1. Wind Notes
2012

2. Wind The HORIZONTAL MOVEMENT of air.
Caused by Differences in TEMPERATURE and PRESSURE

3. Warm Air

4. Cold Air

5. DIFFERENCES IN PRESSURE
DIFFERENCES IN PRESSURE
Rising air creates: LOW PRESSURE
If air is lifted up, that means there is Less air pushing down on earth.
Sinking air creates: HIGH PRESSURE
If air is sinking, then air is pushing down on the surface of earth with a High amount of pressure.

6. THE CREATION OF WIND
Differences in temperature cause air to rise and sink all over earth’s surface.
Rising and sinking air create high and low pressure.
THE ATMOSPHERE DOES NOT LIKE UNBALANCED PRESSURE...
IT TRYS TO EQUAL OUT BY MOVING AIR FROM High to Low PRESSURE.
H L

7. Types of Wind: SEA BREEZE Air moves from the Sea.
Occurs during the day.
During the day, air over the sea is cool. The cool air is more dense, sinks, and forms high pressure.
During the day, the land heats up and air above it becomes less dense and rises. Rising air creates low

8. Types of Wind: LAND BREEZE Air moves from the Land
Occurs during the night.
During the night, the land cools quickly and the dense air above it begins to sink creating high pressure.
During the night, the sea stays warm and the less dense warm air above it rises creating low pressure.

9. Warm air rises and cold air sinks.
Global Winds
Wind current on a global scale.
Warm air rises and cold air sinks.
Temperature Differences
Rising and sinking air makes pressure differences
Pressure Difference
Mr. Fetch’s Earth Science Classroom

10. Global Temperature Patterns
The sun’s rays are weaker near the poles causing less warming. The air here is cool.
The sun’s rays are stronger near the equator causing more warming. The air here is warm.
Mr. Fetch’s Earth Science Classroom

11. Air moves between the equator and the poles.
Global Winds
Hadley Cells.
Air moves between the equator and the poles.
Global Winds
Mr. Fetch’s Earth Science Classroom

12. The Coriolis Effect Coriolis Effect
Air does not move in a straight line because of Earth’s rotation.
Coriolis Effect
Mr. Fetch’s Earth Science Classroom

13. Global Winds Northern Hemisphere Southern Hemisphere
Mr. Fetch’s Earth Science Classroom

14. Global Winds Remember, winds are named from where they come. 60°N 30°N
Polar Easterlies - From 90°N to 60°N - Deflected to right
60°N
Prevailing Westerlies - From 30°N to 60°N - Deflected to right
30°N
Easterly Trade Winds - From 30°N to O° - Deflected to right
Doldrums 0°
Easterly Trade Winds - From 30°S to 0° - Deflected to left
30°S
Prevailing Westerlies - From 30°S to 60°S - Deflected to left
60°S
Polar Easterlies - From 90°S to 60°S - Deflected to left
Mr. Fetch’s Earth Science Classroom