[1] 刘波,马柱国,冯锦明.1960-2004年新疆地区地表水热过程的数值模拟研究[J].中国沙漠,2012,32(2):491-502. [2] 张燕,徐建华,吕光辉.西北干旱区新疆水资源足迹及利用效率动态评估[J].中国沙漠,2008,28(4):915-919. [3] 李红军,李军,何清,等.新疆沙尘暴的趋势和突变研究[J].中国沙漠,2008,28(5):915-919. [4] Schimel D S,House J I,Hibbard K A,et al.Recent patterns and mechanisms of carbon exchange by terrestrial ecosystems[J].Nature,2001,414:169-172. [5] Wever L A,Flanagan L B,Carlson P J.Seasonal and interannual variation in evapotranspiration, energy balance and surface conductance in northern grassland[J].Agricultural and Forest Meteorology,2002,112(1):31-49. [6] 马虹,陈亚宁,李卫红.陆地生态系统CO2与水热通量的研究进展[J].新疆环境保护,2012,34(2):1-8. [7] Houghton R A,Davidson A E,Woodwell G M.Missing sinks,feedbacks, and understanding the role of terrestrial ecosystem in the global carbon balance[J].Global Biogeochemical Cycles,1998,12:25-34. [8] Dickinson R E.Land-atmosphere interaction[J].Reviews of Geophysics,1995,(S2):917-922. [9] Wilson K B,Baldocchi D D.Seasonal and interannual variability of energy fluxes over a broadleaved temperate deciduous forest in North America[J].Agricultural and Forest Meteorology,2000,100(1):1-18. [10] 王兵,刘世荣,崔向慧,等.全球陆地生态系统水热平衡规律研究进展[J].世界林业研究,2002,15(1):9-28. [11] 张强,曹晓彦.敦煌地区荒漠戈壁地表热量和辐射平衡特征的研究[J].大气科学,2003,27(2):245-254. [12] Hamerlynck E P,Huxman T E,Charlet T N,et al.Effects of elevated CO2 (FACE) on the functional ecology of the drought-deciduous Mojave Desert shrub,Lycium andersonii[J].Environmental and Experimental Botany,2002,48(2):93-106. [13] Barr A G,Morgenstern K,Black T A,et al.Surface energy balance closure by the eddy-covariance method above three boreal forest stands and implications for the measurement of the CO2 flux[J].Agricultural and Forest Meteorology,2006,140:322-337. [14] Mielnicka P,Dugasa W A,Mitchellb K,et al.Long-term measurements of CO2 flux and evapotranspiration in a Chihuahuan desert grassland[J].Journal of Arid Environments,2005,60(3):423-436. [15] Hastings S J,Oechel W C,Melo A M.Diurnal,seasonal and annual variation in the net ecosystem CO2 exchange of a desert shrub community (Sarcocaulescent) in Baja California,Mexico[J].Global Change Biology,2005,11(6):927-939. [16] Wohlfahrt G,Fenstermaker L F,Arnone J A.Large annual net ecosystem CO2 uptake of a Mojave Desert ecosystem[J].Global Change Biology,2008,14(7):1475-1487. [17] 王旭,尹光彩,周国逸,等.鼎湖山针阔混交林旱季能量平衡研究[J].热带亚热带植物学报,2005,13(3):205-210. [18] Dou J X,Zhang Y P,Yu G R,et al.Inter-annual and seasonal variations of energy and water vapour fluxes above a tropical seasonal rain forest in Xishuangbanna,SW China[J].Acta Ecologica Sinica,2007,27(8):3099-3109. [19] 马伟强,马耀明.西北干旱区地表能量初步分析[J].干旱区研究,2006,23(1):76-82. [20] 岳平,牛生杰,张强,等.春季晴天与阴天草原辐射和能量平衡特征的一次对比观测[J].中国沙漠,2010,30(6):1464-1468. [21] 陈世强,吕世华,奥银焕,等.夏季不同天气背景和灌溉条件下绿洲地表辐射和能量平衡特征[J].冰川冻土,2011,33(3):532-538. [22] 苗世光,窦军霞,Chen F,等.北京城市地表能量平衡特征观测分析[J].中国科学(地球科学),2012,42(9):1394-1402. [23] 徐亚琪,陈妮娜,高西宁,等.科尔沁草甸草地生长季能量平衡特征[J].气象与环境学报,2012,28(3):31-36. [24] Wang R Y,Yang X G,Ba D H,et al.Changes of sensible and latent heat on a typical clear day on dry-farming land in semi-arid region during different development phases of crop[J].Arid Meteorology,2004,22(4):26-39. [25] Cleverly J R,Dahm C N,Thibault J R,et al.Seasonal estimates of actual evapotranspiration from Tamarix ramosissima stands using three-dimensional eddy covariance[J].Journal of Arid Environments,2002,52(2):181-197. [26] 陈敏,陈亚宁,李卫红,等.不同地下水埋深柽柳、芦苇的生理响应[J].干旱区地理,2009,32(1):72-80. [27] 张喜焕,杨太新,辛贺明,等.不同柽柳种光合特性比较[J].西北农业学报,2010,19(12):113-117. [28] Zhuang L,Chen Y N.Physiological response of Tamarix ramosissima underwater stress along the lower reaches of Tarim River[J].Chinese Science Bulletin,2006,51(9):1123-1129. [29] 刘冰,赵文智.荒漠绿洲过渡带柽柳和泡泡刺光合作用及水分代谢的生态适应性[J].中国沙漠,2009,29(1):101-107. [30] Zhao L J,Xiao H L,Chen G L,et al.A preliminary study of water sources of riparian plants in the lower reaches of the Heihe basin[J].Acta Geoscientica Sinica,2008,29(6):709-718. [31] 彭守璋,赵传燕,彭焕华,等.黑河下游柽柳种群地上生物量及耗水量的空间分布[J].应用生态学报,2010,21(8):1940-1946. [32] Nippert J B,Butler Jr J J,Kluitenberg G J,et al.Patterns of Tamarix water use during a record drought[J].Oecologia,2010,162(2):283-292. [33] 郝兴明,陈亚宁,李卫红,等.胡杨根系水力提升作用的证据及其生态学意义[J].植物生态学报,2009,33(6):1125-1131. [34] Song X,Yu G R,Liu Y F,et al.Comparison of flux measurement by open-path and close-path eddy covariance systems[J].Science in China(Series D:Earth Sciences),2005,48(Suppl.Ⅰ):74-84. [35] Shi T T,Guan D X,Wu J B.Measurement of evapotranspiration above broad-leaved-Korean pine forests in the Changbaishan Mountains with eddy covariance technique[J].Journal of Beijing Forestry University,2006,28(6):1-8. [36] Massman W J,Lee X.Eddy covariance flux corrections and un-certainties in long-term studies of carbon and energy exchanges[J].Agricultural and Forest Meteorology,2002,113:121-144. [37] 李正泉,于贵瑞,温学发,等.中国通量观测网络(ChinaFLUX)能量平衡闭合状况的评价[J].中国科学(D辑:地球科学),2004,34(S2):46-56. [38] Wilson K B,Goldstein A H, Falge E,et al.Energy balance closure at FLUXNET sites[J].Agricultural and Forest Meteorology,2002,113(1/4):223-243. [39] McCaughey J H.Energy balance storage terms in a mature mixed forest at Petawawa,Ontario-a case study[J].Boundary-Layer Meteorology,1985,31:89-101. [40] 郭建侠,卞林根,戴永久.玉米生育期地表能量平衡的多时间尺度特征分析及不平衡原因的探索[J].中国科学(D辑:地球科学),2008,38(9):1103-1111. [41] Baldocchi D D,Law B E,Anthoni P M.On measuring and modeling energy fluxes above the floor of a homogeneous and heterogeneous conifer forest[J].Agricultural and Forest Meteorology,2000,102:187-206. [42] Kustas W P,Prueger J H,Hatfield J L,et al.Variability in soil heat flux from a mesquite dune site[J].Agricultural and Forest Meteorology,2000,103(3):49-264. |