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Earth’s Water Balance. Changes of State. Water Vapor in the Air. Humidity. Saturation Vapor Pressure Rises with Temperature. Amount of Water Vapor Required for Saturation Rises with Temperature. DEW Point Temperature. Pseudoadiabatic Chart. Air Lifting Mechanisms.
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Saturation Vapor Pressure Rises with Temperature
Amount of Water Vapor Required for Saturation Rises with Temperature
Changes in Relative Humidity with Temperature
Sling Psychrometer
Air Cools at Dry Adiabatic Rate until Reaching Dew Point Then Cools at Wet Adiabatic Rate
Arid Conditions Caused by Removal of Moisture from Air by Orographic Lifting
Uplifting by Convergence
Air Warmer than its Surroundings Rises
Rising Air Cooler than Environment Tends Toward Stability
Absolute Stability; Environmental Lapse Rate less than Wet Adiabatic Rate
Absolute Instability; Environmental Lapse Rate greater than Dry Adiabatic Rate
Conditional Stability; Environmental Lapse Rate between the Dry and Wet Adiabatic Rates
Frontal Convergence: Extra-tropical Cyclone – Vertical X sectional View