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    The CIRCE Simulations: Regional Climate Change Projections with Realistic Representation of the Mediterranean Sea

    Source: Bulletin of the American Meteorological Society:;2012:;volume( 094 ):;issue: 001::page 65
    Author:
    Gualdi, S.
    ,
    Somot, S.
    ,
    Li, L.
    ,
    Artale, V.
    ,
    Adani, M.
    ,
    Bellucci, A.
    ,
    Braun, A.
    ,
    Calmanti, S.
    ,
    Carillo, A.
    ,
    Dell'Aquila, A.
    ,
    Déqué, M.
    ,
    Dubois, C.
    ,
    Elizalde, A.
    ,
    Harzallah, A.
    ,
    Jacob, D.
    ,
    L'Hévéder, B.
    ,
    May, W.
    ,
    Oddo, P.
    ,
    Ruti, P.
    ,
    Sanna, A.
    ,
    Sannino, G.
    ,
    Scoccimarro, E.
    ,
    Sevault, F.
    ,
    Navarra, A.
    DOI: 10.1175/BAMS-D-11-00136.1
    Publisher: American Meteorological Society
    Abstract: rticle, the authors describe an innovative multimodel system developed within the Climate Change and Impact Research: The Mediterranean Environment (CIRCE) European Union (EU) Sixth Framework Programme (FP6) project and used to produce simulations of the Mediterranean Sea regional climate. The models include high-resolution Mediterranean Sea components, which allow assessment of the role of the basin and in particular of the air?sea feedbacks in the climate of the region. The models have been integrated from 1951 to 2050, using observed radiative forcings during the first half of the simulation period and the Intergovernmental Panel on Climate Change (IPCC) Special Report on Emissions Scenarios (SRES) A1B scenario during the second half. The projections show a substantial warming (about 1.5°?2°C) and a significant decrease of precipitation (about 5%) in the region for the scenario period. However, locally the changes might be even larger. In the same period, the projected surface net heat loss decreases, leading to a weaker cooling of the Mediterranean Sea by the atmosphere, whereas the water budget appears to increase, leading the basin to lose more water through its surface than in the past. Overall, these results are consistent with the findings of previous scenario simulations, such as the Prediction of Regional Scenarios and Uncertainties for Defining European Climate Change Risks and Effects (PRUDENCE), Ensemble-Based Predictions of Climate Changes and Their Impacts (ENSEMBLES), and phase 3 of the Coupled Model Intercomparison Project (CMIP3). The agreement suggests that these findings are robust to substantial changes in the configuration of the models used to make the simulations. Finally, the models produce a 2021?50 mean steric sea level rise that ranges between +7 and +12 cm, with respect to the period of reference.
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      The CIRCE Simulations: Regional Climate Change Projections with Realistic Representation of the Mediterranean Sea

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    contributor authorGualdi, S.
    contributor authorSomot, S.
    contributor authorLi, L.
    contributor authorArtale, V.
    contributor authorAdani, M.
    contributor authorBellucci, A.
    contributor authorBraun, A.
    contributor authorCalmanti, S.
    contributor authorCarillo, A.
    contributor authorDell'Aquila, A.
    contributor authorDéqué, M.
    contributor authorDubois, C.
    contributor authorElizalde, A.
    contributor authorHarzallah, A.
    contributor authorJacob, D.
    contributor authorL'Hévéder, B.
    contributor authorMay, W.
    contributor authorOddo, P.
    contributor authorRuti, P.
    contributor authorSanna, A.
    contributor authorSannino, G.
    contributor authorScoccimarro, E.
    contributor authorSevault, F.
    contributor authorNavarra, A.
    date accessioned2017-06-09T16:44:01Z
    date available2017-06-09T16:44:01Z
    date copyright2013/01/01
    date issued2012
    identifier issn0003-0007
    identifier otherams-73172.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4215257
    description abstractrticle, the authors describe an innovative multimodel system developed within the Climate Change and Impact Research: The Mediterranean Environment (CIRCE) European Union (EU) Sixth Framework Programme (FP6) project and used to produce simulations of the Mediterranean Sea regional climate. The models include high-resolution Mediterranean Sea components, which allow assessment of the role of the basin and in particular of the air?sea feedbacks in the climate of the region. The models have been integrated from 1951 to 2050, using observed radiative forcings during the first half of the simulation period and the Intergovernmental Panel on Climate Change (IPCC) Special Report on Emissions Scenarios (SRES) A1B scenario during the second half. The projections show a substantial warming (about 1.5°?2°C) and a significant decrease of precipitation (about 5%) in the region for the scenario period. However, locally the changes might be even larger. In the same period, the projected surface net heat loss decreases, leading to a weaker cooling of the Mediterranean Sea by the atmosphere, whereas the water budget appears to increase, leading the basin to lose more water through its surface than in the past. Overall, these results are consistent with the findings of previous scenario simulations, such as the Prediction of Regional Scenarios and Uncertainties for Defining European Climate Change Risks and Effects (PRUDENCE), Ensemble-Based Predictions of Climate Changes and Their Impacts (ENSEMBLES), and phase 3 of the Coupled Model Intercomparison Project (CMIP3). The agreement suggests that these findings are robust to substantial changes in the configuration of the models used to make the simulations. Finally, the models produce a 2021?50 mean steric sea level rise that ranges between +7 and +12 cm, with respect to the period of reference.
    publisherAmerican Meteorological Society
    titleThe CIRCE Simulations: Regional Climate Change Projections with Realistic Representation of the Mediterranean Sea
    typeJournal Paper
    journal volume94
    journal issue1
    journal titleBulletin of the American Meteorological Society
    identifier doi10.1175/BAMS-D-11-00136.1
    journal fristpage65
    journal lastpage81
    treeBulletin of the American Meteorological Society:;2012:;volume( 094 ):;issue: 001
    contenttypeFulltext
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