Abstract : 1C.19
Climatology of the Bora lee-side area

JožE Rakovec, Mark ŽAgar
joze.rakovec@fmf.uni-lj.si
University of Ljubljana, Department of Physics, Chair of meteorology

Classical description of Bora suppose the warm air mass in the lee side of the mountain ridge. Also two of the contemporary explanations of this phenomenon imply the same feature: the hydraulic jump with a free surface, and the resonant vertically propagating gravity waves with a discontinuity in temperature and stability. The dependence of the Bora strength, duration etc. on the advection of warm air mass into the Adriatic basin will be discussed .climatologically.