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    Sea ice dynamics influence halogen deposition to Svalbard

    Access Status
    Open access via publisher
    Authors
    Spolaor, A.
    Gabrieli, J.
    Martma, T.
    Kohler, J.
    Björkman, M.
    Isaksson, E.
    Varin, C.
    Vallelonga, P.
    Plane, J.
    Barbante, C.
    Date
    2013
    Type
    Journal Article
    
    Metadata
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    Citation
    Spolaor, A. and Gabrieli, J. and Martma, T. and Kohler, J. and Björkman, M.B. and Isaksson, E. and Varin, C. and Vallelonga, P. and Plane, J.M. and Barbante, C. 2013. Sea ice dynamics influence halogen deposition to Svalbard. Cryosphere. 7 (5): pp. 1645-1658.
    Source Title
    Cryosphere
    DOI
    10.5194/tc-7-1645-2013
    ISSN
    1994-0416
    URI
    http://hdl.handle.net/20.500.11937/26785
    Collection
    • Curtin Research Publications
    Abstract

    Sea ice is an important parameter in the climate system and its changes impact upon the polar albedo and atmospheric and oceanic circulation. Iodine (I) and bromine (Br) have been measured in a shallow firn core drilled at the summit of the Holtedahlfonna glacier (Northwest Spitsbergen, Svalbard). Changing I concentrations can be linked to the March–May maximum sea ice extension. Bromine enrichment, indexed to the Br / Na sea water mass ratio, appears to be influenced by changes in the seasonal sea ice area. I is emitted from marine biota and so the retreat of March–May sea ice coincides with enlargement of the open-ocean surface which enhances marine primary production and consequent I emission. The observed Br enrichment could be explained by greater Br emissions during the Br explosions that have been observed to occur mainly above first year sea ice during the early springtime. In this work we present the first comparison between halogens in surface snow and Arctic sea ice extension. Although further investigation is required to characterize potential depositional and post-depositional processes, these preliminary findings suggest that I and Br can be linked to variability in the spring maximum sea ice extension and seasonal sea ice surface area.

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