干旱区生态环境知识资源中心(Arid): 基于MODIS数据的无定河流域蒸散模拟

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	基于MODIS数据的无定河流域蒸散模拟
其他题名	Estimation of evapotranspiration over Wuding River Basin with an eco-hydrological model and MODIS data
	陈丹 1; 莫兴国 1; 林忠辉 1; 刘苏峡 2
ISSN	1000-0585
出版年	2006
卷号	25 期号:4 页码:617-623
中文摘要	利用黄土高原无定河流域水文气象资料、MODIS数据及GIS背景信息，应用分布式生态水文模型（VIP模型），按250m空间分辨率模拟了该流域水量平衡各分量的时空分布。结果表明：2000～2003年无定河流域年蒸散量分别为300mm、397mm、460mm和443mm；流域蒸散有明显的由南向北，由东到西的梯度递减特征，降水量和地表植被覆盖度的差异是其空间变异的主要因素；蒸腾与蒸发空间分异显著，但两者的变化相互补偿，降低了蒸散的空间变异性。整个流域平均而言，不同植被类型间的年蒸散总量差异不明显。白家川等9个子流域年蒸散量的模拟结果与水量平衡法估计结果具有较好的一致性。
英文摘要	A physically distributed eco-hydrological model （VIP model）, under support of Terra-MODIS remotely sensed vegetation index, land use and DEM data, is applied to simulate the temporal and spatial variation of evapotranspiration and other water balance components over the Wuding River Basin on the Loess Plateau, from 2000 to 2003. The spatial resolution of the simulation is 250 m and time step of 1 hour. The results show that the mean evapotranspiration is 300 mm, 397 mm, 460 mm and 443 mm in 2000, 2001, 2002 and 2003, respectively; the annual evapotranspiration amount is the main component of water budget and the evaporation value from soil is a bit larger than the canopy transpiration; evapotranspiration over the basin mainly occurred during summer time, which contributes more than 60 % of the annual amount; and the annual values of evapotranspiration from the vegetation types are similar, though their monthly processes are quite different. This is the common phenomenon in the semi-arid region. Over the whole basin, the annual amount of evapotranspiration and its components are decreasing gradually from the southeastern part to the northwestern part of the basin; the coefficient of variation of evaporation and transpiration is 30% and 14% respectively, whereas that of evapotranspiration is only 9 %0, due to the compensating effect of evaporation and transpiration. The simulated annual evapotranspiration values over the nine subbasins of the Wuding River Basin agree well with the evapotranspiration derived from water balance method, showing that the simulation results of VIP model are reasonable. The result from this study is valuable for assessing water conservation projects and serves as reference for re-vegetation policy making.
中文关键词	无定河流域 ; 蒸散 ; 水量平衡 ; VIP模型
英文关键词	NDVI Wuding River Basin evapotranspiration NDVI water balance VIP model
语种	中文
国家	中国
收录类别	CSCD
WOS类目	GEOSCIENCES MULTIDISCIPLINARY
WOS研究方向	Geology
CSCD记录号	CSCD:2472661
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/219530
作者单位	1.中国科学院, 中国科学院生态网络观测与模拟重点实验室, 北京 100101, 中国; 2.中国科学院, 陆地水循环及地表过程重点实验室, 北京 100101, 中国
推荐引用方式 GB/T 7714	陈丹,莫兴国,林忠辉,等. 基于MODIS数据的无定河流域蒸散模拟[J],2006,25(4):617-623.
APA	陈丹,莫兴国,林忠辉,&刘苏峡.(2006).基于MODIS数据的无定河流域蒸散模拟.,25(4),617-623.
MLA	陈丹,et al."基于MODIS数据的无定河流域蒸散模拟".25.4(2006):617-623.