Atmospheric instability

Atmospheric instability refers to a condition in the atmosphere where vertical movements of air can occur, leading to cloud formation, precipitation, and sometimes severe weather events. In simpler terms, it's a state where the atmospheric conditions are conducive to rising air, which can generate turbulence, storms, or convective activity. ### Key Concepts: 1. **Lapse Rate**: The lapse rate is the rate at which air temperature decreases with altitude.