Impact of tropical SST variations on the linear predictability of the atmospheric circulation in the Atlantic/European region

Seasonal mean values of tropical Sea Surface Temperature (SST) and Atlantic/European Mean Sea Level Pressure (MSLP) from a 301-year coupled ocean/atmosphere model run are analysed statistically. Relations between the two fields are identified on both interannual and interdecadal timescales. It is sh...

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Main Author: Feddersen, H.
Other Authors: Feddersen, H.; Climate Research Division, Danish Meteorological Institute, Copenhagen, Denmark, Climate Research Division, Danish Meteorological Institute, Copenhagen, Denmark
Format: Article in Journal/Newspaper
Language:English
Published: INGV 2003
Subjects:
Online Access:http://hdl.handle.net/2122/729
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spelling ftingv:oai:www.earth-prints.org:2122/729 2024-06-09T07:48:16+00:00 Impact of tropical SST variations on the linear predictability of the atmospheric circulation in the Atlantic/European region Feddersen, H. Feddersen, H.; Climate Research Division, Danish Meteorological Institute, Copenhagen, Denmark Climate Research Division, Danish Meteorological Institute, Copenhagen, Denmark 2003 892167 bytes application/pdf http://hdl.handle.net/2122/729 en eng INGV Annals of Geophysics 1/46 (2003) http://hdl.handle.net/2122/729 open interactions climate variability 01. Atmosphere::01.01. Atmosphere::01.01.02. Climate article 2003 ftingv 2024-05-15T08:04:29Z Seasonal mean values of tropical Sea Surface Temperature (SST) and Atlantic/European Mean Sea Level Pressure (MSLP) from a 301-year coupled ocean/atmosphere model run are analysed statistically. Relations between the two fields are identified on both interannual and interdecadal timescales. It is shown that tropical SST variability affects Atlantic/European MSLP in winter. In particular, there appears to be a statistically significant relation, between the leading modes of variability, the El Niño/Southern Oscillation (ENSO) and the North Atlantic Oscillation (NAO). During cold ENSO (La Niña) years the NAO tends to be in its positive phase, while the opposite is the case during warm ENSO (El Niño) years, although to a lesser extent. Similar analyses that are presented for gridded observational data, confirm this result, although here tropical Atlantic SST appears to be stronger related to the NAO than tropical Pacific SST. The linear predictability of a model simulated NAO index is estimated by making statistical predictions that are based on model simulated tropical SST. It is shown that the predictive skill is rather insensitive to the length of the training period. On the other hand, the skill score estimate can vary significantly as a result of interdecadal variability in the climate system. These results are important to bear in mind when making statistical seasonal forecasts that are based on observed SST. Published JCR Journal open Article in Journal/Newspaper North Atlantic North Atlantic oscillation Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia) Pacific
institution Open Polar
collection Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia)
op_collection_id ftingv
language English
topic interactions
climate variability
01. Atmosphere::01.01. Atmosphere::01.01.02. Climate
spellingShingle interactions
climate variability
01. Atmosphere::01.01. Atmosphere::01.01.02. Climate
Feddersen, H.
Impact of tropical SST variations on the linear predictability of the atmospheric circulation in the Atlantic/European region
topic_facet interactions
climate variability
01. Atmosphere::01.01. Atmosphere::01.01.02. Climate
description Seasonal mean values of tropical Sea Surface Temperature (SST) and Atlantic/European Mean Sea Level Pressure (MSLP) from a 301-year coupled ocean/atmosphere model run are analysed statistically. Relations between the two fields are identified on both interannual and interdecadal timescales. It is shown that tropical SST variability affects Atlantic/European MSLP in winter. In particular, there appears to be a statistically significant relation, between the leading modes of variability, the El Niño/Southern Oscillation (ENSO) and the North Atlantic Oscillation (NAO). During cold ENSO (La Niña) years the NAO tends to be in its positive phase, while the opposite is the case during warm ENSO (El Niño) years, although to a lesser extent. Similar analyses that are presented for gridded observational data, confirm this result, although here tropical Atlantic SST appears to be stronger related to the NAO than tropical Pacific SST. The linear predictability of a model simulated NAO index is estimated by making statistical predictions that are based on model simulated tropical SST. It is shown that the predictive skill is rather insensitive to the length of the training period. On the other hand, the skill score estimate can vary significantly as a result of interdecadal variability in the climate system. These results are important to bear in mind when making statistical seasonal forecasts that are based on observed SST. Published JCR Journal open
author2 Feddersen, H.; Climate Research Division, Danish Meteorological Institute, Copenhagen, Denmark
Climate Research Division, Danish Meteorological Institute, Copenhagen, Denmark
format Article in Journal/Newspaper
author Feddersen, H.
author_facet Feddersen, H.
author_sort Feddersen, H.
title Impact of tropical SST variations on the linear predictability of the atmospheric circulation in the Atlantic/European region
title_short Impact of tropical SST variations on the linear predictability of the atmospheric circulation in the Atlantic/European region
title_full Impact of tropical SST variations on the linear predictability of the atmospheric circulation in the Atlantic/European region
title_fullStr Impact of tropical SST variations on the linear predictability of the atmospheric circulation in the Atlantic/European region
title_full_unstemmed Impact of tropical SST variations on the linear predictability of the atmospheric circulation in the Atlantic/European region
title_sort impact of tropical sst variations on the linear predictability of the atmospheric circulation in the atlantic/european region
publisher INGV
publishDate 2003
url http://hdl.handle.net/2122/729
geographic Pacific
geographic_facet Pacific
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_relation Annals of Geophysics
1/46 (2003)
http://hdl.handle.net/2122/729
op_rights open
_version_ 1801379931027931136