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    A Comparison of Rainfall, Outgoing Longwave Radiation, and Divergence over the Amazon Basin

    Source: Journal of Climate:;1998:;volume( 011 ):;issue: 011::page 2898
    Author:
    Liebmann, Brant
    ,
    Marengo, JoséA.
    ,
    Glick, John D.
    ,
    Kousky, Vernon E.
    ,
    Wainer, Ilana C.
    ,
    Massambani, Oswaldo
    DOI: 10.1175/1520-0442(1998)011<2898:ACOROL>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Observed rainfall, outgoing longwave radiation (OLR), divergence, and precipitation from the reanalysis project of the National Centers for Environmental Prediction and the National Center for Atmospheric Research are compared over the Amazon Basin. The spatial pattern of the mean and the phase of the annual cycle generally compare well, except that the amplitude of the annual cycle of model precipitation is much smaller than observed. On 10?30-day timescales, it is shown that averaging stations within a 5° radius is approximately equivalent to total wavenumber 20 (T20) spatial scale, although it is more important to have a high density of stations than an exact match of spatial scales. Ideally, there should be one station per 20?000 km2. On 10?30-day scales, observed rainfall is best correlated with OLR. Correlations between OLR and 150-mb divergence are larger than between observed rainfall and divergence or between rainfall and model precipitation. For example, if 10?30-day filtered OLR and divergence are truncated at T20 and rainfall is averaged to include stations within a 5° radius, OLR is correlated with rainfall at about ?0.6, OLR is correlated with divergence at about ?0.35, and rainfall is correlated with divergence at about 0.2. At least part of the lack of correlation is due to inadequate spatial sampling of rainfall. Correlations improve with larger spatial scale. The major seasonal transitions from dry to rainy regimes are captured well by OLR but not by the model quantities. The mean diurnal cycle is represented reasonably by 150-mb divergence.
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      A Comparison of Rainfall, Outgoing Longwave Radiation, and Divergence over the Amazon Basin

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    contributor authorLiebmann, Brant
    contributor authorMarengo, JoséA.
    contributor authorGlick, John D.
    contributor authorKousky, Vernon E.
    contributor authorWainer, Ilana C.
    contributor authorMassambani, Oswaldo
    date accessioned2017-06-09T15:41:36Z
    date available2017-06-09T15:41:36Z
    date copyright1998/11/01
    date issued1998
    identifier issn0894-8755
    identifier otherams-5086.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4190467
    description abstractObserved rainfall, outgoing longwave radiation (OLR), divergence, and precipitation from the reanalysis project of the National Centers for Environmental Prediction and the National Center for Atmospheric Research are compared over the Amazon Basin. The spatial pattern of the mean and the phase of the annual cycle generally compare well, except that the amplitude of the annual cycle of model precipitation is much smaller than observed. On 10?30-day timescales, it is shown that averaging stations within a 5° radius is approximately equivalent to total wavenumber 20 (T20) spatial scale, although it is more important to have a high density of stations than an exact match of spatial scales. Ideally, there should be one station per 20?000 km2. On 10?30-day scales, observed rainfall is best correlated with OLR. Correlations between OLR and 150-mb divergence are larger than between observed rainfall and divergence or between rainfall and model precipitation. For example, if 10?30-day filtered OLR and divergence are truncated at T20 and rainfall is averaged to include stations within a 5° radius, OLR is correlated with rainfall at about ?0.6, OLR is correlated with divergence at about ?0.35, and rainfall is correlated with divergence at about 0.2. At least part of the lack of correlation is due to inadequate spatial sampling of rainfall. Correlations improve with larger spatial scale. The major seasonal transitions from dry to rainy regimes are captured well by OLR but not by the model quantities. The mean diurnal cycle is represented reasonably by 150-mb divergence.
    publisherAmerican Meteorological Society
    titleA Comparison of Rainfall, Outgoing Longwave Radiation, and Divergence over the Amazon Basin
    typeJournal Paper
    journal volume11
    journal issue11
    journal titleJournal of Climate
    identifier doi10.1175/1520-0442(1998)011<2898:ACOROL>2.0.CO;2
    journal fristpage2898
    journal lastpage2909
    treeJournal of Climate:;1998:;volume( 011 ):;issue: 011
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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