Transcript
Page 1: Winds & Climate World Climate Patterns World Geo 3200/3202 Unit 2 November 2010

Winds & ClimateWorld Climate PatternsWorld Geo 3200/3202Unit 2November 2010

Page 2: Winds & Climate World Climate Patterns World Geo 3200/3202 Unit 2 November 2010

Lesson Outcomes

•2.3.1 Define the term prevailing winds. (k) •2.3.2 Describe conditions that result in

land breezes and sea breezes. (k) •2.3.3 State the impact of the Coriolis

effect on wind direction. (k) •2.3.4 Infer how wind systems relate to

major pressure belts. (a)

Page 3: Winds & Climate World Climate Patterns World Geo 3200/3202 Unit 2 November 2010

High Pressure & Low Pressure

• Winds blow from regions of high atmospheric pressure to areas of low atmospheric pressure.

• High and low pressures in the earth’s atmosphere are responsible for wind.

• Air under high pressure has a tendency to want to “escape” towards low pressure areas

Page 4: Winds & Climate World Climate Patterns World Geo 3200/3202 Unit 2 November 2010

High Pressure & Low Pressure

• Think—Air inside a balloon. If left untied the air will escape the high pressure of the balloon and create a wind blowing from high pressure inside the balloon to relatively low pressure outside the balloon.

• Think—Exhaling: when you exhale the air leaves your lungs because you create a high pressure inside your chest cavity and breath (wind is created from high pressure inside your chest to a lower pressure outside your chest.

Page 5: Winds & Climate World Climate Patterns World Geo 3200/3202 Unit 2 November 2010

Prevailing Winds• Regular, predictable,

normal wind direction are known as prevailing winds

• They are caused by global convection cells in the earth's atmosphere. (fig 4.10 on pg. 63)

Page 6: Winds & Climate World Climate Patterns World Geo 3200/3202 Unit 2 November 2010
Page 7: Winds & Climate World Climate Patterns World Geo 3200/3202 Unit 2 November 2010

Prevailing Winds• The global convection cells are created because of

the differential heating of the earth's surface.

• As the equatorial regions heats the air it rises creating a low pressure at the equator.

• The air falls to earth 30º  North and south creating high pressure belts.

• The other lows and highs can be predicted every 30º of latitude.

• Remember that wind directions move from highs to lows

Page 8: Winds & Climate World Climate Patterns World Geo 3200/3202 Unit 2 November 2010

• Low pressure belts are created at the equator & at 60° N & S

• High pressure belts are created at 30° N & S and at the poles

• Remember that wind directions move from highs to lows

Page 9: Winds & Climate World Climate Patterns World Geo 3200/3202 Unit 2 November 2010

Local Winds….Sea Breezes (4.8 p 61)• In the day time the land heats much faster than

the water (land has greater thermal conductive & water has the ability to dissipate heat at a faster rate)

• As a result, the air over the land heats & rises creating a relatively low pressure over the land

• The air pressure over the water/sea would be cooler and relatively high

• Winds therefore would blow from the sea towards the land as the cool ocean air moves in to replace the warm rising air above the land

Page 10: Winds & Climate World Climate Patterns World Geo 3200/3202 Unit 2 November 2010

Local Winds….Sea Breezes (4.8 p 61)• The wind is blowing off the

sea hence the name sea breeze

• We experience this in a lot of summer time situations.

• The opposite is true for ‘land breeze’.

Page 11: Winds & Climate World Climate Patterns World Geo 3200/3202 Unit 2 November 2010
Page 12: Winds & Climate World Climate Patterns World Geo 3200/3202 Unit 2 November 2010

Sea Breezes• Remember—winds are named for where they

come from;

▫ Easterly winds come out of the east;

▫ Southerly winds come out of the south;

▫ Sea breezes come from the sea.

▫ Land breezes comes from the land.

Page 13: Winds & Climate World Climate Patterns World Geo 3200/3202 Unit 2 November 2010

Global Convection Cells

• Alternating high and low pressures result from the convection cells. A low pressure belt is created at the equator and at 60º N and 60º S while high pressure belts are created at 30º N and 30ºS and at the poles.

• Prevailing Winds form global patterns because of these global pressure belts. They follow the laws of physics and blow from the high pressure belts to the low pressure belts.

Page 14: Winds & Climate World Climate Patterns World Geo 3200/3202 Unit 2 November 2010

Prevailing Wind Names •0-30º N = Northeast

trade winds •0-30º S = Southeast trade

winds •30-60º N and 30-60º S =

Prevailing Westerly winds •60-90º N = North Polar

easterlies •60-90º N = South Polar

easterlies

Page 15: Winds & Climate World Climate Patterns World Geo 3200/3202 Unit 2 November 2010

Coriolis Effect• The Coriolis effect explains why the winds

are deflected in the directions indicated on the in figure 4.11.

Page 16: Winds & Climate World Climate Patterns World Geo 3200/3202 Unit 2 November 2010

Coriolis Effect• The coroilis effect is a law

of physics that sates: objects in motion in the northern hemisphere are deflected to the right while in the southern hemisphere they are deflected to the left.

• Therefore winds in the north are deflected right and the winds in the south are deflected left.

Page 17: Winds & Climate World Climate Patterns World Geo 3200/3202 Unit 2 November 2010

Local Weather Patterns

•In our area, Eastern North America, prevailing winds are generally from west to east

•Generally, air masses move along a path from southwest to northeast

•We see this regularly in our weather patterns as low pressure systems (hurricanes, blizzards) move from the Eastern seaboard of the USA up to Atlantic Canada & over NL

Page 18: Winds & Climate World Climate Patterns World Geo 3200/3202 Unit 2 November 2010

Local Weather Patterns

Page 19: Winds & Climate World Climate Patterns World Geo 3200/3202 Unit 2 November 2010

Review

•What causes wind to blow? DIFFERENCES IN AIR PRESSURE

•What causes winds to be deflected from a straight path? CORIOLIS FORCE

•What causes the development of global convection cells and pressure belts. DIFFERENTIAL HEATING OF THE EARTH

•Winds that normally blow in a region are referred to as _?_. PREVAILING

Page 20: Winds & Climate World Climate Patterns World Geo 3200/3202 Unit 2 November 2010

Review•When do sea breezes occur?  DAY WHEN

LAND IS HOTTER THAN SEA •What name is given to the prevailing

winds between 60 and 90 degrees N. NORTH POLAR EASTERLIES

•What name is given to the prevailing winds between 60 and 90 degrees S. SOUTH POLAR EASTERLIES

•What name is given to the prevailing winds between 30 and 60 degrees N. WESTERLY

Page 21: Winds & Climate World Climate Patterns World Geo 3200/3202 Unit 2 November 2010

Review•What name is given to the prevailing

winds between 60 and 90 degrees S? WESTERLY

•What name is given to the prevailing winds between 0 and 30 degrees N? Northeast trade winds

•What name is given to the prevailing winds between 0 and 30 degrees S. SOUTHEAST TRADE WINDS

•When hot air rises what type of pressure is created?


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