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Published byBruno Hodge Modified over 9 years ago
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Earth’s Water Balance
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Changes of State
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Water Vapor in the Air
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Humidity
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Saturation Vapor Pressure Rises with Temperature
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Amount of Water Vapor Required for Saturation Rises with Temperature
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DEW Point Temperature
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Pseudoadiabatic Chart
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Air Lifting Mechanisms
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Relative Humidity Increases with Additional Water Vapor
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Relative Humidity Increases with Decrease of Temperature
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Changes in Relative Humidity with Temperature
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Sling Psychrometer
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Atmospheric Stability
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Air Cools at Dry Adiabatic Rate until Reaching Dew Point Then Cools at Wet Adiabatic Rate
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Orographic Lifting
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Arid Conditions Caused by Removal of Moisture from Air by Orographic Lifting
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Frontal Wedging
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Uplifting by Convergence
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Cloud Cover from Convergence over Florida
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Localized Convective Lifting
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Air Warmer than its Surroundings Rises
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Rising Air Cooler than Environment Tends Toward Stability
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Absolute Stability; Environmental Lapse Rate less than Wet Adiabatic Rate
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Absolute Instability; Environmental Lapse Rate greater than Dry Adiabatic Rate
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Conditional Stability; Environmental Lapse Rate between the Dry and Wet Adiabatic Rates
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Orographic Lifting
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Orographic Lifting Forming a Rain Shadow Desert
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Convective Uplifting
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Frontal Convergence: Extra-tropical Cyclone – Plan View
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Frontal Convergence: Extra-tropical Cyclone – Vertical X sectional View
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Cumulonimbus Cloud
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People Caught in a Downpour!
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Cloud Types
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Cirrus Clouds
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Cirrostratus Clouds
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Cirrocumulus Clouds
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Altocumulus Clouds
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Reynold’s Transport Theorem
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