The CAPE values between 500 and 1000 J/kg can be found over the Adriatic Sea. The atmosphere is potentialy unstable. The influence of
orographic lifting plays an important role in the onset and development of severe convection which happend over
the island of Rab and later over
inland (Lika).
The highest CAPE values (over 2500 J/kg) can be noticed over the east Croatia and further to the south, over the border
with Bosnia and Hercegovina
and Serbia. Discrepancy between CAPE values and real convection can be noticed.