2003: Extratropical Southern Hemisphere cyclones: Harbingers of climate change
In concert with a poleward shift in baroclinicity, the synoptic environment south of 408S appears to have changed significantly over recent decades. South of 408S and north of the Antarctic Ocean the number of cyclones has dramatically decreased, while over the Antarctic Ocean a modest increase has...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.464.2842 2023-05-15T13:51:38+02:00 2003: Extratropical Southern Hemisphere cyclones: Harbingers of climate change John C. Fyfe The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.464.2842 http://www.cccma.ec.gc.ca/papers/jfyfe/PDF/Fyfe2003a.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.464.2842 http://www.cccma.ec.gc.ca/papers/jfyfe/PDF/Fyfe2003a.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.cccma.ec.gc.ca/papers/jfyfe/PDF/Fyfe2003a.pdf text ftciteseerx 2016-01-08T06:48:40Z In concert with a poleward shift in baroclinicity, the synoptic environment south of 408S appears to have changed significantly over recent decades. South of 408S and north of the Antarctic Ocean the number of cyclones has dramatically decreased, while over the Antarctic Ocean a modest increase has occurred. A global climate model with anthropogenic forcing produces similar historical changes, and under a ‘‘business-as-usual’ ’ emissions scenario predicts that the number of sub-Antarctic Ocean cyclones will drop by over 30 % between now and century’s end. 1. Text Antarc* Antarctic Antarctic Ocean Unknown Antarctic Antarctic Ocean The Antarctic |
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English |
description |
In concert with a poleward shift in baroclinicity, the synoptic environment south of 408S appears to have changed significantly over recent decades. South of 408S and north of the Antarctic Ocean the number of cyclones has dramatically decreased, while over the Antarctic Ocean a modest increase has occurred. A global climate model with anthropogenic forcing produces similar historical changes, and under a ‘‘business-as-usual’ ’ emissions scenario predicts that the number of sub-Antarctic Ocean cyclones will drop by over 30 % between now and century’s end. 1. |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
John C. Fyfe |
spellingShingle |
John C. Fyfe 2003: Extratropical Southern Hemisphere cyclones: Harbingers of climate change |
author_facet |
John C. Fyfe |
author_sort |
John C. Fyfe |
title |
2003: Extratropical Southern Hemisphere cyclones: Harbingers of climate change |
title_short |
2003: Extratropical Southern Hemisphere cyclones: Harbingers of climate change |
title_full |
2003: Extratropical Southern Hemisphere cyclones: Harbingers of climate change |
title_fullStr |
2003: Extratropical Southern Hemisphere cyclones: Harbingers of climate change |
title_full_unstemmed |
2003: Extratropical Southern Hemisphere cyclones: Harbingers of climate change |
title_sort |
2003: extratropical southern hemisphere cyclones: harbingers of climate change |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.464.2842 http://www.cccma.ec.gc.ca/papers/jfyfe/PDF/Fyfe2003a.pdf |
geographic |
Antarctic Antarctic Ocean The Antarctic |
geographic_facet |
Antarctic Antarctic Ocean The Antarctic |
genre |
Antarc* Antarctic Antarctic Ocean |
genre_facet |
Antarc* Antarctic Antarctic Ocean |
op_source |
http://www.cccma.ec.gc.ca/papers/jfyfe/PDF/Fyfe2003a.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.464.2842 http://www.cccma.ec.gc.ca/papers/jfyfe/PDF/Fyfe2003a.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766255604860452864 |