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Lapse Rate
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Summary
Lapse rate refers to the rate at which air temperature decreases with an increase in altitude in the atmosphere. It plays a crucial role in weather patterns, atmospheric stability, and the formation of clouds and precipitation.
Concepts
Adiabatic Process
Environmental Lapse Rate
Dry Adiabatic Lapse Rate
Moist Adiabatic Lapse Rate
Atmospheric Stability
Temperature Inversion
Troposphere
Convection
Thermodynamics
Weather Patterns
Relevant Degrees
Meteorology 88%
External Geodynamics 13%
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