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    A Method of Determination of Dynamic Influence of the Forest on the Boundary Layer Using Two Doppler Sodars

    Source: Journal of Applied Meteorology:;1989:;volume( 028 ):;issue: 008::page 705
    Author:
    Mazaudier, Christine
    ,
    Weill, Alain
    DOI: 10.1175/1520-0450(1989)028<0705:AMODOD>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Doppler sodar soundings of wind velocities were routinely performed during the intensive phase of the HAPEX?MOBILHY experiment over two different canopies: forested and bare ground. The purpose of the experiment was to observe the turbulent frictional effect induced by the forest canopy. Different effects were observed: 1) the frictional forest effect depends on the magnitude and direction of the wind system; and 2) the wind speed reduction over the forest is observed up to heights equal to or greater than 65 m. In the layer from the top of the trees (19 m) up to 50 m the speed is reduced by 30%?60%. Above 50 m, the wind speed is reduced by 10%?15%. These observations are consistent with an estimated forest surface layer thickness of 30 m. Finally this paper proposes a method to derive the differential ?forested/unforested? turbulent friction from data.
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      A Method of Determination of Dynamic Influence of the Forest on the Boundary Layer Using Two Doppler Sodars

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4146700
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    contributor authorMazaudier, Christine
    contributor authorWeill, Alain
    date accessioned2017-06-09T14:02:47Z
    date available2017-06-09T14:02:47Z
    date copyright1989/08/01
    date issued1989
    identifier issn0894-8763
    identifier otherams-11469.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4146700
    description abstractDoppler sodar soundings of wind velocities were routinely performed during the intensive phase of the HAPEX?MOBILHY experiment over two different canopies: forested and bare ground. The purpose of the experiment was to observe the turbulent frictional effect induced by the forest canopy. Different effects were observed: 1) the frictional forest effect depends on the magnitude and direction of the wind system; and 2) the wind speed reduction over the forest is observed up to heights equal to or greater than 65 m. In the layer from the top of the trees (19 m) up to 50 m the speed is reduced by 30%?60%. Above 50 m, the wind speed is reduced by 10%?15%. These observations are consistent with an estimated forest surface layer thickness of 30 m. Finally this paper proposes a method to derive the differential ?forested/unforested? turbulent friction from data.
    publisherAmerican Meteorological Society
    titleA Method of Determination of Dynamic Influence of the Forest on the Boundary Layer Using Two Doppler Sodars
    typeJournal Paper
    journal volume28
    journal issue8
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1989)028<0705:AMODOD>2.0.CO;2
    journal fristpage705
    journal lastpage710
    treeJournal of Applied Meteorology:;1989:;volume( 028 ):;issue: 008
    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
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