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contributor authorVan de Wiel, B. J. H.
contributor authorMoene, A. F.
contributor authorSteeneveld, G. J.
contributor authorBaas, P.
contributor authorBosveld, F. C.
contributor authorHoltslag, A. A. M.
date accessioned2017-06-09T16:34:13Z
date available2017-06-09T16:34:13Z
date copyright2010/08/01
date issued2010
identifier issn0022-4928
identifier otherams-70165.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4211916
description abstractIn the present work Blackadar?s concept of nocturnal inertial oscillations is extended. Blackadar?s concept describes frictionless inertial oscillations above the nocturnal inversion layer. The current work includes frictional effects within the nocturnal boundary layer. It is shown that the nocturnal wind speed profile describes an oscillation around the nocturnal equilibrium wind vector, rather than around the geostrophic wind vector (as in the Blackadar case). By using this perspective, continuous time-dependent wind profiles are predicted. As such, information on both the height and the magnitude of the nocturnal low-level jet is available as a function of time. Preliminary analysis shows that the proposed extension performs well in comparison with observations when a simple Ekman model is used to represent the equilibrium state in combination with a realistic initial velocity profile. In addition to jet dynamics, backward inertial oscillations are predicted at lower levels close to the surface, which also appear to be present in observations. The backward oscillation forms an important mechanism behind weakening low-level winds during the afternoon transition. Both observational and theoretical modeling studies are needed to explore this phenomenon further.
publisherAmerican Meteorological Society
titleA Conceptual View on Inertial Oscillations and Nocturnal Low-Level Jets
typeJournal Paper
journal volume67
journal issue8
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/2010JAS3289.1
journal fristpage2679
journal lastpage2689
treeJournal of the Atmospheric Sciences:;2010:;Volume( 067 ):;issue: 008
contenttypeFulltext


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