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

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Relative Humidity (cont.)! If air contains ½ the amount required forsaturation the RH = 50%! If air is saturated, RH= 100%! How does RH change? – two ways– Change the temperature (capacity for watervapor)– Change the amount of water vapor in the air
Change of RH that results from dailytemperature change
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 16 and 17: How saturationvapor pressuredepends
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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