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Frost flowers growing in the Arctic ocean‐atmosphere–sea ice–snow interface: 1. Chemical composition

Identifieur interne : 002075 ( Istex/Corpus ); précédent : 002074; suivant : 002076

Frost flowers growing in the Arctic ocean‐atmosphere–sea ice–snow interface: 1. Chemical composition

Auteurs : Thomas A. Douglas ; Florent Domine ; Manuel Barret ; Cort Anastasio ; Harry J. Beine ; Jan Bottenheim ; Amanda Grannas ; Stephan Houdier ; Stoyka Netcheva ; Glenn Rowland ; Ralf Staebler ; Alexandra Steffen

Source :

RBID : ISTEX:4BA967A5C932EEC0AFE20E0FEDDD4E33BC41A150

Abstract

Frost flowers, intricate featherlike crystals that grow on refreezing sea ice leads, have been implicated in lower atmospheric chemical reactions. Few studies have presented chemical composition information for frost flowers over time and many of the chemical species commonly associated with Polar tropospheric reactions have never been reported for frost flowers. We undertook this study on the sea ice north of Barrow, Alaska to quantify the major ion, stable oxygen and hydrogen isotope, alkalinity, light absorbance by soluble species, organochlorine, and aldehyde composition of seawater, brine, and frost flowers. For many of these chemical species we present the first measurements from brine or frost flowers. Results show that major ion and alkalinity concentrations, stable isotope values, and major chromophore (NO3− and H2O2) concentrations are controlled by fractionation from seawater and brine. The presence of these chemical species in present and future sea ice scenarios is somewhat predictable. However, aldehydes, organochlorine compounds, light absorbing species, and mercury (part 2 of this research and Sherman et al. (2012)) are deposited to frost flowers through less predictable processes that probably involve the atmosphere as a source. The present and future concentrations of these constituents in frost flowers may not be easily incorporated into future sea ice or lower atmospheric chemistry scenarios. Thinning of Arctic sea ice will likely present more open sea ice leads where young ice, brine, and frost flowers form. How these changing ice conditions will affect the interactions between ice, brine, frost flowers and the lower atmosphere is unknown.

Url:
DOI: 10.1029/2011JD016460

Links to Exploration step

ISTEX:4BA967A5C932EEC0AFE20E0FEDDD4E33BC41A150

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<p xml:id="jgrd17498-para-0001" label="1">Frost flowers, intricate featherlike crystals that grow on refreezing sea ice leads, have been implicated in lower atmospheric chemical reactions. Few studies have presented chemical composition information for frost flowers over time and many of the chemical species commonly associated with Polar tropospheric reactions have never been reported for frost flowers. We undertook this study on the sea ice north of Barrow, Alaska to quantify the major ion, stable oxygen and hydrogen isotope, alkalinity, light absorbance by soluble species, organochlorine, and aldehyde composition of seawater, brine, and frost flowers. For many of these chemical species we present the first measurements from brine or frost flowers. Results show that major ion and alkalinity concentrations, stable isotope values, and major chromophore (NO
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<affiliation>Air Quality Research Division, Environment Canada, Toronto, Ontario, Canada</affiliation>
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<name type="personal">
<namePart type="given">Amanda</namePart>
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<affiliation>Department of Chemistry, Villanova University, Villanova, Pennsylvania, USA</affiliation>
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<name type="personal">
<namePart type="given">Stephan</namePart>
<namePart type="family">Houdier</namePart>
<affiliation>Laboratoire de Glaciologie et Géophysique de l'Environnement, CNRS-INSU and Université Joseph Fourier-Grenoble I, Saint-Martin d'Hères, France</affiliation>
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<name type="personal">
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<namePart type="family">Netcheva</namePart>
<affiliation>Air Quality Research Division, Environment Canada, Toronto, Ontario, Canada</affiliation>
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<name type="personal">
<namePart type="given">Glenn</namePart>
<namePart type="family">Rowland</namePart>
<affiliation>Department of Chemistry, Villanova University, Villanova, Pennsylvania, USA</affiliation>
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<name type="personal">
<namePart type="given">Ralf</namePart>
<namePart type="family">Staebler</namePart>
<affiliation>Air Quality Research Division, Environment Canada, Toronto, Ontario, Canada</affiliation>
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<name type="personal">
<namePart type="given">Alexandra</namePart>
<namePart type="family">Steffen</namePart>
<affiliation>Air Quality Research Division, Environment Canada, Toronto, Ontario, Canada</affiliation>
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<publisher>Blackwell Publishing Ltd</publisher>
<dateIssued encoding="w3cdtf">2012-07-27</dateIssued>
<dateCaptured encoding="w3cdtf">2011-06-23</dateCaptured>
<dateValid encoding="w3cdtf">2011-12-15</dateValid>
<edition>Douglas, T. A., et al. (2012), Frost flowers growing in the Arctic ocean‐atmosphere–sea ice–snow interface: 1. Chemical composition, J. Geophys. Res., 117, D00R09, doi:10.1029/2011JD016460.</edition>
<copyrightDate encoding="w3cdtf">2012</copyrightDate>
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<languageTerm type="code" authority="iso639-2b">eng</languageTerm>
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<abstract>Frost flowers, intricate featherlike crystals that grow on refreezing sea ice leads, have been implicated in lower atmospheric chemical reactions. Few studies have presented chemical composition information for frost flowers over time and many of the chemical species commonly associated with Polar tropospheric reactions have never been reported for frost flowers. We undertook this study on the sea ice north of Barrow, Alaska to quantify the major ion, stable oxygen and hydrogen isotope, alkalinity, light absorbance by soluble species, organochlorine, and aldehyde composition of seawater, brine, and frost flowers. For many of these chemical species we present the first measurements from brine or frost flowers. Results show that major ion and alkalinity concentrations, stable isotope values, and major chromophore (NO3− and H2O2) concentrations are controlled by fractionation from seawater and brine. The presence of these chemical species in present and future sea ice scenarios is somewhat predictable. However, aldehydes, organochlorine compounds, light absorbing species, and mercury (part 2 of this research and Sherman et al. (2012)) are deposited to frost flowers through less predictable processes that probably involve the atmosphere as a source. The present and future concentrations of these constituents in frost flowers may not be easily incorporated into future sea ice or lower atmospheric chemistry scenarios. Thinning of Arctic sea ice will likely present more open sea ice leads where young ice, brine, and frost flowers form. How these changing ice conditions will affect the interactions between ice, brine, frost flowers and the lower atmosphere is unknown.</abstract>
<abstract type="short">Brine and frost flowers on sea ice have interactions with the lower atmosphere Frost flowers have some predictable and some unpredictable chemical composition Changing sea ice regimes likely mean more brine and frost flowers in the future</abstract>
<note type="additional physical form">Tab‐delimited Table 1.Tab‐delimited Table 2.Tab‐delimited Table 3.Tab‐delimited Table 4.Tab‐delimited Table 5.</note>
<subject>
<genre>keywords</genre>
<topic>frost flowers</topic>
<topic>polar atmospheric chemistry</topic>
<topic>sea ice</topic>
</subject>
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<titleInfo>
<title>Journal of Geophysical Research: Atmospheres</title>
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<titleInfo type="abbreviated">
<title>J. Geophys. Res.</title>
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<topic authorityURI="http://psi.agu.org/specialSection/OASIS1">The Ocean‐Atmosphere‐Sea Ice‐Snowpack (OASIS09)</topic>
<topic authorityURI="http://psi.agu.org/subset/ACH">Composition and Chemistry</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/0400">BIOGEOSCIENCES</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/0412">Biogeochemical kinetics and reaction modeling</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/0414">Biogeochemical cycles, processes, and modeling</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/0700">CRYOSPHERE</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/0738">Ice</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/0750">Sea ice</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/0793">Biogeochemistry</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/1000">GEOCHEMISTRY</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/1022">Composition of the hydrosphere</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/1050">Marine geochemistry</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/1600">GLOBAL CHANGE</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/1615">Biogeochemical cycles, processes, and modeling</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/1800">HYDROLOGY</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/1863">Snow and ice</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/4500">OCEANOGRAPHY: PHYSICAL</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/4540">Ice mechanics and air/sea/ice exchange processes</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/4800">OCEANOGRAPHY: BIOLOGICAL AND CHEMICAL</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/4805">Biogeochemical cycles, processes, and modeling</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/4835">Marine inorganic chemistry</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/4845">Nutrients and nutrient cycling</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/4850">Marine organic chemistry</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/4900">PALEOCEANOGRAPHY</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/4912">Biogeochemical cycles, processes, and modeling</topic>
</subject>
<subject>
<genre>article-category</genre>
<topic>Composition and Chemistry</topic>
</subject>
<identifier type="ISSN">0148-0227</identifier>
<identifier type="eISSN">2156-2202</identifier>
<identifier type="DOI">10.1002/(ISSN)2156-2202d</identifier>
<identifier type="CODEN">JGREA2</identifier>
<identifier type="PublisherID">JGRD</identifier>
<part>
<date>2012</date>
<detail type="volume">
<caption>vol.</caption>
<number>117</number>
</detail>
<detail type="issue">
<caption>no.</caption>
<number>D14</number>
</detail>
<extent unit="pages">
<start>n/a</start>
<end>n/a</end>
<total>15</total>
</extent>
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<identifier type="DOI">10.1029/2011JD016460</identifier>
<identifier type="ArticleID">2011JD016460</identifier>
<accessCondition type="use and reproduction" contentType="copyright">Copyright 2012 by the American Geophysical Union</accessCondition>
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