Short-term climatic fluctuations forced by thermal anomalies
A two level, global, spectral model using pressure as a vertical coordinate was developed. The system of equations describing the model is nonlinear and quasi-geostrophic (linear balance). Static stability is variable in the model. A moisture budget is calculated in the lower layer only. Convective...
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ftnasantrs:oai:casi.ntrs.nasa.gov:19840042956 2023-05-15T18:18:15+02:00 Short-term climatic fluctuations forced by thermal anomalies Hanna, A. F. Stevens, D. E. Reiter, E. R. Unclassified, Unlimited, Publicly available Jan 1, 1984 http://ntrs.nasa.gov/search.jsp?R=19840042956 unknown http://ntrs.nasa.gov/search.jsp?R=19840042956 Accession ID: 84A25743 Copyright Other Sources 47 Journal of the Atmospheric Sciences; 41; 122-141 1984 ftnasantrs 2012-02-15T15:51:12Z A two level, global, spectral model using pressure as a vertical coordinate was developed. The system of equations describing the model is nonlinear and quasi-geostrophic (linear balance). Static stability is variable in the model. A moisture budget is calculated in the lower layer only. Convective adjustment is used to avoid supercritical temperature lapse rates. The mechanical forcing of topography is introduced as a vertical velocity at the lower boundary. Solar forcing is specified assuming a daily mean zenith angle. The differential diabatic heating between land and sea is parameterized. On land and sea ice surfaces, a steady state thermal energy equation is solved to calculate the surface temperature. On the oceans, the sea surface temperature is specified as the climatological average for January. The model is used to simulate the January, February and March circulations. Previously announced in STAR as N83-14822 Other/Unknown Material Sea ice NASA Technical Reports Server (NTRS) |
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Open Polar |
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NASA Technical Reports Server (NTRS) |
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ftnasantrs |
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unknown |
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47 |
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47 Hanna, A. F. Stevens, D. E. Reiter, E. R. Short-term climatic fluctuations forced by thermal anomalies |
topic_facet |
47 |
description |
A two level, global, spectral model using pressure as a vertical coordinate was developed. The system of equations describing the model is nonlinear and quasi-geostrophic (linear balance). Static stability is variable in the model. A moisture budget is calculated in the lower layer only. Convective adjustment is used to avoid supercritical temperature lapse rates. The mechanical forcing of topography is introduced as a vertical velocity at the lower boundary. Solar forcing is specified assuming a daily mean zenith angle. The differential diabatic heating between land and sea is parameterized. On land and sea ice surfaces, a steady state thermal energy equation is solved to calculate the surface temperature. On the oceans, the sea surface temperature is specified as the climatological average for January. The model is used to simulate the January, February and March circulations. Previously announced in STAR as N83-14822 |
format |
Other/Unknown Material |
author |
Hanna, A. F. Stevens, D. E. Reiter, E. R. |
author_facet |
Hanna, A. F. Stevens, D. E. Reiter, E. R. |
author_sort |
Hanna, A. F. |
title |
Short-term climatic fluctuations forced by thermal anomalies |
title_short |
Short-term climatic fluctuations forced by thermal anomalies |
title_full |
Short-term climatic fluctuations forced by thermal anomalies |
title_fullStr |
Short-term climatic fluctuations forced by thermal anomalies |
title_full_unstemmed |
Short-term climatic fluctuations forced by thermal anomalies |
title_sort |
short-term climatic fluctuations forced by thermal anomalies |
publishDate |
1984 |
url |
http://ntrs.nasa.gov/search.jsp?R=19840042956 |
op_coverage |
Unclassified, Unlimited, Publicly available |
genre |
Sea ice |
genre_facet |
Sea ice |
op_source |
Other Sources |
op_relation |
http://ntrs.nasa.gov/search.jsp?R=19840042956 Accession ID: 84A25743 |
op_rights |
Copyright |
_version_ |
1766194758647021568 |