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Published byAri Budiman Modified over 5 years ago
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DYK: **The atmosphere contains only about 0.001% of the total volume of water on the planet (about 1.46 x 109 km3). **The rate at which water evaporates into Earth’s atmosphere is about 5.1 x 1017 liters per year.
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Weather is affected by the amount of water in the air.
Don’t forget transpiration.
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Humidity the amount of water vapor (moisture) in the air
warm air can hold more moisture
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Relative Humidity Relative Humidity (%)=amount of moisture in the air compared to how much moisture the air can hold (100%=saturated) evaporational cooling use psychrometer and chart 2 thing affect RH amount of water vapor temperature—RH decreases as the temperature rises and RH increases as temperature drops
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EX: If the dry bulb reads 10°C,
and the difference between the wet and dry-bulb thermometers is 8°C, what is the RH? ____%
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Condensation gas (water vapor) COOLS and becomes a liquid
air must be saturated (RH=100%) Dew Point (measure as class activity—using jar, water, ice and thermometer) temperature where condensation occurs this is the temperature that dew and frost forms and the temperature where fog/clouds form
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Humid vs. Dry Air Masses Dry Humid Warm Moist Low density
Rising air current Counter clockwise rotation Anti-cyclonic Cool Dry High density Falling air current Clockwise rotation Cyclonic
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