Isentropic zonal average formalism and the near-surface circulation

The isentropic zonal average formalism is extended to include a rigorous treatment of the bottom boundary of the atmosphere. We define a ‘surface zone’, where isentropes in the latitudinal plane are interrupted by the earth's surface. The zonal average equations of motion and their time average...

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Main Authors: Koh, Tieh Yong., Plumb, R. Alan.
Other Authors: School of Physical and Mathematical Sciences
Format: Journal Article
Language:English
Published: 2013
Subjects:
Online Access:https://hdl.handle.net/10356/95692
http://hdl.handle.net/10220/8964
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author Koh, Tieh Yong.
Plumb, R. Alan.
author2 School of Physical and Mathematical Sciences
author_facet School of Physical and Mathematical Sciences
Koh, Tieh Yong.
Plumb, R. Alan.
author_sort Koh, Tieh Yong.
collection NTU
description The isentropic zonal average formalism is extended to include a rigorous treatment of the bottom boundary of the atmosphere. We define a ‘surface zone’, where isentropes in the latitudinal plane are interrupted by the earth's surface. The zonal average equations of motion and their time average in isentropic coordinates are rederived in the presence of the surface zone. Applying the extended formalism to a baroclinic wave model, we show that near-surface equatorward mean flow is driven by eastward surface form drag in isentropic coordinates, which in turn is related to poleward geostrophic potential temperature flux at the surface. A potential vorticity–potential temperature picture of extratropical general circulation dynamics above and within the surface zone is presented. We highlight the importance of poleward mean flow in the upper region of the surface zone and investigate the antisymmetric distribution of mean meridional mass flow about the median potential temperature of surface air.
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spelling ntu-10356/956922020-03-07T12:37:20Z Isentropic zonal average formalism and the near-surface circulation Koh, Tieh Yong. Plumb, R. Alan. School of Physical and Mathematical Sciences DRNTU::Science::Physics::Meteorology and climatology The isentropic zonal average formalism is extended to include a rigorous treatment of the bottom boundary of the atmosphere. We define a ‘surface zone’, where isentropes in the latitudinal plane are interrupted by the earth's surface. The zonal average equations of motion and their time average in isentropic coordinates are rederived in the presence of the surface zone. Applying the extended formalism to a baroclinic wave model, we show that near-surface equatorward mean flow is driven by eastward surface form drag in isentropic coordinates, which in turn is related to poleward geostrophic potential temperature flux at the surface. A potential vorticity–potential temperature picture of extratropical general circulation dynamics above and within the surface zone is presented. We highlight the importance of poleward mean flow in the upper region of the surface zone and investigate the antisymmetric distribution of mean meridional mass flow about the median potential temperature of surface air. 2013-01-30T09:06:58Z 2019-12-06T19:19:57Z 2013-01-30T09:06:58Z 2019-12-06T19:19:57Z 2004 2004 Journal Article Koh, T. Y., & Plumb, R. (2004). Isentropic zonal average formalism and the near-surface circulation. Quarterly Journal of the Royal Meteorological Society, 130(600), 1631-1653. https://hdl.handle.net/10356/95692 http://hdl.handle.net/10220/8964 10.1256/qj.02.219 en Quarterly journal of the royal meteorological society © 2004 Royal Meteorological Society.
spellingShingle DRNTU::Science::Physics::Meteorology and climatology
Koh, Tieh Yong.
Plumb, R. Alan.
Isentropic zonal average formalism and the near-surface circulation
title Isentropic zonal average formalism and the near-surface circulation
title_full Isentropic zonal average formalism and the near-surface circulation
title_fullStr Isentropic zonal average formalism and the near-surface circulation
title_full_unstemmed Isentropic zonal average formalism and the near-surface circulation
title_short Isentropic zonal average formalism and the near-surface circulation
title_sort isentropic zonal average formalism and the near surface circulation
topic DRNTU::Science::Physics::Meteorology and climatology
url https://hdl.handle.net/10356/95692
http://hdl.handle.net/10220/8964
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