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    Why Hasn’t Earth Warmed as Much as Expected?

    Source: Journal of Climate:;2010:;volume( 023 ):;issue: 010::page 2453
    Author:
    Schwartz, Stephen E.
    ,
    Charlson, Robert J.
    ,
    Kahn, Ralph A.
    ,
    Ogren, John A.
    ,
    Rodhe, Henning
    DOI: 10.1175/2009JCLI3461.1
    Publisher: American Meteorological Society
    Abstract: he observed increase in global mean surface temperature (GMST) over the industrial era is less than 40% of that expected from observed increases in long-lived greenhouse gases together with the best-estimate equilibrium climate sensitivity given by the 2007 Assessment Report of the Intergovernmental Panel on Climate Change (IPCC). Possible reasons for this warming discrepancy are systematically examined here. The warming discrepancy is found to be due mainly to some combination of two factors: the IPCC best estimate of climate sensitivity being too high and/or the greenhouse gas forcing being partially offset by forcing by increased concentrations of atmospheric aerosols; the increase in global heat content due to thermal disequilibrium accounts for less than 25% of the discrepancy, and cooling by natural temperature variation can account for only about 15%. Current uncertainty in climate sensitivity is shown to preclude determining the amount of future fossil fuel CO2 emissions that would be compatible with any chosen maximum allowable increase in GMST; even the sign of such allowable future emissions is unconstrained. Resolving this situation, by empirical determination of the earth?s climate sensitivity from the historical record over the industrial period or through use of climate models whose accuracy is evaluated by their performance over this period, is shown to require substantial reduction in the uncertainty of aerosol forcing over this period.
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      Why Hasn’t Earth Warmed as Much as Expected?

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4210611
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    contributor authorSchwartz, Stephen E.
    contributor authorCharlson, Robert J.
    contributor authorKahn, Ralph A.
    contributor authorOgren, John A.
    contributor authorRodhe, Henning
    date accessioned2017-06-09T16:30:04Z
    date available2017-06-09T16:30:04Z
    date copyright2010/05/01
    date issued2010
    identifier issn0894-8755
    identifier otherams-68992.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4210611
    description abstracthe observed increase in global mean surface temperature (GMST) over the industrial era is less than 40% of that expected from observed increases in long-lived greenhouse gases together with the best-estimate equilibrium climate sensitivity given by the 2007 Assessment Report of the Intergovernmental Panel on Climate Change (IPCC). Possible reasons for this warming discrepancy are systematically examined here. The warming discrepancy is found to be due mainly to some combination of two factors: the IPCC best estimate of climate sensitivity being too high and/or the greenhouse gas forcing being partially offset by forcing by increased concentrations of atmospheric aerosols; the increase in global heat content due to thermal disequilibrium accounts for less than 25% of the discrepancy, and cooling by natural temperature variation can account for only about 15%. Current uncertainty in climate sensitivity is shown to preclude determining the amount of future fossil fuel CO2 emissions that would be compatible with any chosen maximum allowable increase in GMST; even the sign of such allowable future emissions is unconstrained. Resolving this situation, by empirical determination of the earth?s climate sensitivity from the historical record over the industrial period or through use of climate models whose accuracy is evaluated by their performance over this period, is shown to require substantial reduction in the uncertainty of aerosol forcing over this period.
    publisherAmerican Meteorological Society
    titleWhy Hasn’t Earth Warmed as Much as Expected?
    typeJournal Paper
    journal volume23
    journal issue10
    journal titleJournal of Climate
    identifier doi10.1175/2009JCLI3461.1
    journal fristpage2453
    journal lastpage2464
    treeJournal of Climate:;2010:;volume( 023 ):;issue: 010
    contenttypeFulltext
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