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Recent trends of groundwater temperatures in Austria

机译:奥地利地下水温度的最新趋势

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Climate change is one of if not the most pressing challenge modern society faces. Increasing temperatures are observed all over the planet and the impact of climate change on the hydrogeological cycle has long been shown. However, so far we have insufficient knowledge on the influence of atmospheric warming on shallow groundwater temperatures. While some studies analyse the implication climate change has for selected wells, large-scale studies are so far lacking. Here we focus on the combined impact of climate change in the atmosphere and local hydrogeological conditions on groundwater temperatures in 227 wells in Austria, which have in part been observed since 1964. A linear analysis finds a temperature change of +0.7 +/- 0.8 K in the years from 1994 to 2013. In the same timeframe surface air temperatures in Austria increased by 0.5 +/- 0.3 K, displaying a much smaller variety. However, most of the extreme changes in groundwater temperatures can be linked to local hydrogeological conditions. Correlation between groundwater temperatures and nearby surface air temperatures was additionally analysed. They vary greatly, with correlation coefficients of 0.3 in central Linz to 0.8 outside of Graz. In contrast, the correlation of nationwide groundwater temperatures and surface air temperatures is high, with a correlation coefficient of 0.83. All of these findings indicate that while atmospheric climate change can be observed in nationwide groundwater temperatures, individual wells are often primarily dominated by local hydrogeological conditions. In addition to the linear temperature trend, a step-wise model was also applied that identifies climate regime shifts, which were observed globally in the late 70s, 80s, and 90s. Hinting again at the influence of local conditions, at most 22 % of all wells show these climate regime shifts. However, we were able to identify an additional shift in 2007, which was observed by 37 % of all wells. Overall, the step-wise representation
机译:气候变化是如果不是最紧迫的挑战现代社会面临的挑战之一。在地球上观察到越来越多的温度,长期以来已经显示了气候变化对水文循环的影响。然而,到目前为止,我们对大气升温对浅层地下水温度的影响不足。虽然一些研究分析了所选井的含义气候变化,但大规模研究缺乏。在这里,我们专注于气候变化在奥地利227孔的地下水温度下对地下水温度的综合影响,自1964年以来一直观察到。线性分析发现+0.7 +/- 0.8 k的温度变化从1994年到2013年的几年。在奥地利的相同时间范围内,奥地利的气温增加0.5 +/- 0.3克,呈现更小的品种。然而,地下水温度的大部分极端变化都可以与当地的水文地质条件相关联。另外分析了地下水温度与附近表面空气温度之间的相关性。它们的差异很大,相关系数为0.3,中央林茨中的0.8到格拉茨以外的0.8。相反,全国地下水温度和表面空气温度的相关性高,相关系数为0.83。所有这些发现表明,虽然在全国地下水温度下可以观察到大气气候变化,但个体井通常主要由当地水文地质条件占主导地位。除了线性温度趋势之外,还应用了一种阶跃模型,其识别气候制度偏移,在70年代后期,80s和90年代在全球中观察到。再次暗示当地条件的影响,最多22%的井都显示出这些气候政权转变。但是,我们能够在2007年确定额外的班次,观察到所有井的37%。总的来说,逐步表示

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