An investigation of the main features of large-scale synoptic patterns over
Europe and the adjacent areas for extreme winter periods during 1980-1995
over the Eastern Mediterranean (EM) is performed. The NASA reanalysis data
set is used to investigate composite sea level pressure (SLP), geopotential
height of the 500hPa surface (H-500) and precipitation-wet, normal and dry
patterns for each month during the period October-March. It is found that
the wet and dry cool seasons in the EM are associated with distinct SLP and
H-500 anomaly patterns over Europe and the adjacent regions. During the dr
y spells large-scale positive SLP/H-500 anomaly areas prevail over Eastern
Europe. A negative SLP anomaly is normally found during these periods over
southwestern and Western Europe. During the wet cool seasons in the EM ther
e are mainly negative SLP/H-500 anomaly areas over Eastern Europe to the no
rth east of the EM. Positive SLP/H-500 anomalies are found over Western Eur
ope. During wet months a trough zone between the Siberian and the Azorean H
ighs is positioned over the eastern part of the Mediterranean.
During dry months the Siberian anticyclone is more intensive and the zone w
ith low surface pressure is displaced to the central part of the northern M
editerranean.