Meteorology
Atmospheric instability refers to the tendency of air parcels to rise or fall in the atmosphere, depending on their temperature and moisture content compared to the surrounding air. This condition is critical for the development of storms and severe weather events, as it determines whether rising air can continue to ascend, leading to the formation of clouds and precipitation. In the context of tropical cyclones, atmospheric instability plays a vital role in their formation, intensification, and overall dynamics.
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