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Weather and Climate

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Title: Weather and Climate


1
Weather and Climate
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  • Weather is the condition of the bottom layer of
    the earths atmosphere in one place over a short
    period of time.
  • Weather is the day-to-day conditions of a
    particular place.

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  • Climate is the term for weather patterns that an
    area typically experiences over an extended
    period of time.
  • Temperatures, precipitation, seasons, etc.

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What factors influence climate?
  • The movement of the earth on its axis is called
    rotation.
  • One complete orbit around the sun is called a
    revolution.

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  • Earths rotation and tilt

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Latitude effects climate
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  • Equinox When the earth is not tilted and the
    suns rays fall directly on the equator.
  • Actually means Equal night. Around March 21
    and September 23

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  • Tropic of Cancer 23 ½ degrees N, the
    northernmost point on the Earth to receive direct
    rays of the sun
  • Tropic of Capricorn 23 ½ degrees S, the
    southernmost point on the Earth to receive direct
    rays of the sun

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  • Solstice When the suns rays hit the tropic of
    Cancer. The farthest tilt north and is the
    beginning of summer in the Northern H. and the
    beginning of winter in the Southern H. (around
    June 21).
  • When the earth tilts the other way we have the
    opposite. Around Dec. 22)

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The Poles
  • Because of the earths tilt the poles have
    continuous sunlight or darkness for six months
    out of the year.
  • March 20 September 23
  • September 23- March 20

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  • The greenhouse effect traps solar radiation as
    heat within the atmosphere.

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Factors Effecting Climate
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Low Latitudes
  • Between 30 Degrees N and 30 degrees S latitude.
  • Receive direct sunlight year round
  • Warm and hot climates

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High Latitudes
  • The earths polar regions (between 60 and 90
    degrees latitude)
  • Arctic Circle and Antarctic Circle (66 ½ degrees
    latitude)
  • Have 6 months of sunlight and 6 months of
    darkness

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Mid Latitudes
  • Between 30 and 60 degrees latitude
  • A temperate climate, ranging from fairly hot to
    fairly cold
  • Dramatic seasonal changes.

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  • Elevation
  • Air temperature decreases at a rate of 3.5 F for
    every 1000 feet in elevation.
  • Mount Kilimanjaro is located almost on the
    equator but has snow caps year round.

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Mt. Kilimanjaro
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Wind
  • Wind is caused by air flowing from high pressure
    to low pressure. Since the Earth is rotating,
    however, the air does not flow directly from high
    to low pressure, but it is deflected to the right
    (in the Northern Hemisphere to the left in the
    Southern Hemisphere), so that the wind flows
    around the high and low pressure areas.
  • For small, short-lived systems (such as in the
    cold outflow of a thunderstorm) the wind will
    flow directly from high pressure to low pressure.
  • video

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  • Prevailing Winds Global winds that blow in a
    fairly constant pattern.
  • Doldrums At the equator, global winds are
    diverted north and south, leaving a narrow,
    generally windless band know as the doldrums

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Oceans and climate
  • Water heats and cools slower than land.
  • Oceans tend to have a moderating effect on
    climate, meaning that places close to oceans
    dont have as extreme differences between their
    warmest and coldest days.

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Ocean currents
  • Cold and warm streams of water that move through
    the oceans.
  • Ocean currents affect climate in the coastal
    areas in which they flow

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Precipitation
  • Humidity The amount of water vapor contained in
    the atmosphere.
  • Precipitation is the forms of water that fall
    from the atmosphere to the earths surface.
  • Rain, snow, hail, sleet,

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What causes precipitation
  • Precipitation forms when air temperature changes.
  • Warm air holds more water than cold air.
  • When air cools it can no longer hold as much
    water. Tiny droplets of water gather together an
    form clouds.
  • Precipitation forms when more water collects in
    clouds then they can hold.

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Convectional precipitation
  • In convectional precipitation, unequal heating of
    the surface causes an air parcel to become warmer
    and less dense than the surrounding air. Because
    it is less dense, it rises. As it moves upward,
    it cools, and condensation with precipitation may
    occur.

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Frontal precipitation
  • Frontal precipitation results when the leading
    edge( front) of  a warm air mass meets a cool air
    mass. The warmer air mass is forced up over the
    cool air. As it rises the warm air cools,
    moisture in the air condenses and forms clouds,
    resulting in precipitation.

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Orographic Precipitationalso called the Rain
Shadow Effect
  • Orographic precipitation results when warm moist
    air of the ocean is forced to rise by large
    mountains. As the air rises it cools, moisture in
    the air condenses and clouds and precipitation
    result on the windward side of the mountain while
    the leeward side receives very little.

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Leeward side
Windward side
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El Nino
  • The periodic change in the pattern of ocean
    currents, water temperatures, and weather in the
    mid-Pacific region
  • It doesnt occur every year but is occurring more
    frequently.
  • It affects climate around the world.
  • Video

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Climate Regions
  • Climates are organized into 5 regions tropical,
    dry, mid latitude, high latitude, and highland
  • These large regions are divided into further
    climate zones

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Tropical Climates
  • Tropical climates found in low latitudes include
    tropical wet and tropical dry
  • Tropical wet climates are hot (80 F) and have
    high rainfall all year
  • Tropical dry climates have dry winters and wet
    summers, along with high temperatures year-round

45
Dry Climates
  • Two types of dry climates are desert and steppe
  • Deserts have little rainfall and temperature
    varies from heat in the day to cool at night
  • Natural vegetation includes scattered shrubs and
    cacti
  • Often bordering deserts are steppes, dry largely
    treeless grasslands

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Mid Latitude Climates
  • Marine west coast on western coastlines that
    have cool summers and abundant rainfall
  • Mediterranean Mild rainy winters and hot dry
    summers
  • Humid subtropical Short, mild winters and
    year-round rain
  • Humid continental warm summers and cold winters
    with varying precipitation

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High Latitude Climates
  • Subarctic climates experience bitterly cold
    winters and short, cool summers
  • Permafrost, a thin layer of soil beneath the
    surface is permanently frozen
  • Tundra regions are closer to the Poles and have
    dark, bitter winters
  • Ice cap regions are covered often by 2-3 miles of
    snow and ice

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Highland Climates
  • High mountain areas experience year-round cold
    temperatures because of elevation
  • These can be found in any latitude zone where
    mountains are high enough

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