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    Climate Change Projections for the Twenty-First Century and Climate Change Commitment in the CCSM3

    Source: Journal of Climate:;2006:;volume( 019 ):;issue: 011::page 2597
    Author:
    Meehl, Gerald A.
    ,
    Washington, Warren M.
    ,
    Santer, Benjamin D.
    ,
    Collins, William D.
    ,
    Arblaster, Julie M.
    ,
    Hu, Aixue
    ,
    Lawrence, David M.
    ,
    Teng, Haiyan
    ,
    Buja, Lawrence E.
    ,
    Strand, Warren G.
    DOI: 10.1175/JCLI3746.1
    Publisher: American Meteorological Society
    Abstract: Climate change scenario simulations with the Community Climate System Model version 3 (CCSM3), a global coupled climate model, show that if concentrations of all greenhouse gases (GHGs) could have been stabilized at the year 2000, the climate system would already be committed to 0.4°C more warming by the end of the twenty-first century. Committed sea level rise by 2100 is about an order of magnitude more, percentage-wise, compared to sea level rise simulated in the twentieth century. This increase in the model is produced only by thermal expansion of seawater, and does not take into account melt from ice sheets and glaciers, which could at least double that number. Several tenths of a degree of additional warming occurs in the model for the next 200 yr in the Intergovernmental Panel on Climate Change (IPCC) Special Report on Emissions Scenarios (SRES) B1 and A1B scenarios after stabilization in the year 2100, but with twice as much sea level rise after 100 yr, and doubling yet again in the next 100 yr to 2300. At the end of the twenty-first century, the warming in the tropical Pacific for the A2, A1B, and B1 scenarios resembles an El Niño?like response, likely due to cloud feedbacks in the model as shown in an earlier version. Greatest warming occurs at high northern latitudes and over continents. The monsoon regimes intensify somewhat in the future warmer climate, with decreases of sea level pressure at high latitudes and increases in the subtropics and parts of the midlatitudes. There is a weak summer midlatitude soil moisture drying in this model as documented in previous models. Sea ice distributions in both hemispheres are somewhat overextensive, but with about the right ice thickness at the end of the twentieth century. Future decreases in sea ice with global warming are proportional to the temperature response from the forcing scenarios, with the high forcing scenario, A2, producing an ice-free Arctic in summer by the year 2100.
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      Climate Change Projections for the Twenty-First Century and Climate Change Commitment in the CCSM3

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    contributor authorMeehl, Gerald A.
    contributor authorWashington, Warren M.
    contributor authorSanter, Benjamin D.
    contributor authorCollins, William D.
    contributor authorArblaster, Julie M.
    contributor authorHu, Aixue
    contributor authorLawrence, David M.
    contributor authorTeng, Haiyan
    contributor authorBuja, Lawrence E.
    contributor authorStrand, Warren G.
    date accessioned2017-06-09T17:01:52Z
    date available2017-06-09T17:01:52Z
    date copyright2006/06/01
    date issued2006
    identifier issn0894-8755
    identifier otherams-78214.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4220859
    description abstractClimate change scenario simulations with the Community Climate System Model version 3 (CCSM3), a global coupled climate model, show that if concentrations of all greenhouse gases (GHGs) could have been stabilized at the year 2000, the climate system would already be committed to 0.4°C more warming by the end of the twenty-first century. Committed sea level rise by 2100 is about an order of magnitude more, percentage-wise, compared to sea level rise simulated in the twentieth century. This increase in the model is produced only by thermal expansion of seawater, and does not take into account melt from ice sheets and glaciers, which could at least double that number. Several tenths of a degree of additional warming occurs in the model for the next 200 yr in the Intergovernmental Panel on Climate Change (IPCC) Special Report on Emissions Scenarios (SRES) B1 and A1B scenarios after stabilization in the year 2100, but with twice as much sea level rise after 100 yr, and doubling yet again in the next 100 yr to 2300. At the end of the twenty-first century, the warming in the tropical Pacific for the A2, A1B, and B1 scenarios resembles an El Niño?like response, likely due to cloud feedbacks in the model as shown in an earlier version. Greatest warming occurs at high northern latitudes and over continents. The monsoon regimes intensify somewhat in the future warmer climate, with decreases of sea level pressure at high latitudes and increases in the subtropics and parts of the midlatitudes. There is a weak summer midlatitude soil moisture drying in this model as documented in previous models. Sea ice distributions in both hemispheres are somewhat overextensive, but with about the right ice thickness at the end of the twentieth century. Future decreases in sea ice with global warming are proportional to the temperature response from the forcing scenarios, with the high forcing scenario, A2, producing an ice-free Arctic in summer by the year 2100.
    publisherAmerican Meteorological Society
    titleClimate Change Projections for the Twenty-First Century and Climate Change Commitment in the CCSM3
    typeJournal Paper
    journal volume19
    journal issue11
    journal titleJournal of Climate
    identifier doi10.1175/JCLI3746.1
    journal fristpage2597
    journal lastpage2616
    treeJournal of Climate:;2006:;volume( 019 ):;issue: 011
    contenttypeFulltext
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