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Improving AVSWAT Stream Flow Simulation by Incorporating Groundwater Recharge Prediction in the Upstream Lesti Watershed, East Java, Indonesia

机译:通过结合印度尼西亚东爪哇省勒斯蒂上游流域的地下水补给量预测来改进AVSWAT流模拟

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摘要

The upstream Lesti watershed is one of the major watersheds of East Java in Indonesia, covering about 38093 hectares. Although there are enough water resources to meet current demands in the basin, many challenges including high spatial and temporal variability in precipitation from year to year exist. It is essential to understand how the climatic condition affects Lesti River stream flow in each sub basin. This study investigated the applicability of using the Soil and Water Assessment Tool (SWAT) with the incorporation of groundwater recharge prediction in stream flow simulation in the upstream Lesti watershed. Four observation wells in the upstream Lesti watershed were used to evaluate the seasonal and annual variations in the water level and estimate the groundwater recharge in the deep aquifer. The results show that annual water level rise was within the 2800 - 5700 mm range in 2007, 3900 - 4700 mm in 2008, 3200 - 5100 mm in 2009, and 2800 - 4600 mm in 2010. Based on the specific yield and the measured water level rise, the area-weighted groundwater predictions at the watershed outlet are 736, 820.9, 786.7, 306 4 mm in 2007, 2008, 2009, and 2010, respectively. The consistency test reveals that the R-square statistical value is greater than 0.7, and the DV (%) ranged from 32 - 55.3% in 2007 - 2010. Overall, the SWAT model performs better in the wet season flow simulation than the dry season. It is suggested that the SWAT model needs to be improved for stream flow simulation in tropical regions.
机译:上游Lesti流域是印度尼西亚东爪哇省的主要流域之一,占地约38093公顷。尽管流域有足够的水资源来满足当前的需求,但仍存在许多挑战,包括每年降水量的高时空变化。了解气候条件如何影响每个子流域的勒斯蒂河水流至关重要。这项研究调查了将土壤和水评估工具(SWAT)与地下水补给预测结合用于上游Lesti流域的水流模拟中的适用性。上游Lesti流域的四个观测井用于评估水位的季节和年度变化,并估算深层含水层中的地下水补给量。结果表明,2007年的年度水位上升幅度在2800-5700 mm范围内,2008年为3900-4700 mm,2009年为3200-5100 mm,2010年为2800-4600 mm。基于比产量和测得的水随着水位的上升,流域出口处的加权面积地下水预测值在2007年,2008年,2009年和2010年分别为736、820.9、786.7、306 4 mm。一致性测试显示,R平方统计值大于0.7,并且DV(%)在2007年-2010年的范围为32-55.3%。总体而言,SWAT模型在雨季流量模拟中的表现要好于旱季。 。建议为热带地区的水流模拟需要改进SWAT模型。

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