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    The Annual March of Heat Storage and Export in the Tropical Atlantic Ocean

    Source: Journal of Physical Oceanography:;1986:;Volume( 016 ):;issue: 004::page 694
    Author:
    Hastenrath, Stefan
    ,
    Merle, Jacques
    DOI: 10.1175/1520-0485(1986)016<0694:TAMOHS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The annual cycle and spatial patterns of subsurface heat storage Qt and divergence of heat transport Qv in the tropical Atlantic Ocean (30°N?20°S, east of 80°W) are studied on the basis of subsurface temperature soundings complied until 1978 and evaluations of the net heat gain through the ocean surface (Qt+Qv) from long-term ship observations (1911?70). The net oceanic heat gain (Qt+Qv) follows in large part, but not exclusively, the annual cycle of insolation with largest gain in the respective summer, and loss in the winter half-year. The Qt has an annual range and spatial gradients considerably larger than those of (Qt+Qv). Poleward of about 15°N, Qt exhibits an annual cycle similar to (Qt+Qv) and insolation. By contrast, temporal and spatial variations of Qt are more complicated in the equatorial Atlantic (about 10°N?10°S). For the average over this latitude band, heat depletion (negative Qt) is found around March-May and largest storage around August?September. The divergence of oceanic heat transport Qv is obtained as the difference between (Qt+Qv) and Qt, and exhibits patterns broadly complementary to those of Qt. Calendar monthly maps indicate two major systems of annual cycle changes of Qt. (i) A west?east seasaw variation is apparent in the equatorial belt (about 10°S?10°N), with heat depletion prevailing in the western equatorial Atlantic around March and April, and heat storage continuing in the Gulf of Guinea from January to around May. This heat budget pattern is associated with a deepening of isothermal surfaces to the west from about May to July, with concomitant shallowing in the Gulf of Guinea. (ii) The zone 0?15°N is dominated by a northwestward shift of a band of negative Qt from around March to August, and an inverse displacement thereafter. Both systems (i) and (ii) of seasonal changes in Qt broadly parallel the annual cycle of the surface wind field over the tropical Atlantic, characterized by extrema around April and August.
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      The Annual March of Heat Storage and Export in the Tropical Atlantic Ocean

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4163941
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    contributor authorHastenrath, Stefan
    contributor authorMerle, Jacques
    date accessioned2017-06-09T14:47:51Z
    date available2017-06-09T14:47:51Z
    date copyright1986/04/01
    date issued1986
    identifier issn0022-3670
    identifier otherams-26987.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4163941
    description abstractThe annual cycle and spatial patterns of subsurface heat storage Qt and divergence of heat transport Qv in the tropical Atlantic Ocean (30°N?20°S, east of 80°W) are studied on the basis of subsurface temperature soundings complied until 1978 and evaluations of the net heat gain through the ocean surface (Qt+Qv) from long-term ship observations (1911?70). The net oceanic heat gain (Qt+Qv) follows in large part, but not exclusively, the annual cycle of insolation with largest gain in the respective summer, and loss in the winter half-year. The Qt has an annual range and spatial gradients considerably larger than those of (Qt+Qv). Poleward of about 15°N, Qt exhibits an annual cycle similar to (Qt+Qv) and insolation. By contrast, temporal and spatial variations of Qt are more complicated in the equatorial Atlantic (about 10°N?10°S). For the average over this latitude band, heat depletion (negative Qt) is found around March-May and largest storage around August?September. The divergence of oceanic heat transport Qv is obtained as the difference between (Qt+Qv) and Qt, and exhibits patterns broadly complementary to those of Qt. Calendar monthly maps indicate two major systems of annual cycle changes of Qt. (i) A west?east seasaw variation is apparent in the equatorial belt (about 10°S?10°N), with heat depletion prevailing in the western equatorial Atlantic around March and April, and heat storage continuing in the Gulf of Guinea from January to around May. This heat budget pattern is associated with a deepening of isothermal surfaces to the west from about May to July, with concomitant shallowing in the Gulf of Guinea. (ii) The zone 0?15°N is dominated by a northwestward shift of a band of negative Qt from around March to August, and an inverse displacement thereafter. Both systems (i) and (ii) of seasonal changes in Qt broadly parallel the annual cycle of the surface wind field over the tropical Atlantic, characterized by extrema around April and August.
    publisherAmerican Meteorological Society
    titleThe Annual March of Heat Storage and Export in the Tropical Atlantic Ocean
    typeJournal Paper
    journal volume16
    journal issue4
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1986)016<0694:TAMOHS>2.0.CO;2
    journal fristpage694
    journal lastpage708
    treeJournal of Physical Oceanography:;1986:;Volume( 016 ):;issue: 004
    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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