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Weather in Action: Downslope Winds
The image below shows a field of springtime stratocumulus clouds that developed across New
York and Pennsylvania with a northwest wind flow.
Why were there no clouds over New Jersey or southeastern portions of New York and Pennsylvania?
Take a look at the topography (below) of the region and compare it to the
field of stratocumulus.
As the northwest wind crossed the Appalachian Mountains and began
descending toward the east coast, the air underwent a basic meteorological process called
adiabatic compression.
As a parcel of air rises, there is less and less air above it so the air parcel expands
due to the decreasing surrounding air pressure. Likewise, as an air parcel descends there is
more and more air above it so the parcel becomes compressed. The Ideal Gas Law (PV=nRT)
tells us that if the pressure of an air parcel changes but all other aspects of the parcel
remain the same, there must be a corresponding change in temperature to keep the equation
balanced. Thus, rising air expands and cools while descending air compresses and warms.
Since the amount of moisture in the parcel does not change but the temperature increases,
the humidity of the parcel decreases. As the humidity decreases, the clouds evaporate.
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