基于qswat模型的湿润热带高原流域水文行为研究

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摘要

一个地区的水资源规划和管理需要了解该地区的水平衡。本文利用带有QGIS接口的水土评价工具(SWAT)对喀拉拉邦瓦拉帕塔纳姆河流域Palapuzha流域的水平衡成分进行了分析。瓦拉帕塔南河的流域面积为1867平方公里。面积456平方公里。卡纳塔克邦的一个地区。该流域年平均降雨量为3600毫米。帕拉普扎流域的流域面积为237.25平方公里。公里,年平均降雨量4562毫米。QSWAT模型已经使用8年(2000-2007)的数据进行了校准和验证,这8年的降水和河流流量数据都是可用的。该模型在标定期和验证期成功模拟了月流量,Nash Sutcliffe效率和相关系数均大于0.75,百分比偏差小于10%,表明该模型对Valapattanam河流域的月流量具有较好的预测效果。利用该校准模型计算了帕拉普扎流域不同的水平衡分量。研究结果将为高原热带湿润流域水资源系统的可持续发展和规划提供参考
本文章由计算机程序翻译,如有差异,请以英文原文为准。
HYDROLOGIC BEHAVIOUR OF HIGHLAND CATCHMENT IN HUMID TROPICAL REGION USING QSWAT MODEL
Water resources planning and management of a region requires an understanding of the water balance in the region. The Soil and Water Assessment Tool (SWAT) with QGIS interface (QSWAT) has been used here to arrive at the water balance components in the Palapuzha watershed of Valapattanam river basin in Kerala. Valapattanam river drains an area of 1867 sq.km. with 456 sq.km. area in Karnataka State. The river basin receives an average annual rainfall of 3600 mm. The Palapuzha watershed drains an area of 237.25 sq.km with an average annual rainfall of 4562 mm. The QSWAT model has been calibrated and validated using data for a period of eight years (2000-2007) for which both rainfall and streamflow data are available. The model was successful in simulating monthly streamflow during the calibration and validation periods with Nash Sutcliffe efficiency and correlation co-efficient greater than 0.75 and percent bias less than 10%, showing that the model is very good for predicting streamflow in Valapattanam river basin. This calibrated model was used to arrive at the different water balance components in the Palapuzha watershed. The results obtained will be useful for the sustainable development and planning of the water resources system in the highland humid tropical watersheds
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