Links of the significant wave height distribution in the Mediterranean sea with the Northern Hemisphere teleconnection patterns

This study analyzes the link between the SWH (Significant Wave Height) distribution in the Mediterranean Sea during the second half of the 20th century and the Northern Hemisphere SLP (Sea Level Pressure) teleconnection patterns. The SWH distribution is computed using the WAM (WAve Model) forced by...

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Published in:Advances in Geosciences
Main Authors: Lionello, P., Galati, M. B.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/adgeo-17-13-2008
https://adgeo.copernicus.org/articles/17/13/2008/
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spelling ftcopernicus:oai:publications.copernicus.org:adgeo38151 2023-05-15T17:34:01+02:00 Links of the significant wave height distribution in the Mediterranean sea with the Northern Hemisphere teleconnection patterns Lionello, P. Galati, M. B. 2018-01-15 application/pdf https://doi.org/10.5194/adgeo-17-13-2008 https://adgeo.copernicus.org/articles/17/13/2008/ eng eng doi:10.5194/adgeo-17-13-2008 https://adgeo.copernicus.org/articles/17/13/2008/ eISSN: 1680-7359 Text 2018 ftcopernicus https://doi.org/10.5194/adgeo-17-13-2008 2020-07-20T16:26:52Z This study analyzes the link between the SWH (Significant Wave Height) distribution in the Mediterranean Sea during the second half of the 20th century and the Northern Hemisphere SLP (Sea Level Pressure) teleconnection patterns. The SWH distribution is computed using the WAM (WAve Model) forced by the surface wind fields provided by the ERA-40 reanalysis for the period 1958–2001. The time series of mid-latitude teleconnection patterns are downloaded from the NOAA web site. This study shows that several mid-latitude patterns are linked to the SWH field in the Mediterranean, especially in its western part during the cold season: East Atlantic Pattern (EA), Scandinavian Pattern (SCA), North Atlantic Oscillation (NAO), East Atlantic/West Russia Pattern (EA/WR) and East Pacific/ North Pacific Pattern (EP/NP). Though the East Atlantic pattern exerts the largest influence, it is not sufficient to characterize the dominant variability. NAO, though relevant, has an effect smaller than EA and comparable to other patterns. Some link results from possibly spurious structures. Patterns which have a very different global structure are associated to similar spatial features of the wave variability in the Mediterranean Sea. These two problems are, admittedly, shortcomings of this analysis, which shows the complexity of the response of the Mediterranean SWH to global scale SLP teleconnection patterns. Text North Atlantic North Atlantic oscillation Copernicus Publications: E-Journals Pacific Advances in Geosciences 17 13 18
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description This study analyzes the link between the SWH (Significant Wave Height) distribution in the Mediterranean Sea during the second half of the 20th century and the Northern Hemisphere SLP (Sea Level Pressure) teleconnection patterns. The SWH distribution is computed using the WAM (WAve Model) forced by the surface wind fields provided by the ERA-40 reanalysis for the period 1958–2001. The time series of mid-latitude teleconnection patterns are downloaded from the NOAA web site. This study shows that several mid-latitude patterns are linked to the SWH field in the Mediterranean, especially in its western part during the cold season: East Atlantic Pattern (EA), Scandinavian Pattern (SCA), North Atlantic Oscillation (NAO), East Atlantic/West Russia Pattern (EA/WR) and East Pacific/ North Pacific Pattern (EP/NP). Though the East Atlantic pattern exerts the largest influence, it is not sufficient to characterize the dominant variability. NAO, though relevant, has an effect smaller than EA and comparable to other patterns. Some link results from possibly spurious structures. Patterns which have a very different global structure are associated to similar spatial features of the wave variability in the Mediterranean Sea. These two problems are, admittedly, shortcomings of this analysis, which shows the complexity of the response of the Mediterranean SWH to global scale SLP teleconnection patterns.
format Text
author Lionello, P.
Galati, M. B.
spellingShingle Lionello, P.
Galati, M. B.
Links of the significant wave height distribution in the Mediterranean sea with the Northern Hemisphere teleconnection patterns
author_facet Lionello, P.
Galati, M. B.
author_sort Lionello, P.
title Links of the significant wave height distribution in the Mediterranean sea with the Northern Hemisphere teleconnection patterns
title_short Links of the significant wave height distribution in the Mediterranean sea with the Northern Hemisphere teleconnection patterns
title_full Links of the significant wave height distribution in the Mediterranean sea with the Northern Hemisphere teleconnection patterns
title_fullStr Links of the significant wave height distribution in the Mediterranean sea with the Northern Hemisphere teleconnection patterns
title_full_unstemmed Links of the significant wave height distribution in the Mediterranean sea with the Northern Hemisphere teleconnection patterns
title_sort links of the significant wave height distribution in the mediterranean sea with the northern hemisphere teleconnection patterns
publishDate 2018
url https://doi.org/10.5194/adgeo-17-13-2008
https://adgeo.copernicus.org/articles/17/13/2008/
geographic Pacific
geographic_facet Pacific
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source eISSN: 1680-7359
op_relation doi:10.5194/adgeo-17-13-2008
https://adgeo.copernicus.org/articles/17/13/2008/
op_doi https://doi.org/10.5194/adgeo-17-13-2008
container_title Advances in Geosciences
container_volume 17
container_start_page 13
op_container_end_page 18
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