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    On Thermal Expansion over the Last Hundred Years

    Source: Journal of Climate:;1995:;volume( 008 ):;issue: 011::page 2881
    Author:
    de Wolde, J. R.
    ,
    Bintanja, R.
    ,
    Oerlemans, J.
    DOI: 10.1175/1520-0442(1995)008<2881:OTEOTL>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Estimates of sea level rise during the period 1856?1991 due to thermal expansion are presented. The estimates are based on an ocean model that consists of three zonally averaged ocean basins representing the Atlantic, Pacific, and Indian Oceans. These basins are connected by a circumpolar basin that represents the Southern Ocean. The ocean circulation in the model was prescribed. Surface ocean forcing was calculated from observed sea surface temperatures. Global mean forcing and regionally varying forcing were distinguished. Different parameterizations of ocean heat mixing were incorporated. According to the model presented, global mean sea level rise caused by thermal expansion over the last hundred years ranged from 2.2 to 5.1 cm, a best estimate being 3.5 cm.
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      On Thermal Expansion over the Last Hundred Years

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4183556
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    contributor authorde Wolde, J. R.
    contributor authorBintanja, R.
    contributor authorOerlemans, J.
    date accessioned2017-06-09T15:28:15Z
    date available2017-06-09T15:28:15Z
    date copyright1995/11/01
    date issued1995
    identifier issn0894-8755
    identifier otherams-4464.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4183556
    description abstractEstimates of sea level rise during the period 1856?1991 due to thermal expansion are presented. The estimates are based on an ocean model that consists of three zonally averaged ocean basins representing the Atlantic, Pacific, and Indian Oceans. These basins are connected by a circumpolar basin that represents the Southern Ocean. The ocean circulation in the model was prescribed. Surface ocean forcing was calculated from observed sea surface temperatures. Global mean forcing and regionally varying forcing were distinguished. Different parameterizations of ocean heat mixing were incorporated. According to the model presented, global mean sea level rise caused by thermal expansion over the last hundred years ranged from 2.2 to 5.1 cm, a best estimate being 3.5 cm.
    publisherAmerican Meteorological Society
    titleOn Thermal Expansion over the Last Hundred Years
    typeJournal Paper
    journal volume8
    journal issue11
    journal titleJournal of Climate
    identifier doi10.1175/1520-0442(1995)008<2881:OTEOTL>2.0.CO;2
    journal fristpage2881
    journal lastpage2891
    treeJournal of Climate:;1995:;volume( 008 ):;issue: 011
    contenttypeFulltext
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