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    On the Computation of Isobaric Wet-Bulb Temperature and Saturation Temperature over Ice

    Source: Journal of Applied Meteorology:;1974:;volume( 013 ):;issue: 006::page 726
    Author:
    Chappell, Charles F.
    ,
    Magaziner, E. L.
    ,
    Fritsch, J. Michael
    DOI: 10.1175/1520-0450(1974)013<0726:OTCOIW>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Non-iterative methods for computing isobaric wet-bulb temperature and the temperature at the lifted sublimation level are presented. These quantities are then computed by these direct techniques and compared to values derived through iterative methods. In the case of the isobaric wet-bulb temperature, differences in the two methods are less than 1C over normal ranges of atmospheric temperature and pressure for dewpoint depressions <30C. Differences in the two methods are less than 0.03C for the temperature at the lifted sublimation level over the same range of dewpoint depression.
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      On the Computation of Isobaric Wet-Bulb Temperature and Saturation Temperature over Ice

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4231511
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    • Journal of Applied Meteorology

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    contributor authorChappell, Charles F.
    contributor authorMagaziner, E. L.
    contributor authorFritsch, J. Michael
    date accessioned2017-06-09T17:35:48Z
    date available2017-06-09T17:35:48Z
    date copyright1974/09/01
    date issued1974
    identifier issn0021-8952
    identifier otherams-8780.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4231511
    description abstractNon-iterative methods for computing isobaric wet-bulb temperature and the temperature at the lifted sublimation level are presented. These quantities are then computed by these direct techniques and compared to values derived through iterative methods. In the case of the isobaric wet-bulb temperature, differences in the two methods are less than 1C over normal ranges of atmospheric temperature and pressure for dewpoint depressions <30C. Differences in the two methods are less than 0.03C for the temperature at the lifted sublimation level over the same range of dewpoint depression.
    publisherAmerican Meteorological Society
    titleOn the Computation of Isobaric Wet-Bulb Temperature and Saturation Temperature over Ice
    typeJournal Paper
    journal volume13
    journal issue6
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1974)013<0726:OTCOIW>2.0.CO;2
    journal fristpage726
    journal lastpage728
    treeJournal of Applied Meteorology:;1974:;volume( 013 ):;issue: 006
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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