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Impacts of Climate and Land Use/Cover Change on Streamflow Using SWAT and a Separation Method for the Xiying River Basin in Northwestern China

机译:西北地区西营河流域的SWAT和分离方法对气候和土地利用/覆盖变化对径流的影响

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A better understanding of the effects of climate change and land use/cover change (LUCC) on streamflow promotes the long-term water planning and management in the arid regions of northwestern China. In this paper, the Soil and Water Assessment Tool (SWAT) and a separation approach were used to evaluate and separate the effects of climate change and LUCC on streamflow in the Xiying River basin. The SWAT model was calibrated by the hydro-meteorological data from 1980–1989 to obtain the optimum parameters, which were validated by the subsequent application to the period between 1990–2008. Moreover, streamflow under several scenarios with different climate change and land use conditions in 1990–2008 and 2010–2069 were further investigated. Results indicate that, in the period of 1990–2008, the streamflow was dominated by climate change ( i.e. , changes in precipitation and temperature), which led to a 102.8% increase in the mean annual streamflow, whereas LUCC produced a decrease of 2.8%. Furthermore, in the future period of 2010–2039, the mean annual streamflow will decrease by 5.4% and 4.5% compared with the data of 1961–1990 under scenarios A2 and B2, respectively, while it will decrease by 21.2% and 16.9% in the period of 2040–2069, respectively.
机译:更好地了解气候变化和土地利用/覆被变化(LUCC)对径流的影响,可以促进中国西北干旱地区的长期水资源规划和管理。本文利用土壤水评估工具(SWAT)和分离方法来评估和分离气候变化和LUCC对西营河流域水流的影响。利用1980-1989年的水文气象数据对SWAT模型进行了校准,以获得最佳参数,随后对1990-2008年这一时期的应用验证了最优参数。此外,还进一步研究了1990-2008年和2010-2069年在不同气候变化和土地利用条件下的几种情景下的径流。结果表明,在1990-2008年期间,河流流量主要受气候变化(即降水和温度的变化)的影响,导致年平均流量增加102.8%,而LUCC减少了2.8%。 。此外,在情景A2和情景B2下,与1961-1990年的数据相比,在2010-2039年的未来年平均年流量将分别减少5.4%和4.5%,而在情景A2和B2下将分别减少21.2%和16.9%。分别为2040年至2069年。

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