Extratropical Influence of Upper Tropospheric Equatorial Zonal Wind
Variations in the global tropospheric zonal mean zonal wind ([U]) during boreal winter are investigated using Rotated Empirical Orthogonal Functions applied to monthly means. The first two modes correspond to the Northern and Southern Annular Mode and modes 3 and 4 represent variability in the tropi...
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ftoceanrep:oai:oceanrep.geomar.de:28584 2023-05-15T13:15:04+02:00 Extratropical Influence of Upper Tropospheric Equatorial Zonal Wind Gollan, Gereon Greatbatch, Richard John 2015-04-15 text https://oceanrep.geomar.de/id/eprint/28584/ https://oceanrep.geomar.de/id/eprint/28584/1/poster_zonmeanwind.pdf en eng https://oceanrep.geomar.de/id/eprint/28584/1/poster_zonmeanwind.pdf Gollan, G. and Greatbatch, R. J. (2015) Extratropical Influence of Upper Tropospheric Equatorial Zonal Wind. [Poster] In: EGU General Assembly 2015. , 12.–17.04.2015 , Vienna, Austria . Conference or Workshop Item NonPeerReviewed 2015 ftoceanrep 2023-04-07T15:18:57Z Variations in the global tropospheric zonal mean zonal wind ([U]) during boreal winter are investigated using Rotated Empirical Orthogonal Functions applied to monthly means. The first two modes correspond to the Northern and Southern Annular Mode and modes 3 and 4 represent variability in the tropics. One is related to El Nino Southern Oscillation and the other has variability that is highly correlated with the time series of [U] at 150 hPa between 5 ◦ N and 5 ◦ S ([U150]e) and is related to activity of the Madden-Julian Oscillation (MJO). High amplitude of the MJO with strong precipitation anomalies over the western tropical Pacific (late MJO phases) are associated with the westerly phase of [U150]e (and vice versa). The extratropical response to [U150]e is investigated using linear regressions of 500 hPa geopotential height onto the [U150]e time series. Use is made of reanalysis data and of the ensemble mean output from a relaxation experiment using the European Center for Medium Range Weather Forecasts (ECMWF) model in which the tropical atmosphere is relaxed towards reanalysis data. Both the 45- year ECMWF reanalysis (ERA-40) and the ERA-Interim reanalysis data sets are used for the relaxation experiment as well as for the regression analysis. Therefore the analysis is covering 52 boreal winters from 1960/61 to 2012/13. The regression analysis reveals a robust shift of the Aleutian low and a wave train across the North Atlantic associated with [U150]e. It is found that the subtropical Rossby waveguides and the link between the North Pacific and North Atlantic are stronger during the easterly phase of [U150]e. The wave train over the North Atlantic is associated with Rossby wave sources over the subtropical North Pacific and North America. Conference Object aleutian low North Atlantic OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Pacific |
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OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) |
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ftoceanrep |
language |
English |
description |
Variations in the global tropospheric zonal mean zonal wind ([U]) during boreal winter are investigated using Rotated Empirical Orthogonal Functions applied to monthly means. The first two modes correspond to the Northern and Southern Annular Mode and modes 3 and 4 represent variability in the tropics. One is related to El Nino Southern Oscillation and the other has variability that is highly correlated with the time series of [U] at 150 hPa between 5 ◦ N and 5 ◦ S ([U150]e) and is related to activity of the Madden-Julian Oscillation (MJO). High amplitude of the MJO with strong precipitation anomalies over the western tropical Pacific (late MJO phases) are associated with the westerly phase of [U150]e (and vice versa). The extratropical response to [U150]e is investigated using linear regressions of 500 hPa geopotential height onto the [U150]e time series. Use is made of reanalysis data and of the ensemble mean output from a relaxation experiment using the European Center for Medium Range Weather Forecasts (ECMWF) model in which the tropical atmosphere is relaxed towards reanalysis data. Both the 45- year ECMWF reanalysis (ERA-40) and the ERA-Interim reanalysis data sets are used for the relaxation experiment as well as for the regression analysis. Therefore the analysis is covering 52 boreal winters from 1960/61 to 2012/13. The regression analysis reveals a robust shift of the Aleutian low and a wave train across the North Atlantic associated with [U150]e. It is found that the subtropical Rossby waveguides and the link between the North Pacific and North Atlantic are stronger during the easterly phase of [U150]e. The wave train over the North Atlantic is associated with Rossby wave sources over the subtropical North Pacific and North America. |
format |
Conference Object |
author |
Gollan, Gereon Greatbatch, Richard John |
spellingShingle |
Gollan, Gereon Greatbatch, Richard John Extratropical Influence of Upper Tropospheric Equatorial Zonal Wind |
author_facet |
Gollan, Gereon Greatbatch, Richard John |
author_sort |
Gollan, Gereon |
title |
Extratropical Influence of Upper Tropospheric Equatorial Zonal Wind |
title_short |
Extratropical Influence of Upper Tropospheric Equatorial Zonal Wind |
title_full |
Extratropical Influence of Upper Tropospheric Equatorial Zonal Wind |
title_fullStr |
Extratropical Influence of Upper Tropospheric Equatorial Zonal Wind |
title_full_unstemmed |
Extratropical Influence of Upper Tropospheric Equatorial Zonal Wind |
title_sort |
extratropical influence of upper tropospheric equatorial zonal wind |
publishDate |
2015 |
url |
https://oceanrep.geomar.de/id/eprint/28584/ https://oceanrep.geomar.de/id/eprint/28584/1/poster_zonmeanwind.pdf |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
aleutian low North Atlantic |
genre_facet |
aleutian low North Atlantic |
op_relation |
https://oceanrep.geomar.de/id/eprint/28584/1/poster_zonmeanwind.pdf Gollan, G. and Greatbatch, R. J. (2015) Extratropical Influence of Upper Tropospheric Equatorial Zonal Wind. [Poster] In: EGU General Assembly 2015. , 12.–17.04.2015 , Vienna, Austria . |
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1766266801705975808 |