Hydrologic Cycle + Saturation +Temp/Condensation

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14 Terms

1

How much water vapor is in Earth's atmosphere at any given time?

3.75×10^16 gallons

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2

How often is the atmospheric water vapor recycled in one year?

40 times per year

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3

What is the average residence time of a water molecule in the atmosphere?

9 days, providing latent energy per 9 days

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4

What happens when water vapor condenses or freezes?

It releases latent energy, which contributes to earths energy balance

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5

What provides the energy for global evaporation?

The Sun, which sustains atmospheric water vapor levels.

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6

What is the hydrologic cycle?

The continuous movement of water through evaporation, condensation, precipitation, infiltration, runoff, and transpiration, driven by the Sun.

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7

What is the colloquial meaning of "saturation"?

"full”, unable to hold more without releasing equal amount. Has to be relative to other variable.

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8

What does it mean when the air is unsaturated with respect to liquid water?

More water molecules evaporate than condense, meaning evaporation continues spontaneously.

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9

What does it mean when air is saturated with respect to liquid water?

No more water vapor can be added without forcing an equal amount to condense back into liquid.

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10

Temperature

Average KE

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11

How does temperature affect condensation?

Condensation is more likely in colder air.

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12

Why does warm air hold more water vapor than cold air?

warm air molecules are less likely to condense, meaning more water vapor is required to reach saturation.

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13

What are two ways air can reach saturation?

Adding more water vapor, or cooling the air

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14

Limiting Value of Humidity

The maximum amount of water vapor air can hold at a given temperature (saturation point).

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