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Leewaves1+2.jpg, Details.jpg: At around ten o'clock in the morning
these orographic Leewave clouds arose above the Karavankes in Carinthia.
These are Altocumulus lenticularis clouds with a laminar layering.
LWclouds1-5.jpg show an Altocumulus Leewave cloud field which is
illuminated by the low-standing sun in the arctic. The colours are
represented true to original. LWclouds6+7.jpg, LWclouds8-10.jpg: These Leewave clouds arose in
the medium level south from the Pyrenees at north-westerly flow.
Leewave clouds very often occur here. So it is no surprise that
Salvador Dali painted them in several pictures, for example in "Femme
a la fenetre a Figueras". |
The wave itself remains stationary, whereas the foam on the water oscillates like a roller coaster (see the first wave peak in Waterwaves1.jpg). Several peaks of stationary waves can be noticed in these images. In wave peaks of the atmospheric Leewave clouds super-saturation caused by fast adiabatic expansion can occur and clouds can be formed then. These Leewave clouds "mark" the peaks of the otherwise invisible Leewaves. Further kinds of atmospheric Leewave clouds can be found in chapter
Brown
Cloud and Polar Stratospheric Clouds. |
LeeWaves1.jpg, LeeWaves2.jpg, Details.jpg: S. Borrmann, Pulpit
Rock, Carinthia, 25 December 2001 |