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The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

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Page 1: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy
Page 2: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

The movement of air, from high The movement of air, from high pressure to low pressure.pressure to low pressure.

Copyright © 2010 Ryan P. Murphy

Page 3: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

The wind is caused by the different The wind is caused by the different temperatures (and therefore air temperatures (and therefore air pressure differences) around a planet.pressure differences) around a planet.This is caused by the Sun.This is caused by the Sun.

Copyright © 2010 Ryan P. Murphy

Page 4: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

The topography of the land The topography of the land (Mountain Effect)(Mountain Effect)

Copyright © 2010 Ryan P. Murphy

Page 5: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

• An important renewable resource.

Page 6: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

• Brings rain – Without wind, the land wouldn’t get the evaporated water from the oceans.

Copyright © 2010 Ryan P. Murphy

Page 7: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

• Activity! Draw the globe below.

0

30N

30S

60N

60S

Equator

Page 8: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

Global Winds (Word Bank) Global Winds (Word Bank) Go back to drawing of globeGo back to drawing of globe

- Doldrums- Doldrums- Horse latitudes- Horse latitudes- Trade Winds- Trade Winds- Prevailing Westerlies- Prevailing Westerlies- Polar Easterlies- Polar Easterlies

Copyright © 2010 Ryan P. Murphy

Page 9: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

• Doldrums- Areas of no wind , occurs at the equator, air here heats up fast causing low pressure.

Copyright © 2010 Ryan P. Murphy

Page 10: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

• Horse Latitudes- Areas of no wind occurs at 30N + 30, air stops moving toward the poles and sinks.

Copyright © 2010 Ryan P. Murphy

Page 11: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

• Horse Latitudes- Areas of no wind occurs at 30N + 30, air stops moving toward the poles and sinks.

Copyright © 2010 Ryan P. Murphy

When boats couldn’t find winds they would drop their weight. Often horses.

Page 12: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

• Horse latitudes again.

Copyright © 2010 Ryan P. Murphy

Page 13: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

• Trade Winds- Surface winds are blown toward the equator because the horse latitudes produce areas of high pressure.– Coriolis force curves the wind.

Copyright © 2010 Ryan P. Murphy

Page 14: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

• Prevailing Westerlies- Winds blowing toward the pole, move from west to east, occurs between 30+ 60

Copyright © 2010 Ryan P. Murphy

Page 15: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy
Page 16: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

• Polar Easterlies- Cold air sinks and heads toward the equator, Coriolis Effect curves the winds

Copyright © 2010 Ryan P. Murphy

Page 17: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy
Page 18: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

• What is the name of the winds under the boxes below?

Copyright © 2010 Ryan P. Murphy

Page 19: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

The rotation of the earth (which The rotation of the earth (which causes the Coriolis Force).causes the Coriolis Force).

Copyright © 2010 Ryan P. Murphy

Page 20: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

Coriolis Force: A rotating body Coriolis Force: A rotating body deflects.deflects.

Copyright © 2010 Ryan P. Murphy

Page 21: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

• Pressure gradient forces cause the hurricanes to spin opposite of the Coriolis Force.

Copyright © 2010 Ryan P. Murphy

Page 22: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

• Pressure gradient forces cause the hurricanes to spin opposite of the Coriolis Force but the Coriolis Force keeps Atlantic forming hurricanes from crossing the equator and sends them NW.

Copyright © 2010 Ryan P. Murphy

Page 23: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy
Page 24: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

• Coriolis Force means that you can’t fly in a straight line on a moving planet.

Copyright © 2010 Ryan P. Murphy

Page 25: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy
Page 26: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

Most importantly, wind travels from Most importantly, wind travels from areas of high pressure to areas of areas of high pressure to areas of low pressure!low pressure!

High Pressure Wind

Low Pressure

Copyright © 2010 Ryan P. Murphy

Coriolis Force

Page 27: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

The Jet Stream: Any of the high-The Jet Stream: Any of the high-speed, high-altitude air currents that speed, high-altitude air currents that circle the earth in a westerly circle the earth in a westerly direction. direction.

Copyright © 2010 Ryan P. Murphy

Page 28: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

• Flying times can be significantly shorter going from California to New York than vice versa because of the Jet Stream (100+kph)

Copyright © 2010 Ryan P. Murphy

Page 29: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy
Page 30: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy
Page 31: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

• Jet Stream: Like the ocean current in the movie except in the air.

Copyright © 2010 Ryan P. Murphy

Page 32: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

Sea Breeze (Day): The breeze that Sea Breeze (Day): The breeze that blows from the sea toward the land blows from the sea toward the land during the day. during the day.

Copyright © 2010 Ryan P. Murphy

Page 33: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

Sea Breeze (Day): The breeze that Sea Breeze (Day): The breeze that blows from the sea toward the land blows from the sea toward the land during the day.during the day.

Copyright © 2010 Ryan P. Murphy

Page 34: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

Sea Breeze (Day): The breeze that Sea Breeze (Day): The breeze that blows from the sea toward the land blows from the sea toward the land during the day.during the day.

Copyright © 2010 Ryan P. Murphy

Page 35: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

Sea Breeze (Day): The breeze that Sea Breeze (Day): The breeze that blows from the sea toward the land blows from the sea toward the land during the day.during the day.

Copyright © 2010 Ryan P. Murphy

Page 36: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

Sea Breeze (Day): The breeze that Sea Breeze (Day): The breeze that blows from the sea toward the land blows from the sea toward the land during the day.during the day.

Copyright © 2010 Ryan P. Murphy

Page 37: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

Sea Breeze (Day): The breeze that Sea Breeze (Day): The breeze that blows from the sea toward the land blows from the sea toward the land during the day.during the day.

Copyright © 2010 Ryan P. Murphy

Page 38: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

Sea Breeze (Day): The breeze that Sea Breeze (Day): The breeze that blows from the sea toward the land blows from the sea toward the land during the day. during the day.

Copyright © 2010 Ryan P. Murphy

Page 39: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

Sea Breeze (Day): The breeze that Sea Breeze (Day): The breeze that blows from the sea toward the land blows from the sea toward the land during the day.during the day.

Copyright © 2010 Ryan P. Murphy

Page 40: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

Caused by air rising over the warmer Caused by air rising over the warmer land (day) and is replaced by cooler land (day) and is replaced by cooler air from above the sea.air from above the sea.

Copyright © 2010 Ryan P. Murphy

Page 41: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

Land Breeze (Night): The breeze that Land Breeze (Night): The breeze that blows from the land toward the sea. blows from the land toward the sea.

Copyright © 2010 Ryan P. Murphy

Page 42: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

• Land Breeze (Night): The breeze that blows Land Breeze (Night): The breeze that blows from the land toward the sea. from the land toward the sea. – High specific heat of water slowly releases High specific heat of water slowly releases

stored energy from the day during the night stored energy from the day during the night making the water warmer than the land.making the water warmer than the land.

Copyright © 2010 Ryan P. Murphy

Page 43: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

• Land Breeze (Night): The breeze that blows Land Breeze (Night): The breeze that blows from the land toward the sea. from the land toward the sea. – High specific heat of water slowly releases High specific heat of water slowly releases

stored energy from the day during the night stored energy from the day during the night making the water warmer than the land.making the water warmer than the land.

Copyright © 2010 Ryan P. Murphy

Page 44: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

• Land Breeze (Night): The breeze that blows Land Breeze (Night): The breeze that blows from the land toward the sea. from the land toward the sea. – High specific heat of water slowly releases High specific heat of water slowly releases

stored energy from the day during the night stored energy from the day during the night making the water warmer than the land.making the water warmer than the land.

Copyright © 2010 Ryan P. Murphy

Page 45: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

• Land Breeze (Night): The breeze that blows Land Breeze (Night): The breeze that blows from the land toward the sea. from the land toward the sea. – High specific heat of water slowly releases High specific heat of water slowly releases

stored energy from the day during the night stored energy from the day during the night making the water warmer than the land.making the water warmer than the land.

Copyright © 2010 Ryan P. Murphy

Page 46: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

• Which is a sea breeze and which is a land breeze?

Copyright © 2010 Ryan P. Murphy

Page 47: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

• Which is a sea breeze and which is a land breeze?

Copyright © 2010 Ryan P. Murphy

Page 48: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

• Which is a sea breeze and which is a land breeze?

Copyright © 2010 Ryan P. Murphy

Page 49: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

• Which is a sea breeze and which is a land breeze?

Copyright © 2010 Ryan P. Murphy

Page 50: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

• Which is a sea breeze and which is a land breeze?

Copyright © 2010 Ryan P. Murphy

Page 51: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

Mountain Winds: Mountains can Mountain Winds: Mountains can create strong winds. create strong winds. Warm air risesWarm air rises up Mtn. up Mtn. (day)(day)

Copyright © 2010 Ryan P. Murphy

Page 52: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

Mountain Winds: Mountains can Mountain Winds: Mountains can create strong winds. create strong winds. Warm air risesWarm air rises up Mtn. up Mtn. (day),(day), Cool air sinks down Cool air sinks down Mtn. (Night)Mtn. (Night)

Copyright © 2010 Ryan P. Murphy

Page 53: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

• Mountain Winds (Day)

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Page 54: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

• Mountain Winds (Night)

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Page 55: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

Mountain Rain Shadow Effect: Mountain Rain Shadow Effect:

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Page 56: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

WetWet DryDry

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Page 57: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy
Page 58: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy
Page 59: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy

• Water availability varies greatly on this planet.

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Page 60: The movement of air, from high pressure to low pressure. The movement of air, from high pressure to low pressure. Copyright © 2010 Ryan P. Murphy