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Unexpected Response of High Alpine Lake Waters to Climate Warming

机译:高高山湖泊水域对气候变暖的意外反应

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Overthe past two decades, we have observed a substantial rise in solute concentration at two remote high mountain lakes in catchments of metamorphic rocks in the European Alps. At Rasass See, the electrical conductivity increased 18-fold. Unexpectedly high nickel concentrations at Rasass See, which exceeded the limit in drinking water by more than 1 order of magnitude, cannot be related to catchment geology. We attribute these changes in lake water quality to solute release from the ice of an active rock glacier in the catchment as a response to climate warming. Similar processes occurred at the higher elevation lake Schwarzsee ob Solden, where electrical conductivity has risen 3-fold during the past two decades.
机译:在过去的二十年中,我们观察到欧洲阿尔卑斯山变质岩流域中两个偏远的高山湖泊中的溶质浓度显着增加。在Rasass See,电导率增加了18倍。拉萨斯湖(Rasass See)的镍浓度出乎意料地高,超过饮用水中的限制超过1个数量级,这与集水区地质无关。我们将湖泊水质的这些变化归因于流域活跃岩石冰川冰中的溶质释放,以响应气候变暖。 Schwarzsee ob Solden高海拔湖也发生了类似的过程,在过去的二十年中,那里的电导率上升了三倍。

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