Numerical simulation of subsynoptic-scale cyclogenesis around an idealized Antarctic continent
Abstract: A three-dimensional numerical model of 100 km horizontal resolution was used to simulate subsynoptic-scale cyclogenesis around an idealized Antarctic continent. The simulation resolved a series of subsynoptic-scale cyclones around the idealized continent. These cyclones form adjacent to th...
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Universidad de Magallanes
2017
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oai:scielo:S0718-686X20170003000052018-02-22Numerical simulation of subsynoptic-scale cyclogenesis around an idealized Antarctic continentCarrasco,Jorge F. numerical model katabatic winds subsynoptic-scale cyclones instability Abstract: A three-dimensional numerical model of 100 km horizontal resolution was used to simulate subsynoptic-scale cyclogenesis around an idealized Antarctic continent. The simulation resolved a series of subsynoptic-scale cyclones around the idealized continent. These cyclones form adjacent to the confluence zones of katabatic winds. Their movements indicate an eastward direction going away from their initial point of formation. Baroclinic instability appears as primary mechanism for the development of these cyclones.info:eu-repo/semantics/openAccessUniversidad de MagallanesAnales del Instituto de la Patagonia v.45 n.3 20172017-12-01text/htmlhttp://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-686X2017000300005en10.4067/S0718-686X2017000300005 |
institution |
Scielo Chile |
collection |
Scielo Chile |
language |
English |
topic |
numerical model katabatic winds subsynoptic-scale cyclones instability |
spellingShingle |
numerical model katabatic winds subsynoptic-scale cyclones instability Carrasco,Jorge F. Numerical simulation of subsynoptic-scale cyclogenesis around an idealized Antarctic continent |
description |
Abstract: A three-dimensional numerical model of 100 km horizontal resolution was used to simulate subsynoptic-scale cyclogenesis around an idealized Antarctic continent. The simulation resolved a series of subsynoptic-scale cyclones around the idealized continent. These cyclones form adjacent to the confluence zones of katabatic winds. Their movements indicate an eastward direction going away from their initial point of formation. Baroclinic instability appears as primary mechanism for the development of these cyclones. |
author |
Carrasco,Jorge F. |
author_facet |
Carrasco,Jorge F. |
author_sort |
Carrasco,Jorge F. |
title |
Numerical simulation of subsynoptic-scale cyclogenesis around an idealized Antarctic continent |
title_short |
Numerical simulation of subsynoptic-scale cyclogenesis around an idealized Antarctic continent |
title_full |
Numerical simulation of subsynoptic-scale cyclogenesis around an idealized Antarctic continent |
title_fullStr |
Numerical simulation of subsynoptic-scale cyclogenesis around an idealized Antarctic continent |
title_full_unstemmed |
Numerical simulation of subsynoptic-scale cyclogenesis around an idealized Antarctic continent |
title_sort |
numerical simulation of subsynoptic-scale cyclogenesis around an idealized antarctic continent |
publisher |
Universidad de Magallanes |
publishDate |
2017 |
url |
http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-686X2017000300005 |
work_keys_str_mv |
AT carrascojorgef numericalsimulationofsubsynopticscalecyclogenesisaroundanidealizedantarcticcontinent |
_version_ |
1714205708662079488 |