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Wind Notes. Why Air Moves. Wind is created by differences in air pressure Bigger difference = faster wind Caused by unequal heating of earth. Air. The air by the equator is warm and rises Low pressure The air by the poles is cold and dense High pressure

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why air moves
Why Air Moves
  • Wind is created by differences in air pressure
  • Bigger difference = faster wind
    • Caused by unequal heating of earth
slide3
Air
  • The air by the equator is warm and rises
    • Low pressure
  • The air by the poles is cold and dense
    • High pressure
  • Wind will then travel from poles to equator
    • Move from area of high pressure to area of low
pressure belts
Pressure Belts
  • Wind travels in small belt patters
  • It never travels too far because it will cool as it moves and sink back down
  • Moves at a about 30 degrees at a time or down the earth
earth s rotation affects wind direction
Earth’s rotation affects wind direction
  • Without the earths rotation the global winds would flow directly from the poles to the equator.
  • Coriolis Effect
    • Influence of Earth’s rotation on objects that move over Earth.
the coriolis effect
The Coriolis Effect
  • The wind does not travel perfectly north to south
  • Earth’s rotation causes wind to travel in a curved path
coriolis effect
Coriolis Effect
  • Global winds curve as Earth turns beneath them.
  • Northern Hemisphere
    • Winds curve to the right
  • Southern Hemisphere
    • Winds curve to the left
  • Only noticeable for winds that travel long distances.
  • Causes global winds to travel along 3 routes in each hemisphere
    • Routes are called global wind belts
types of wind
Types of Wind
  • Local wind
    • Sea Breeze
    • Land Breeze
    • Monsoon – Seasonal changes in wind
  • Global wind
    • Doldrums / Horse Latitudes
    • Easterlies / Westerlies
    • Jet Stream
  • Both caused by uneven heating
global winds
Global Winds

Sunlight is concentrated near the equator because it strikes the surface directly

  • The distance winds travel varies.
  • Some winds die out quickly
  • Global winds
    • Winds that travel long distances in steady patterns over several weeks
    • Caused by uneven heating between the equator and the north and south poles

Sunlight is more spread out near the poles because it strikes at a lower angle

global winds continued
Global Winds Continued
  • Near the equator concentrated sunlight heats the surface to a high temperature. Warm air rises, producing low pressure.
  • In regions closer to the poles, the sunlight is more spread out. The air above them is cooler and dense. Sinking dense air produces high pressure that sets global winds in motion.
calm regions
Calm Regions
  • Doldrums
    • Low-pressure zones near equator
    • The rising, moist air produces clouds and heavy rain.
  • Horse Latitudes
    • High-pressure zones located 30 degrees north and south of the equator.
    • Clear and dry weather
wind belts
Wind Belts
  • Coriolis effect creates 3 wind belts in each hemisphere
  • Trade Winds
    • Blow from east. Move towards equator. Die out as they near the equator
  • Westerlies
    • Blow from the west. Move towards the poles. Brings storms across much of the U.S.
  • Easterlies
    • Blow from the east. Move towards mid-latitudes. Storms occur when cold air from easterlies meets the warm air of the westerlies.
effects of wind on travel
Effects of Wind on Travel
  • How would wind effect travel?
    • Sailors used to dread traveling through the doldrums and the horse latitudes because there wasn’t enough wind.
    • To avoid the calm regions, sailors sought out global wind belts
    • Sailors rely on trade winds to get across the ocean
jet streams flow near the top of the troposphere
Jet streams flow near the top of the troposphere
  • Jet streams
    • Flow in upper troposphere
    • Travels west to east
    • Often moves at high speeds (greater than 124 mi/hr).
    • Form because Earth’s

surface is heated

unevenly.

    • Loop north and south
jet streams
Jet Streams
  • Each hemisphere has 2 jet streams
  • Subtropical jet stream
    • Flow closer to poles in SUMMER
  • Polar jet stream
    • Has a strong influence of weather
    • Can pull cold air down from Canada or pull warm air up.
    • Strong storms form along its loops
patterns of heating and cooling cause local winds
Patterns of heating and cooling cause local winds
  • Local Winds
    • Some winds change daily in a regular pattern.
    • Blow within small areas
  • Land breezes and Sea breezes are similar but opposite.
land breeze
Land Breeze
  • Wind blows from the land to the ocean
  • Happens during the Night
  • Land cools down causing it to have a low air pressure
  • Water maintains its temperature causing it to have a higher air pressure
  • Air will move from high pressure to low pressure
  • It will move from the land to water