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    Melting of Ice and Sea Ice into Seawater and Frazil Ice Formation

    Source: Journal of Physical Oceanography:;2014:;Volume( 044 ):;issue: 007::page 1751
    Author:
    McDougall, Trevor J.
    ,
    Barker, Paul M.
    ,
    Feistel, Rainer
    ,
    Galton-Fenzi, Ben K.
    DOI: 10.1175/JPO-D-13-0253.1
    Publisher: American Meteorological Society
    Abstract: he thermodynamic consequences of the melting of ice and sea ice into seawater are considered. The International Thermodynamic Equation Of Seawater?2010 (TEOS-10) is used to derive the changes in the Conservative Temperature and Absolute Salinity of seawater that occurs as a consequence of the melting of ice and sea ice into seawater. Also, a study of the thermodynamic relationships involved in the formation of frazil ice enables the calculation of the magnitudes of the Conservative Temperature and Absolute Salinity changes with pressure when frazil ice is present in a seawater parcel, assuming that the frazil ice crystals are sufficiently small that their relative vertical velocity can be ignored. The main results of this paper are the equations that describe the changes to these quantities when ice and seawater interact, and these equations can be evaluated using computer software that the authors have developed and is publicly available in the Gibbs SeaWater (GSW) Oceanographic Toolbox of TEOS-10.
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      Melting of Ice and Sea Ice into Seawater and Frazil Ice Formation

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4226676
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    contributor authorMcDougall, Trevor J.
    contributor authorBarker, Paul M.
    contributor authorFeistel, Rainer
    contributor authorGalton-Fenzi, Ben K.
    date accessioned2017-06-09T17:20:20Z
    date available2017-06-09T17:20:20Z
    date copyright2014/07/01
    date issued2014
    identifier issn0022-3670
    identifier otherams-83450.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4226676
    description abstracthe thermodynamic consequences of the melting of ice and sea ice into seawater are considered. The International Thermodynamic Equation Of Seawater?2010 (TEOS-10) is used to derive the changes in the Conservative Temperature and Absolute Salinity of seawater that occurs as a consequence of the melting of ice and sea ice into seawater. Also, a study of the thermodynamic relationships involved in the formation of frazil ice enables the calculation of the magnitudes of the Conservative Temperature and Absolute Salinity changes with pressure when frazil ice is present in a seawater parcel, assuming that the frazil ice crystals are sufficiently small that their relative vertical velocity can be ignored. The main results of this paper are the equations that describe the changes to these quantities when ice and seawater interact, and these equations can be evaluated using computer software that the authors have developed and is publicly available in the Gibbs SeaWater (GSW) Oceanographic Toolbox of TEOS-10.
    publisherAmerican Meteorological Society
    titleMelting of Ice and Sea Ice into Seawater and Frazil Ice Formation
    typeJournal Paper
    journal volume44
    journal issue7
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/JPO-D-13-0253.1
    journal fristpage1751
    journal lastpage1775
    treeJournal of Physical Oceanography:;2014:;Volume( 044 ):;issue: 007
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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