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长期的降水和温度变化已经对氮负荷产生了影响。

Long-Term Changes in Precipitation and Temperature Have Already Impacted Nitrogen Loading.

机构信息

Department of Earth System Science , Stanford University , Stanford , California 94305 United States.

Department of Global Ecology , Carnegie Institution for Science , Stanford , California 94305 United States.

出版信息

Environ Sci Technol. 2019 May 7;53(9):5080-5090. doi: 10.1021/acs.est.8b06898. Epub 2019 Apr 23.

Abstract

Increases in nitrogen loading over the past several decades have led to widespread water quality impairments across the U.S. Elevated awareness of the influence of climate variability on nitrogen loading has led to several studies investigating future climate change impacts on water quality. However,  it remains unclear whether long-term climate impacts can already be observed in the historical record. Here, we quantify long-term trends in total nitrogen loading over the period 1987-2012 across the contiguous U.S. and attribute these trends to long-term changes in nitrogen inputs and climatic variables. We find that annual precipitation, extreme springtime precipitation, and springtime temperature are key drivers of trends in historical loading in most regions. These decadal climate trends have either  amplified or offset loading trends expected from nitrogen inputs alone. We also find that rising temperatures have been insufficient to offset precipitation-induced loading increases, suggesting that future increases in temperature under climate change may have limited potential to counteract loading increases expected as a result of anticipated changes in precipitation. This work demonstrates the important role of decadal climate variability in long-term nitrogen loading, emphasizing the need to consider climate change risks when designing and monitoring nutrient reduction programs.

摘要

在过去几十年中,氮负荷的增加导致美国各地的水质普遍受损。人们越来越意识到气候变异性对氮负荷的影响,这导致了几项研究调查未来气候变化对水质的影响。然而,长期气候影响是否已经可以在历史记录中观察到仍然不清楚。在这里,我们量化了 1987 年至 2012 年期间美国大陆地区总氮负荷的长期趋势,并将这些趋势归因于氮输入和气候变量的长期变化。我们发现,年降水量、极端春季降水量和春季温度是大多数地区历史负荷趋势的关键驱动因素。这些十年气候趋势要么放大了,要么抵消了仅由氮输入引起的负荷趋势。我们还发现,气温上升还不足以抵消降水引起的负荷增加,这表明气候变化下未来气温的升高可能难以抵消预期降水变化导致的负荷增加。这项工作表明了年代际气候变异性在长期氮负荷中的重要作用,强调在设计和监测养分减排计划时需要考虑气候变化风险。

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