基于SEBAL模型的渭-库绿洲蒸散量特征及影响因子研究
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摘要
对渭-库绿洲蒸散发量的估算在绿洲水资源管理和分配以及生态环境的保护方面扮演着重要作用,同时对于深刻了解流域水循环和水文过程也具有重要意义。本文以渭干河-库车河绿洲为研究靶区,将Landsat TM/OLI遥感数据与地面气象站点实测数据相结合,利用SEBAL模型估算了渭-库绿洲1997年和2016年的日蒸散量,并对日蒸散量的空间分布特征及日蒸散量与相关地表参数的相关性进行了分析。结果表明:渭-库绿洲日蒸散量的空间分布表现为西高东低,北高南低的分布特征,其高值出现在水体和植被覆盖较多的绿洲内部区域,低值则分布在研究区东、东南和西部的低植被覆盖区域;在日蒸散量与植被指数(NDVI、SAVI、LAI)、水体指数(MNDWI、NDWI、TVI、VSWI、TVDI)和地表温度(LST)等地表参数的相关性方面,研究时段内全部地表参数与日ET具有较高的相关关系,Pearson相关系数都通过0.01水平的显著性检验,其中NDWI与日蒸散量表现出了最好的相关性,表明在渭-库绿洲水分对日蒸散量分布与变化的影响是最大的。
The arid zone refers to the arid climate area, which accounts for about 30% of the land area. The common characteristics are: the precipitation is low and the change rate is large, the ranges of both the daily and annual temperature are large, and the evaporation is far greater than the precipitation. Thus, the estimation of evapotranspiration in the Ugan and Kuqa Rivers Delta Oasis plays an important role in the management and allocation of water resources. At the same time, it has a great significance to understand the water cycle and hydrological process of the study area. In this paper takes the Ugan and Kuqa Rivers Delta Oasis as the study site, the daily evapotranspiration of Ugan and Kuqa Rivers Delta Oasis in 1997(August 30) and 2016(August 2)was estimated, and the spatial distribution characteristics of daily evapotranspiration, and the correlation between daily evapotranspiration and relative surface parameters were analyzed by combining Landsat TM/OLI remote sensing images with meteorological data, and using SEBAL model. The results showed that the spatial distribution of daily evapotranspiration in the Ugan and Kuqa Rivers Delta Oasis was characterized by distribution patterns of high to low from west to east, and from north to south. The high value appeares in the oasis area covered with abundant water and vegetation, and the low value is distributed in the east, southeast and west part of the study area with the low vegetation coverage. In terms of the correlation between the daily evapotranspiration and surface parameters, such as vegetation indices(NDVI, SAVI, LAI), water indices(MNDWI, NDWI, TVI, VSWI, TVDI) and land surface temperature(LST), the daily evapotranspiration showed the good correlation with every index. The Pearson correlation coefficients past the significance test at 0.01 level, especially with a best correlation with NDWI. the results indicate that water bodies are the most important factor for distribution and changes of the daily evapotranspiration in the Ugan and Kuqa Rivers Delta Oasis.
The arid zone refers to the arid climate area, which accounts for about 30% of the land area. The common characteristics are: the precipitation is low and the change rate is large, the ranges of both the daily and annual temperature are large, and the evaporation is far greater than the precipitation. Thus, the estimation of evapotranspiration in the Ugan and Kuqa Rivers Delta Oasis plays an important role in the management and allocation of water resources. At the same time, it has a great significance to understand the water cycle and hydrological process of the study area. In this paper takes the Ugan and Kuqa Rivers Delta Oasis as the study site, the daily evapotranspiration of Ugan and Kuqa Rivers Delta Oasis in 1997(August 30) and 2016(August 2)was estimated, and the spatial distribution characteristics of daily evapotranspiration, and the correlation between daily evapotranspiration and relative surface parameters were analyzed by combining Landsat TM/OLI remote sensing images with meteorological data, and using SEBAL model. The results showed that the spatial distribution of daily evapotranspiration in the Ugan and Kuqa Rivers Delta Oasis was characterized by distribution patterns of high to low from west to east, and from north to south. The high value appeares in the oasis area covered with abundant water and vegetation, and the low value is distributed in the east, southeast and west part of the study area with the low vegetation coverage. In terms of the correlation between the daily evapotranspiration and surface parameters, such as vegetation indices(NDVI, SAVI, LAI), water indices(MNDWI, NDWI, TVI, VSWI, TVDI) and land surface temperature(LST), the daily evapotranspiration showed the good correlation with every index. The Pearson correlation coefficients past the significance test at 0.01 level, especially with a best correlation with NDWI. the results indicate that water bodies are the most important factor for distribution and changes of the daily evapotranspiration in the Ugan and Kuqa Rivers Delta Oasis.
引文
[1]贺广均,冯学智,肖鹏峰,等.一种基于植被指数-地表温度特征空间的蒸散指数[J].干旱区地理,2015,38(5):887-899.[He G J,Feng X Z,Xiao P F,et al.An evapotranspiration index from Ts-VI feature space[J].Arid Land Geography,2015,38(5):887-899.]
[2]马耀明,王介民.非均匀陆面上区域蒸发(散)研究概况[J].高原气象,1997,16(4):446-452.[Ma Y M,Wang J M.Asurvey in the study of area evaporation(evapotranspiration)over the heterogeneous landscape[J].Plateau Meteorology,1997,16(4):446-452.]
[3]Wang J,Bastiaanssen W G M,Ma Y,et al.Aggregation of land surface parameters in the oasis-desert systems of north-west China[J].Hydrological Processes,1998,12(13-14):2133-2147.
[4]曾丽红,宋开山,张柏,等.应用Landsat数据和SEBAL模型反演区域蒸散发及其参数估算[J].遥感技术与应用,2008,23(3):255-263.[Zeng L H,Song K S,Zhang B,et al.Applying Landsat data and SEBAL model to inverse regional evapotranspiration and its parameters estimation[J].Remote Sensing Technology and Application,2008,23(3):255-263.]
[5]Bastiaanssen W G M,Menenti M,Feddes R A,et al.The Surface Energy Balance Algorithm for Land(SEBAL):Part 1 formulation[J].Journal of Hydrology,1998,212(98):801-811.
[6]Norman J M,Kustas W P,Humes K S.Source approach for estimating soil and vegetation energy fluxes in observations of directional radiometric surface temperature[J].Agricultural and Forest Meteorology,1995,77(3):263-293.
[7]Roerink G J,Su Z,Menenti M.S-SEBI:A simple remote sensing algorithm to estimate the surface energy balance[J].Physics and Chemistry of the Earth Part B Hydrology Oceans and Atmosphere,2000,25(2):147-157.
[8]Su Z.The Surface Energy Balance System(SEBS)for estimation of turbulent heat fluxes[J].Hydrology and Earth System Sciences,1999,6(1):85-100.
[9]Tang R,Li Z L,Chen K S,et al.Spatial-scale effect on the SEBAL model for evapotranspiration estimation using remote sensing data[J].Agricultural and Forest Meteorology,2013,174(174):28-42.
[10]Tang R,Li Z L.Evaluation of two end-member-based models for regional land surface evapotranspiration estimation from MODIS data[J].Agricultural and Forest Meteorology,2015,202(202):69-82.
[11]Santos C A G,Silva R M D,Silva A M,et al.Estimation of evapotranspiration for different land covers in a Brazilian semi-arid region:A case study of the Brígida River basin,Brazil[J].Journal of South American Earth Sciences,2017,74:54-66.
[12]魏天锋.基于SEBAL模型的博尔塔拉河流域典型植被生态需水估算[D].乌鲁木齐:新疆大学,2015.[Wei T F.Estimated ecological water requirement of typical vegetation in Boertala Rever Basin based on RS and SEBALmodel[D].Urumqi:Xinjiang University,2015.]
[13]杨肖丽,任立良,袁飞,等.利用SEBAL模型对沙拉沐沦河流域蒸散发的分析[J].干旱区研究,2010,27(4):507-514.[Yang X L,Ren L L,Yuan F,et al.Study on evapotranspiration in the Shalamulun River Basin using SEBALmodel and MODIS data[J].Arid Zone Research,2010,27(4):507-514.]
[14]韩惠.基于遥感技术的祖厉河流域土地利用/土地覆盖变化与蒸散发研究[D].兰州:兰州大学,2006.[Han H.Investigation of LUCC and ET in Zuli Basin of the loess plateau using remotely sensed data[D].Lanzhou:Lanzhou University,2006.]
[15]张殿君,张学霞,武鹏飞.黄土高原典型流域土地利用变化对蒸散发影响研究[J].干旱区地理(汉文版),2011,34(3):400-408.[Zhang D J,Zhang X X,Wu P F.Relationship between ET and LUCC in a typical watershed of loess plateau over the past 20 years[J].Arid Land Geography,2011,34(3):400-408.]
[16]李宝富,陈亚宁,李卫红,等.基于遥感和SEBAL模型的塔里木河干流区蒸散发估算[J].地理学报,2011,66(9):1230-1238.[Li B F,Chen Y N,Li W H,et al.Remote sensing and the SEBAL model for estimating evapotranspiration in the Tarim River[J].Acta Geographica Sinica,2011,66(9):1230-1238.]
[17]谭娇,丁建丽,陈文倩,等.基于多变量时间序列模型的地下水埋深预测--以渭库绿洲为例[J].节水灌溉,2017(9):55-59.[Tan J,Ding J L,Chen W Q,et al.Groundwater depth prediction based on multivariate time series model:A case study on Weigan and Kuq Rivers Delta Oasis[J].Water Saving Irrigation,2017(9):55-59.]
[18]王娟,张飞,于海洋,等.基于LUCC的渭干河-库车河三角洲绿洲水文及生态特征[J].水土保持研究,2016,23(2):236-242.[Wang J,Zhang F,Yu H Y,et al.Analysis on the hydrological and ecological characteristics based on the LUCC in Weigan and Kuqa River[J].Research of Soil and Water Conservation,2016,23(2):236-242.]
[19]玉苏甫·买买提,阿热孜古丽·图尔荪,艾萨迪拉·玉苏甫.渭-库河三角洲绿洲农作物需水量分析[J].节水灌溉,2015(11):85-88.[Yusup Mamat,Arzigul Tursun,Asadilla Yusup.Analysis of crop water requirement in WeiganKuqa River Delta Oasis of Xinjiang[J].Water Saving Irrigation,2015(11):85-88.]
[20]张飞,郭玉川,姜红涛,等.气候和土地利用/覆盖变化对渭干河-库车河三角洲绿洲水资源的影响[J].湖北农业科学,2014,53(23):5716-5723.[Zhang F,Guo Y C,JH T,et al.Impacts of climate and land use-cover change on water resources in the Delta Oasis of Weigan RiverKuqa River[J].Hubei Agricultural Sciences,2014,53(23):5716-5723.]
[21]满苏尔·沙比提,帕尔哈提·艾孜木,玉素浦江·如.渭干河-库车河三角洲绿洲近50a来生态环境变化特征及防治对策[J].干旱区资源与环境,2004,18(4):13-18.[Mansur Sabit,Parhat Aizim,Yusupjan Rusul.Analysis on the changes of ecological environment characters and it's countermeasures of Wigan-Kuqa River[J].Journal of Arid Land Resources and Environment,2004,18(4):13-18.]
[22]Anselin L,Syabri I,Kho Y.Geo Da:An introduction to spatial data analysis[J].Geographical Analysis,2006,38(1):5-22.
[23]Anselin L.Local indicators of spatial association LISA[J].Geographical Analysis,1995,27(2):93-115.
[24]马秋梅,刘新亮,李勇,等.基于Landsat 8数据的亚热带小流域蒸散发估算及时空特征分析[J].生态与农村环境学报,2016,32(6):901-907.[Ma Q M,Liu X L,Li Y,et al.Estimation and spatio-temporal distribution of evapotranspiration in small-scaled catchments in subtropics of China based on Landsat 8 data[J].Journal of Ecology and Rural Environment,2016,32(6):901-907.]
[25]童瑞,杨肖丽,任立良,等.黄河流域1961-2012年蒸散发时空变化特征及影响因素分析[J].水资源保护,2015,31(3):16-21.[Tong R,Yang X L,R L L,et al.Temporal and spatial characteristics of evapotranspiration in the Yellow River Basin during 1961-2012 and analysis of its influence factors[J].Water Resources Protection,2015,31(3):16-21.]
[26]金学杰,周剑.基于SEBS模型和Landsat 8数据的黑河下游蒸散发时空特性分析[J].冰川冻土,2017,39(3):572-582.[Jin X J,Zhou J.Analysis of spatial-temporal characteristics of evapotranspiration in the lower reaches of Heihe River based on surface energy balance system model and Landsat 8 data[J].Journal of Glaciology and Geocryology,2017,39(3):572-582.]
[27]Rouse J W.Monitoring the vernal advancement and retrogradation(greenwave effect)of natural vegetation[J].Nasa/gsfct Type Report,1974.
[28]Huete A R.A soil-adjusted vegetation index[J].Remote Sensing of Environment,1988,27(3):295-309.
[29]Boegh E,Soegaard H,Broge N,et al.Airborne multispectral data for quantifying leaf area index,nitrogen concentration,and photosynthetic efficiency in agriculture[J].Remote Sensing of Environment,2002,81(2-3):179-193.
[30]徐涵秋.基于谱间特征和归一化指数分析的城市建筑用地信息提取[J].地理研究,2005,24(2):311-320.[Xu H Q.Fast information extraction of urban built-up land based on the analysis of spectral signature and normalized difference index[J].Geographical Research,2005,24(2):311-320.]
[31]Mcfeeters S K.The use of the normalized difference water index(NDWI)in the delineation of open water features[J].International Journal of Remote Sensing,1996,17(7):1425-1432.
[32]闫峰,覃志豪,李茂松,等.农业旱灾监测中土壤水分遥感反演研究进展[J].自然灾害学报,2006,15(6):114-121.[Yan F,Qin Z H,Li M S,et al.Progress in soil moisture estimation from remote sensing data for agricultural drought monitoring[J].Journal of Natural Disasters,2006,15(6):114-121.]
[33]Sandholt I,Rasmussen K,Andersen J.A simple interpretation of the surface temperature/vegetation index space for assessment of surface moisture status[J].Remote Sensing of Environment,2002,79(2):213-224.
[34]吴志刚,江滔,樊艳磊,等.基于Landsat8数据的地表温度反演及分析研究--以武汉市为例[J].工程地球物理学报,2016,13(1):135-142.[Wu Z G,Jiang T,Fan Y L,et al.Land surface temperature retrieval and result analysis based on landsat8 data in Wuhan city[J].Chinese Journal of Engineering Geophysics,2016,13(1):135-142.]
[35]陈云浩,李晓兵,史培军.中国西北地区蒸发散量计算的遥感研究[J].地理学报,2001,56(3):261-268.[Chen Y H,Li X B,Shi P J.Regional evapotranspiration estimation over Northwest China using remote sensing[J].Acta Geographica Sinica,2001,56(3):261-268.]
[36]喻露露,张晓祥,李杨帆,等.海口市海岸带生态系统服务及其时空变异[J].生态学报,2016,36(8):2431-2441.[Yu L L,Zhang X X,Li Y F,et al.Coastal ecosystem services and their spatial-temporal variation in Haikou,China[J].Acta Ecologica Sinica,2016,36(8):2431-2441.]
[37]麦尔耶姆·亚森,买买提·沙吾提,吐尔逊·艾山,等.新疆渭干河-库车河三角洲绿洲耕地时空变化特征分析[J].中国农业科学,2017,50(18):3506-3518.[Maieryemu Yasen,Maimaiti Shawuti,Tuerxun Aishan,et al.Spatial-Temporal Characteristics of Cropland in the Ugan-Kuqa River Delta Oasis[J].Scientia Agricultura Sinica,2017,50(18):3506-3518.]
[38]郭玉川,董新光.SEBAL模型在干旱区区域蒸散发估算中的应用[J].遥感信息,2007(3):75-78.[Guo Y C,Dong X G.The SEBAL Model for estimating regional evaportranspiration in arid regions[J].Remote Sensing Information,2007(3):75-78.]
[39]代鹏超,牛苏娟,毋兆鹏,等.新疆精河流域实际蒸散发时空变化特征[J].生态与农村环境学报,2017,33(7):600-606.[Dai P C,Niu S J,Wu Z P,et al.Temporal and spatial characteristics of actual evapotranspiration in Jinghe Watershed,Xinjiang[J].Journal of Ecology and Rural Environment,2017,33(7):600-606.]
[40]马宏伟,王乃昂,朱金峰,等.石羊河流域蒸发蒸腾量遥感反演及灵敏度分析[J].水资源与水工程学报,2010,21(6):76-80.[Ma H W,Wang N A,Zhu J F,et al.analysis of evapotranspiration using satellite remote and its sensitivity in Shiyang River Basin[J].Journal of Water Resources and Water Engineering,2010,21(6):76-80.]
[41]张圆,郑江华,刘志辉,等.基于Landsat8遥感影像和SEBS模型的呼图壁县蒸散量时空格局分析[J].生态科学,2016,35(2):26-32.[Zhang Y,Zheng J H,Liu Z H,et al.Spatial and temporal distribution of evapotranspiration in the hutubi County based on Landsat8 data and SEBSmodel[J].Ecological Science,2016,35(2):26-32.]
[42]Shuttleworth W,Gurney R,Hsu A,et al.FIFE:The variation in energy partition at surface flux sites[J].IAHSPublication,1989,186:67-74.
[43]Tang R,Li Z L,Sun X.Temporal upscaling of instantaneous evapotranspiration:An intercomparison of four methods using eddy covariance measurements and MO-DIS data[J].Remote Sensing of Environment,2013,138(138):102-118.
[44]Tang R,Li Z.An improved constant evaporative fraction method for estimating daily evapotranspiration from remotely sensed instantaneous observations[J].Geophysical Research Letters,2017,44(5):2319-2326.
[45]Tang R,Li Z L.Estimating daily evapotranspiration from remotely sensed instantaneous observations with simplified derivations of a theoretical model[J].Journal of Geophysical Research Atmospheres,2017,122(19):10177-10190.
[46]程春晓,徐宗学,张淑荣,等.黑河流域上中游植被蒸散发时空演变趋势及其影响因子分析[J].北京师范大学学报(自然科学版),2014(5):535-542.[Cheng C X,Xu Z X,Zhang S R,et al.Temporal-spatial variation in evapotranspiration in the Heihe River basin and their correlation with different meteorological/hydrological factors[J].Journal of Beijing Normal University(Natural Science),2014(5):535-542.]
[47]徐永明,赵巧华,巴雅尔,等.基于MODIS数据的博斯腾湖流域地表蒸散时空变化[J].地理科学,2012,32(11):1353-1357.[Xu Y M,Zhao Q H,Ba Y E,et al.Spatio-temporal variations of land surface evapotranspiration of Bosten Lake based on MODIS data[J].Scientia Geographica Sinica,2012,32(11):1353-1357.]
[2]马耀明,王介民.非均匀陆面上区域蒸发(散)研究概况[J].高原气象,1997,16(4):446-452.[Ma Y M,Wang J M.Asurvey in the study of area evaporation(evapotranspiration)over the heterogeneous landscape[J].Plateau Meteorology,1997,16(4):446-452.]
[3]Wang J,Bastiaanssen W G M,Ma Y,et al.Aggregation of land surface parameters in the oasis-desert systems of north-west China[J].Hydrological Processes,1998,12(13-14):2133-2147.
[4]曾丽红,宋开山,张柏,等.应用Landsat数据和SEBAL模型反演区域蒸散发及其参数估算[J].遥感技术与应用,2008,23(3):255-263.[Zeng L H,Song K S,Zhang B,et al.Applying Landsat data and SEBAL model to inverse regional evapotranspiration and its parameters estimation[J].Remote Sensing Technology and Application,2008,23(3):255-263.]
[5]Bastiaanssen W G M,Menenti M,Feddes R A,et al.The Surface Energy Balance Algorithm for Land(SEBAL):Part 1 formulation[J].Journal of Hydrology,1998,212(98):801-811.
[6]Norman J M,Kustas W P,Humes K S.Source approach for estimating soil and vegetation energy fluxes in observations of directional radiometric surface temperature[J].Agricultural and Forest Meteorology,1995,77(3):263-293.
[7]Roerink G J,Su Z,Menenti M.S-SEBI:A simple remote sensing algorithm to estimate the surface energy balance[J].Physics and Chemistry of the Earth Part B Hydrology Oceans and Atmosphere,2000,25(2):147-157.
[8]Su Z.The Surface Energy Balance System(SEBS)for estimation of turbulent heat fluxes[J].Hydrology and Earth System Sciences,1999,6(1):85-100.
[9]Tang R,Li Z L,Chen K S,et al.Spatial-scale effect on the SEBAL model for evapotranspiration estimation using remote sensing data[J].Agricultural and Forest Meteorology,2013,174(174):28-42.
[10]Tang R,Li Z L.Evaluation of two end-member-based models for regional land surface evapotranspiration estimation from MODIS data[J].Agricultural and Forest Meteorology,2015,202(202):69-82.
[11]Santos C A G,Silva R M D,Silva A M,et al.Estimation of evapotranspiration for different land covers in a Brazilian semi-arid region:A case study of the Brígida River basin,Brazil[J].Journal of South American Earth Sciences,2017,74:54-66.
[12]魏天锋.基于SEBAL模型的博尔塔拉河流域典型植被生态需水估算[D].乌鲁木齐:新疆大学,2015.[Wei T F.Estimated ecological water requirement of typical vegetation in Boertala Rever Basin based on RS and SEBALmodel[D].Urumqi:Xinjiang University,2015.]
[13]杨肖丽,任立良,袁飞,等.利用SEBAL模型对沙拉沐沦河流域蒸散发的分析[J].干旱区研究,2010,27(4):507-514.[Yang X L,Ren L L,Yuan F,et al.Study on evapotranspiration in the Shalamulun River Basin using SEBALmodel and MODIS data[J].Arid Zone Research,2010,27(4):507-514.]
[14]韩惠.基于遥感技术的祖厉河流域土地利用/土地覆盖变化与蒸散发研究[D].兰州:兰州大学,2006.[Han H.Investigation of LUCC and ET in Zuli Basin of the loess plateau using remotely sensed data[D].Lanzhou:Lanzhou University,2006.]
[15]张殿君,张学霞,武鹏飞.黄土高原典型流域土地利用变化对蒸散发影响研究[J].干旱区地理(汉文版),2011,34(3):400-408.[Zhang D J,Zhang X X,Wu P F.Relationship between ET and LUCC in a typical watershed of loess plateau over the past 20 years[J].Arid Land Geography,2011,34(3):400-408.]
[16]李宝富,陈亚宁,李卫红,等.基于遥感和SEBAL模型的塔里木河干流区蒸散发估算[J].地理学报,2011,66(9):1230-1238.[Li B F,Chen Y N,Li W H,et al.Remote sensing and the SEBAL model for estimating evapotranspiration in the Tarim River[J].Acta Geographica Sinica,2011,66(9):1230-1238.]
[17]谭娇,丁建丽,陈文倩,等.基于多变量时间序列模型的地下水埋深预测--以渭库绿洲为例[J].节水灌溉,2017(9):55-59.[Tan J,Ding J L,Chen W Q,et al.Groundwater depth prediction based on multivariate time series model:A case study on Weigan and Kuq Rivers Delta Oasis[J].Water Saving Irrigation,2017(9):55-59.]
[18]王娟,张飞,于海洋,等.基于LUCC的渭干河-库车河三角洲绿洲水文及生态特征[J].水土保持研究,2016,23(2):236-242.[Wang J,Zhang F,Yu H Y,et al.Analysis on the hydrological and ecological characteristics based on the LUCC in Weigan and Kuqa River[J].Research of Soil and Water Conservation,2016,23(2):236-242.]
[19]玉苏甫·买买提,阿热孜古丽·图尔荪,艾萨迪拉·玉苏甫.渭-库河三角洲绿洲农作物需水量分析[J].节水灌溉,2015(11):85-88.[Yusup Mamat,Arzigul Tursun,Asadilla Yusup.Analysis of crop water requirement in WeiganKuqa River Delta Oasis of Xinjiang[J].Water Saving Irrigation,2015(11):85-88.]
[20]张飞,郭玉川,姜红涛,等.气候和土地利用/覆盖变化对渭干河-库车河三角洲绿洲水资源的影响[J].湖北农业科学,2014,53(23):5716-5723.[Zhang F,Guo Y C,JH T,et al.Impacts of climate and land use-cover change on water resources in the Delta Oasis of Weigan RiverKuqa River[J].Hubei Agricultural Sciences,2014,53(23):5716-5723.]
[21]满苏尔·沙比提,帕尔哈提·艾孜木,玉素浦江·如.渭干河-库车河三角洲绿洲近50a来生态环境变化特征及防治对策[J].干旱区资源与环境,2004,18(4):13-18.[Mansur Sabit,Parhat Aizim,Yusupjan Rusul.Analysis on the changes of ecological environment characters and it's countermeasures of Wigan-Kuqa River[J].Journal of Arid Land Resources and Environment,2004,18(4):13-18.]
[22]Anselin L,Syabri I,Kho Y.Geo Da:An introduction to spatial data analysis[J].Geographical Analysis,2006,38(1):5-22.
[23]Anselin L.Local indicators of spatial association LISA[J].Geographical Analysis,1995,27(2):93-115.
[24]马秋梅,刘新亮,李勇,等.基于Landsat 8数据的亚热带小流域蒸散发估算及时空特征分析[J].生态与农村环境学报,2016,32(6):901-907.[Ma Q M,Liu X L,Li Y,et al.Estimation and spatio-temporal distribution of evapotranspiration in small-scaled catchments in subtropics of China based on Landsat 8 data[J].Journal of Ecology and Rural Environment,2016,32(6):901-907.]
[25]童瑞,杨肖丽,任立良,等.黄河流域1961-2012年蒸散发时空变化特征及影响因素分析[J].水资源保护,2015,31(3):16-21.[Tong R,Yang X L,R L L,et al.Temporal and spatial characteristics of evapotranspiration in the Yellow River Basin during 1961-2012 and analysis of its influence factors[J].Water Resources Protection,2015,31(3):16-21.]
[26]金学杰,周剑.基于SEBS模型和Landsat 8数据的黑河下游蒸散发时空特性分析[J].冰川冻土,2017,39(3):572-582.[Jin X J,Zhou J.Analysis of spatial-temporal characteristics of evapotranspiration in the lower reaches of Heihe River based on surface energy balance system model and Landsat 8 data[J].Journal of Glaciology and Geocryology,2017,39(3):572-582.]
[27]Rouse J W.Monitoring the vernal advancement and retrogradation(greenwave effect)of natural vegetation[J].Nasa/gsfct Type Report,1974.
[28]Huete A R.A soil-adjusted vegetation index[J].Remote Sensing of Environment,1988,27(3):295-309.
[29]Boegh E,Soegaard H,Broge N,et al.Airborne multispectral data for quantifying leaf area index,nitrogen concentration,and photosynthetic efficiency in agriculture[J].Remote Sensing of Environment,2002,81(2-3):179-193.
[30]徐涵秋.基于谱间特征和归一化指数分析的城市建筑用地信息提取[J].地理研究,2005,24(2):311-320.[Xu H Q.Fast information extraction of urban built-up land based on the analysis of spectral signature and normalized difference index[J].Geographical Research,2005,24(2):311-320.]
[31]Mcfeeters S K.The use of the normalized difference water index(NDWI)in the delineation of open water features[J].International Journal of Remote Sensing,1996,17(7):1425-1432.
[32]闫峰,覃志豪,李茂松,等.农业旱灾监测中土壤水分遥感反演研究进展[J].自然灾害学报,2006,15(6):114-121.[Yan F,Qin Z H,Li M S,et al.Progress in soil moisture estimation from remote sensing data for agricultural drought monitoring[J].Journal of Natural Disasters,2006,15(6):114-121.]
[33]Sandholt I,Rasmussen K,Andersen J.A simple interpretation of the surface temperature/vegetation index space for assessment of surface moisture status[J].Remote Sensing of Environment,2002,79(2):213-224.
[34]吴志刚,江滔,樊艳磊,等.基于Landsat8数据的地表温度反演及分析研究--以武汉市为例[J].工程地球物理学报,2016,13(1):135-142.[Wu Z G,Jiang T,Fan Y L,et al.Land surface temperature retrieval and result analysis based on landsat8 data in Wuhan city[J].Chinese Journal of Engineering Geophysics,2016,13(1):135-142.]
[35]陈云浩,李晓兵,史培军.中国西北地区蒸发散量计算的遥感研究[J].地理学报,2001,56(3):261-268.[Chen Y H,Li X B,Shi P J.Regional evapotranspiration estimation over Northwest China using remote sensing[J].Acta Geographica Sinica,2001,56(3):261-268.]
[36]喻露露,张晓祥,李杨帆,等.海口市海岸带生态系统服务及其时空变异[J].生态学报,2016,36(8):2431-2441.[Yu L L,Zhang X X,Li Y F,et al.Coastal ecosystem services and their spatial-temporal variation in Haikou,China[J].Acta Ecologica Sinica,2016,36(8):2431-2441.]
[37]麦尔耶姆·亚森,买买提·沙吾提,吐尔逊·艾山,等.新疆渭干河-库车河三角洲绿洲耕地时空变化特征分析[J].中国农业科学,2017,50(18):3506-3518.[Maieryemu Yasen,Maimaiti Shawuti,Tuerxun Aishan,et al.Spatial-Temporal Characteristics of Cropland in the Ugan-Kuqa River Delta Oasis[J].Scientia Agricultura Sinica,2017,50(18):3506-3518.]
[38]郭玉川,董新光.SEBAL模型在干旱区区域蒸散发估算中的应用[J].遥感信息,2007(3):75-78.[Guo Y C,Dong X G.The SEBAL Model for estimating regional evaportranspiration in arid regions[J].Remote Sensing Information,2007(3):75-78.]
[39]代鹏超,牛苏娟,毋兆鹏,等.新疆精河流域实际蒸散发时空变化特征[J].生态与农村环境学报,2017,33(7):600-606.[Dai P C,Niu S J,Wu Z P,et al.Temporal and spatial characteristics of actual evapotranspiration in Jinghe Watershed,Xinjiang[J].Journal of Ecology and Rural Environment,2017,33(7):600-606.]
[40]马宏伟,王乃昂,朱金峰,等.石羊河流域蒸发蒸腾量遥感反演及灵敏度分析[J].水资源与水工程学报,2010,21(6):76-80.[Ma H W,Wang N A,Zhu J F,et al.analysis of evapotranspiration using satellite remote and its sensitivity in Shiyang River Basin[J].Journal of Water Resources and Water Engineering,2010,21(6):76-80.]
[41]张圆,郑江华,刘志辉,等.基于Landsat8遥感影像和SEBS模型的呼图壁县蒸散量时空格局分析[J].生态科学,2016,35(2):26-32.[Zhang Y,Zheng J H,Liu Z H,et al.Spatial and temporal distribution of evapotranspiration in the hutubi County based on Landsat8 data and SEBSmodel[J].Ecological Science,2016,35(2):26-32.]
[42]Shuttleworth W,Gurney R,Hsu A,et al.FIFE:The variation in energy partition at surface flux sites[J].IAHSPublication,1989,186:67-74.
[43]Tang R,Li Z L,Sun X.Temporal upscaling of instantaneous evapotranspiration:An intercomparison of four methods using eddy covariance measurements and MO-DIS data[J].Remote Sensing of Environment,2013,138(138):102-118.
[44]Tang R,Li Z.An improved constant evaporative fraction method for estimating daily evapotranspiration from remotely sensed instantaneous observations[J].Geophysical Research Letters,2017,44(5):2319-2326.
[45]Tang R,Li Z L.Estimating daily evapotranspiration from remotely sensed instantaneous observations with simplified derivations of a theoretical model[J].Journal of Geophysical Research Atmospheres,2017,122(19):10177-10190.
[46]程春晓,徐宗学,张淑荣,等.黑河流域上中游植被蒸散发时空演变趋势及其影响因子分析[J].北京师范大学学报(自然科学版),2014(5):535-542.[Cheng C X,Xu Z X,Zhang S R,et al.Temporal-spatial variation in evapotranspiration in the Heihe River basin and their correlation with different meteorological/hydrological factors[J].Journal of Beijing Normal University(Natural Science),2014(5):535-542.]
[47]徐永明,赵巧华,巴雅尔,等.基于MODIS数据的博斯腾湖流域地表蒸散时空变化[J].地理科学,2012,32(11):1353-1357.[Xu Y M,Zhao Q H,Ba Y E,et al.Spatio-temporal variations of land surface evapotranspiration of Bosten Lake based on MODIS data[J].Scientia Geographica Sinica,2012,32(11):1353-1357.]