author_facet Raible, Christoph C.
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author Raible, Christoph C.
Luksch, Ute
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spellingShingle Raible, Christoph C.
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Atmospheric Science Letters
Precipitation and Northern Hemisphere regimes
Atmospheric Science
author_sort raible, christoph c.
spelling Raible, Christoph C. Luksch, Ute Fraedrich, Klaus 1530-261X 1530-261X Wiley Atmospheric Science http://dx.doi.org/10.1016/j.atmoscilet.2003.12.001 <jats:title>Abstract</jats:title><jats:p>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. Copyright © 2004 Royal Meteorological Society. Published by Elsevier Ltd. All rights reserved.</jats:p> Precipitation and Northern Hemisphere regimes Atmospheric Science Letters
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title Precipitation and Northern Hemisphere regimes
title_unstemmed 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_short Precipitation and Northern Hemisphere regimes
title_sort precipitation and northern hemisphere regimes
topic Atmospheric Science
url http://dx.doi.org/10.1016/j.atmoscilet.2003.12.001
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physical 43-55
description <jats:title>Abstract</jats:title><jats:p>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. Copyright © 2004 Royal Meteorological Society. Published by Elsevier Ltd. All rights reserved.</jats:p>
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author Raible, Christoph C., Luksch, Ute, Fraedrich, Klaus
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author_sort raible, christoph c.
container_issue 1-4
container_start_page 43
container_title Atmospheric Science Letters
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description <jats:title>Abstract</jats:title><jats:p>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. Copyright © 2004 Royal Meteorological Society. Published by Elsevier Ltd. All rights reserved.</jats:p>
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spelling Raible, Christoph C. Luksch, Ute Fraedrich, Klaus 1530-261X 1530-261X Wiley Atmospheric Science http://dx.doi.org/10.1016/j.atmoscilet.2003.12.001 <jats:title>Abstract</jats:title><jats:p>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. Copyright © 2004 Royal Meteorological Society. Published by Elsevier Ltd. All rights reserved.</jats:p> Precipitation and Northern Hemisphere regimes Atmospheric Science Letters
spellingShingle Raible, Christoph C., Luksch, Ute, Fraedrich, Klaus, Atmospheric Science Letters, Precipitation and Northern Hemisphere regimes, Atmospheric Science
title 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_short Precipitation and Northern Hemisphere regimes
title_sort precipitation and northern hemisphere regimes
title_unstemmed Precipitation and Northern Hemisphere regimes
topic Atmospheric Science
url http://dx.doi.org/10.1016/j.atmoscilet.2003.12.001