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    Annual Cycle of Surface Longwave Radiation

    Source: Journal of Applied Meteorology and Climatology:;2011:;volume( 050 ):;issue: 006::page 1212
    Author:
    Mlynczak, Pamela E.
    ,
    Smith, G. Louis
    ,
    Wilber, Anne C.
    ,
    Stackhouse, Paul W.
    DOI: 10.1175/2011JAMC2663.1
    Publisher: American Meteorological Society
    Abstract: he annual cycles of upward and downward longwave fluxes at the earth?s surface are investigated by use of the NASA Global Energy and Water Cycle Experiment (GEWEX) Surface Radiation Budget Dataset. Principal component analysis is used to quantify the annual cycles. Because of the immense difference between the heat capacity of land and ocean, the surface of the earth is partitioned into these two categories. Over land, the first principal component describes over 95% of the variance of the annual cycle of the upward and downward longwave fluxes. Over ocean the first term describes more than 87% of these annual cycles. Empirical orthogonal functions show the corresponding geographical distributions of these cycles. Phase-plane diagrams of the annual cycles of upward longwave fluxes as a function of net shortwave flux show the thermal inertia of land and ocean.
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      Annual Cycle of Surface Longwave Radiation

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4213576
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    contributor authorMlynczak, Pamela E.
    contributor authorSmith, G. Louis
    contributor authorWilber, Anne C.
    contributor authorStackhouse, Paul W.
    date accessioned2017-06-09T16:39:20Z
    date available2017-06-09T16:39:20Z
    date copyright2011/06/01
    date issued2011
    identifier issn1558-8424
    identifier otherams-71660.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4213576
    description abstracthe annual cycles of upward and downward longwave fluxes at the earth?s surface are investigated by use of the NASA Global Energy and Water Cycle Experiment (GEWEX) Surface Radiation Budget Dataset. Principal component analysis is used to quantify the annual cycles. Because of the immense difference between the heat capacity of land and ocean, the surface of the earth is partitioned into these two categories. Over land, the first principal component describes over 95% of the variance of the annual cycle of the upward and downward longwave fluxes. Over ocean the first term describes more than 87% of these annual cycles. Empirical orthogonal functions show the corresponding geographical distributions of these cycles. Phase-plane diagrams of the annual cycles of upward longwave fluxes as a function of net shortwave flux show the thermal inertia of land and ocean.
    publisherAmerican Meteorological Society
    titleAnnual Cycle of Surface Longwave Radiation
    typeJournal Paper
    journal volume50
    journal issue6
    journal titleJournal of Applied Meteorology and Climatology
    identifier doi10.1175/2011JAMC2663.1
    journal fristpage1212
    journal lastpage1224
    treeJournal of Applied Meteorology and Climatology:;2011:;volume( 050 ):;issue: 006
    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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