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1. Wind is caused by the uneven heating of
the Earth and its atmosphere
2. These temperature differences lead to
the creation of high pressure and low
pressure areas
3. Wind – the movement of air from an
area of high pressure to an area of low
pressure
Wind Formation:
1. Tilt in orbit around the sun
2. Curved surface of the Earth
3. Equator receives the most
radiation, poles receive the least
Cause ofTemperature Differences:
1. Warm air is less dense than cold air so it
rises
2. Cold air sinks and moves along the
Earth’s surface
Density of Air:
The tendency of a moving object to follow a
curved path rather than a straight one due
to Earth’s rotation
 Only perceived, the object/air is moving
along a straight line, but the air is moving
underneath it
Coriolis Effect:
Windless zone of the equator due to hot air
rising straight up
Doldrums:
From the equator to 30 degrees latitude
North or South, air descending on the
Earth’s surface creates steady winds
TradeWinds:
From 30 degrees to 60 degrees, wind
moves from west to east, responsible for
movement of weather in the US
Westerlies:
Cold air that blows from the Northeast to
Southwest near the poles
Easterlies:
Narrow belt of strong winds near top of
troposphere, blow from west to
east, average 60-110 miles per
hour, position changes daily and
seasonally, major effect on weather
Jet Stream
Concept: Land heats up and cools down
faster than water
LocalWinds:
Wind blowing from land to sea during the
night
Caused by:
• Water cools off slower so it warms the air
above it causing it to rise
• Air above land moves in to replace it
Land Breeze:
Wind blowing from sea to land during the
day
Caused by:
• Land warmed faster by the sun
• Air warmed above land rises
• Air above water moves in to replace it
Sea Breeze:
16. movement of air notes

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16. movement of air notes

  • 1.
  • 2. 1. Wind is caused by the uneven heating of the Earth and its atmosphere 2. These temperature differences lead to the creation of high pressure and low pressure areas 3. Wind – the movement of air from an area of high pressure to an area of low pressure Wind Formation:
  • 3. 1. Tilt in orbit around the sun 2. Curved surface of the Earth 3. Equator receives the most radiation, poles receive the least Cause ofTemperature Differences:
  • 4. 1. Warm air is less dense than cold air so it rises 2. Cold air sinks and moves along the Earth’s surface Density of Air:
  • 5. The tendency of a moving object to follow a curved path rather than a straight one due to Earth’s rotation  Only perceived, the object/air is moving along a straight line, but the air is moving underneath it Coriolis Effect:
  • 6.
  • 7. Windless zone of the equator due to hot air rising straight up Doldrums:
  • 8. From the equator to 30 degrees latitude North or South, air descending on the Earth’s surface creates steady winds TradeWinds:
  • 9. From 30 degrees to 60 degrees, wind moves from west to east, responsible for movement of weather in the US Westerlies:
  • 10. Cold air that blows from the Northeast to Southwest near the poles Easterlies:
  • 11.
  • 12.
  • 13. Narrow belt of strong winds near top of troposphere, blow from west to east, average 60-110 miles per hour, position changes daily and seasonally, major effect on weather Jet Stream
  • 14. Concept: Land heats up and cools down faster than water LocalWinds:
  • 15. Wind blowing from land to sea during the night Caused by: • Water cools off slower so it warms the air above it causing it to rise • Air above land moves in to replace it Land Breeze:
  • 16. Wind blowing from sea to land during the day Caused by: • Land warmed faster by the sun • Air warmed above land rises • Air above water moves in to replace it Sea Breeze: