Sc perlucidus
/ 0 Comments / in Low Levels, StratocumulusFormation of stratocumulus due to an upper low directing a cold airmass over the Central Mediterranean. However, only relatively few clouds have formed due to low humidity which can be clearly seen in the attached weather sounding. Of course, instability was present due to the contrast with a warmer surface. The first photo shows cumuliform clouds caused by the explained process
Leave a Reply
Want to join the discussion?Feel free to contribute!