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Oasis Irrigation-Induced Hydro-Climatic Effects: A Case Study in the Hyper-Arid Region of Northwest China

机译:绿洲灌溉引起的水文气候效应:以西北高干旱地区为例

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The response of potential evapotranspiration (ET0) to widespread irrigation is important to fully understand future regional climate changes and to infer adaptive management of agricultural water resources. The quantitative impact of irrigation on ET0 from 1960 to 2013 was evaluated using historical time series data of daily meteorological observations in the hyper-arid region of northwest China. The decreasing trends in ET0 were accelerated for meteorological stations in regions with oasis agriculture, especially in the summer and during the growing season. Irrigation led to a cooling effect on temperature, increased relative humidity and precipitation. All of these changes contributed to a larger decrease of ET0 trend. The findings of this study advance our insight into the effects of irrigation on dynamics in ET0 and meteorological factors. Further investigations to understand how ET0 responds to climate change and agricultural irrigation could provide guidance for determining effective measures of water resources for adapting to global change.
机译:对广泛灌溉的潜在蒸散量(ET0)的响应对于充分了解未来的区域气候变化以及推断农业水资源的适应性管理非常重要。利用西北高干旱地区每日气象观测的历史时间序列数据,评估了1960年至2013年灌溉对ET0的定量影响。对于绿洲农业地区的气象站,ET0的下降趋势加速了,特别是在夏季和生长季节。灌溉导致温度下降,相对湿度和降水增加。所有这些变化导致了ET0趋势的较大下降。这项研究的结果使我们深入了解了灌溉对ET0动态和气象因素的影响。进一步的调查以了解ET0如何应对气候变化和农业灌溉可以为确定水资源的有效措施以适应全球变化提供指导。

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