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    Inconsistencies in the “New” Windchill Chart at Low Wind Speeds

    Source: Journal of Applied Meteorology and Climatology:;2006:;volume( 045 ):;issue: 005::page 787
    Author:
    Shitzer, Avraham
    ,
    de Dear, Richard
    DOI: 10.1175/JAM2373.1
    Publisher: American Meteorological Society
    Abstract: An apparent error was detected in the calculation of windchill equivalent temperatures (WCETs) in the ?new? chart and corresponding equation that were adopted in 2001 by the weather services in the United States and Canada. The problem is caused by significant discontinuities in WCETs at the assumed ?calm? wind speed condition of 1.34 m s?1. As a result, published WCETs are not equal to, as they should be by definition, but are lower than air temperatures at the assumed calm wind speed condition. This inconsistency further propagates to higher wind speeds beyond the assumed calm condition. In this paper, a straightforward correction is proposed to circumvent these inconsistencies of the new windchill. The proposed correction makes this transition gradual rather than abrupt by applying it to the expression used for estimating the effects of wind on the convective heat exchange coefficient between humans and their cold and windy environment.
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      Inconsistencies in the “New” Windchill Chart at Low Wind Speeds

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4216517
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    contributor authorShitzer, Avraham
    contributor authorde Dear, Richard
    date accessioned2017-06-09T16:47:54Z
    date available2017-06-09T16:47:54Z
    date copyright2006/05/01
    date issued2006
    identifier issn1558-8424
    identifier otherams-74306.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4216517
    description abstractAn apparent error was detected in the calculation of windchill equivalent temperatures (WCETs) in the ?new? chart and corresponding equation that were adopted in 2001 by the weather services in the United States and Canada. The problem is caused by significant discontinuities in WCETs at the assumed ?calm? wind speed condition of 1.34 m s?1. As a result, published WCETs are not equal to, as they should be by definition, but are lower than air temperatures at the assumed calm wind speed condition. This inconsistency further propagates to higher wind speeds beyond the assumed calm condition. In this paper, a straightforward correction is proposed to circumvent these inconsistencies of the new windchill. The proposed correction makes this transition gradual rather than abrupt by applying it to the expression used for estimating the effects of wind on the convective heat exchange coefficient between humans and their cold and windy environment.
    publisherAmerican Meteorological Society
    titleInconsistencies in the “New” Windchill Chart at Low Wind Speeds
    typeJournal Paper
    journal volume45
    journal issue5
    journal titleJournal of Applied Meteorology and Climatology
    identifier doi10.1175/JAM2373.1
    journal fristpage787
    journal lastpage790
    treeJournal of Applied Meteorology and Climatology:;2006:;volume( 045 ):;issue: 005
    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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