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    Evaporation from Nonvegetated Surfaces: Surface Aridity Methods and Passive Microwave Remote Sensing

    Source: Journal of Applied Meteorology:;1999:;volume( 038 ):;issue: 009::page 1346
    Author:
    Cahill, Anthony T.
    ,
    Parlange, Marc B.
    ,
    Jackson, Thomas J.
    ,
    O’Neill, Peggy
    ,
    Schmugge, T. J.
    DOI: 10.1175/1520-0450(1999)038<1346:EFNSSA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The use of remotely sensed near-surface soil moisture for the estimation of evaporation is investigated. Two widely used parameterizations of evaporation, the so-called α and ? methods, which use near-surface soil moisture to reduce some measure of potential evaporation, are studied. The near-surface soil moisture is provided by a set of L- and S-band microwave radiometers, which were mounted 13 m above the surface. It is shown that soil moisture measured with a passive microwave sensor in combination with the ? method yields reliable estimates of evaporation, whereas the α method is not as robust.
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      Evaporation from Nonvegetated Surfaces: Surface Aridity Methods and Passive Microwave Remote Sensing

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4148141
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    • Journal of Applied Meteorology

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    contributor authorCahill, Anthony T.
    contributor authorParlange, Marc B.
    contributor authorJackson, Thomas J.
    contributor authorO’Neill, Peggy
    contributor authorSchmugge, T. J.
    date accessioned2017-06-09T14:07:08Z
    date available2017-06-09T14:07:08Z
    date copyright1999/09/01
    date issued1999
    identifier issn0894-8763
    identifier otherams-12766.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4148141
    description abstractThe use of remotely sensed near-surface soil moisture for the estimation of evaporation is investigated. Two widely used parameterizations of evaporation, the so-called α and ? methods, which use near-surface soil moisture to reduce some measure of potential evaporation, are studied. The near-surface soil moisture is provided by a set of L- and S-band microwave radiometers, which were mounted 13 m above the surface. It is shown that soil moisture measured with a passive microwave sensor in combination with the ? method yields reliable estimates of evaporation, whereas the α method is not as robust.
    publisherAmerican Meteorological Society
    titleEvaporation from Nonvegetated Surfaces: Surface Aridity Methods and Passive Microwave Remote Sensing
    typeJournal Paper
    journal volume38
    journal issue9
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1999)038<1346:EFNSSA>2.0.CO;2
    journal fristpage1346
    journal lastpage1351
    treeJournal of Applied Meteorology:;1999:;volume( 038 ):;issue: 009
    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