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152:. 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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279:Maitland, Derek; Taylor, Chris (1998).
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250:World Meteorological Organization
220:World Meteorological Organization
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156:with cooling at the surface by
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186:Wanderer above the Sea of Fog
328:. You can help Knowledge by
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281:Traveler's China companion
256:. Eumetcal. Archived from
226:. Eumetcal. Archived from
201:depicting this phenomenon.
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193:composed in 1818 by the
148:conditions such as in a
78:Uniform with ondulations
36:Sea fog (disambiguation)
30:For the lunar mare, see
324:–related article is a
199:Caspar David Friedrich
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34:. For other uses, see
150:temperature inversion
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119:stratocumulus clouds
70:Family C (Low-level)
57:Chamonix-Mont-Blanc
285:Globe Pequot Press
154:high-pressure area
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158:radiative cooling
98:Sea of clouds in
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16:(Redirected from
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283:. Old Saybrook:
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287:. p. 20.
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264:February 22,
262:. Retrieved
258:the original
254:"Sea of fog"
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234:February 22,
232:. Retrieved
228:the original
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191:oil painting
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162:marine layer
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380:Cloud stubs
104:Philippines
100:Mount Pulag
32:Mare Nubium
369:Categories
206:References
123:sea of fog
75:Appearance
18:Sea of fog
179:Huangshan
173:The term
140:Formation
117:layer of
146:air mass
115:overcast
197:artist
375:Clouds
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189:is an
113:is an
322:cloud
320:This
326:stub
289:ISBN
266:2015
236:2015
131:fog
129:or
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