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Water in the Atmosphere 18.1

Earth science 18.1

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Page 1: Earth science 18.1

Water in the Atmosphere 18.1

Page 2: Earth science 18.1

Precipitation

• Any form of water that falls from a cloud.

Page 3: Earth science 18.1

Latent Heat • The energy absorbed or released during

a change in state.

Page 4: Earth science 18.1

Evaporation

• The process of converting a liquid to a gas.

Page 5: Earth science 18.1

Condensation

• The change of state from a gas to a liquid.

Page 6: Earth science 18.1

Sublimation • The conversion of a solid directly to a gas

without passing through the liquid state.

Page 7: Earth science 18.1

Deposition • The process by which an agent of erosion

loses energy and drops the sediment it is carrying; also the process by which water vapor is changed directly to a solid without passing through the liquid state.

Page 8: Earth science 18.1

Humidity

• A general term referring to water vapor in the air but not to liquid droplets of fog, cloud, or rain.

Page 9: Earth science 18.1

Saturated• The state of air that contains the maximum

quantity of water vapor that it can hold at any given temperature and pressure.

Page 10: Earth science 18.1

Relative Humidity

• The ratio of the air’s water-vapor content to its water-vapor capacity.

Page 11: Earth science 18.1

Dew Point • The temperature to which air has to be cooled

in order to reach saturation.

Page 12: Earth science 18.1

Hygrometer

• An instrument designed to measure relative humidity.

Page 13: Earth science 18.1

Key Concept

• When it comes to understanding atmospheric processes, water vapor is the most important gas in the atmosphere.

Page 14: Earth science 18.1

Key Concept

• The process of changing state requires that energy is transferred in the form of heat.

Page 15: Earth science 18.1

Key Concept

• When saturated, warm air contains more water vapor than saturated cold air.