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Oceanic influence on atmospheric mercury at coastal and inland sites: a springtime noreaster in New England

机译:海洋对沿海和内陆地点的大气汞的影响:新英格兰的春季noreaster

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Continuous measurements of elemental (Hg0) and reactive mercury wereconducted at two sites in New Hampshire during a powerful April 2007noreaster. During the most intense period of the storm, enhancements of~30–50 ppqv in Hg0 were observed at a coastal and a highelevation inland site. This enhancement occurred simultaneously withelevated mixing ratios of three marine tracers, CH3I, CH2Br2and CHBr3. These observations suggest a marine source of Hg0,possibly outgassing from the ocean surface during strong turbulence. TheHg0 enhancement observed 100 km inland suggests that the impact ofcoastal storms on terrestrial Hg cycling may not be limited to near-shoreenvironments. Combining Hg0 and marine tracer measurements during thestorm with estimates of oceanic tracer fluxes during previous strong stormsyields an order-of-magnitude estimate of the oceanic source of Hg0during the storm (~7 ppqv h−1) which can account for theobserved enhancement at the field sites.
机译:2007年4月,在新罕布什尔州的一次强大的Noreaster演习中,连续进行了元素(Hg 0 )和活性汞的连续测量。在风暴最强烈的时期,在沿海和高海拔内陆地区观测到Hg 0 的〜30–50 ppqv增强。三种海洋示踪剂CH 3 I,CH 2 Br 2 和CHBr 3 。这些观察结果表明,Hg 0 的海洋来源,可能在强烈湍流时从海面释放出。内陆100 km观测到的Hg 0 增强表明,沿海风暴对陆地Hg循环的影响可能不仅限于近岸环境。将风暴期间的Hg 0 和海洋示踪剂测量值与先前强风暴期间的海洋示踪剂通量估计值相结合,可得出风暴期间Hg 0 的海洋来源的数量级估计值(〜7 ppqv h -1 ),这可以说明在现场站点上观察到的增强。

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