WMO/CAS/WWW SIXTH INTERNATIONAL WORKSHOP on TROPICAL CYCLONES Topic 2a: The Catarina Phenomenon Rapporteur:
Sea Surface Temperatures (SSTs) warmer than 26.5 o C and Environmental Vertical Wind Shear (EVWS, defined as the magnitude of the difference between the 200 and 850 hPa vector winds) lower than 8 m/s offer ideal conditions for Tropical Cyclone (TC) development. Thus it has been accepted that hurrica...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.175.5041 2023-05-15T18:20:51+02:00 WMO/CAS/WWW SIXTH INTERNATIONAL WORKSHOP on TROPICAL CYCLONES Topic 2a: The Catarina Phenomenon Rapporteur: Pedro L. Silva Dias Manoel Gan John L. Beven Re Pezza Greg Holl Augusto Pereira Francisco De Assis Diniz Marcelo Seluchi Hugo J. Braga The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.175.5041 http://severe.worldweather.org/iwtc/document/Topic_2a_Pedro_Silva_Dias.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.175.5041 http://severe.worldweather.org/iwtc/document/Topic_2a_Pedro_Silva_Dias.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://severe.worldweather.org/iwtc/document/Topic_2a_Pedro_Silva_Dias.pdf text ftciteseerx 2016-01-07T16:12:41Z Sea Surface Temperatures (SSTs) warmer than 26.5 o C and Environmental Vertical Wind Shear (EVWS, defined as the magnitude of the difference between the 200 and 850 hPa vector winds) lower than 8 m/s offer ideal conditions for Tropical Cyclone (TC) development. Thus it has been accepted that hurricanes could not form over the South Atlantic Ocean due to the very intense climatological vertical wind shear Text South Atlantic Ocean Unknown |
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English |
description |
Sea Surface Temperatures (SSTs) warmer than 26.5 o C and Environmental Vertical Wind Shear (EVWS, defined as the magnitude of the difference between the 200 and 850 hPa vector winds) lower than 8 m/s offer ideal conditions for Tropical Cyclone (TC) development. Thus it has been accepted that hurricanes could not form over the South Atlantic Ocean due to the very intense climatological vertical wind shear |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Pedro L. Silva Dias Manoel Gan John L. Beven Re Pezza Greg Holl Augusto Pereira Francisco De Assis Diniz Marcelo Seluchi Hugo J. Braga |
spellingShingle |
Pedro L. Silva Dias Manoel Gan John L. Beven Re Pezza Greg Holl Augusto Pereira Francisco De Assis Diniz Marcelo Seluchi Hugo J. Braga WMO/CAS/WWW SIXTH INTERNATIONAL WORKSHOP on TROPICAL CYCLONES Topic 2a: The Catarina Phenomenon Rapporteur: |
author_facet |
Pedro L. Silva Dias Manoel Gan John L. Beven Re Pezza Greg Holl Augusto Pereira Francisco De Assis Diniz Marcelo Seluchi Hugo J. Braga |
author_sort |
Pedro L. Silva Dias |
title |
WMO/CAS/WWW SIXTH INTERNATIONAL WORKSHOP on TROPICAL CYCLONES Topic 2a: The Catarina Phenomenon Rapporteur: |
title_short |
WMO/CAS/WWW SIXTH INTERNATIONAL WORKSHOP on TROPICAL CYCLONES Topic 2a: The Catarina Phenomenon Rapporteur: |
title_full |
WMO/CAS/WWW SIXTH INTERNATIONAL WORKSHOP on TROPICAL CYCLONES Topic 2a: The Catarina Phenomenon Rapporteur: |
title_fullStr |
WMO/CAS/WWW SIXTH INTERNATIONAL WORKSHOP on TROPICAL CYCLONES Topic 2a: The Catarina Phenomenon Rapporteur: |
title_full_unstemmed |
WMO/CAS/WWW SIXTH INTERNATIONAL WORKSHOP on TROPICAL CYCLONES Topic 2a: The Catarina Phenomenon Rapporteur: |
title_sort |
wmo/cas/www sixth international workshop on tropical cyclones topic 2a: the catarina phenomenon rapporteur: |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.175.5041 http://severe.worldweather.org/iwtc/document/Topic_2a_Pedro_Silva_Dias.pdf |
genre |
South Atlantic Ocean |
genre_facet |
South Atlantic Ocean |
op_source |
http://severe.worldweather.org/iwtc/document/Topic_2a_Pedro_Silva_Dias.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.175.5041 http://severe.worldweather.org/iwtc/document/Topic_2a_Pedro_Silva_Dias.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766199440851337216 |