Unequal Heating, Air Pressure and Winds

1. Unequal Heating, Air Pressure and Winds

2. Atmosphere • Atmosphere: a mixture of gases that surrounds Earth: acts like a blanket • Contains oxygen • Protects from sun • Keeps heat in • Protects from meteors

3. Composition of Troposphere • Nitrogen=78% • Oxygen=21% • Other 1%=water vapor, CO2 and other

4. Weather Factors

5. Greenhouse Effect • These gases absorb the heat and act as a “blanket” to keep Earth warm. • Some greenhouse gases: water, methane, carbon dioxide.

6. Air Pressure Review • Air has mass. • Air takes up space. • Air has density. • Air pressure is the weight of a column of air pressing down on an area.

7. Atmosphere/Pressure • Pressure strongest at surface-more air above you • *as altitude (height above surface) increases, air pressure decreases • Stack of books

8. Air Pressure As Air Pressure decreases, so does density.

9. Convection Currents!

10. Heating and Cooling of Land and Water Mystery…Can You Help Solve It?

11. The Teacher Has Performed An Experiment and Asks That YOU Help Make Some Conclusions About the Data or Information Gathered.

12. Experiment Materials and Procedures: The Teacher Used A Thermometer, A Heat Lamp, A Cup of Sand, and A Cup of Water to Find the Temperatures of Both the Sand and The Water Over Two Hours.

13. DATA FROM THE EXPERIMENT

14. TURN AND TALK! Answer the Questions Cooperatively.

15. CONCLUSION • Land Heats Up And Cools Down Faster Than Water!During the day, land heats faster than a body of water, so the air above the land becomes warmer. The warm air expands and creates a low-pressure system. The cooler air above the body of water blows inland and under the warm air. At night, the opposite happens.

16. Morning at the Beach What is the temperature of the sand? Of the water?

17. Mid-Afternoon at the Beach What is the temperature of the sand? Of the water?

18. Evening at the Beach What is the temperature of the sand? Of the water?

19. Unequal Heating What heats up quicker? What heats up slower? At night, which cools down quicker? Which cool down slower?

20. Unequal Heating Land heats up and cools down quickly. Water heats up and cools down slowly.

21. Unequal Heating Warm air rises and creates a low pressure system. Cold air sinks and creates a high pressure system.

22. Do You Remember How Convection Works?

23. Winds

24. The movement of air caused by differences in air pressure is called WIND.

25. What causes winds? More of a difference in pressure = faster winds Lots of difference

26. Local Winds Have you ever flown a kite at the beach on a hot summer day? Even if there is no wind inland, there may be a cool breeze blowing in from the water toward the beach. This breeze is an example of local winds!

27. Local Winds Local winds are winds that blow over short distances. They are caused by unequal heating of Earth’s surface within a small area. 4 types sea breezes and land breezes Mountain breeze and valley breeze

28. Why is the ocean colder than the land during the day and warmer than the land during the night?

29. Sea Breezes and Land Breezes

30. Sea Breeze (Morning) Land heats up faster than water. Hot air over land rises (Low Pressure), cool air over water falls (High Pressure). Winds move from the water (High Pressure) to the land (Low Pressure).

31. Land Breeze (Evening) Land cools off faster than water. Cool air over land falls (High Pressure), warm air over water rises (Low Pressure). Winds move from the land (High Pressure) to the water (Low Pressure).

32. Let’s Draw Land and Sea Breezes…

33. Let’s Draw Land and Sea Breezes…

34. Animation of Sea Breeze & Land Breeze • http://www.classzone.com/books/earth_science/terc/content/visualizations/es1903/es1903page01.cfm?chapter_no=visualization

36. Valley Breeze (Day) During the day the sun warms the air slopes, creating a valley breeze… at nightfall, the air along the mountain slopes cools…

37. Mountain Breeze (Night) This cool air moves down the slopes into the valley, producing a mountain breeze!

38. Let’s Draw Mountain and Valley Breezes

39. Global Winds Created by unequal heating of Earth’s surface.

40. Global winds Warm air rises from the equator and sinks at the poles. • Warm air = less dense = low pressure • Cool air = more dense = high pressure

41. Global Winds… cont… • The movement of air between the equator and the poles produces global winds. • Coriolis effect produces patterns of air circulation called global winds.

42. GLOBAL WIND PATTERNS

43. Coriolis Effect. • As the Earth rotates, winds and currents move in a curved path, called the coriolis effect.

45. Global Wind Belts Major global wind systems: Polar easterlies, westerlies, and trade winds.

46. Doldrums • Where the trade winds meet around the equator • Very little wind because the warm air rising = low pressure

47. Horse Latitudes • High pressure areas… 300N and 300S • Very weak winds

48. Jet Streams Bands of high speed winds Upper troposphere and lower stratosphere Blow from west to east at speeds of 200-400 km/hr. Help airplanes save fuel and time when traveling east.

49. Atmosphere

50. Anemometer- a device used to measure wind speed. Wind vanes measure wind direction.