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141:. Humidity can then reach saturation and condensation leads to a very uniform stratocumulus cloud, stratus cloud or fog. Above this layer, the air must be dry. This is a common situation in a
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In both cases, the phenomenon looks very similar to the open ocean. The comparison is even more complete if some mountain peaks rise above the clouds, thus resembling islands.
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A sea of clouds forms generally in valleys or over seas in very stable
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Description of layer of clouds as viewed from above, resembling waves
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at night in summer, or advection of cold air in winter or in a
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268:Maitland, Derek; Taylor, Chris (1998).
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239:World Meteorological Organization
209:World Meteorological Organization
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145:with cooling at the surface by
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175:Wanderer above the Sea of Fog
317:. You can help Knowledge by
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270:Traveler's China companion
245:. Eumetcal. Archived from
215:. Eumetcal. Archived from
190:depicting this phenomenon.
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182:composed in 1818 by the
137:conditions such as in a
67:Uniform with ondulations
25:Sea fog (disambiguation)
19:For the lunar mare, see
313:–related article is a
188:Caspar David Friedrich
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23:. For other uses, see
139:temperature inversion
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108:stratocumulus clouds
59:Family C (Low-level)
46:Chamonix-Mont-Blanc
274:Globe Pequot Press
143:high-pressure area
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147:radiative cooling
87:Sea of clouds in
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253:February 22,
251:. Retrieved
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243:"Sea of fog"
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223:February 22,
221:. Retrieved
217:the original
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180:oil painting
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151:marine layer
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369:Cloud stubs
93:Philippines
89:Mount Pulag
21:Mare Nubium
358:Categories
195:References
112:sea of fog
64:Appearance
168:Huangshan
162:The term
129:Formation
106:layer of
135:air mass
104:overcast
186:artist
364:Clouds
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178:is an
102:is an
311:cloud
309:This
315:stub
278:ISBN
255:2015
225:2015
120:fog
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