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Recovery from episodic acidification delayed by drought and high sea salt deposition

机译:从干旱和高海盐沉积推迟的间歇性酸化中恢复

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For the prediction of episodic acidification large uncertainties areconnected to climatic variability and its effect on drought conditions andsea-salt episodes. In this study data on 342 hydrological episodes in 25Swedish streams, sampled over 10 years, have been analyzed using a recentlydeveloped episode model. The results demonstrate that drought is the mostimportant factor modulating the magnitude of the anthropogenic influence onpH and ANC during episodes. These modulating effects are especiallypronounced in southern and central Sweden, where the historically high aciddeposition has resulted in significant S pools in catchment soils. Theresults also suggest that the effects of episodic acidification are becomingless severe in many streams, but this amelioration is less clear in coastalstreams subject to high levels of sea-salt deposition. Concurrently with theamelioration of the effects of episodic acidification, regional climatemodels predict that temperatures will increase in Sweden during the comingdecades, accompanied by reductions in summer precipitation and more frequentstorms during fall and winter in large areas of the country. If thesepredictions are realized delays in streams' recovery from episodicacidification events can be expected.
机译:为了预测间歇性酸化,将很大的不确定性与气候变化及其对干旱条件和海盐事件的影响联系在一起。在这项研究中,使用最近开发的情节模型分析了25个瑞典河流中342个水文情节的数据,这些数据是在10年中采样的。结果表明,干旱是调节发作期间人为因素对pH和ANC影响程度的最重要因素。这些调节作用在瑞典南部和中部尤为明显,那里历史上的高酸沉积导致集水区土壤中形成大量的S库。结果还表明,在许多河流中,突发性酸化的影响变得不那么严重,但这种减轻作用在受到海盐沉积水平高的沿海河流中却并不明显。伴随着突发性酸化作用的改善,区域气候模型预测瑞典将在未来的几十年内升高温度,伴随着夏季降水的减少以及该国大部分地区秋季和冬季的暴风雨更加频繁。如果实现了这些预测,则可以预期流从间歇酸化事件中恢复的延迟。

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