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Frost flowers and sea-salt aerosols over seasonal sea-ice areas in northwestern Greenland during winter–spring

机译:霜花和海盐雾化在季节性海冰区域在冬天春天的西北格陵兰岛

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Sea salts and halogens in aerosols, frost flowers, and brine play an important role in atmospheric chemistry in polar regions. Simultaneous sampling and observations of frost flowers, brine, and aerosol particles were conducted around Siorapaluk in northwestern Greenland during December 2013 to March 2014. Results show that water-soluble frost flower and brine components are sea-salt components (e.g., Na+, Cl?, Mg2+, K+, Ca2+, Br?, and iodine). Concentration factors of sea-salt components of frost flowers and brine relative to seawater were 1.14–3.67. Sea-salt enrichment of Mg2+, K+, Ca2+, and halogens (Cl?, Br?, and iodine) in frost flowers is associated with sea-salt fractionation by precipitation of mirabilite and hydrohalite. High aerosol number concentrations correspond to the occurrence of higher abundance of sea-salt particles in both coarse and fine modes, and blowing snow and strong winds. Aerosol number concentrations, particularly in coarse mode, are increased considerably by release from the sea-ice surface under strong wind conditions. Sulfate depletion by sea-salt fractionation was found to be limited in sea-salt aerosols because of the presence of non-sea-salt (NSS) SO42?. However, coarse and fine sea-salt particles were found to be rich in Mg. Strong Mg enrichment might be more likely to proceed in fine sea-salt particles. Magnesium-rich sea-salt particles might be released from the surface of snow and slush layer (brine) on sea ice and frost flowers. Mirabilite-like and ikaite-like particles were identified only in aerosol samples collected near new sea-ice areas. From the field evidence and results from earlier studies, we propose and describe sea-salt cycles in seasonal sea-ice areas.
机译:在气溶胶,霜花和盐水中的海盐和卤素在极地地区的大气化学中发挥着重要作用。 2013年12月至2014年3月,在格陵兰州西北部的Siorapaluk周围进行同时取样和观察。结果表明,水溶性霜花和盐水组分是海盐组分(例如,Na +,Cl? ,mg2 +,k +,ca2 +,br?,碘)。相对于海水霜花和盐水海盐成分的浓度因素为1.14-3.67。 Mg2 +,K +,Ca2 +和卤素花中的富含Mg2 +,K +,Ca2 +和卤素(Cl-3 Brα,和碘)与Mirabilite和氢卤石沉淀的海盐分馏有关。高气溶胶数浓度对应于粗糙和精细模式中较高丰富的海盐颗粒,吹雪和强风。通过在强风条件下从海冰表面释放,气溶胶数浓度,特别是粗糙模式的浓度显着增加。由于非海盐(NSS)SO42的存在,发现海盐分馏的硫酸盐耗尽被发现在海盐气溶胶中受到限制。然而,发现粗糙和精细的海盐颗粒富含Mg。强烈的Mg富集可能更有可能进行细盐颗粒。富含镁的海盐颗粒可能从雪地和泥土层(盐水)的表面释放出海冰和霜花。仅在新的海冰区域收集的气溶胶样品中鉴定了mirabilite样和易象颗粒。从现场证据和结果来自早期研究,我们提出并描述了季节性海冰区的海盐周期。

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