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The dry adiabatic rate of change for unsaturated air is per 1000 m.
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Classroom Contents
Earth Science - Lift and Instability
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- 1 ADIABATIC TEMPERATURE CHANGES
- 2 OROGRAPHIC LIFTING
- 3 FRONTAL LIFTING
- 4 CONVERGENCE
- 5 LOCALIZED CONVECTIVE LIFTING
- 6 ATMOSPHERIC STABILITY
- 7 ABSOLUTE STABILITY
- 8 ABSOLUTE INSTABILITY
- 9 CONDITIONAL INSTABILITY
- 10 STABILITY AND DAILY WEATHER
- 11 The dry adiabatic rate of change for unsaturated air is per 1000 m.
- 12 When elevated terrain, such as a mountain range, acts as a barrier to the flow of air
- 13 When the environmental lapse rate is less than the wet adiabatic rate prevails.
