A Mathematical Model of Sea Breezes Along the Alaskan Beaufort Sea Coast: Part IISource: Journal of Applied Meteorology:;1982:;volume( 021 ):;issue: 007::page 906Author:Kozo, Thomas L.
DOI: 10.1175/1520-0450(1982)021<0906:AMMOSB>2.0.CO;2Publisher: American Meteorological Society
Abstract: A nonlinear, time-dependent, two-dimensional sea breeze model allowing imposition of prevailing large-scale wind conditions has been developed. The model is an extension of Estoque's model with modifications in the treatment of the continuity equation, eddy diffusivity (unstable conditions), surface heating function and the numerical scheme. The model is applied to a cross section of the Beaufort Sea Coast using typically measured arctic conditions as input. These include u-w plane velocity vectors, isotachs of the u, v and w wind velocity components, temperature contours, surface wind vectors at varying distances from the coastline, and wind speed and direction profiles for various simulated synoptic wind directions. The mathematical results reproduced measurements of atmospheric boundary layer turning of the wind with height (pilot balloon data), temporal surface wind vector turning and inversion height variations, while also giving evidence that sea breeze circulation could be strengthened by weak offshore (southwesterly and westerly winds) opposing synoptic winds.
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contributor author | Kozo, Thomas L. | |
date accessioned | 2017-06-09T13:58:51Z | |
date available | 2017-06-09T13:58:51Z | |
date copyright | 1982/07/01 | |
date issued | 1982 | |
identifier issn | 0021-8952 | |
identifier other | ams-10296.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4145397 | |
description abstract | A nonlinear, time-dependent, two-dimensional sea breeze model allowing imposition of prevailing large-scale wind conditions has been developed. The model is an extension of Estoque's model with modifications in the treatment of the continuity equation, eddy diffusivity (unstable conditions), surface heating function and the numerical scheme. The model is applied to a cross section of the Beaufort Sea Coast using typically measured arctic conditions as input. These include u-w plane velocity vectors, isotachs of the u, v and w wind velocity components, temperature contours, surface wind vectors at varying distances from the coastline, and wind speed and direction profiles for various simulated synoptic wind directions. The mathematical results reproduced measurements of atmospheric boundary layer turning of the wind with height (pilot balloon data), temporal surface wind vector turning and inversion height variations, while also giving evidence that sea breeze circulation could be strengthened by weak offshore (southwesterly and westerly winds) opposing synoptic winds. | |
publisher | American Meteorological Society | |
title | A Mathematical Model of Sea Breezes Along the Alaskan Beaufort Sea Coast: Part II | |
type | Journal Paper | |
journal volume | 21 | |
journal issue | 7 | |
journal title | Journal of Applied Meteorology | |
identifier doi | 10.1175/1520-0450(1982)021<0906:AMMOSB>2.0.CO;2 | |
journal fristpage | 906 | |
journal lastpage | 924 | |
tree | Journal of Applied Meteorology:;1982:;volume( 021 ):;issue: 007 | |
contenttype | Fulltext |