The Structure, Energetics and Propagation of Rotating Convective Storms. Part I: Energy Exchange with the Mean FlowSource: Journal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 002::page 113Author:Lilly, Douglas K.
DOI: 10.1175/1520-0469(1986)043<0113:TSEAPO>2.0.CO;2Publisher: American Meteorological Society
Abstract: A three-dimensional buoyant convective element responds to the existence of mean vertical shear by developing rotation about a vertical axis, with the rotational kinetic energy abstracted from that of the mean flow. This process is illustrated with the aid of linear analysis. From consideration of nonlinear processes it is concluded that a portion of the rotational energy is transformed into that of the overturning velocity field, thus enhancing further buoyant energy release. The storm structure which is optimal for energy transfer from the mean flow to rotational disturbances is a single updraft propagating with the mean flow and with counter-rotating vortices on both sides. The transfer of energy from rotational to overturning modes is, however, optimized by laterally propagating updrafts with coincident vortices.
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contributor author | Lilly, Douglas K. | |
date accessioned | 2017-06-09T14:26:10Z | |
date available | 2017-06-09T14:26:10Z | |
date copyright | 1986/01/01 | |
date issued | 1986 | |
identifier issn | 0022-4928 | |
identifier other | ams-19212.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4155304 | |
description abstract | A three-dimensional buoyant convective element responds to the existence of mean vertical shear by developing rotation about a vertical axis, with the rotational kinetic energy abstracted from that of the mean flow. This process is illustrated with the aid of linear analysis. From consideration of nonlinear processes it is concluded that a portion of the rotational energy is transformed into that of the overturning velocity field, thus enhancing further buoyant energy release. The storm structure which is optimal for energy transfer from the mean flow to rotational disturbances is a single updraft propagating with the mean flow and with counter-rotating vortices on both sides. The transfer of energy from rotational to overturning modes is, however, optimized by laterally propagating updrafts with coincident vortices. | |
publisher | American Meteorological Society | |
title | The Structure, Energetics and Propagation of Rotating Convective Storms. Part I: Energy Exchange with the Mean Flow | |
type | Journal Paper | |
journal volume | 43 | |
journal issue | 2 | |
journal title | Journal of the Atmospheric Sciences | |
identifier doi | 10.1175/1520-0469(1986)043<0113:TSEAPO>2.0.CO;2 | |
journal fristpage | 113 | |
journal lastpage | 125 | |
tree | Journal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 002 | |
contenttype | Fulltext |