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

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...

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Main Authors: K. Hara, S. Matoba, M. Hirabayashi, T. Yamasaki
Format: Article
Language:English
Published: Copernicus Publications 2017-07-01
Series:Atmospheric Chemistry and Physics
Online Access:https://www.atmos-chem-phys.net/17/8577/2017/acp-17-8577-2017.pdf
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spelling doaj-63f5807d6bf24eae9512520ff7377b0b2020-11-24T23:46:58ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242017-07-01178577859810.5194/acp-17-8577-2017Frost flowers and sea-salt aerosols over seasonal sea-ice areas in northwestern Greenland during winter–springK. Hara0S. Matoba1M. Hirabayashi2T. Yamasaki3Department of Earth System Science, Faculty of Science, Fukuoka University, Fukoka, JapanInstitute of Low Temperature Science, Hokkaido University, Hokkaido, JapanNational Institute of Polar Research, Tokyo, JapanAvangnaq, Osaka, JapanSea 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<sup>+</sup>, Cl<sup>−</sup>, Mg<sup>2+</sup>, K<sup>+</sup>, Ca<sup>2+</sup>, Br<sup>−</sup>, 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 Mg<sup>2+</sup>, K<sup>+</sup>, Ca<sup>2+</sup>, and halogens (Cl<sup>−</sup>, Br<sup>−</sup>, 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) SO<sub>4</sub><sup>2−</sup>. 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.https://www.atmos-chem-phys.net/17/8577/2017/acp-17-8577-2017.pdf
collection DOAJ
language English
format Article
sources DOAJ
author K. Hara
S. Matoba
M. Hirabayashi
T. Yamasaki
spellingShingle K. Hara
S. Matoba
M. Hirabayashi
T. Yamasaki
Frost flowers and sea-salt aerosols over seasonal sea-ice areas in northwestern Greenland during winter–spring
Atmospheric Chemistry and Physics
author_facet K. Hara
S. Matoba
M. Hirabayashi
T. Yamasaki
author_sort K. Hara
title Frost flowers and sea-salt aerosols over seasonal sea-ice areas in northwestern Greenland during winter–spring
title_short Frost flowers and sea-salt aerosols over seasonal sea-ice areas in northwestern Greenland during winter–spring
title_full Frost flowers and sea-salt aerosols over seasonal sea-ice areas in northwestern Greenland during winter–spring
title_fullStr Frost flowers and sea-salt aerosols over seasonal sea-ice areas in northwestern Greenland during winter–spring
title_full_unstemmed Frost flowers and sea-salt aerosols over seasonal sea-ice areas in northwestern Greenland during winter–spring
title_sort frost flowers and sea-salt aerosols over seasonal sea-ice areas in northwestern greenland during winter–spring
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2017-07-01
description 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<sup>+</sup>, Cl<sup>−</sup>, Mg<sup>2+</sup>, K<sup>+</sup>, Ca<sup>2+</sup>, Br<sup>−</sup>, 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 Mg<sup>2+</sup>, K<sup>+</sup>, Ca<sup>2+</sup>, and halogens (Cl<sup>−</sup>, Br<sup>−</sup>, 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) SO<sub>4</sub><sup>2−</sup>. 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.
url https://www.atmos-chem-phys.net/17/8577/2017/acp-17-8577-2017.pdf
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