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Future Riverine Inorganic Nitrogen Load to the Baltic Sea From Sweden : An Ensemble Approach to Assessing Climate Change Effects

机译:从瑞典到波罗的海的未来河流无机氮负荷:评估气候变化影响的综合方法

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摘要

The dramatic increase of bioreactive nitrogen entering the Earth’s ecosystems continues toattract growing attention. Increasingly large quantities of inorganic nitrogen are flushed from land towater, accelerating freshwater, and marine eutrophication. Multiple, interacting, and potentiallycountervailing drivers control the future hydrologic export of inorganic nitrogen. In this paper, we attempt toresolve these land-water interactions across boreal/hemiboreal Sweden in the face of a changing climatewith help of a versatile modeling framework to maximize the information value of existing measurementtime series. We combined 6,962 spatially distributed water chemistry observations spread over 31 years withdaily streamflow and air temperature records. An ensemble of climate model projections, hydrologicalsimulations, and several parameter parsimonious regression models was employed to project future riverineinorganic nitrogen dynamics across Sweden. The median predicted increase in total inorganic nitrogenexport from Sweden (2061–2090) due to climate change was 14% (interquartile range 0–29%), based on theensemble of 7,500 different predictions for each study site. The overall export as well as the seasonal patternof inorganic nitrogen loads in a future climate are mostly influenced by longer growing seasons and morewinter flow, which offset the expected decline in spring flood. The predicted increase in inorganic nitrogenloading due to climate change means that the political efforts for reducing anthropogenic nitrogen inputsneed to be increased if ambitions for reducing the eutrophication of the Baltic Sea are to be achieved.
机译:进入地球生态系统的生物反应性氮的急剧增加继续吸引着越来越多的关注。越来越多的无机氮从陆地被冲刷到水中,加速淡水和海洋富营养化。多种,相互作用的和潜在的抵消驱动因素控制着未来无机氮的水文出口。在本文中,我们试图借助通用的建模框架来解决气候变化的情况下瑞典北部/半沿海地区的这些陆地与水之间的相互作用,从而最大化现有测量时间序列的信息价值。我们将分布在31年内的6,962个空间分布的水化学观测结果与每日的流量和气温记录相结合。一组气候模型预测,水文模拟和几个参数简约回归模型被用来预测整个瑞典未来的河床无机氮动态。根据每个研究地点的7,500种不同预测的合计,由于气候变化,瑞典(2061-2090年)出口的无机氮总量的中位数预测值为14%(四分位数范围为0-29%)。未来气候中无机氮负荷的整体出口以及季节性模式主要受到生长季节的延长和冬季流量的增加的影响,这抵消了春季洪水预期的减少。预计由于气候变化而导致的无机氮负荷的增加意味着,要实现减少波罗的海富营养化的雄心,就必须加大减少人为氮输入的政治努力。

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