Diabatic quasi-geostrophic surface frontogenesis.

P. R. Bannon; M. Mak

doi:10.1175/1520-0469(1984)041<2189:DQGSF>2.0.CO;2

Diabatic quasi-geostrophic surface frontogenesis.

P. R. Bannon, M. Mak

Meteorology and Atmospheric Science

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4 Scopus citations

Abstract

Diabatic processes are included in a quasi-geostrophic model of surface frontogenesis due to an imposed horizontal deformation field. Analytic solutions are found for prescribed heating and for conditional instability of the second kind parameterizations of cumulus convection. The solutions for prescribed heating show that condensational heating has no direct effect on the surface potential temperature field. -from Authors

Original language	English (US)
Pages (from-to)	2189-2201
Number of pages	13
Journal	Journal of the Atmospheric Sciences
Volume	41
Issue number	14
DOIs	https://doi.org/10.1175/1520-0469(1984)041<2189:DQGSF>2.0.CO;2
State	Published - 1984

All Science Journal Classification (ASJC) codes

Atmospheric Science

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10.1175/1520-0469(1984)041<2189:DQGSF>2.0.CO;2

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title = "Diabatic quasi-geostrophic surface frontogenesis.",

abstract = "Diabatic processes are included in a quasi-geostrophic model of surface frontogenesis due to an imposed horizontal deformation field. Analytic solutions are found for prescribed heating and for conditional instability of the second kind parameterizations of cumulus convection. The solutions for prescribed heating show that condensational heating has no direct effect on the surface potential temperature field. -from Authors",

author = "Bannon, {P. R.} and M. Mak",

year = "1984",

doi = "10.1175/1520-0469(1984)041<2189:DQGSF>2.0.CO;2",

language = "English (US)",

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journal = "Journal of the Atmospheric Sciences",

issn = "0022-4928",

publisher = "American Meteorological Society",

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T1 - Diabatic quasi-geostrophic surface frontogenesis.

AU - Bannon, P. R.

AU - Mak, M.

PY - 1984

Y1 - 1984

N2 - Diabatic processes are included in a quasi-geostrophic model of surface frontogenesis due to an imposed horizontal deformation field. Analytic solutions are found for prescribed heating and for conditional instability of the second kind parameterizations of cumulus convection. The solutions for prescribed heating show that condensational heating has no direct effect on the surface potential temperature field. -from Authors

AB - Diabatic processes are included in a quasi-geostrophic model of surface frontogenesis due to an imposed horizontal deformation field. Analytic solutions are found for prescribed heating and for conditional instability of the second kind parameterizations of cumulus convection. The solutions for prescribed heating show that condensational heating has no direct effect on the surface potential temperature field. -from Authors

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U2 - 10.1175/1520-0469(1984)041<2189:DQGSF>2.0.CO;2

DO - 10.1175/1520-0469(1984)041<2189:DQGSF>2.0.CO;2

M3 - Article

AN - SCOPUS:0021638930

SN - 0022-4928

VL - 41

SP - 2189

EP - 2201

JO - Journal of the Atmospheric Sciences

JF - Journal of the Atmospheric Sciences

IS - 14

ER -

Diabatic quasi-geostrophic surface frontogenesis.

Abstract

All Science Journal Classification (ASJC) codes

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