Deep convection in the Arctic: The evaluation of results from an OGCM with a new convection parameterization
The current generation of ocean general circulation models (OGCMS) uses a convective adjustment scheme to remove static instabilities and to parameterize shallow and deep convection. In simulations used to examine climate-related scenarios, investigators found that in the Arctic regions, the OGCM si...
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Pacific Northwest Laboratory
1995
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ftunivnotexas:info:ark/67531/metadc676684 2023-05-15T14:52:32+02:00 Deep convection in the Arctic: The evaluation of results from an OGCM with a new convection parameterization Paluszkiewicz, T. Hibler, L.F. Romea, R.D. United States. Department of Energy. 1995-01-01 7 p. Text http://digital.library.unt.edu/ark:/67531/metadc676684/ English eng Pacific Northwest Laboratory other: DE95008927 rep-no: PNL-SA--25416 rep-no: CONF-950153--2 grantno: AC06-76RL01830 osti: 35357 http://digital.library.unt.edu/ark:/67531/metadc676684/ ark: ark:/67531/metadc676684 4. conference on polar meteorology and oceanography, Dallas, TX (United States), 15-20 Jan 1995 Oceanic Circulation Seas General Circulation Models Stratification 54 Environmental Sciences Parametric Analysis Convection Arctic Regions Accuracy Article 1995 ftunivnotexas 2016-04-09T22:11:18Z The current generation of ocean general circulation models (OGCMS) uses a convective adjustment scheme to remove static instabilities and to parameterize shallow and deep convection. In simulations used to examine climate-related scenarios, investigators found that in the Arctic regions, the OGCM simulations did not produce a realistic vertical density structure, did not create the correct quantity of deep water, and did not use a time-scale of adjustment that is in agreement with tracer ages or observations. A possible weakness of the models is that the convective adjustment scheme does not represent the process of deep convection adequately. Consequently, a penetrative plume mixing scheme has been developed to parameterize the process of deep open-ocean convection in OGCMS. This new deep convection parameterization was incorporated into the Semtner and Chervin (1988) OGCM. The modified model (with the new parameterization) was run in a simplified Nordic Seas test basin: under a cyclonic wind stress and cooling, stratification of the basin-scale gyre is eroded and deep mixing occurs in the center of the gyre. In contrast, in the OGCM experiment that uses the standard convective adjustment algorithm, mixing is delayed and is wide-spread over the gyre. Article in Journal/Newspaper Arctic Nordic Seas University of North Texas: UNT Digital Library Arctic |
institution |
Open Polar |
collection |
University of North Texas: UNT Digital Library |
op_collection_id |
ftunivnotexas |
language |
English |
topic |
Oceanic Circulation Seas General Circulation Models Stratification 54 Environmental Sciences Parametric Analysis Convection Arctic Regions Accuracy |
spellingShingle |
Oceanic Circulation Seas General Circulation Models Stratification 54 Environmental Sciences Parametric Analysis Convection Arctic Regions Accuracy Paluszkiewicz, T. Hibler, L.F. Romea, R.D. Deep convection in the Arctic: The evaluation of results from an OGCM with a new convection parameterization |
topic_facet |
Oceanic Circulation Seas General Circulation Models Stratification 54 Environmental Sciences Parametric Analysis Convection Arctic Regions Accuracy |
description |
The current generation of ocean general circulation models (OGCMS) uses a convective adjustment scheme to remove static instabilities and to parameterize shallow and deep convection. In simulations used to examine climate-related scenarios, investigators found that in the Arctic regions, the OGCM simulations did not produce a realistic vertical density structure, did not create the correct quantity of deep water, and did not use a time-scale of adjustment that is in agreement with tracer ages or observations. A possible weakness of the models is that the convective adjustment scheme does not represent the process of deep convection adequately. Consequently, a penetrative plume mixing scheme has been developed to parameterize the process of deep open-ocean convection in OGCMS. This new deep convection parameterization was incorporated into the Semtner and Chervin (1988) OGCM. The modified model (with the new parameterization) was run in a simplified Nordic Seas test basin: under a cyclonic wind stress and cooling, stratification of the basin-scale gyre is eroded and deep mixing occurs in the center of the gyre. In contrast, in the OGCM experiment that uses the standard convective adjustment algorithm, mixing is delayed and is wide-spread over the gyre. |
author2 |
United States. Department of Energy. |
format |
Article in Journal/Newspaper |
author |
Paluszkiewicz, T. Hibler, L.F. Romea, R.D. |
author_facet |
Paluszkiewicz, T. Hibler, L.F. Romea, R.D. |
author_sort |
Paluszkiewicz, T. |
title |
Deep convection in the Arctic: The evaluation of results from an OGCM with a new convection parameterization |
title_short |
Deep convection in the Arctic: The evaluation of results from an OGCM with a new convection parameterization |
title_full |
Deep convection in the Arctic: The evaluation of results from an OGCM with a new convection parameterization |
title_fullStr |
Deep convection in the Arctic: The evaluation of results from an OGCM with a new convection parameterization |
title_full_unstemmed |
Deep convection in the Arctic: The evaluation of results from an OGCM with a new convection parameterization |
title_sort |
deep convection in the arctic: the evaluation of results from an ogcm with a new convection parameterization |
publisher |
Pacific Northwest Laboratory |
publishDate |
1995 |
url |
http://digital.library.unt.edu/ark:/67531/metadc676684/ |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Nordic Seas |
genre_facet |
Arctic Nordic Seas |
op_source |
4. conference on polar meteorology and oceanography, Dallas, TX (United States), 15-20 Jan 1995 |
op_relation |
other: DE95008927 rep-no: PNL-SA--25416 rep-no: CONF-950153--2 grantno: AC06-76RL01830 osti: 35357 http://digital.library.unt.edu/ark:/67531/metadc676684/ ark: ark:/67531/metadc676684 |
_version_ |
1766323773789700096 |