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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Main Author: John C. Fyfe
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.464.2842
http://www.cccma.ec.gc.ca/papers/jfyfe/PDF/Fyfe2003a.pdf
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spelling 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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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.
author2 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
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Antarctic Ocean
The Antarctic
genre Antarc*
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genre_facet Antarc*
Antarctic
Antarctic Ocean
op_source http://www.cccma.ec.gc.ca/papers/jfyfe/PDF/Fyfe2003a.pdf
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http://www.cccma.ec.gc.ca/papers/jfyfe/PDF/Fyfe2003a.pdf
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