File:Туман схилів. Fog slopes.jpg

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Українська: Туман схилів — теплове явище, найчастіше за все виникає на гірських схилах та пов'язане з адіабатичним охолодженням повітря при його підйомі по схилу. Його можна розглядати як низькі хмари
English: Fog slopes is the thermal phenomenon that most often occurs on the slopes and is associated with adiabatic air cooling at its climbing the slope. It can be viewed as the low clouds.
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Author Olena Dodchuk

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current18:31, 4 October 2015Thumbnail for version as of 18:31, 4 October 20153,543 × 2,348 (5.16 MB)Olena Dodchuk (talk | contribs)User created page with UploadWizard

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