1 / 49

WINDS

WINDS. What is wind?. HORIZONTAL MOVEMENT OF AIR FROM AN ARERA OF HIGH PRESSURE TO AN AREA OF LOW PRESSURE. What causes wind?. DIFFERENCES IN AIR PRESSURE. How do scientists measure wind speed?. ANEMOMETER. SCIENCE ALERT. HEAT IS ALWAYS TRANSFERRED FROM WARMER OBJECTS TO COOLER OBJECTS.

alamea
Download Presentation

WINDS

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript

  1. WINDS

  2. What is wind? HORIZONTAL MOVEMENT OF AIR FROM AN ARERA OF HIGH PRESSURE TO AN AREA OF LOW PRESSURE

  3. What causes wind? DIFFERENCES IN AIR PRESSURE

  4. How do scientists measure wind speed? ANEMOMETER

  5. SCIENCE ALERT HEAT IS ALWAYS TRANSFERRED FROM WARMER OBJECTS TO COOLER OBJECTS

  6. What is “WIND CHILL FACTOR”? Wind blowing over your body and removing heat.

  7. I. WHAT IS WIND? a) Horizontal movement of air from an area of high pressure to an area of low pressure. b) Wind speed is measured with an ANEMOMETER c) WIND CHILL FACTOR is the amount of heat being removed from your body as cold wind blows over your body.

  8. SCIENCE ALERT WARMER AIR IS LESS DENSE THAN COOLER AIR “Cold air follows the warm air”

  9. LOCAL WINDS Blow over short distances Caused by unequal heating of the Earth’s surface within a small area

  10. LOCAL WINDS LAND BREEZE SEA BREEZE

  11. SEA BREEZE – winds coming from a body of water

  12. LAND BREEZE – winds coming from a land mass

  13. II. Local Winds • a) Caused by unequal heating of the Earth’s surface within a small area for a short distance • b) SEA BREEZE • Takes more energy to heat up a body of water than it does land. • Cooler air from a body of water takes the place of warm air over land • c) LAND BREEZE • Cooler air from a land mass takes the place of the warm air over the water

  14. GLOBAL WINDS

  15. What are “GLOBAL WINDS”? Like local winds, they are caused by unequal heating of the earths surface but occurs over a larger area.

  16. How is the SUNS energy distributed over the EARTHS surface?

  17. AREA OF MOST DIRECT ENERGY

  18. AREA OF LEAST DIRECT ENERGY Because of the curvature of the EARTH, the SUN’S energy is spread out over a larger area …

  19. …as a result, it’s cooler at the POLES than it is at the EQUATOR

  20. What are “GLOBAL CONVECTION CURRENTS”? Temperature differences between the EQUATOR and the POLES produce giant convection currents.

  21. What is the “CORIOLIS EFFECT”? The way the Earth's rotation makes global winds curve

  22. If we had no EARTH rotation… WIND PATH WIND PATH

  23. …but because the EARTH rotates counter-clockwise…

  24. …the actual wind path is…

  25. III. Global Winds a) Like local winds, global winds are caused by unequal heating of the earths surface but occurs over a larger area. b) Temperature differences between the EQUATOR and the POLES produce global convection currents. c) Coriolis Effect is the way the Earth's rotation makes global winds curve.

  26. What are the GLOBAL WIND BELTS? Belts of winds and calm areas that circle the EARTH

  27. The CORIOLIS EFFECT produces calm areas…

  28. DOLDRUMS • Regions near the EQUATOR with little or no winds. • Warm air rises steadily, creating an area of low pressure. • Cool air moves in but is heated before it moves far.

  29. HORSE LATITUDES • At about 30º north and south latitudes the warm air stops moving towards the poles and sinks creating another belt of calm air. • Named because ships in this area could not move because of a lack of winds. Sailors running out of food and water would throw their horses overboard.

  30. HORSE LATITUDES

  31. What are the major GLOBAL WIND BELTS? • Trade Winds • Polar Easterlies • Prevailing Westerlies

  32. The CORIOLIS EFFECT produces wind belts…

  33. TRADE WINDS • As the warm air sinks into the HORSE LATITUDES it produces a high pressure that causes surface winds to blow towards the equator. • The CORIOLIS EFFECT allows the winds to move towards the west.

  34. TRADE WINDS

  35. PREVAILING WESTERLIES • Located between 30º to 60º latitudes north and south winds blow towards the poles are turned towards the east by the CORIOLIS EFFECT.

  36. PREVAILING WESTERLIES

  37. POLAR EASTERLIES • Cold air near the poles sink and flow back towards the lower latitudes. • The COLIOLIS EFFECT shifts these winds back to the west.

  38. POLAR EASTERLIES

  39. JET STREAMS • Bands of high speed winds (200 to 400 Kph) • Located 10 km above the Earth’s surface • Blow west to east • Caused by the meeting of different air temperature masses

  40. IV. Global Wind Belts • Belts of winds and calm areas that circle the EARTH b) DOLDRUMS • Regions near the EQUATOR with little or no winds. • Warm air rises steadily, creating an area of low pressure. • Cool air moves in but is heated before it moves far.

  41. c)HORSE LATITUDES a) At about 30º north and south latitudes the warm air stops moving towards the poles and sinks creating another belt of calm air. b) Named because ships in this area could not move because of a lack of winds. Sailors running out of food and water would throw their horses overboard.

  42. d) Trade winds • As the warm air sinks into the HORSE LATITUDES it produces a high pressure that causes surface winds to blow towards the equator. • The CORIOLIS EFFECT allows the winds to move towards the west.

  43. e) Prevailing Westerlies • Located between 30º to 60º latitudes north and south winds blow towards the poles are turned towards the east by the CORIOLIS EFFECT. f)Polar Easterlies • Cold air near the poles sink and flow back towards the lower latitudes. • The COLIOLIS EFFECT shifts these winds back to the west.

  44. g) Jet Stream • Bands of high speed winds (200 to 400 Kph) b) Located 10 km above the Earth’s surface c) Blow west to east d) Caused by the meeting of different air temperature masses

More Related