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    Analyzing the Concurrence of Meteorological Droughts and Warm Periods, with Implications for the Determination of Evaporative Regime

    Source: Journal of Climate:;2009:;volume( 022 ):;issue: 012::page 3331
    Author:
    Koster, R. D.
    ,
    Schubert, S. D.
    ,
    Suarez, M. J.
    DOI: 10.1175/2008JCLI2718.1
    Publisher: American Meteorological Society
    Abstract: The hydroclimatic conditions under which a seasonal meteorological drought (below-normal seasonal rainfall) can induce an increase in seasonal air temperature are investigated, first with an atmospheric general circulation model (AGCM) and then with observations. Geographical differences in the dryness?warmth connection abound in the AGCM; in the United States, for example, identified evaporative controls tend to tie meteorological droughts to warmer temperatures in the South but not in the Northeast. The strong agreement between AGCM and observations-based geographical patterns of drought-induced warming supports the idea that the same evaporative controls are also present in nature. A powerful side benefit of the analysis of drought-induced warming is a Northern Hemisphere map, derived solely from observations, showing where total boreal summer evaporation is controlled by soil moisture, energy availability, or both.
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      Analyzing the Concurrence of Meteorological Droughts and Warm Periods, with Implications for the Determination of Evaporative Regime

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4208747
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    contributor authorKoster, R. D.
    contributor authorSchubert, S. D.
    contributor authorSuarez, M. J.
    date accessioned2017-06-09T16:24:31Z
    date available2017-06-09T16:24:31Z
    date copyright2009/06/01
    date issued2009
    identifier issn0894-8755
    identifier otherams-67313.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4208747
    description abstractThe hydroclimatic conditions under which a seasonal meteorological drought (below-normal seasonal rainfall) can induce an increase in seasonal air temperature are investigated, first with an atmospheric general circulation model (AGCM) and then with observations. Geographical differences in the dryness?warmth connection abound in the AGCM; in the United States, for example, identified evaporative controls tend to tie meteorological droughts to warmer temperatures in the South but not in the Northeast. The strong agreement between AGCM and observations-based geographical patterns of drought-induced warming supports the idea that the same evaporative controls are also present in nature. A powerful side benefit of the analysis of drought-induced warming is a Northern Hemisphere map, derived solely from observations, showing where total boreal summer evaporation is controlled by soil moisture, energy availability, or both.
    publisherAmerican Meteorological Society
    titleAnalyzing the Concurrence of Meteorological Droughts and Warm Periods, with Implications for the Determination of Evaporative Regime
    typeJournal Paper
    journal volume22
    journal issue12
    journal titleJournal of Climate
    identifier doi10.1175/2008JCLI2718.1
    journal fristpage3331
    journal lastpage3341
    treeJournal of Climate:;2009:;volume( 022 ):;issue: 012
    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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