[1] 雍斌, 张万昌, 刘传胜. 水文模型与陆面模式耦合研究进展. 冰川冻土, 2006, 28(6): 269-079.[2] 黄洪峰. 土壤植物大气相互作用原理及模拟研究. 北京: 气象出版社, 1997.[3] 李润奎, 朱阿兴, 李宝林,等. 流域水文模型对土壤数据响应的多尺度分析. 地理科学进展, 2011, 30(1): 80-86.[4] 陈腊娇, 朱阿兴, 秦承志, 等. 流域生态水文模型研究进展. 地理科学进展, 2011, 30(5): 535-544.[5] Chen F, Mitchell K E, Schaake J, et al. Modeling of landsurfaceevaporation by four schemes and comparisonwith FIFE observations. Journal of Geophysical Research,1996, 101(D3): 7251-7268.[6] Chen F, Janic Z, Mitchell K E. Impact of atmospheric surfacelayer parameterizations in the new land-surfacescheme of the NCEP mesoscale Eta model. Bound-LayerMeteorology, 1997, 85(3): 391-421.[7] Chen F, Mitchell K E. Using the GEWEX/ISLSCP forcingdata to simulate global soil moisture fields and hydrologicalcycle for 1987-1988. Journal of MeteorologicalSociety of Japan, 1999, 77(1B): 167-182.[8] Wood E F, Lettenmaier D P, Liang X, et al. The projectfor intercomparison of land-surface parameterizationschemes (PILPS) phase 2(c) Red-Arkanss river basin experiment:1. Experiment description and summary intercomparisons.Global and Planetary Change, 1998, 19(1-4): 115-135.[9] Mahrt L, and Michael E K. The influence of atmosphericstability on potential evaporation. Journal of Climate AppliedMeteorology, 1984, 23(2): 222-234.[10] Pan H L. A two-layer model of soil hydrology.Bound.-Layer Meteorology, 1984, 29(1): 1-20.[11] Richard E, Mascart P. The influence of soil and vegetationon the development of mesoscale circulations. Journalof Climate Applied .Meteorology, 1987, 26(11):1483-1495.[12]高艳红, 程国栋, 崔文瑞, 等. 陆面水文过程与大气模式的耦合及其在黑河流域的应用. 地球科学进展, 2006,21(12): 1283-1292.[13] Schaake J C, Koren V I, Duan Q Y, et al. A simple waterbalance model (SWB) for estimating runoff at differentspatial and temporal scales. Journal of Geophysical Research,1996, 101(D3): 7461-7475.[14] Betts A K, Chen F, Mitchell K E, et al. Assessment of theland-surface and boundary-layer models in two operationalversions of the NCEP Eta model using FIFE data.MonthlyWeather Review, 1997, 125(11): 2896-2916.[15] 陈莹莹, 施建成, 杜今阳, 等. 基于GLDAS 的中国区地表能量平衡数值试验. 水科学进展, 2009, 20(1): 25-31.[16] 褚健婷, 夏军, 许崇育. 气候变化条件下海河流域日降水统计降尺度研究. 自然资源学报, 2008, 23(6): 1068-1077.[17] Gutman G, Ignatov A. The derivation of the green vegetationfraction from NOAA/AVHRR data for use in numericalweather prediction models. International. Journal ofRemote Sensing, 1998, 19(8): 1533-1543.[18] Hansen M C, Defries R S, Townshendj R G, et al. Globalland cover classification at 1km spatial resolution using aclassification tree approach. International. Journal of RemoteSensing, 2000, 21(6-7): 1331-1364.[19] 孙晓敏, 袁国富, 朱治林, 等. 生态水文过程观测与模拟的发展与展望. 地理科学进展, 2010, 29(11):1293-1300.[20]李俊, 于强, 孙晓敏, 等. 华北平原农田生态系统碳交换及其环境调控机制. 中国科学: D辑, 2006, 36(增刊Ⅰ):210-223.[21]伏玉玲, 于贵瑞, 王艳芬, 等. 水分胁迫对内蒙古羊草草原生态系统光合和呼吸作用的影响. 中国科学: D 辑,2006, 36(增刊Ⅰ): 183-193. |