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    The Relationship between Total Precipitable Water and Surface Dew Point

    Source: Journal of Applied Meteorology:;1981:;volume( 020 ):;issue: 001::page 3
    Author:
    Viswanadham, Y.
    DOI: 10.1175/1520-0450(1981)020<0003:TRBTPW>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Mean monthly and annual values of total precipitable water are compared with mean monthly and annual values of surface dew point for each 5° latitude circle from the equator to 85°S. The correlation coefficients are lower for latitudes 0?20°S than for latitudes 25?85°S. The degree of relationship between mean monthly values of total precipitable water and mean monthly values of surface dew point is good in winter for all latitudes but much weaker in warmer months for latitudes 0?20°S. The computed regression equations give excellent estimates of monthly mean zonally averaged precipitable water from surface dew point for middle and higher latitudes in cooler seasons. Zonally averaged values of the moisture profile power index ? for the Southern Hemisphere are presented. This power index is highly variable (?0.26 to +4.57) even for mean monthly moisture profiles. These results are useful for the zonally averaged climatic models.
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      The Relationship between Total Precipitable Water and Surface Dew Point

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    contributor authorViswanadham, Y.
    date accessioned2017-06-09T13:57:59Z
    date available2017-06-09T13:57:59Z
    date copyright1981/01/01
    date issued1981
    identifier issn0021-8952
    identifier otherams-10008.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4145078
    description abstractMean monthly and annual values of total precipitable water are compared with mean monthly and annual values of surface dew point for each 5° latitude circle from the equator to 85°S. The correlation coefficients are lower for latitudes 0?20°S than for latitudes 25?85°S. The degree of relationship between mean monthly values of total precipitable water and mean monthly values of surface dew point is good in winter for all latitudes but much weaker in warmer months for latitudes 0?20°S. The computed regression equations give excellent estimates of monthly mean zonally averaged precipitable water from surface dew point for middle and higher latitudes in cooler seasons. Zonally averaged values of the moisture profile power index ? for the Southern Hemisphere are presented. This power index is highly variable (?0.26 to +4.57) even for mean monthly moisture profiles. These results are useful for the zonally averaged climatic models.
    publisherAmerican Meteorological Society
    titleThe Relationship between Total Precipitable Water and Surface Dew Point
    typeJournal Paper
    journal volume20
    journal issue1
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1981)020<0003:TRBTPW>2.0.CO;2
    journal fristpage3
    journal lastpage8
    treeJournal of Applied Meteorology:;1981:;volume( 020 ):;issue: 001
    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