Influence of Scandinavian pattern on temperature anomalies over Eastern Europe

Authors

  • А. Б. Полонский Marine Hydrophysical Institute of NASU, Ukraine
  • И. А. Кибальчич Odessa State Environmental University, Ukraine

Keywords:

Scandinavian pattern, temperature anomalies, method of "composites"

Abstract

Scandinavian pattern’s influence on surface air temperature anomalies over Eastern Europe and the Black Sea region using reanalysis data of the NCEP / NCAR and method of "composites" has been analyzed. It is shown that the oscillation in positive phase is accompanied by significant cooling in Volgograd and Rostov regions of Russia, as well as to the east and north of Ukraine in January and February. The cause of these anomalies is essential in shaping the sustainable transport of arctic air masses from the north-east with a positive phase of the oscillation, when surface anticyclone over Scandinavia is most developed.

Author Biographies

А. Б. Полонский, Marine Hydrophysical Institute of NASU

Doctor of Sciences (Geography), Full Professor

И. А. Кибальчич, Odessa State Environmental University

Postgraduate Student

References

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Cholaw Bueh, Hisashi Nakamura - Scandinavian pattern and its climatic impact. (2007). Q. J. R. Meteorol. Soc., 133, 2117–2131

Dariush Rahimi1, Seyedeh Maryam Afzali (2013). Downscaling the Rainfall and the Teleconnection Indices in South-Western Iran. J. Basic. Appl. Sci. Res., 3(5)1005-1012.

Climate Prediction Center. NOAA. Retrieved from: http://www.cpc.ncep.noaa.gov/data/teledoc/scand.shtml

Published

2013-12-05

Issue

Section

Geography