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    On the Estimation of Antarctic Iceberg Melt Rate

    Source: Journal of Physical Oceanography:;1980:;Volume( 010 ):;issue: 010::page 1681
    Author:
    Neshyba, Steve
    ,
    Josberger, Edward G.
    DOI: 10.1175/1520-0485(1980)010<1681:OTEOAI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Estimates of Antarctic iceberg melt rates made from field observations, iceberg distribution statistics, laboratory experiments and theoretical studies give a wide range of values. Evaluation of the errors associated with each method allows for the quantitative first-order correction for both the effect of bubbles released from the melting ice on the convective heat transfer and the effect of other forms of iceberg deterioration besides sidewall melting. The results provide a best estimate for the melt rate of 5, 17 and 55 m year?1 at a temperature elevation above the freezing point of Td = 2, 4 and 8°C, respectively. Also, the laboratory, theoretical and field observations indicate that the melt-rate dependence is proportional to Td1.6.
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      On the Estimation of Antarctic Iceberg Melt Rate

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    contributor authorNeshyba, Steve
    contributor authorJosberger, Edward G.
    date accessioned2017-06-09T14:45:37Z
    date available2017-06-09T14:45:37Z
    date copyright1980/10/01
    date issued1980
    identifier issn0022-3670
    identifier otherams-26139.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4163000
    description abstractEstimates of Antarctic iceberg melt rates made from field observations, iceberg distribution statistics, laboratory experiments and theoretical studies give a wide range of values. Evaluation of the errors associated with each method allows for the quantitative first-order correction for both the effect of bubbles released from the melting ice on the convective heat transfer and the effect of other forms of iceberg deterioration besides sidewall melting. The results provide a best estimate for the melt rate of 5, 17 and 55 m year?1 at a temperature elevation above the freezing point of Td = 2, 4 and 8°C, respectively. Also, the laboratory, theoretical and field observations indicate that the melt-rate dependence is proportional to Td1.6.
    publisherAmerican Meteorological Society
    titleOn the Estimation of Antarctic Iceberg Melt Rate
    typeJournal Paper
    journal volume10
    journal issue10
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1980)010<1681:OTEOAI>2.0.CO;2
    journal fristpage1681
    journal lastpage1685
    treeJournal of Physical Oceanography:;1980:;Volume( 010 ):;issue: 010
    contenttypeFulltext
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