Electronic Resource

AN ANALYSIS OF SOME WIND PROFILES IN THE ATMOS PHERIC FRICTION LAYER

التفاصيل البيبلوغرافية
العنوان: AN ANALYSIS OF SOME WIND PROFILES IN THE ATMOS PHERIC FRICTION LAYER
المؤلفون: AIR FORCE CAMBRIDGE RESEARCH LABS L G HANSCOM FIELD MASS, Taylor,R.J.
المصدر: DTIC AND NTIS
بيانات النشر: 1963-08
نوع الوثيقة: Electronic Resource
مستخلص: In the layer of atmosphere between the surface and a level where the wind is close to the geo strophic (the 'friction layer'), the assumption is commonly made that the shearing stress and velocity gradient are parallel. Theoretical rea sons are advanced to indicate that this assump tion is probably not valid and some analyses of observed wind profiles made on this assumption are shown to yield unrealistic results. Although the analyses are open to some criticism on the basis of instrumental inaccuracy and lack of horizontal uniformity of the observing site, the general conclusion is reached that paral lelism of stress and velocity gradient cannot, in our present state of knowledge, be relied upon. (Author)
مصطلحات الفهرس: (*WIND, STATISTICAL ANALYSIS), TURBULENT BOUNDARY LAYER, ATMOSPHERIC MOTION., FRICTION LAYER, GEOSTROPHIC WINDS, THERMAL WIND, Text
URL: https://apps.dtic.mil/docs/citations/AD0418503
الاتاحة: Open access content. Open access content
APPROVED FOR PUBLIC RELEASE
ملاحظة: text/html
English
Other Numbers: DTICE AD0418503
831448539
المصدر المساهم: From OAIster®, provided by the OCLC Cooperative.
رقم الانضمام: edsoai.ocn831448539
قاعدة البيانات: OAIster