Sea of clouds

{{Short description|Description of layer of clouds as viewed from above, resembling waves}}

{{for multi|the lunar mare|Mare Nubium|other uses|Sea fog (disambiguation)}}

{{Infobox cloud type

| name = Sea of clouds

| image location = Chamonix valley clouds.jpg

| image name = Sea of clouds in Chamonix-Mont-Blanc.

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| altitude_m =

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| level = low

| appearance = Uniform with ondulations

| precipitation = no

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File:Mount Pulag, Kabayan, Philippines (Unsplash).jpg, Philippines]]

A sea of clouds is an overcast layer of stratocumulus clouds, as viewed from above, with a relatively uniform top which shows undulations of very different lengths resembling waves on the sea.{{cite web | url= http://www.eumetcal.org/euromet/glossary/seaofclo.htm | title= Sea of clouds | author= World Meteorological Organization | author-link= World Meteorological Organization | publisher= Eumetcal | accessdate= February 22, 2015 | url-status= dead | archiveurl= https://web.archive.org/web/20160303185423/http://www.eumetcal.org/euromet/glossary/seaofclo.htm | archivedate= March 3, 2016 }} A sea of fog is formed from stratus clouds or fog and does not show undulations.{{cite web | url= http://www.eumetcal.org/euromet/glossary/seaoffog.htm | title= Sea of fog | author= World Meteorological Organization | author-link= World Meteorological Organization | publisher= Eumetcal | accessdate= February 22, 2015 | url-status= dead | archiveurl= https://web.archive.org/web/20160303190850/http://www.eumetcal.org/euromet/glossary/seaoffog.htm | archivedate= March 3, 2016 }}

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.

Formation

A sea of clouds forms generally in valleys or over seas in very stable air mass conditions such as in a temperature inversion. 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 high-pressure area with cooling at the surface by radiative cooling at night in summer, or advection of cold air in winter or in a marine layer.

Artistic uses

References

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{{commons category|Sea of clouds}}

Category:Clouds

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