishov V,史江峰,等,2004.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,49(3):270-274.
刘禹,解利,李强,等,2012.公元1820年以来甘肃东大山地区树轮宽度对3-9月平均最低温度的响应分析[J].地球环境学报,3(3):900-907.DOI:10.7515/JEE201203008.
刘禹,王雷,史江峰,等,2005.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,25(5):540-544.
马利民,刘禹,蔡秋芳,等,2003a.贺兰山树轮晚材宽度记录中的降水量变化[J].海洋地质与第四纪地质,23(4):109-114.DOI:10.16562/j.cnki.0256-1492.2003.04.016.
马利民,刘禹,赵建夫,2003b.贺兰山油松年轮中稳定碳同位素含量和环境的关系[J].环境科学,24(5):49-53.DOI:10.13227/j.hjkx.2003.05.009.
彭小梅,2013.黑河下游胡杨树木年轮学研究[D].北京:中国科学院大学,1-72.
彭小梅,肖生春,程国栋,等,2016.胡杨(Populus euphratica)树轮记录的20世纪40年代前后黑河下游分水过程及其生态影响[J].中国沙漠,36(1):206-215.DOI:10.7522/j.issn.1000-694X.2016.00006.
史江峰,刘禹,蔡秋芳,等,2007.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,27(1):95-100.DOI:10.16562/j.cnki.0256-1492.2007.01.012.
孙军艳,刘禹,蔡秋芳,等,2006.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,26(5):799-807.
谭敬,杨文斌,齐凯,等,2006.阿拉善盟四大沙漠“决口”与“握手”状况调查及治理对策[J].内蒙古林业科技,32(3):4-7.
汤绪,钱维宏,梁萍,2006.东亚夏季风边缘带的气候特征[J].高原气象,25(3):375-381.
田全彦,肖生春,彭小梅,等,2015.胡杨(Populus euphratica)与柽柳(Tamarix ramosissima)径向生长特征对比[J].中国沙漠,35(6):1512-1519.DOI:10.7522/j.issn.1000-6 94X.2015.00007.
万炜,颜长珍,肖生春,等,2018.1975-2015年阿拉善高原沙漠化过程、格局与驱动机制[J].中国沙漠,38(1):17-29.DOI:10.7522/j.issn.1000-694X.2017.00086.
王宝鉴,黄玉霞,何金海,等,2004.东亚夏季风期间水汽输送与西北干旱的关系[J].高原气象,23(6):912-918.
王可丽,江灏,赵红岩,2005.西风带与季风对中国西北地区的水汽输送[J].水科学进展,16(3):432-438.DOI:10.14042/j.cnki.32.1309.2005.03.021.
王炜,梁存柱,朱宗元,等,2001.梭梭年轮测定方法及生长动态的研究[J].干旱区资源与环境,15(2):67-75.DOI:10.13448/j.cnki.jal re.2001.02.013.
吴祥定,1990.树木年轮与气候变化[M].北京:气象出版社.
肖生春,陈小红,丁爱军,2017.近现代阿拉善荒漠气候变化与环境演变机制研究进展[J].中国沙漠,37(6):1102-1110.DOI:10.7522/j.issn.1000-694X.2017.000 02.
肖生春,肖洪浪,2006a.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,28(2):000039-45.DOI:10.13332/j.1000-1522.2006.02.007.
肖生春,肖洪浪,彭小梅,2012.黑河下游胡杨季节尺度径向生长变化研究[J].冰川冻土,34(3):706-712.
肖生春,肖洪浪,彭小梅,2013.梭梭(Haloxylon ammodendron)不宜用于树木年轮学研究[J].中国沙漠,33(6):1692-1698.DOI:10.7522/j.issn.1000-694X.2013.00243.
肖生春,肖洪浪,司建华,等,2005.干旱区多枝柽柳的生长特性[J].西北植物学报,25(5):1012-1016.
肖生春,肖洪浪,司建华,等,2010.胡杨(Populus euphratica)径向生长日变化特征分析[J].冰川冻土,32(4):816-822.
肖生春,肖洪浪,宋耀选,等,2006b.荒漠植被红砂(Reaumurta soongorica)水热响应的年轮学研究[J].中国沙漠,26(4):548-552.
肖生春,肖洪浪,周茂先,等,2004.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,26(5):557-562.
杨理,杨持,杨春明,等,1996.四合木(Tetraena mongolica)营养生长和降水、气温的关系[J].内蒙古大学学报:自然科学版,27(6):816-85.
张凯,司建华,王润元,等,2008.气候变化对阿拉善荒漠植被的影响研究[J].中国沙漠,28(5):879-885.
张庆乐,刘卫国,刘禹,等,2005.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,34(1):51-56.
张永香,於琍,尹红,2015.巴丹吉林沙漠南缘191 a来年降水量重建及初步分析[J].沙漠与绿洲气象,9(1):12-16.DOI:10.3969/j.issn.1002-0799.2015.01.003.
赵守栋,何新,张冰琦,等,2013.贺兰山东坡高山林线青海云杉(Picea crassifolia)径向生长对气候因子的响应[J].北京师范大学学报(自然科学版),49(5):501-505.
Cai Q F,Liu Y,2007.January to August temperature variability since1776 inferred from tree-ring width of Pinus tabulaeformis in Helan Mountain[J].Journal of Geographical Sciences,17(3):293-303.DOI:10.1007/s11442-007-0293-5.
Chen F,Yuan Y J,Wei W S,et al,2012.Tree-ring-based reconstruction of precipitation in the Changling Mountains,China,since A.D.1691[J].Int J Biometeorol,56(4):765-74.DOI:10.1007/s00484-011-0431-8.
Cook E R,Meko D M,Stahle D W,et al,1999.Drought reconstructions for the continental United States[J].Journal of Climate,12(4):1145-1162.
Gou X H,Gao L L,Deng Y,et al,2015.An 850-year tree-ring-based reconstruction of drought history in the western Qilian Mountains of northwestern China[J].International Journal of Climatology,35(11):3308-3319.
Liang E Y,Liu W W,Ren P,et al,2015.The alpine dwarf shrub Cassiope fastigiata in the Himalayas:does it reflect site-specific climatic signals in its annual growth rings?[J].Trees,29(1):79-86.
Liu X H,Zhang X W,Zhao L J,et al,2017.Tree ringδ18O reveals no long-term change of atmospheric water demand since 1800 in the northern Great Hinggan Mountains,China[J].Journal of Geophysical Research Atmospheres,122(13):6697-6712.
Liu Y,Cai Q F,Liu W G,et al,2008.Monsoon precipitation variation recorded by tree-ringδ18O in arid Northwest China since AD 1878[J].Chemical Geology,252(1-2):56-61.DOI:10.1016/j.chemg eo.2008.01.024.
Liu Y,Cai Q F,Shi J F,et al,2005.Seasonal precipitation in the south-central Helan Mountain region,China,reconstructed from tree-ring width for the past 224 years[J].Canadian Journal of Forest Research,35(10):2403-2412.
Liu Y,Lei Y,Sun B,et al,2013.Annual precipitation variability inferred from tree-ring width chronologies in the Changling-Shoulu region,China,during AD 1853-2007[J].Dendrochronologia,31(4):290-296.DOI:10.1016/j.dendro.2013.02.001.
Liu Y,Ma L M,Cai Q F,et al,2002.Reconstruction of summer temperature(June-August)at Mt.Helan,China,from tree-ring stable carbon isotope values since AD 1890[J].Sciencein China(Earth Sciences),45(12):1127-1136.DOI:10.1360/02yd9109.
Liu Y,Shi J F,Shishov V,et al,2004.Reconstruction of May-July precipitation in the north Helan Mountain,Inner Mongolia since A.D.1726 from tree-ring late-wood widths[J].Chinese Science Bulletin,49(4):405-409,doi:10.1007/bf02900325.
Liu Y,Sun C F,Li Q,et al,2016.A Picea crassifolia Tree-Ring WidthBased Temperature Reconstruction for the Mt.Dongda Region,Northwest China,and Its Relationship to Large-Scale Climate Forcing[J].Plos One,11(8).DOI:10.1371/journal.pone.0160963.
Peng X M,Xiao S C,Cheng G D,et al,2015.Human activity impacts on the stem radial growth of Populus euphratica riparian forests in China’s Ejina Oasis,using tree-ring analysis[J].Trees,31(2):379-392.DOI:10.1007/s00468-015-1287-z.
Peng X M,Xiao S C,Xiao H L,2013.Preliminary dendrochronological studies on Populus euphratica in the lower reaches of the Heihe River basin in northwest China[J].Dendrochronologia,31(3):242-249.
Peng X M,Xiao S C,Cheng G D,et al,2017.Microcoring and dendrometer-detected intra-annual wood formation of Populus euphratica in the Ejina Oasis,northwestern China[J].Sciences In Cold And Arid Regions,9(1):54-66.DOI:10.3724/SP.J.1226.2017.00054.
Rydval M,Loader N J,Gunnarson B E,et al,2017.Reconstructing 800years of summer temperatures in Scotland from tree rings[J].Climate Dynamics,49(9-10):2951-2974.DOI:10.1007/s00382-016-3478-8.
Si J H,Feng Q,Cao S K,et al,2014.Water use sources of desert riparian Populus euphratica forests[J].Environmental Monitoring&Assessment,186(9):5469-77.DOI:10.1007/s10661-014-3796-4.
Wang J L,Yang B,Qin C,et al,2014.Tree-ring inferred annual mean temperature variations on the southeastern Tibetan Plateau during the last millennium and their relationships with the Atlantic Multidecadal Oscillation[J].Climate Dynamics,43(3-4):627-640.DOI:10.1007/s00382-013-1802-0.
Xiao S C,Xiao H L,Si J H,et al,2005.Lake level changes recorded by tree rings of lakeshore shrubs:a case study at the Lake West-Juyan,Inner Mongolia,China[J].Journal of Integrative Plant Biology,47(11):1303-1314.
Xiao S C,Xiao H L,Peng X M,et al,2014a.Daily and seasonal stem radial activity of Populus euphratica and its association with hydroclimatic factors in the lower reaches of China’s Heihe River basin[J].Environmental Earth Sciences,72(2):609-621.DOI:10.1007/s12665-013-2982-y.
Xiao S C,Peng X M,Tian Q Y,2015a.Climatic and human drivers of recent lake-level change in East Juyan Lake,China[J].Regional Environmental Change,16(4):1063-1073.DOI:10.1007/s10113-01 5-0822-1.
Xiao S C,Xiao H L,2007a.Radial growth of Tamarix ramosissima responds to changes in the water regime in an extremely arid region of northwestern China[J].Environmental Geology,53(3):543-551.DOI:10.1007/s00254-007-0666-1.
Xiao S C,Xiao H L,Kobayashi O,et al,2007b.Dendroclimatological Investigations of Sea Buckthorn(Hippophae rhamnoides)and Reconstruction of the Equilibrium Line Altitude of the July First Glacier in the Western Qilian Mountains,Northwestern China[J].TreeRing Research,63(1):15-26.
Xiao S C,Xiao H L,Peng X M,et al,2014b.Intra-annual stem diameter growth of Tamarix ramosissima and association with hydroclimatic factors in the lower reaches of China’s Heihe River[J].Journal of Arid Land,6(4):498-510.DOI:10.1007/s40333-013-0248-x.
Xiao S C,Xiao H L,Peng X M,et al,2015b.Dendroecological assessment of Korshinsk peashrub(Caragana korshinskii Kom.)from the perspective of interactions among growth,climate,and topography in the western Loess Plateau,China[J].Dendrochronologia,33:61-68.DOI:10.1016/j.d endro.2015.01.001.
Xiao S C,Xiao H L,Dong Z B,et al,2012.Dry/wet variation recorded by shrub tree-rings in the central Badain Jaran Desert of northwestern China[J].Journal of Arid Environments,87:85-94.DOI:10.1016/j.jaridenv.2012.06.013.
Zhang Q B,Li Z S,Liu P X,et al,2012.On the vulnerability of oasis forest to changing environmental conditions:perspectives from tree rings[J].Landscape Ecology,27(3):343-353.DOI:10.1007/s1098 0-011-9685-0.
Zhang Q B,Evans M N,Lyu L,2015.Moisture dipole over the Tibetan Plateau during the past five and a half centuries[J].Nat Commun,6:8062.DOI:10.1038/ncomms9062.
蔡秋芳,2009.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,29(6):131-136.DOI:10.3724/SP.J.1140.2 009.06131.
陈峰,魏文寿,袁玉江,等,2013.基于多点树轮序列的1768-2006年甘肃降水量变化[J].中国沙漠,33(5):1520-1526.DOI:10.7522/j.issn.1000-694X.2013.00218.
陈峰,袁玉江,魏文寿,等,2010a.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,26(5):82-86.
陈峰,袁玉江,魏文寿,等,2010b.树轮记录的贺兰山北部5-7月PDSI变化[J].气候变化研究进展,6(5):344-348.
陈峰,袁玉江,魏文寿,等,2011.树轮记录的贺兰山北部近208年5-7月温度变化[J].应用气象学报,22(4):463-471.
陈婕,黄伟,靳立亚,等,2018.东亚夏季风的气候北界指标及其年际变化研究[J].中国科学(地球科学),48(1):93-101.DOI:10.1360/N072017-00150.
丁爱军,肖生春,彭小梅,等,2018.霸王(Sarcozygium xanthoxylon)灌木年轮记录的1902-2015年阿拉善荒漠中部气候干湿变化[J].中国沙漠,38(2):1-9.DOI:10.7522/j.issn.1000-694X.2017.0010 0.
杜方红,李伟,云敏瑞,等,2006.额济纳绿洲生态环境的百年演变[J].环境保护,(10):73-77.DOI:10.14026/j.cnki.0253-9705.2006.10.020.
范子昂,魏文寿,陈峰,等,2012.树轮记录的腾格里沙漠东缘1775-2005年降水变化[J].中国沙漠,32(4):996-1002.
高尚玉,鲁瑞洁,强明瑞,等,2006.140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,51(3):326-331.
黄荣凤,张国盛,王林和,等,2004.影响毛乌素沙地臭柏年轮宽度变化的主要气候因子分析[J].干旱区资源与环境,18(6):164-169.DOI:10.13448/j.cnki.jal re.2004.06.032.
黄荣辉,徐予红,周连童,1999.我国夏季降水的年代际变化及华北干旱化趋势[J].高原气象,18(4):465-476.
黄玉霞,王宝鉴,王研峰,等,2017.甘肃省夏季暴雨日数特征及其与大气环流关系[J].高原气象,36(1):183-194.DOI:10.7522/j.issn.1000-0534.2015.00118.
雷光炳,2009.寿鹿山自然保护区青海云杉梢斑螟的观测与防治[J].甘肃林业(3):37-38.
李栋梁,邵鹏程,王慧,等,2013.中国东亚副热带夏季风北边缘带研究进展[J].高原气象,32(1):305-314.DOI:1000-0534(2013)01-0305-10.
李栋梁,张茜,姚慧茹,等,2016.北印度夏季风与中国河套及邻近地区盛夏降水的联系[J].高原气象,35(6):1512-1523.DOI:10.7522/j.issn.1000-0534.2016.00075.
李钢,闫海枫,王科,等,2018.东大山植物资源多样性分析[J].林业科技通讯(7):23-26.
李钢铁,史晴,任改莲,等,1995.确定梭梭年龄的初步探讨[J].内蒙古林学院学报,17(2):52-55.
李森,李凡,孙武,等,2004.黑河下游额济纳绿洲现代荒漠化过程及其驱动机制[J].地理科学,24(1):61-67.DOI:10.13249/j.cnki.sgs.200 4.01.011.
李媛媛,秦宁生,时兴合,等,2015.近714年扎曲河流域径流量的重建和变化特征[J].高原气象,34(4):1065-1073.DOI:10.7522/j.issn.1000-0534.2014.00018.
刘普幸,陈发虎,勾晓华,等,2005.额济纳旗近100 a来胡杨年表的建立与响应分析[J].中国沙漠,25(5):764-768.
刘禹,Shishov V,史江峰,等,2004.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,49(3):270-274.
刘禹,解利,李强,等,2012.公元1820年以来甘肃东大山地区树轮宽度对3-9月平均最低温度的响应分析[J].地球环境学报,3(3):900-907.DOI:10.7515/JEE201203008.
刘禹,王雷,史江峰,等,2005.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,25(5):540-544.
马利民,刘禹,蔡秋芳,等,2003a.贺兰山树轮晚材宽度记录中的降水量变化[J].海洋地质与第四纪地质,23(4):109-114.DOI:10.16562/j.cnki.0256-1492.2003.04.016.
马利民,刘禹,赵建夫,2003b.贺兰山油松年轮中稳定碳同位素含量和环境的关系[J].环境科学,24(5):49-53.DOI:10.13227/j.hjkx.2003.05.009.
彭小梅,2013.黑河下游胡杨树木年轮学研究[D].北京:中国科学院大学,1-72.
彭小梅,肖生春,程国栋,等,2016.胡杨(Populus euphratica)树轮记录的20世纪40年代前后黑河下游分水过程及其生态影响[J].中国沙漠,36(1):206-215.DOI:10.7522/j.issn.1000-694X.2016.00006.
史江峰,刘禹,蔡秋芳,等,2007.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,27(1):95-100.DOI:10.16562/j.cnki.0256-1492.2007.01.012.
孙军艳,刘禹,蔡秋芳,等,2006.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,26(5):799-807.
谭敬,杨文斌,齐凯,等,2006.阿拉善盟四大沙漠“决口”与“握手”状况调查及治理对策[J].内蒙古林业科技,32(3):4-7.
汤绪,钱维宏,梁萍,2006.东亚夏季风边缘带的气候特征[J].高原气象,25(3):375-381.
田全彦,肖生春,彭小梅,等,2015.胡杨(Populus euphratica)与柽柳(Tamarix ramosissima)径向生长特征对比[J].中国沙漠,35(6):1512-1519.DOI:10.7522/j.issn.1000-6 94X.2015.00007.
万炜,颜长珍,肖生春,等,2018.1975-2015年阿拉善高原沙漠化过程、格局与驱动机制[J].中国沙漠,38(1):17-29.DOI:10.7522/j.issn.1000-694X.2017.00086.
王宝鉴,黄玉霞,何金海,等,2004.东亚夏季风期间水汽输送与西北干旱的关系[J].高原气象,23(6):912-918.
王可丽,江灏,赵红岩,2005.西风带与季风对中国西北地区的水汽输送[J].水科学进展,16(3):432-438.DOI:10.14042/j.cnki.32.1309.2005.03.021.
王炜,梁存柱,朱宗元,等,2001.梭梭年轮测定方法及生长动态的研究[J].干旱区资源与环境,15(2):67-75.DOI:10.13448/j.cnki.jal re.2001.02.013.
吴祥定,1990.树木年轮与气候变化[M].北京:气象出版社.
肖生春,陈小红,丁爱军,2017.近现代阿拉善荒漠气候变化与环境演变机制研究进展[J].中国沙漠,37(6):1102-1110.DOI:10.7522/j.issn.1000-694X.2017.000 02.
肖生春,肖洪浪,2006a.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,28(2):000039-45.DOI:10.13332/j.1000-1522.2006.02.007.
肖生春,肖洪浪,彭小梅,2012.黑河下游胡杨季节尺度径向生长变化研究[J].冰川冻土,34(3):706-712.
肖生春,肖洪浪,彭小梅,2013.梭梭(Haloxylon ammodendron)不宜用于树木年轮学研究[J].中国沙漠,33(6):1692-1698.DOI:10.7522/j.issn.1000-694X.2013.00243.
肖生春,肖洪浪,司建华,等,2005.干旱区多枝柽柳的生长特性[J].西北植物学报,25(5):1012-1016.
肖生春,肖洪浪,司建华,等,2010.胡杨(Populus euphratica)径向生长日变化特征分析[J].冰川冻土,32(4):816-822.
肖生春,肖洪浪,宋耀选,等,2006b.荒漠植被红砂(Reaumurta soongorica)水热响应的年轮学研究[J].中国沙漠,26(4):548-552.
肖生春,肖洪浪,周茂先,等,2004.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,26(5):557-562.
杨理,杨持,杨春明,等,1996.四合木(Tetraena mongolica)营养生长和降水、气温的关系[J].内蒙古大学学报:自然科学版,27(6):816-85.
张凯,司建华,王润元,等,2008.气候变化对阿拉善荒漠植被的影响研究[J].中国沙漠,28(5):879-885.
张庆乐,刘卫国,刘禹,等,2005.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,34(1):51-56.
张永香,於琍,尹红,2015.巴丹吉林沙漠南缘191 a来年降水量重建及初步分析[J].沙漠与绿洲气象,9(1):12-16.DOI:10.3969/j.issn.1002-0799.2015.01.003.
赵守栋,何新,张冰琦,等,2013.贺兰山东坡高山林线青海云杉(Picea crassifolia)径向生长对气候因子的响应[J].北京师范大学学报(自然科学版),49(5):501-505.