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WINDS.

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Presentation on theme: "WINDS."— 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 DIFFERENCES IN AIR PRESSURE
What causes wind? DIFFERENCES IN AIR PRESSURE

4                              

5                                                                   

6 How do scientists measure wind speed?
ANEMOMETER

7 HEAT IS ALWAYS TRANSFERRED FROM WARMER OBJECTS TO COOLER OBJECTS
SCIENCE ALERT HEAT IS ALWAYS TRANSFERRED FROM WARMER OBJECTS TO COOLER OBJECTS

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

9 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.

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

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

12 LOCAL WINDS LAND BREEZE SEA BREEZE

13 SEA BREEZE – winds coming from a body of water

14 LAND BREEZE – winds coming from a land mass

15 II. Local Winds b) SEA BREEZE c) LAND BREEZE
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

16 GLOBAL WINDS

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

18 How is the SUNS energy distributed over the EARTHS surface?

19 AREA OF MOST DIRECT ENERGY

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

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

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

23

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

25 If we had no EARTH rotation…
WIND PATH WIND PATH

26 …but because the EARTH rotates counter-clockwise…

27 …the actual wind path is…

28 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.

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

30 The CORIOLIS EFFECT produces calm areas…

31 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.

32

33 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.

34 HORSE LATITUDES

35 What are the major GLOBAL WIND BELTS?
Trade Winds Polar Easterlies Prevailing Westerlies

36 The CORIOLIS EFFECT produces wind belts…

37 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.

38 TRADE WINDS

39 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.

40 PREVAILING WESTERLIES

41 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.

42 POLAR EASTERLIES

43 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

44

45 Belts of winds and calm areas that circle the EARTH
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.

46 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.

47 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.

48 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.

49 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


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