Comparative analysis of the long‐term variability of winter surface temperature in the Black and Aegean Seas during 1982–2004 associated with the large‐scale atmospheric forcing

• Published in: International Journal of Climatology
• Main Authors: Kazmin, Alexander S., Zatsepin, Andrei G., Kontoyiannis, Harilaos
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2009
• Subjects: North Atlantic; North Atlantic oscillation
• Online Access: http://dx.doi.org/10.1002/joc.1985; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjoc.1985; https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.1985

Abstract Satellite and reanalysis data for the period 1982–2004 were used to study the long‐term variability of the winter‐mean sea surface temperature (SST) in the Black and Aegean Seas and its connection with the major atmospheric forcing: surface air temperature (SAT), surface wind and North Atlantic Oscillation (NAO) and East Atlantic‐West Russia (EAWR) teleconnection patterns. In spite of some differences, the general tendencies of SST variability in both basins are similar. The major climatic event (i.e. SST decreases below the climatic mean followed by the sharp increase of SST, occurred during the period 1986–1999) and its connection with the atmospheric forcing are evident both in the Black and Aegean Seas. During the investigated period, the south‐western wind regime occurred over the Black Sea and the north‐eastern wind regime over the Aegean. It is shown that the variability of the meridional component of the surface wind (which provides the most of the atmospheric heat transport into the basins) is well correlated with the large‐scale atmospheric patterns (NAO and EAWR). The major difference is that in the Black Sea the NAO intensification/weakening results in the weakening/strengthening of the southern wind, whereas in the Aegean Sea EAWR/NAO intensification/weakening produce strengthening/weakening of the northern wind. The long‐term variability of the SST is well correlated with the variability of the SAT, which in turn is highly correlated with the meridional component of the surface wind. However, a remarkable feature is that in the Black Sea an increase/decrease of the SAT is associated with the strengthening/weakening of the southern wind. On the contrary, in the Aegean Sea, an increase/decrease of the SAT is associated with the weakening/strengthening of the northern wind. The simple basic scheme of influence of the large‐scale atmospheric forcing on the long‐term SST variability during the positive NAO and EAWR phase is proposed. Copyright © 2009 Royal Meteorological Society