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Global Wind Patterns

Global Wind Patterns

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Global Wind Patterns. What is Wind?. Wind is the movement of air from an area of higher pressure to an area of lower pressure . Warmer air expands , becoming less dense than colder air. This causes air pressure to be generally lower where air is heated. The Coriolis Effect. - PowerPoint PPT Presentation

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Page 1: Global Wind Patterns

Global Wind Patterns

Page 2: Global Wind Patterns

What is Wind?

• Wind is the movement of air from an area of higher pressure to an area of lower pressure. Warmer air expands, becoming less dense than colder air. This causes air pressure to be generally lower where air is heated.

Page 3: Global Wind Patterns

The Coriolis Effect

http www.youtube.com/watch?v=mcPs_OdQOYU

• Coriolis Effect – Rotation of the Earth causes moving air and water to change directions• Northern Hemisphere winds curve to the right• Southern Hemisphere winds curve to the left.

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• The Coriolis Effect - The tendency for any moving body on or above the earth's surface, such as an air or water current, to drift sideways from its course because of the earth's rotation. This affects Earth’s winds and water movement. Air moves to the right in the Northern Hemisphere. In the Southern Hemisphere, they move to the left.

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Warm Moist Air Rises

Page 8: Global Wind Patterns

Warm Moist Air Rises

Cool Dry Air Sinks

Cool Dry Air Sinks

Page 9: Global Wind Patterns

Warm Moist Air Rises

Cool Dry Air Sinks

Cool Dry Air Sinks

Cold Moist Air Rises

Cold Moist Air Rises

Page 10: Global Wind Patterns

Warm Moist Air Rises

Cool Dry Air Sinks

Cool Dry Air Sinks

Cold Moist Air Rises

Cold Moist Air Rises

Very Cold Air Sinks

Very Cold Air Sinks

Page 11: Global Wind Patterns

Warm Moist Air Rises

Cool Dry Air Sinks

Cool Dry Air Sinks

Cold Moist Air Rises

Cold Moist Air Rises

Very Cold Air Sinks

Very Cold Air Sinks

H

L

H

H

H

L

L

Page 12: Global Wind Patterns

H

L

H

H

H

L

L

Wind Moves from HIGH to LOW

Page 13: Global Wind Patterns

Objects are deflected to the

RIGHT in the Northern Hemisphere

Page 14: Global Wind Patterns

Global Winds• Global Winds - Wind gets its name from the

direction it is blowing FROM!

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Winds in the Upper Troposphere

• The jet stream is a current of fast moving air found in the upper levels of the troposphere.

Page 21: Global Wind Patterns

Jet Stream• Discovered in 1940’s• Can be found in the upper troposphere• Strong high speed and high pressure• Moves west to east across the US, movingstorms

Page 22: Global Wind Patterns

• The polar jet stream forms at the boundary of cold, dry polar air to the north and warmer, more moist tropical air to the south.

Page 23: Global Wind Patterns

What brings certain weather phenomenon?

El Nino La Nina• occurs when the surface

temperature rises above the normal water temperature in the Equatorial Pacific Ocean creating more humidity in the atmosphere

• Known to increase number of hurricanes

• Occur more frequently (every 3-7 years)

occurs when the surface temperature falls below the normal water temperature in the Equatorial Pacific Ocean creating a more dry atmosphere

Known to create drought conditions

Page 24: Global Wind Patterns

GLOBAL FORCES• The following global forces can affect the

formation of surface currents.

Page 25: Global Wind Patterns

Equator

Earth’s Rotation

Continental DeflectionGlobal Forces

Page 26: Global Wind Patterns

Continental Deflection

Since the Earth’s surface is not fully covered by water, currents cannot move freely around the world. So when surface currents meet continents, they deflect, or change direction.

2

1

3

Predict what will happen with each labeled area.

Page 27: Global Wind Patterns

Equator

Earth’s Rotation

Continental Deflection

Coriolis Effect

Global Forces

Page 28: Global Wind Patterns

Coriolis Effect

The Earth’s rotation causes surface currents to move in curved paths rather than in a straight line.

North Pole

Earth’s Rotation

Page 29: Global Wind Patterns

Equator

Earth’s Rotation

Continental Deflection

Coriolis Effect

Global ForcesGlobal Winds

Page 30: Global Wind Patterns

Global WindsGlobal winds are affected by their latitude and the Coriolis Effect. In the tropics winds blow from the east to the west. In more temperate areas, the winds blow from the west to the east. Near the poles the winds blow from the east to the west.

Tradewinds

Tradewinds

Westerlies

Westerlies

Polar Easterlies

Polar Easterlies

Page 31: Global Wind Patterns

Equator

Earth’s Rotation

Continental Deflection

Coriolis Effect

Global Forces TransparencyGlobal Winds

Deep Ocean Currents

Page 32: Global Wind Patterns

Deep Ocean Currents

• Deep cold currents move water toward the equator.

• Cold water rises to replace warm water leaving.

• Warm water travels near the surface toward polar regions.

• Warm water replaces cold water.

Page 33: Global Wind Patterns

Equator

Earth’s Rotation

Continental DeflectionSince the Earth’s surface is not fully covered by water, currents cannot move freely around the world. So when surface currents meet continents, they deflect, or changedirection.

Coriolis EffectThe Earth’s rotation causes surface currents to move in curved paths rather than in a straight line.

Global Forces Global WindsGlobal winds are affected by their latitude and the Coriolis Effect. In the tropics winds blow from the east to the west. In more temperate areas, the winds blow from the west to the east. Near the poles the winds blow from the east to the west.

Deep Ocean CurrentsDeep cold currents move water toward the equator.Cold water rises to replace warm water leaving.Warm water travels near the surface toward polar regions.Warm water replaces cold water.