Cloud Formation Mechanisms: Orographic Lift and Frontal Systems
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Atmospheric Phenomena and Cloud Formation
Orographic Clouds: Formation and Rain Shadow
Orographic clouds arise from the shock produced by a moist air mass against a mountain, causing it to climb until it reaches its condensation level. Typically, development is horizontal (strata) and causes precipitation of the cloud in contact with the slope (horizontal precipitation).
Once the air mass is over the top of the mountain, the cloud has lost most of its water. The remainder converts into vapor as it warms while descending the side it was promoted on. As a result, this mountainside is known as a dry or rain shadow.
Convective Clouds Originating on a Front
Convective clouds on a front are those originating from a front—a contact zone between two air... Continue reading "Cloud Formation Mechanisms: Orographic Lift and Frontal Systems" »