[1] 夏军.水文尺度问题.水利学报,1993,24(5):32~37.[2] 刘贤赵,论水文尺度问题.干旱区地理,2004,27(1):61~65.[3] 丁晶,王文圣.水文相似和尺度分析.水电能源科学,2004,22(1):1~4.[4] Wood E F.Scale analyses for land-surface hydrology. In : Garrison Sposito, ed. Scale Dependence and Scale Invariance in Hydrology. Cambridge :Cambridge University Press,1998.1~29.[5] 陈军锋,李秀彬,张明.模型模拟梭磨河流域气候波动和土地覆被变化对流域水文的影响.中国科学D辑(地球科学).2004,34(7):668~674.[6] 袁艺,史培军.土地利用对流域降雨径流关系的影响——SCS 模型在深圳市的应用.北京师范大学学报(自然科学版),2001.37(1):131~136.[7] Bormann H, Fab T, Giertz S, et al.From local hydrological process analysis to regional hydrological model application in Benin: Concept, results and perspectives. Physics and Chemistry of the Earth,2005,30:347~356.[8] Stefan Uhlenbrook, Stefan Roser, Nils Tilch. Hydrological process representation at the meso-scale: The potential of a distributed, conceptual catchment model. Journal of Hydrology,2004, 291:278~296.[9] 王根绪,张钰,刘桂民,等. 马营河流域1967~2000 年土地利用变化对河流径流的影响. 中国科学D辑(地球科学).2005,35(7):671~681.[10] 冉圣宏,李秀彬,吕昌河.土地覆被及生态服务价值变化的多时间尺度模拟—以四川省渔子溪流域为例.地理学报,2006,61(10):1113~1120.[11] Justin P Wright, William S C Gurney,Clive G Jones.Patch dynamics in a landscape modified by ecosystem engineers. OIKOS,2004,105(2):336~348.[12] 尹国康.黄河中游多沙粗沙区水沙变化原因分析.地理学报,1998,53(2):184~183.[13] Aaron Yair, Naama Raz-Yassif.Hydrological processes in a small arid catchment: Scale effects of rainfall and slope length. Geomorphology,2004,61:155~169.[14] 陈军锋,张明.梭磨河流域气候波动和土地覆被变化对径流影响的模拟.地理研究,2003,22(1):73~78.[15] 李春晖,杨志峰.黄河流域NDVI时空变化及其与降水/径流关系.地理研究,2004,23(6):753~759.[16] 李双成,蔡运龙,地理尺度转换若干问题的初步探讨.地理研究,2005,24(1):11~18. |