Section 1-3 Global Convection and Wind Belts. What We’ll Discuss Today Convection Cells and...

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Section 1-3 Global Convection and Wind Belts

Transcript of Section 1-3 Global Convection and Wind Belts. What We’ll Discuss Today Convection Cells and...

Page 1: Section 1-3 Global Convection and Wind Belts. What We’ll Discuss Today Convection Cells and Pressure Belts Coriolis Effect Prevailing Winds.

Section 1-3

Global Convection and Wind Belts

Page 2: Section 1-3 Global Convection and Wind Belts. What We’ll Discuss Today Convection Cells and Pressure Belts Coriolis Effect Prevailing Winds.

What We’ll Discuss Today

• Convection Cells and Pressure Belts • Coriolis Effect• Prevailing Winds

Page 3: Section 1-3 Global Convection and Wind Belts. What We’ll Discuss Today Convection Cells and Pressure Belts Coriolis Effect Prevailing Winds.

Convection Cells

http://www.boqueteweather.com/climate_article.htm

Where is the air…

dry and sinking - high pressure?(look for clear skies)

humid and rising - low pressure ?(look for clouds)

changing latitude as it flows along the surface?

Do You See the Convection Cells?(follow the arrows)

Page 4: Section 1-3 Global Convection and Wind Belts. What We’ll Discuss Today Convection Cells and Pressure Belts Coriolis Effect Prevailing Winds.

The Coriolis Effect

“Turning of Air Masses because of the Spinning of the Earth”

Paper Plate Demonstration

The Effect on air masses which are changing latitude

Effect on air moving toward the equator

• Turns left

Effect on air moving toward the poles

• Turns Right

NOTE: Because of the Coriolis Effect, winds in large air masses associated with pressure systems rotate...

Clockwise in High Pressure Systems and Counterclockwise in Low Pressure Systems

remember the clock is high and the counter is low

Page 5: Section 1-3 Global Convection and Wind Belts. What We’ll Discuss Today Convection Cells and Pressure Belts Coriolis Effect Prevailing Winds.

3-D View of Global ConvectionRising Air: low pressure rain band

Sinking Air: high pressure dry

Notice air changing latitudes at surface curves like on our plates

Page 6: Section 1-3 Global Convection and Wind Belts. What We’ll Discuss Today Convection Cells and Pressure Belts Coriolis Effect Prevailing Winds.

Convection Cells cause upper atmosphere “Jet Streams”

Jet Streams (GREEN AREAS)form where convectioncells meet in the upper atmosphere

Page 7: Section 1-3 Global Convection and Wind Belts. What We’ll Discuss Today Convection Cells and Pressure Belts Coriolis Effect Prevailing Winds.

Convection Cells and Jet Streams Go Together

Page 8: Section 1-3 Global Convection and Wind Belts. What We’ll Discuss Today Convection Cells and Pressure Belts Coriolis Effect Prevailing Winds.

Jet Streams Meander

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1-3 Notes Quiz: Global Pressure and Wind Belts Name: _________________

1. List the latitudes with Global Low Pressure Belts with consistently large amounts of precipitation.

(HINT: look at latitudes North and South - there are three)

2. List the latitudes with Global High Pressure Belts with consistently very little precipitation.

(HINT: there are four)

3. Where and why do jet streams occur?

4. What is the name (and source) for winds moving toward the equator?

5. What is the name (and source) for winds moving toward the poles?

Use the last slide of the presentation to help you complete the sketch on the back of this page

Page 10: Section 1-3 Global Convection and Wind Belts. What We’ll Discuss Today Convection Cells and Pressure Belts Coriolis Effect Prevailing Winds.

What happens to a “Straight Line” on a stationary plate

What happens to a “Straight Line” on a stationary plate

Stationary Earth(imaginary)

Spinning Earth(reality)

Page 11: Section 1-3 Global Convection and Wind Belts. What We’ll Discuss Today Convection Cells and Pressure Belts Coriolis Effect Prevailing Winds.

Sketch and label the…Convection Cells (with arrow for direction), Pressure Belts (H and L), Prevailing Winds, and Jet Stream locations on this Model

Equator

Page 12: Section 1-3 Global Convection and Wind Belts. What We’ll Discuss Today Convection Cells and Pressure Belts Coriolis Effect Prevailing Winds.