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Changes in groundwater drought associated with anthropogenic warming

机译:与人为变暖相关的地下水干旱变化

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Here we present the first empirical evidence for changes in groundwater drought associated with anthropogenic warming in the absence of long-term changes in precipitation. Analysing standardised indices of monthly groundwater levels, precipitation and temperature, using two unique groundwater level data sets from the Chalk aquifer, UK, for the period 1891 to 2015, we show that precipitation deficits are the main control on groundwater drought formation and propagation. However, long-term changes in groundwater drought are shown to be associated with anthropogenic warming over the study period. These include increases in the frequency and intensity of individual groundwater drought months, and increases in the frequency, magnitude and intensity of episodes of groundwater drought, as well as an increasing tendency for both longer episodes of groundwater drought and for an increase in droughts of less than 1 year in duration. We also identify a transition from a coincidence of episodes of groundwater drought with precipitation droughts at the end of the 19th century, to an increasing coincidence with both precipitation droughts and with hot periods in the early 21st century. In the absence of long-term changes in precipitation deficits, we infer that the changing nature of groundwater droughts is due to changes in evapotranspiration (ET) associated with anthropogenic warming. We note that although the water tables are relatively deep at the two study sites, a thick capillary fringe of at least 30 m in the Chalk means that ET should not be limited by precipitation at either site. ET may be supported by groundwater through major episodes of groundwater drought and, hence, long-term changes in ET associated with anthropogenic warming may drive long-term changes in groundwater drought phenomena in the Chalk aquifer. Given the ex-tent of shallow groundwater globally, anthropogenic warming may widely effect changes to groundwater drought characteristics in temperate environm
机译:在这里,我们在没有长期的降水变化的情况下,我们提出了与人为升温相关的地下水干旱变化的第一证据。分析每月地下水位,降水量和温度的标准化指数,英国粉笔含水层的两个独特地下水位数据套装,展示了1891年至2015年,我们表明降水缺陷是地下水干旱形成和传播的主要控制。然而,地下水干旱的长期变化显示在研究期间与人为温暖有关。这些包括增加各个地下水干旱月份的频率和强度,并且地下水干旱发作的频率,幅度和强度的增加,以及对地下水干旱的较长发作的越来越大的趋势以及较少的干旱增加超过1年的持续时间。在19世纪末,我们还确定了从地下水干旱与降水干旱的巧合的转型,以增加两世纪初期的降水干旱和炎热的时期。在没有长期的降水缺陷变化的情况下,我们推断地下水干旱的变化性质是由于与人为变暖相关的蒸发(ET)的变化。我们注意到,尽管水表在两种研究部位相对深,但粉笔中的厚毛细管条纹至少为30μm意味着ET不应受到任一位点沉淀的限制。通过地下水来支持地下水通过地下水干旱的主要发作来支持,因此,与人为变暖的ET的长期变化可能会驱动白垩含水层的地下水干旱现象的长期变化。鉴于全球浅层地下水的出帐篷,人为变暖可能在温带环境中对地下水干旱特性的显着影响

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