Over complex, mountainous terrain the near-surface winds can form intricate
patterns as large-scale winds and locally forced wind systems interplay. S
witzerland, with its mountainous topography and dense meteorological networ
k of 115 automated surface stations, ideally serves as a study area for suc
h wind system interactions. Applying an automated classification scheme to
the wind data of one single year (1995), 16 distinct near-surface flow patt
erns were found. These patterns also show characteristic distributions in m
agnitude and areal extent of temperature, global radiation and precipitatio
n. An Is-year climatology of flow patterns was created with an identificati
on method for fewer stations. This allowed the determination of annual and
diurnal variations in the frequencies of occurrence of the different flow p
atterns, revealing pronounced daytime and night-time classes characterized
by thermally forced winds. Transition probabilities between the flow patter
ns were computed as well. The relationship between the near-surface wind pa
tterns and the synoptic flow situation was investigated with a comparison w
ith synoptic weather types defined for the Alpine region. The results show
clear but not unequivocal interdependencies between the synoptic weather ty
pe and the near-surface flow pattern. Copyright (C) 2001 Royal Meteorologic
al Society.