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On the usefulness of remote sensing input data for spatially distributed hydrological modelling: case of the Tarim River basin in China

机译:论遥感输入数据在空间分布水文建模中的实用性-以中国塔里木河流域为例

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The ecological situation of the Tarim River basin in China seriously declined since the early 1950s, mainly due to a strong increase in water abstraction for irrigation purposes. To restore the ecological system and support sustainable development of the Tarim River basin region in China, more hydrological studies are demanded to properly understand the processes of the watershed and efficiently manage the water resources. Such studies are, however, complicated due to the limited data availability, especially in the mountainous headwater regions of the Tarim River basin. This study investigated the usefulness of remote sensing (RS) data to overcome that lack of data in the spatially distributed hydrological modelling of the basin. Complementary to the conventional station-based (SB) data, the RS products that are directly used in this study include precipitation, evapotranspiration and leaf area index. They are derived from raw image data of the Chinese Fengyun meteorological satellite and from the Moderate Resolution Imaging Spectroradiometer (MODIS). The MODIS land surface temperature was used to calculate the atmospheric temperature lapse rate to describe the temperature dependency on topographical variations. Moreover, MODIS-based snow cover images were used to obtain model initial conditions and as validation reference for the snow model component. Comparison of model results based on RS input versus conventional SB input exhibited similar results in terms of high and low river runoff extremes, cumulative runoff volumes in both runoff and snow melting seasons and spatial and temporal variability of snow cover. During summer time, when the snow cover shrinks in the permanent glacier region, it was found that the model resolution influences the model results dramatically, hence, showing the importance of detailed (RS based) spatially distributed input data. Copyright © 2011 John Wiley & Sons, Ltd.
机译:自1950年代初以来,中国塔里木河流域的生态状况严重下降,这主要归因于灌溉用水的大量增加。为了恢复塔里木河流域地区的生态系统并支持其可持续发展,需要开展更多的水文学研究以正确理解流域的过程并有效地管理水资源。但是,由于数据可用性有限,尤其是在塔里木河流域的山区源头地区,此类研究非常复杂。这项研究调查了遥感(RS)数据在克服流域空间分布水文模型中缺乏数据的有用性。与常规的基于站点的数据(SB)互补,本研究中直接使用的RS产品包括降水,蒸散和叶面积指数。它们来自中国风云气象卫星的原始图像数据和中分辨率成像光谱仪(MODIS)。 MODIS地表温度用于计算大气温度下降率,以描述温度对地形变化的依赖性。此外,基于MODIS的积雪图像被用于获取模型初始条件,并作为积雪模型组件的验证参考。比较基于RS输入和传统SB输入的模型结果,在高低径流径流量,径流量和融雪季节的累积径流量以及积雪的时空变化方面,显示出相似的结果。在夏季,当永久冰川区域的积雪缩小时,发现模型分辨率会极大地影响模型结果,因此显示出详细的(基于RS)空间分布输入数据的重要性。版权所有©2011 John Wiley&Sons,Ltd.

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