Frost flowers and sea-salt aerosols over seasonal sea-ice areas in north-western Greenland

K. Hara, S. Matoba, M. Hirabayashi, Tetsuhide Yamasaki
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引用次数: 1

Abstract

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 watersoluble 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) SO2− 4 . 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 seasalt 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.
格陵兰岛西北部季节性海冰地区的霜花和海盐气溶胶
气溶胶、霜花和盐水中的海盐和卤素在极地大气化学中起着重要作用。2013年12月至2014年3月,在格陵兰西北部的Siorapaluk附近进行了霜花、盐水和气溶胶颗粒的同步采样和观测。结果表明,水溶性霜花和卤水组分主要为海盐组分(Na、Cl、Mg2+、K、Ca2+、Br和碘)。霜花和卤水的海盐组分相对于海水的浓度因子为1.14 ~ 3.67。霜花中Mg2+、K、Ca2+和卤素(Cl、Br和碘)的海盐富集与mirabilite和hydrohalite的沉淀对海盐的分馏有关。高气溶胶数浓度对应于海盐颗粒在粗态和细态中丰度较高的出现,以及吹雪和强风。在强风条件下,海冰表面的释放大大增加了气溶胶数量浓度,特别是在粗模式下。由于非海盐(NSS) SO2−4的存在,海盐分馏导致的硫酸盐耗竭在海盐气溶胶中受到限制。粗海盐和细海盐均富含镁元素。强Mg富集可能更倾向于在细海盐颗粒中进行。富镁海盐颗粒可能从海冰和霜花上的雪和泥层(盐水)表面释放出来。Mirabilite-like和ikite -like颗粒仅在新海冰区附近收集的气溶胶样本中被发现。根据现场证据和早期研究结果,我们提出并描述了季节性海冰区的海盐循环。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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