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    Production of Temporally Consistent Gridded Precipitation and Temperature Fields for the Continental United States

    Source: Journal of Hydrometeorology:;2005:;Volume( 006 ):;issue: 003::page 330
    Author:
    Hamlet, Alan F.
    ,
    Lettenmaier, Dennis P.
    DOI: 10.1175/JHM420.1
    Publisher: American Meteorological Society
    Abstract: The availability of long-term gridded datasets of precipitation, temperature, and other surface meteorological variables offers the potential for deriving a range of land surface conditions that have not been directly observed. These include, for instance, soil moisture, snow water equivalent, evapotranspiration, runoff, and subsurface moisture transport. However, gridding procedures can themselves introduce artificial trends due to incorporation of stations with different record lengths and locations. Hence, existing gridded datasets are in general not appropriate for estimation of long-term trends. Methods are described here for adjustment of gridded daily precipitation and temperature maxima and minima over the continental United States based on newly available (in electronic form) U.S. Cooperative Observer station data archived at the National Climatic Data Center from the early 1900s on. The intent is to produce gridded meteorological datasets that can be used, in conjunction with hydrologic modeling, for long-term trend analysis of simulated hydrologic variables.
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      Production of Temporally Consistent Gridded Precipitation and Temperature Fields for the Continental United States

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4224429
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    contributor authorHamlet, Alan F.
    contributor authorLettenmaier, Dennis P.
    date accessioned2017-06-09T17:13:44Z
    date available2017-06-09T17:13:44Z
    date copyright2005/06/01
    date issued2005
    identifier issn1525-755X
    identifier otherams-81427.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4224429
    description abstractThe availability of long-term gridded datasets of precipitation, temperature, and other surface meteorological variables offers the potential for deriving a range of land surface conditions that have not been directly observed. These include, for instance, soil moisture, snow water equivalent, evapotranspiration, runoff, and subsurface moisture transport. However, gridding procedures can themselves introduce artificial trends due to incorporation of stations with different record lengths and locations. Hence, existing gridded datasets are in general not appropriate for estimation of long-term trends. Methods are described here for adjustment of gridded daily precipitation and temperature maxima and minima over the continental United States based on newly available (in electronic form) U.S. Cooperative Observer station data archived at the National Climatic Data Center from the early 1900s on. The intent is to produce gridded meteorological datasets that can be used, in conjunction with hydrologic modeling, for long-term trend analysis of simulated hydrologic variables.
    publisherAmerican Meteorological Society
    titleProduction of Temporally Consistent Gridded Precipitation and Temperature Fields for the Continental United States
    typeJournal Paper
    journal volume6
    journal issue3
    journal titleJournal of Hydrometeorology
    identifier doi10.1175/JHM420.1
    journal fristpage330
    journal lastpage336
    treeJournal of Hydrometeorology:;2005:;Volume( 006 ):;issue: 003
    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