[1]Stanhill G,Cohen S.Global dimming:A review of the evidence for a widespread and significant reduction in global radiation with discussion of its probable causes and possible agricultural consequences[J].Agricultural and Forest Meteorology,2001,107(4):255-278.[2]Ohmura A,Wild M.Is the hydrological cycle accelerating[J].Science,2002,298:1345-1346.[3]Roderick M L,Rotstayn L D,Farquhar G D.On the attribution of changing pan evaporation[J].Geophysical Research Letters,2007,34,L17403.[4]Roderick M L,Farquhar G D.Changes in Australian pan evaporation from 1970 to 2002[J].International Journal of Climatology,2004,24(9):1077-1090.[5]Roderick M L,Farquhar G D.Changes in New Zealand pan evaporation since the 1970s[J].International Journal of Climatology,2005,25:2031-2039.[6]Thomas A.Spatial and temporal characteristics of potential evapotranspiration trends over China [J].International Journal of Climatology,2000,20(4):381-396.[7]Linacre E T.Evaporation t rends [J].Theoretical and Applied Climatology,2004,79:11-21.[8]Chattopadhyay N,Hulme M.Evaporation and potential evapotranspiration in India under conditions on recent and future climate change[J].Agricultural and Forest Meteorology,1997,87:55-73.[9]Brutsaert W,Parlange M B.Hydrologic cycle explains the evaporation paradox[J].Nature,1998,396:30.[10]Peterson T C,Golubev V S,Groisman P Y.Evaporation losing its strength[J].Nature,1995,337:687-688.[11]Chattoopadhyay N,Hulme M.Evaporation and potential evapotranspiration in India under conditions of recent and future climate change[J].Agricultural and Forest Meteorology,1997,87(1):55-72.[12]Peterson T C,Golubev V S,Groisman P Y.Evaporation losing its strength[J].Nature,1995,377:687-688[13]Cohen S,Stanhill G.Evaporative climate changes at Bet Dagan,Israel,1964-1998[J].Agricultural and Forest Meteorology,2002,111(2):83-91.[14]Ramanathan V,Crutzen P J,Kiehl J T,et al.Aerosols,climate,and t he hydrological cycle[J].Science,2001,294:2119-2124.[15]任国玉,郭军.中国水面蒸发量的变化[J].自然资源学报,2006,21(1):31-44.[16]曾燕,邱新法,刘昌明,等.1960-2000年中国蒸发皿蒸发量的气候变化特征[J].水科学进展,2007,18(3):311-318.[17]刘波,马柱国.过去45年中国干湿气候区域变化特征[J].干旱区地理,2007,30(1):7-15.[18]刘波.近四十年中国蒸发皿蒸发变化与气候变化的关系及潜在蒸散的估算[D].南京:南京信息工程大学,2005.[19]左洪超,李栋梁,胡隐樵.近40 a中国气候变化趋势及其同蒸发皿观测的蒸发量变化的关系[J].科学通报,2005,50(11):1125-1130.[20]左洪超,鲍艳,张存杰,等.蒸发皿蒸发量的物理意义、近40年变化趋势的分析和数值试验研究[J].地球物理学报,2006,49(3):680-688.[21]王艳君,姜彤,许崇育.长江流域蒸发皿蒸发量及影响因素变化趋势[J].自然资源学报,2005,20(6):864-870.[22]王艳君,姜彤,许崇育,等.长江流域1961-2000年蒸发量变化趋势研究[J].气候变化研究进展,2005,1(3):99-105.[23]王艳君,姜彤,许崇育.长江流域20 cm蒸发皿蒸发量的时空变化[J].水科学进展,2006,17(6):830-833.[24]邱新法,刘昌明,曾燕.黄河流域近四十五年蒸发皿蒸发量的气候变化特征[J].自然资源学报,2003,18(4):437-442.[25]郭军,任国玉.黄淮海流域蒸发量的变化及其原因分析[J].水科学进展,2005,16(5):46-52.[26]王建华,卢予北,谢新民.豫北地区蒸发能力及其变化趋势分析[J].河南科学,2003,21(3):343-347.[27]苏宏超,魏文寿,韩萍.新疆近50 a来的气温和蒸发变化[J].冰川冻土,2003,25(2):174-178.[28]安月改,李元华.河北省近50年蒸发量气候变化特征[J].干旱区资源与环境,2005,19(4):159-162.[29]王素萍.近40年江河源区潜在蒸发量变化特征及影响因子分析[J].中国沙漠,2009,29(5):960-965.[30]王素萍,张存杰,韩永翔.甘肃省不同气候区蒸发量变化特征及其影响因子研究[J].中国沙漠,2010,30(3):675-680.[31]马国军,林栋,王万雄.石羊河流域水资源利用与经济发展系统分析[J].中国沙漠,2009,29(5):1003-1007.[32]郭承录,李发明.石羊河流域生态系统存在的问题及治理对策 [J].中国沙漠,2010,30(3):608-613.[33]马国军,刘君娣,林栋,等.石羊河流域水资源利用现状及生态环境效应[J].中国沙漠,2008,28(3):592-597.[34]赵翠莲,杨自辉,刘虎俊,等.石羊河流域水资源利用现状及生态环境效应[J].中国沙漠,2006,26(1):90-95.[35]林振山,邓自旺.子波气候诊断技术的研究[M].北京:气象出版社,1999:24-25.[36]施雅风; 沈永平,胡汝骥,等.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(2):219-226. |