Influence of long-term regional and large-scale atmospheric circulation on the Baltic sea level

Article English OPEN
Andersson, Helén C. (2011)

The connection between variations in the North Atlantic Oscillation (NAO) index and theBaltic sea level has been investigated for the period 1825–1997. The association between theNAO and the strength of the zonal geostrophic wind stress over the Northwest Atlantic suggestsan NAO impact on Baltic sea level variations, because the monthly mean sea level mainly isdetermined by externally driven variations caused by wind conditions over the North Sea.Several period bands were found to have high correlation between oscillations in the winter(JFM) NAO index and the Baltic Sea winter mean sea level. The correlation was, however,higher in the 20th century than in the 19th. During the last two decades, the correlation betweenthe NAO index and the sea level has been exceptionally high. The winter mean of a regionalatmospheric circulation index had a correlation with the Kattegat winter mean sea level of 0.93.With the Baltic sea level the correlation was 0.91, compared with the NAO index correlationfor the same period of 0.74. The regional index also showed a high correlation with the meansummer and mean autumn sea levels, when the corresponding seasonal NAO indices showeda weak connection. The temporal variation of the connection with the NAO index implies aregional atmospheric circulation occasionally differing from the large-scale circulation associatedwith the NAO. Seasonal means of the sea level in Stockholm do, however, reflect theregional wind climate to a large extent, and the Baltic sea level is a useful proxy for identificationsof climatic dependencies in the region.DOI: 10.1034/j.1600-0870.2002.00288.x
  • References (43)
    43 references, page 1 of 5

    Alenius, P. and Makkonen, L. 1981. Variability of the annual maximum ice extent of the Baltic Sea. Arch. Met. Geoph. Biokl. 29B, 393-398.

    Alexandersson, H., Schmidt, T. Iden, K. and Toumenvirta, H. 1998. Long-term variations of the storm climate over NW Europe. T he Global Atmos. Ocean. Syst. 6, 97-120.

    Belgrano, A., Lindahl, O. and Hernroth B. 1998. North Atlantic Oscillation primary productivity and toxic phytoplankton in the Gullmar Fjord, Sweden (1985-1996). Proc. R. Soc. L ondon 266B, 425-430.

    Carlsson, M. 1998a. A coupled three-basin sea level model for the Baltic Sea. Cont. Shelf Res. 18, 1015-1038.

    Carlsson, M. 1998b. The mean sea-level topography in the Baltic Sea determined by oceanographic methods. Marine Geodesy 21, 203-217.

    Chen, D. L. and Hellstr o¨m C. 1999. The influence of the North Atlantic Oscillation on the regional temperature variability in Sweden: spatial and temporal variations. T ellus 51A, 505-516.

    Dean, W. E. Jr and Anderson, R. Y. 1974. Application of some correlation coefficient techniques to timeseries analysis. Math. Geol. 6, 363-372.

    Ekman, M. 1988. The world's longest continued series of sea level observations. Pure Appl. Geophys. 127, 73-77.

    Ekman, M. 1996a. Extreme annual means in the Baltic Sea level during 200 years. Small Publ. Hist. Geophys. 2, 15 pp.

    Ekman, M. 1996b. A common pattern for interannual and periodical sea level variations in the Baltic Sea and adjacent waters. Geophysica 32, 261-272.

  • Related Research Results (1)
    Inferred
    Arctic Sea Ice (2016)
    40%
  • Metrics
    No metrics available
Share - Bookmark