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Earth Sciences 20 Online
OpenStudy (anonymous):

On the side of the mountain away from the wind, air descends, ______ , and dries out the land.

OpenStudy (anonymous):

I can help

OpenStudy (anonymous):

ok good thanks!

OpenStudy (anonymous):

no problume

OpenStudy (anonymous):

Orographic lift occurs when an air mass is forced from a low elevation to a higher elevation as it moves over rising terrain. As the air mass gains altitude it quickly cools down adiabatically, which can raise the relative humidity to 100% and create clouds and, under the right conditions, precipitation.

OpenStudy (anonymous):

Leeward winds Downslope winds occur on the leeward side of mountain barriers when a stable air mass is carried over the mountain by strong winds that increase in strength with height. Moisture is removed and latent heat released as the air mass is orographically lifted. As the air mass descends, it is compression heated. The warm foehn wind, locally known as the Chinook wind, Bergwind or Diablo wind or Nor'wester depending on the region, provide examples of this type of wind, and are driven in part by latent heat released by orographic-lifting-induced precipitation.A similar class of winds, the Sirocco, the Bora and Santa Ana winds, are examples where orographic lifting has limited effect since there is limited moisture to remove in the Saharan or other air masses; the Sirocco, Bora and Santa Ana are driven primarily by (adiabatic) compression heating.

OpenStudy (anonymous):

ok thanks, so the blank is leeward winds?

OpenStudy (anonymous):

I think

OpenStudy (anonymous):

yes it is

OpenStudy (anonymous):

thanks!!!!!!!!!!!!!!!!!!!!!

OpenStudy (anonymous):

your welcome

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