Humidity, Condensation, Clouds, and Fog or Water in the Atmosphere

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How saturationvapor pressuredepends ontemperature – ittakes more watervapor to saturatethe air at highertemperatures!!!!
2. Relative HumidityRelative humidity tells us how close the air is tobeing saturatedorRH =water vapor content x 100water vapor capacityRH = actual vapor pressure x 100saturation vapor pressure
Page 3: Where the Water Exists on Earth
Page 6 and 7: What affects evaporation rate?! Win
Page 8 and 9: ! The humidity of the air (humidity
Page 10 and 11: The Amount of Water Vapor theAir Ca
Page 12 and 13: So! For about every 20 F change int
Page 14 and 15: Humidity -Any way of specifying the
Page 18 and 19: Relative Humidity (cont.)! If air c
Page 20 and 21: Relative humidity and human comfort
Page 22 and 23: Fog! Air becomes saturated and drop
Page 24 and 25: Radiation fog! The surface of Earth
Page 27 and 28: Advection fog! When air moves horiz
Page 29 and 30: Mixing fog! Say two volumes of air
Page 33 and 34: Fog climatology - average number of
Page 35 and 36: Cirrus
Page 37 and 38: Cirrostratus
Page 39 and 40: Altostratus
Page 41 and 42: Stratocumulus
Page 43 and 44: “Fair-weather” cumulus
Page 45 and 46: Cumulonimbus

Humidity, Condensation, Clouds, and Fog or Water in the Atmosphere

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