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    The Summertime Atmospheric Hydrologic Cycle over the Southwestern United States

    Source: Journal of Hydrometeorology:;2004:;Volume( 005 ):;issue: 004::page 679
    Author:
    Anderson, Bruce T.
    ,
    Kanamaru, Hideki
    ,
    Roads, John O.
    DOI: 10.1175/1525-7541(2004)005<0679:TSAHCO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: In this paper the authors examine the large-scale summertime hydrologic cycle associated with the northwestern branch of the North American monsoon, centered on the southwestern United States, using a suite of surface-and upper-air-based observations, reanalysis products, and regional model simulations. In general, it is found that on an area-averaged basis, seasonal precipitation is balanced predominantly by evaporation; in addition, this evaporation also supports a net, vertically integrated moisture flux divergence from the region of the same magnitude as the precipitation itself. This vertically integrated large-scale moisture flux divergence is the result of an offsetting balance between convergence of low-level moisture and divergence of moisture aloft (<750 mb). Over the western portion of the domain, most of this low-level moisture convergence is related to advection from the Gulf of California and eastern Pacific; over the eastern portion of the domain, low-level moisture convergence is related to advection from the Gulf of Mexico. The low-level moisture, supplied both by evaporation and advection, is carried aloft primarily by convection (as opposed to large-scale vertical velocities), which then feeds both the precipitation and large-scale divergence fields. The large-scale divergence augments the anticyclonic circulation of moisture aloft, resulting in enhanced exiting fluxes over the Great Plains. A new metric for measuring recycling of moisture in convective semiarid areas is introduced; this metric is designed to better capture the importance of evaporative processes for supporting regional precipitation in these types of environments. Using this metric, it is shown that about 70%?90% of the area-averaged precipitation is the result of evaporative processes, while the remaining 10%?30% is related to low-level convergence of moisture.
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      The Summertime Atmospheric Hydrologic Cycle over the Southwestern United States

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4206395
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    contributor authorAnderson, Bruce T.
    contributor authorKanamaru, Hideki
    contributor authorRoads, John O.
    date accessioned2017-06-09T16:17:42Z
    date available2017-06-09T16:17:42Z
    date copyright2004/08/01
    date issued2004
    identifier issn1525-755X
    identifier otherams-65197.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4206395
    description abstractIn this paper the authors examine the large-scale summertime hydrologic cycle associated with the northwestern branch of the North American monsoon, centered on the southwestern United States, using a suite of surface-and upper-air-based observations, reanalysis products, and regional model simulations. In general, it is found that on an area-averaged basis, seasonal precipitation is balanced predominantly by evaporation; in addition, this evaporation also supports a net, vertically integrated moisture flux divergence from the region of the same magnitude as the precipitation itself. This vertically integrated large-scale moisture flux divergence is the result of an offsetting balance between convergence of low-level moisture and divergence of moisture aloft (<750 mb). Over the western portion of the domain, most of this low-level moisture convergence is related to advection from the Gulf of California and eastern Pacific; over the eastern portion of the domain, low-level moisture convergence is related to advection from the Gulf of Mexico. The low-level moisture, supplied both by evaporation and advection, is carried aloft primarily by convection (as opposed to large-scale vertical velocities), which then feeds both the precipitation and large-scale divergence fields. The large-scale divergence augments the anticyclonic circulation of moisture aloft, resulting in enhanced exiting fluxes over the Great Plains. A new metric for measuring recycling of moisture in convective semiarid areas is introduced; this metric is designed to better capture the importance of evaporative processes for supporting regional precipitation in these types of environments. Using this metric, it is shown that about 70%?90% of the area-averaged precipitation is the result of evaporative processes, while the remaining 10%?30% is related to low-level convergence of moisture.
    publisherAmerican Meteorological Society
    titleThe Summertime Atmospheric Hydrologic Cycle over the Southwestern United States
    typeJournal Paper
    journal volume5
    journal issue4
    journal titleJournal of Hydrometeorology
    identifier doi10.1175/1525-7541(2004)005<0679:TSAHCO>2.0.CO;2
    journal fristpage679
    journal lastpage692
    treeJournal of Hydrometeorology:;2004:;Volume( 005 ):;issue: 004
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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