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2.3 Winds Understand the cause of winds and how winds affect climate 1 2.3.1 Define Prevailing Winds Prevailing Wind Regular, High predictable, normal Low wind direction. Caused by global convection cells when air blows from high pressure to low pressure 2 2.3.2 Describe conditions that results in Land Breeze Sea air warmer than land air Air rises over sea Relative Low pressure over sea H Land air moves to lower pressure 3 L 2.3.2 Describe conditions that results in Sea Breeze Land air warmer than sea air Air rises over land Relative Low pressure over L land Sea air moves to lower pressure 4 H Night Breeze Night Breeze Day Breeze 5 2.3.3 State the impact of the Coirolis Effect on wind direction. Objects in motion tend to deflect To the right in northern hemisphere To the left in southern hemisphere 6 2.3.4 Infer how wind systems relate to major pressure belts Air rising from the equator Settles at the poles Result = 6 convection cells 7 2.3.4 continued… 3 above and 3 below the equator (low). Low pressures result where hot air rises. High pressures result where air 8settles 2.3.4 continued Global highs and lows due to uneven heating of the earth Air moves from high pressure to low pressure creating winds Winds are deflected in the directions indicated on the diagram due to the coiriolis effect. 9 2.3.4 continued L H Equator Low H L 10 H H 2.3.5 Explain how wind systems and temperatures are related How do the prevailing winds affect temperature in: 1. Argentina 2. Columbia 3. Baffin Island 4. Newfoundland 11 2.3.6 Define windward The side of the mountain facing the wind Windward 12 2.3.6 Define Leeward Mountainside sheltered from the wind 13 Leeward 2.3.6 Define Rain Shadow Area with low rainfall on the leeward side of the mountain 14 Rain Shadow 2.3.7 Examine how the type of rainfall is related to the nature of location. 1. Orographic Rainfall 2. Frontal Rainfall 3. Convectional Rainfall 15 1. Orographic rainfall Moisture laden air blows off the sea Forced up by mountains Air cools at higher altitude Cool air holds 16less moisture Chinook winds 1. Orographic Rainfall Clouds condense and rain falls Most rain falls on the windward side Leeward side is often in a dry rain shadow 17 Rain Shadow 2. Frontal Rainfall Warm moisture air meets cold air Warm air is less dense & is forced up over the cooler, more dense air Warm Warm moisture air Air cools at higher altitude 18 Cold Air Weather Front 2. Frontal Rainfall Cool air holds less moisture Clouds condense Precipitation falls Weather Front 19 3. Convectional rainfall Forms in tropics or interior of continents Sun causes large amounts of water to evaporate Hot air rises forms convection currents (hence the name) 20 Often associated with thunderstorms. 3. Convectional rainfall Warm moisture air cools at higher altitude Cool air holds less moisture Clouds condense Rain falls 21 2.3.8 Explain how wind systems and precipitation How do the prevailing winds affect precipitation in: 1. England 2. Midwestern U.S. 3. British Columbia 4. Northern Africa 5. Central Australia Question #26 p. 67 22