An attempt has been made to relate a large-scale airflow classification to
the local weather at two stations in Estonia. To describe the features of t
he general circulation over Europe, the large-scale circulation patterns (G
rosswetterlagen) of the German Weather Service have been chosen. Daily prec
ipitation and temperature deviations from the monthly mean in Parnu and Tar
tu for 1961-1993 have been used. It can be said that the weather in Estonia
shows a good relationship with the general circulation types (Zirkulations
formen) that are defined by means of the Glasswetterlagen. Zonal circulatio
n brings to Estonia wet weather that in winter is warmer than average and i
n summer cooler than average. Mixed circulation is associated with warmer w
inters and average summers. Meridional circulation brings cold winters and
variable weather in summer. To explain the large dispersion of values of me
teorological elements within any one circulation type, a more detailed anal
ysis of the relationships between circulation patterns and meteorological s
ituation in Estonia is needed.