GLOBAL WINDS AND LOCAL WINDS

    Cards (18)

    • Wind is the movement of air.
    • Wind is caused by:
      1. Differences in temperature
      2. Differences in pressure
    • DIFFERENCES IN TEMPRERATURE:
      1. Warm air rises - makes molecules move faster and spread out ; Makes the air less dense (rise)
      2. Cold Air sinks - makes molecules move slower and group together ; makes the air more dense (sink)
    • DIFFERENCES IN PRESSURE:
      1. Rising air creates LOW pressure - if air is lifted UP, there is LESS air pushing down on earth.
      2. Sinking air creates HIGH pressure - if air is SINKING, then air is pushing down on earth with a HIGH amount of pressure.
    • THE CREATION OF WIND:
      1. Differences in temperature cause air to rise up & sink.
      2. Rising and sinking air creates high & low pressure.
      3. The atmosphere equals out pressure by moving air from high to low pressure.
    • THE CREATION OF WIND:
      1. HEATing the air, DECREASES the pressure
      2. COOL air, replaces warm air (HIGH PRESSURE)
      3. As air goes from high - low pressure winds form.
    • Wind is a horizontal movement of air.
    • There are 2 types of winds : local & global.
    • Global winds are patterns of wind that happen all over the world. They are created by the spin of the earth & difference in temperatures.
    • Polar Easterlies are winds that blow close to the north and south poles. (They blow away and curve east to west) (They are cold, dry winds)
    • Prevailing Westerlies are winds that predict most of our weather. (Blow from west to east)
    • Trade winds are winds that circle near the equator. They are used by ships for sailing the ocean.
    • Local winds are winds that are in one particular area.
      TYPES OF LOCAL WINDS
      1. Sea Breeze
      2. Land Breeze
      3. Mountain Breeze
      4. Valley Breeze
    • Sea Breeze : Air moves from the sea during the day.
    • Convection is the main way the atmosphere is heated.
    • Land Breeze : Air moves from the land at night.
    • Valley Breeze : The sun heats the valley air quickly and the warm air rises and moves up the mountain.
    • Mountain Breeze : At night the mountain air cools faster than the valley ; cool Air sinks down the mountain and wind moves in the opposite direction.