chapter 9: weather factors section 4: water in the atmosphere

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Chapter 9: Weather Chapter 9: Weather Factors Factors Section 4: Water In the Atmosphere

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Page 1: Chapter 9: Weather Factors Section 4: Water In the Atmosphere

Chapter 9: Weather Chapter 9: Weather FactorsFactors

Section 4: Water In the Atmosphere

Page 2: Chapter 9: Weather Factors Section 4: Water In the Atmosphere

The Water CycleThe Water CycleWater Cycle – the movement of

water between the atmosphere and Earth’s surface.◦Evaporation◦Condensation◦Precipitation◦Surface runoff

Page 3: Chapter 9: Weather Factors Section 4: Water In the Atmosphere

The Water CycleThe Water CycleEvaporation- water molecules in

liquid water escape into the air as water vapor.

Page 4: Chapter 9: Weather Factors Section 4: Water In the Atmosphere
Page 5: Chapter 9: Weather Factors Section 4: Water In the Atmosphere

HumidityHumidityHumidity - a measure of the

amount of water vapor in the air.Relative Humidity – is the

percentage of water vapor that is actually in the air. ◦Compared to the maximum amount

of water vapor the air can hold at a particular temperature.

Page 6: Chapter 9: Weather Factors Section 4: Water In the Atmosphere

Measuring Relative Measuring Relative Humidity Humidity Relative humidity can be measured

with an instrument called a psychrometer.◦ (sy KRAHM uh tur)◦2 thermometers◦Dry bulb◦Wet bulb

Page 7: Chapter 9: Weather Factors Section 4: Water In the Atmosphere

How Clouds FormHow Clouds FormClouds form when water vapor in

the air condenses to form liquid water or ice crystals.

Condensation – molecules of water vapor in the air become liquid water.

Dew point – the temperature at which condensation begins.◦Above freezing - water droplets◦Below freezing – ice crystals

Page 8: Chapter 9: Weather Factors Section 4: Water In the Atmosphere

How Clouds FormHow Clouds FormThe Role of Particles

◦For water vapor to condense, tiny particles must be present so the water has a surface on which to condense.

◦In cloud formation, most of these particles are salt crystals, dust from soil and smoke.

◦These tiny particles are called nuclei.

Page 9: Chapter 9: Weather Factors Section 4: Water In the Atmosphere
Page 10: Chapter 9: Weather Factors Section 4: Water In the Atmosphere

Types of CloudsTypes of CloudsCirrus Clouds

Cumulus Clouds

Stratus Clouds

Page 11: Chapter 9: Weather Factors Section 4: Water In the Atmosphere

Cirrus CloudsCirrus CloudsWispy, featherOnly at high levels with low

temperatures◦Above 6 kilometers

Made of ice crystals

Page 12: Chapter 9: Weather Factors Section 4: Water In the Atmosphere

Cumulus CloudsCumulus CloudsLook like fluffy, rounded piles of

cottonForm less than 2 kilometers

above groundMay extend upward as much as

18 kilometers

Page 13: Chapter 9: Weather Factors Section 4: Water In the Atmosphere

Stratus CloudsStratus CloudsForm in flat layersCover all or most of the skyA uniform dull, gray color

Page 14: Chapter 9: Weather Factors Section 4: Water In the Atmosphere

Altocumulus and Altocumulus and Altostratus Altostratus Middle level clouds; higher than

regular cumulus and stratus clouds, lower than cirrus clouds.

Between 2 and 6 kilometers above the ground

Page 15: Chapter 9: Weather Factors Section 4: Water In the Atmosphere

FogFogFog – clouds that form at or near

the groundAir above the ground is cooled to

the air’s dew point.Near bodies of water, low-lying

marshes, mountain slopes

Page 16: Chapter 9: Weather Factors Section 4: Water In the Atmosphere