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Low-Pressure Area

Meteorology

A low-pressure area, the opposite of a high-pressure system, is a region where the atmospheric pressure is lower than in the surrounding area. It is commonly associated with inclement weather such as cloud cover, wind, and possible rain or storms, in contrast to the lighter winds and clearer skies typical of high-pressure zones. Winds circulate around a low counterclockwise in the Northern Hemisphere and clockwise in the Southern Hemisphere, driven by the Coriolis effect, and the stronger the pressure difference between a low and a neighboring high, the stronger the winds around the low tend to be. When a rotating low-pressure air mass develops a substantial inward wind spiral, it is classified as a cyclone, the largest and most organized form a low-pressure system can take. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/

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Caused By

Read from this phenomenon's own Wikipedia article (Low-Pressure Area); earth5 pass cause judgment: Atmospheric Circulation.

Source Low-Pressure Area (Wikipedia)

In Discipline

Read from this phenomenon's own Wikipedia article (Low-Pressure Area); earth5 pass discipline judgment: Meteorology.

Source Low-Pressure Area (Wikipedia)
Sources
Low-Pressure Area (Wikipedia)
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