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    Recent Bottom Water Warming in the Pacific Ocean

    Source: Journal of Climate:;2007:;volume( 020 ):;issue: 021::page 5365
    Author:
    Johnson, Gregory C.
    ,
    Mecking, Sabine
    ,
    Sloyan, Bernadette M.
    ,
    Wijffels, Susan E.
    DOI: 10.1175/2007JCLI1879.1
    Publisher: American Meteorological Society
    Abstract: Decadal changes of abyssal temperature in the Pacific Ocean are analyzed using high-quality, full-depth hydrographic sections, each occupied at least twice between 1984 and 2006. The deep warming found over this time period agrees with previous analyses. The analysis presented here suggests it may have occurred after 1991, at least in the North Pacific. Mean temperature changes for the three zonal and three meridional hydrographic sections analyzed here exhibit abyssal warming often significantly different from zero at 95% confidence limits for this time period. Warming rates are generally larger to the south, and smaller to the north. This pattern is consistent with changes being attenuated with distance from the source of bottom water for the Pacific Ocean, which enters the main deep basins of this ocean southeast of New Zealand. Rough estimates of the change in ocean heat content suggest that the abyssal warming may amount to a significant fraction of upper World Ocean heat gain over the past few decades.
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      Recent Bottom Water Warming in the Pacific Ocean

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4207076
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    contributor authorJohnson, Gregory C.
    contributor authorMecking, Sabine
    contributor authorSloyan, Bernadette M.
    contributor authorWijffels, Susan E.
    date accessioned2017-06-09T16:19:37Z
    date available2017-06-09T16:19:37Z
    date copyright2007/11/01
    date issued2007
    identifier issn0894-8755
    identifier otherams-65810.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4207076
    description abstractDecadal changes of abyssal temperature in the Pacific Ocean are analyzed using high-quality, full-depth hydrographic sections, each occupied at least twice between 1984 and 2006. The deep warming found over this time period agrees with previous analyses. The analysis presented here suggests it may have occurred after 1991, at least in the North Pacific. Mean temperature changes for the three zonal and three meridional hydrographic sections analyzed here exhibit abyssal warming often significantly different from zero at 95% confidence limits for this time period. Warming rates are generally larger to the south, and smaller to the north. This pattern is consistent with changes being attenuated with distance from the source of bottom water for the Pacific Ocean, which enters the main deep basins of this ocean southeast of New Zealand. Rough estimates of the change in ocean heat content suggest that the abyssal warming may amount to a significant fraction of upper World Ocean heat gain over the past few decades.
    publisherAmerican Meteorological Society
    titleRecent Bottom Water Warming in the Pacific Ocean
    typeJournal Paper
    journal volume20
    journal issue21
    journal titleJournal of Climate
    identifier doi10.1175/2007JCLI1879.1
    journal fristpage5365
    journal lastpage5375
    treeJournal of Climate:;2007:;volume( 020 ):;issue: 021
    contenttypeFulltext
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