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    A Comparison of the Terrain Height Variance Spectra of the Front Range with that of a Hypothetical Mountain

    Source: Journal of the Atmospheric Sciences:;1984:;Volume( 041 ):;issue: 007::page 1249
    Author:
    Young, George S.
    ,
    Pielke, Roger A.
    ,
    Kessler, Robert C.
    DOI: 10.1175/1520-0469(1984)041<1249:ACOTTH>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The one-dimensional terrain height variance spectra of the Front Range west of Boulder, Colorado, is compared with that of the hypothetical two-dimensional mountain used by several investigators in their modeling studies of downslope winds. The terrain height variance of the hypothetical mountain exceeds that of the Front Range on scales longer than 25 km. On shorter scales, the terrain height variance of the hypothetical mountain decreases at an unrealistic rate. The scales at which terrain features of the Front Range can be considered approximately two-dimensional are determined. On scales longer than 25 km, the Front Range is essentially two-dimensional. However, on shorter scales, the Front Range exhibits equal variance in the along-range and cross-range directions.
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      A Comparison of the Terrain Height Variance Spectra of the Front Range with that of a Hypothetical Mountain

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4154855
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    contributor authorYoung, George S.
    contributor authorPielke, Roger A.
    contributor authorKessler, Robert C.
    date accessioned2017-06-09T14:24:46Z
    date available2017-06-09T14:24:46Z
    date copyright1984/04/01
    date issued1984
    identifier issn0022-4928
    identifier otherams-18809.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4154855
    description abstractThe one-dimensional terrain height variance spectra of the Front Range west of Boulder, Colorado, is compared with that of the hypothetical two-dimensional mountain used by several investigators in their modeling studies of downslope winds. The terrain height variance of the hypothetical mountain exceeds that of the Front Range on scales longer than 25 km. On shorter scales, the terrain height variance of the hypothetical mountain decreases at an unrealistic rate. The scales at which terrain features of the Front Range can be considered approximately two-dimensional are determined. On scales longer than 25 km, the Front Range is essentially two-dimensional. However, on shorter scales, the Front Range exhibits equal variance in the along-range and cross-range directions.
    publisherAmerican Meteorological Society
    titleA Comparison of the Terrain Height Variance Spectra of the Front Range with that of a Hypothetical Mountain
    typeJournal Paper
    journal volume41
    journal issue7
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1984)041<1249:ACOTTH>2.0.CO;2
    journal fristpage1249
    journal lastpage1250
    treeJournal of the Atmospheric Sciences:;1984:;Volume( 041 ):;issue: 007
    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