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    Quantifying the Strength of Soil Moisture–Precipitation Coupling and Its Sensitivity to Changes in Surface Water Budget

    Source: Journal of Hydrometeorology:;2007:;Volume( 008 ):;issue: 003::page 551
    Author:
    Wang, Guiling
    ,
    Kim, Yeonjoo
    ,
    Wang, Dagang
    DOI: 10.1175/JHM573.1
    Publisher: American Meteorological Society
    Abstract: This paper presents a new index to quantify the strength of soil moisture?precipitation coupling in AGCMs and explores how the soil moisture?precipitation coupling in Community Atmosphere Model version 3 (CAM3)?Community Land Model version 3 (CAM3?CLM3) responds to parameterization-induced surface water budget changes. Specifically, this study (a) compares the regions of strong coupling identified by the newly proposed index and the index currently used in the Global Land?Atmosphere Coupling Experiment (GLACE); (b) examines how the surface water budget changes influence the strength of soil moisture?precipitation coupling as measured by the two indexes, respectively; and (c) examines how these changes influence the memory of the coupled land?atmosphere system as measured by the correlation between soil moisture and subsequent precipitation. The new index and the GLACE index are consistent in identifying central North America and West Africa as major regions of strong coupling during June?August (JJA). However, in some areas of western Europe and of subtropical South America where the GLACE index is low, the new index suggests a modest significant coupling during JJA. In response to the surface water budget changes that presumably favor a stronger soil moisture?precipitation coupling, the new index increases, but the GLACE index decreases in a majority of the regions of modest-to-strong coupling, although both show some mixed response. Changes in the land?atmosphere system memory suggest an increase of coupling strength, consistent with results from the new index. The strong dependence of the GLACE index on the relative importance of atmospheric internal variability is identified as a potential cause for the differences between the two indexes. The two indexes emphasize different aspects of soil moisture?precipitation coupling, and one might be more suitable than the other depending on the purpose of individual studies.
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      Quantifying the Strength of Soil Moisture–Precipitation Coupling and Its Sensitivity to Changes in Surface Water Budget

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4224597
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    contributor authorWang, Guiling
    contributor authorKim, Yeonjoo
    contributor authorWang, Dagang
    date accessioned2017-06-09T17:14:10Z
    date available2017-06-09T17:14:10Z
    date copyright2007/06/01
    date issued2007
    identifier issn1525-755X
    identifier otherams-81579.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4224597
    description abstractThis paper presents a new index to quantify the strength of soil moisture?precipitation coupling in AGCMs and explores how the soil moisture?precipitation coupling in Community Atmosphere Model version 3 (CAM3)?Community Land Model version 3 (CAM3?CLM3) responds to parameterization-induced surface water budget changes. Specifically, this study (a) compares the regions of strong coupling identified by the newly proposed index and the index currently used in the Global Land?Atmosphere Coupling Experiment (GLACE); (b) examines how the surface water budget changes influence the strength of soil moisture?precipitation coupling as measured by the two indexes, respectively; and (c) examines how these changes influence the memory of the coupled land?atmosphere system as measured by the correlation between soil moisture and subsequent precipitation. The new index and the GLACE index are consistent in identifying central North America and West Africa as major regions of strong coupling during June?August (JJA). However, in some areas of western Europe and of subtropical South America where the GLACE index is low, the new index suggests a modest significant coupling during JJA. In response to the surface water budget changes that presumably favor a stronger soil moisture?precipitation coupling, the new index increases, but the GLACE index decreases in a majority of the regions of modest-to-strong coupling, although both show some mixed response. Changes in the land?atmosphere system memory suggest an increase of coupling strength, consistent with results from the new index. The strong dependence of the GLACE index on the relative importance of atmospheric internal variability is identified as a potential cause for the differences between the two indexes. The two indexes emphasize different aspects of soil moisture?precipitation coupling, and one might be more suitable than the other depending on the purpose of individual studies.
    publisherAmerican Meteorological Society
    titleQuantifying the Strength of Soil Moisture–Precipitation Coupling and Its Sensitivity to Changes in Surface Water Budget
    typeJournal Paper
    journal volume8
    journal issue3
    journal titleJournal of Hydrometeorology
    identifier doi10.1175/JHM573.1
    journal fristpage551
    journal lastpage570
    treeJournal of Hydrometeorology:;2007:;Volume( 008 ):;issue: 003
    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
    yabeshDSpacePersian