unit 7 clouds and precipitation (18.3)

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Clouds and Precipitation Objectives (Day 1): 1. Describe how clouds form (what do they need?) 2. Identify how mountain ranges effect rain fall. 3. Relate convective flow to the occurrence of severe weather.

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Page 1: Unit 7 clouds and precipitation (18.3)

Clouds and Precipitation

Objectives (Day 1):

1. Describe how clouds form (what do they need?)

2. Identify how mountain ranges effect rain fall.

3. Relate convective flow to the occurrence of severe weather.

Page 2: Unit 7 clouds and precipitation (18.3)

Starter: Does Coke cry?

Does soda know it is

about to die?

What is this water on the

Outside of the can?

Where does it come from?

Page 3: Unit 7 clouds and precipitation (18.3)

Condensation

Cloud Formation

For any form of condensation to occur, the air must be saturated.

• Generally, there must be a surface for water vapor to condense on.

Types of Surfaces

• Condensation nuclei are tiny bits of particulate matter that serve as surfaces on which water vapor condenses when condensation occurs in the air.

Page 4: Unit 7 clouds and precipitation (18.3)

Making Clouds

• How are the 3 ingredients needed to make clouds represented in this demonstration?

• If you had to explain this demonstration to your little brother/sister, how would you it?

• http://www.youtube.com/watch?v=wfzQbNlGL5M

Page 5: Unit 7 clouds and precipitation (18.3)

Cloud Formation by Adiabatic Cooling

Page 6: Unit 7 clouds and precipitation (18.3)

Orographic Lifting and Frontal Wedging

Page 7: Unit 7 clouds and precipitation (18.3)

Convergence and Localized Convective Lifting

Page 8: Unit 7 clouds and precipitation (18.3)

Clouds and Precipitation

Objectives (Day 2):

1. Identify and describe types of clouds.

2. Relate the types of clouds you see to predict the weather.

3. Identify the clouds into (3+1) groups.

4. Describe the Bergeron process.

Page 9: Unit 7 clouds and precipitation (18.3)

Cirrus Clouds

Page 10: Unit 7 clouds and precipitation (18.3)

Types of Clouds

18.3 Cloud Types and Precipitation

High Clouds• Cirrus clouds are high, white, and thin.• Cirrostratus clouds are flat layers of clouds.• Cirrocumulus clouds consist of fluffy masses.

Middle Clouds

• Altostratus clouds create a uniform white to gray sheet covering the sky with the sun or moon visible as a bright spot.

• Altocumulus clouds are composed of rounded masses that differ from cirrocumulus clouds in that altocumulus clouds are larger and denser.

Page 11: Unit 7 clouds and precipitation (18.3)

Types of Clouds

18.3 Cloud Types and Precipitation

Low Clouds• Stratus clouds are best described as sheets or

layers that cover much or all of the sky.

• Nimbostratus clouds are the main precipitation makers.

• Stratocumulus clouds have a scalloped bottom that appears as long parallel rolls or broken rounded patches.

Page 12: Unit 7 clouds and precipitation (18.3)

Cloud Classification

Page 13: Unit 7 clouds and precipitation (18.3)

Types of Clouds

18.3 Cloud Types and Precipitation

Clouds of Vertical Development• Some clouds do not fit into any one of the three

height categories mentioned. Such clouds have their bases in the low height range but often extend upward into the middle or high altitudes.

Page 14: Unit 7 clouds and precipitation (18.3)

Fog

18.3 Cloud Types and Precipitation

Fog is defined as a cloud with its base at or very near the ground.

• As the air cools, it becomes denser and drains into low areas such as river valleys, where thick fog accumulations may occur.

Fog Caused by Cooling

• When cool air moves over warm water, enough moisture may evaporate from the water surface to produce saturation.

Fog Caused by Evaporation

Page 15: Unit 7 clouds and precipitation (18.3)

Clouds and Precipitation

Objectives (Day 3):

1. Explain the 2 ways that clouds may form.

2. Identify types of precipitaion and the conditions in which they form.

Page 16: Unit 7 clouds and precipitation (18.3)

Convection Demonstration

• What makes water vapor rise?

• What makes wind?

• What energy source makes water vapor rise in the lower latitudes?

• What do the outer drops of food dye represent?

• http://www.youtube.com/watch?v=rgyRsMsQsfE

Page 17: Unit 7 clouds and precipitation (18.3)

How Precipitation Forms

18.3 Cloud Types and Precipitation

For precipitation to form, cloud droplets must grow in volume by roughly one million times.

• The Bergeron process is a theory that relates the formation of precipitation to supercooled clouds, freezing nuclei, and the different saturation levels of ice and liquid water.

Cold Cloud Precipitation

Page 18: Unit 7 clouds and precipitation (18.3)

The Bergeron Process

Page 19: Unit 7 clouds and precipitation (18.3)

How Precipitation Forms

18.3 Cloud Types and Precipitation

Cold Cloud Precipitation• Supercooled water is the condition of water

droplets that remain in the liquid state at temperatures well below 0oC.

• Supersaturated air is the condition of air that is more concentrated than is normally possible under given temperature and pressure conditions.

Page 20: Unit 7 clouds and precipitation (18.3)

How Precipitation Forms

18.3 Cloud Types and Precipitation

Warm Cloud Precipitation• The collision-coalescence process is a theory

of raindrop formation in warm clouds (above 0oC) in which large cloud droplets collide and join together with smaller droplets to form a raindrop.

Page 21: Unit 7 clouds and precipitation (18.3)

Forms of Precipitation

18.3 Cloud Types and Precipitation

The type of precipitation that reaches Earth’s surface depends on the temperature profile in the lower few kilometers of the atmosphere.

• In meteorology, the term rain means drops of water that fall from a cloud and have a diameter of at least 0.5 mm.

Rain and Snow

• At very low temperatures (when the moisture content of air is low) light fluffy snow made up of individual six-sided ice crystals forms.

Page 22: Unit 7 clouds and precipitation (18.3)

Forms of Precipitation

18.3 Cloud Types and Precipitation

• Sleet is the fall of clear-to-translucent ice. Rain and Snow

• Hail is produced in cumulonimbus clouds.

• Hailstones begin as small ice pellets that grow by collecting supercooled water droplets as they fall through a cloud.

Page 23: Unit 7 clouds and precipitation (18.3)

Largest Recorded Hailstone

Page 24: Unit 7 clouds and precipitation (18.3)