Precipitation and Northern Hemisphere regimes ...
Rainfall anomalies in a longterm integration of general circulation model highlight the non-stationarity of the ocean–atmosphere coupling in the North Atlantic which becomes manifest in two regimes. Anti-correlations between the precipitation in the tropical and subtropical western Atlantic illustra...
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ftdatacite:10.48350/158572 2024-09-15T18:20:47+00:00 Precipitation and Northern Hemisphere regimes ... Raible, Christoph C. Luksch, Ute Fraedrich, Klaus 2004 https://dx.doi.org/10.48350/158572 https://boris.unibe.ch/158572/ unknown Royal Meteorological Society restricted access publisher holds copyright http://purl.org/coar/access_right/c_16ec 530 Physics Text ScholarlyArticle article-journal journal article 2004 ftdatacite https://doi.org/10.48350/158572 2024-09-02T10:17:31Z Rainfall anomalies in a longterm integration of general circulation model highlight the non-stationarity of the ocean–atmosphere coupling in the North Atlantic which becomes manifest in two regimes. Anti-correlations between the precipitation in the tropical and subtropical western Atlantic illustrate the changes of the Hadley cell with El Niño/Southern Oscillation (ENSO).The precipitation anomaly pattern in the north eastern Atlantic resembles variations of the North Atlantic storm track and the North Atlantic Oscillation (NAO). In the hemispheric regime, where 40% of the NAO variability can be explained by ENSO, both precipitation pattern are connected, whereas in the regional regime the ENSO-link with the North Atlantic storm track and the subtropical 500 hPa geopotential height disappears. ... Text North Atlantic North Atlantic oscillation DataCite |
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530 Physics Raible, Christoph C. Luksch, Ute Fraedrich, Klaus Precipitation and Northern Hemisphere regimes ... |
topic_facet |
530 Physics |
description |
Rainfall anomalies in a longterm integration of general circulation model highlight the non-stationarity of the ocean–atmosphere coupling in the North Atlantic which becomes manifest in two regimes. Anti-correlations between the precipitation in the tropical and subtropical western Atlantic illustrate the changes of the Hadley cell with El Niño/Southern Oscillation (ENSO).The precipitation anomaly pattern in the north eastern Atlantic resembles variations of the North Atlantic storm track and the North Atlantic Oscillation (NAO). In the hemispheric regime, where 40% of the NAO variability can be explained by ENSO, both precipitation pattern are connected, whereas in the regional regime the ENSO-link with the North Atlantic storm track and the subtropical 500 hPa geopotential height disappears. ... |
format |
Text |
author |
Raible, Christoph C. Luksch, Ute Fraedrich, Klaus |
author_facet |
Raible, Christoph C. Luksch, Ute Fraedrich, Klaus |
author_sort |
Raible, Christoph C. |
title |
Precipitation and Northern Hemisphere regimes ... |
title_short |
Precipitation and Northern Hemisphere regimes ... |
title_full |
Precipitation and Northern Hemisphere regimes ... |
title_fullStr |
Precipitation and Northern Hemisphere regimes ... |
title_full_unstemmed |
Precipitation and Northern Hemisphere regimes ... |
title_sort |
precipitation and northern hemisphere regimes ... |
publisher |
Royal Meteorological Society |
publishDate |
2004 |
url |
https://dx.doi.org/10.48350/158572 https://boris.unibe.ch/158572/ |
genre |
North Atlantic North Atlantic oscillation |
genre_facet |
North Atlantic North Atlantic oscillation |
op_rights |
restricted access publisher holds copyright http://purl.org/coar/access_right/c_16ec |
op_doi |
https://doi.org/10.48350/158572 |
_version_ |
1810459171093479424 |