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20-Year Climatology of NO_-~3 and NH_4~+ Wet Deposition at Ny-Alesund, Svalbard

机译:斯瓦尔巴特群岛Ny-Alesund的NO_- ~~ 3和NH_4〜+湿沉降的20年气候学

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摘要

A 20-year dataset of weekly precipitation observations in Ny-Alesund, Svalbard, was analysed to assess atmospheric wet deposition of nitrogen. Mean annual total nitrogen deposition was 74 mg N/(m2 yr) but exhibited large interannual variability and was dominated by highly episodic "strong" events, probably caused by rapid transport from European sources. The majority (90%) of precipitation samples were defined as "weak" (<2mgN/m~2) and contributed an annual baseline of ~17 mg N/(m~2 yr), whereas 10% of precipitation samples were defined as "strong"(>2mgN/m~2) and additionally contributed up to 225 mg N/(m~2 yr). Nitrate deposition largely occurred in samples within the solid-precipitation season (16 September–2 June), and ammonium deposition occurred equally in both solid and liquid seasons. Trends of reactive nitrogen emissions from Europe are uncertain, and increasing cyclonic activity over the North Atlantic caused by a changing climate might lead to more strong deposition events in Svalbard.
机译:分析了斯瓦尔巴特群岛Ny-Alesund的20年每周降水观测数据集,以评估大气中的湿法氮沉降。年平均总氮沉积量为74 mg N /(m2 yr),但年际变化较大,并且以高度间歇性的“强”事件为主,这很可能是由于欧洲来源的​​快速运输所致。大部分(90%)的降水样品被定义为“弱”(<2mgN / m〜2),并贡献了每年基线〜17 mg N /(m〜2年),而10%的降水样品被定义为“弱”。 “强”(> 2mgN / m〜2),另外贡献高达225 mg N /(m〜2年)。硝酸盐沉淀主要发生在固体沉淀季节(9月16日至6月2日)内,铵盐沉淀在固体和液体季节均发生。来自欧洲的反应性氮排放趋势尚不确定,由于气候变化而引起的北大西洋气旋活动的增加可能导致斯瓦尔巴特群岛发生更强烈的沉积事件。

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