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contributor authorHögström, U.
contributor authorSmedman, A.
contributor authorSahleé, E.
contributor authorDrennan, W. M.
contributor authorKahma, K. K.
contributor authorPettersson, H.
contributor authorZhang, F.
date accessioned2017-06-09T16:28:12Z
date available2017-06-09T16:28:12Z
date copyright2009/09/01
date issued2009
identifier issn0022-4928
identifier otherams-68433.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4209991
description abstractAnalysis of the turbulent kinetic energy (TKE) budget for five slightly unstable cases with swell has been performed based on measurements of mechanical production, buoyancy production, turbulent transport, and dissipation at five levels over the sea, from 2.5 to 26 m. The time rate of change and advection of TKE were found to be small, so the TKE residual is interpreted as an estimate of the pressure transport term (Tp). In two cases with high wave age, the Tp term is a gain at all heights. For three cases with smaller wave age, Tp is a loss in the TKE budget below 5?10 m and a gain for greater heights, where the decrease is exponential, thus showing the combined effects of swell waves and a range of waves traveling slower than the wind. The TKE budget for a case with growing sea but similar wind speed and stability as some of the swell cases has Tp close to zero at all heights. It is shown that the observed characteristic wind profile with either a low-level maximum in the 5?10-m range or a distinct ?knee? at that height is an effect of the Tp term.
publisherAmerican Meteorological Society
titleThe Atmospheric Boundary Layer during Swell: A Field Study and Interpretation of the Turbulent Kinetic Energy Budget for High Wave Ages
typeJournal Paper
journal volume66
journal issue9
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/2009JAS2973.1
journal fristpage2764
journal lastpage2779
treeJournal of the Atmospheric Sciences:;2009:;Volume( 066 ):;issue: 009
contenttypeFulltext


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