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Titel Sea-ice Changes in the Sea of Okhotsk and the North Atlantic Oscillation
VerfasserIn Jürgen Bader, Michel Mesquita
Konferenz EGU General Assembly 2014
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 16 (2014)
Datensatznummer 250098604
Publikation (Nr.) Volltext-Dokument vorhandenEGU/EGU2014-14296.pdf
 
Zusammenfassung
The North Atlantic Oscillation (NAO) is the dominant mode of atmospheric variability in the North Atlantic sector. It has significant impacts on temperature and precipitation not only in Europe, but also in North America. Different forcing factors, such as Arctic sea-ice changes, have an influence on the NAO. Here, we will show that sea-ice conditions in the Sea of Okhotsk have an important impact on the NAO. Our conclusion is based on observations and simulations with an atmospheric general circulation model (AGCM) forced by specified anomalous sea-ice concentrations in the Sea of Okhotsk. Changes to the NAO sign observed in late winter, February, could be related to the remote changes in sea ice in the Sea of Okhotsk in January.