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- Q14928328 subject Q16783693.
- Q14928328 subject Q8435481.
- Q14928328 abstract "Marine stratocumulus is a type of stratocumulus cloud that form in the stable air off the west coast of major land masses. The Earth spins on its axis, which results in the Coriolis force pushing the ocean surface water away from the coast in the mid-latitudes. This results in upwelling of cold water from below that creates a pool of cool water at the surface, which in turn cools the air directly above it. The surface cooling results in a large temperature inversion at the top of the marine layer. As the temperature is cooled to the dewpoint, water vapor condenses upon available cloud condensation nuclei, and forms a cloud. The stability of the marine layer prevents deep convection, and thus stratiform clouds are formed.Climate scientists are currently investigating the detailed structure of marine stratocumulus clouds in an attempt to understand their effect on the climate.".
- Q14928328 wikiPageWikiLink Q11871099.
- Q14928328 wikiPageWikiLink Q16783693.
- Q14928328 wikiPageWikiLink Q169973.
- Q14928328 wikiPageWikiLink Q178828.
- Q14928328 wikiPageWikiLink Q182090.
- Q14928328 wikiPageWikiLink Q190096.
- Q14928328 wikiPageWikiLink Q215915.
- Q14928328 wikiPageWikiLink Q40526.
- Q14928328 wikiPageWikiLink Q40564.
- Q14928328 wikiPageWikiLink Q4676957.
- Q14928328 wikiPageWikiLink Q6764294.
- Q14928328 wikiPageWikiLink Q8435481.
- Q14928328 comment "Marine stratocumulus is a type of stratocumulus cloud that form in the stable air off the west coast of major land masses. The Earth spins on its axis, which results in the Coriolis force pushing the ocean surface water away from the coast in the mid-latitudes. This results in upwelling of cold water from below that creates a pool of cool water at the surface, which in turn cools the air directly above it.".
- Q14928328 label "Marine stratocumulus".