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Chapter 17 Climate

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Title: Chapter 17 Climate


1
Chapter 17Climate
  • Climate is the pattern of weather that occurs in
    an area over many years. It determines the types
    of plants or animals that can survive, and it
    influences how people live.
  • Factors that affect climate include temperature,
    precipitation, air pressure, humidity, and number
    of days of sunshine, latitude, landforms,
    location of lakes and oceans, and ocean currents.

2
Latitude and Climate
  • Because solar radiation hits the equator
    directly, the area between 23.5o N and 23.5o S is
    called the tropics.
  • The area between 66.5o N and S and the poles is
    called the polar zones.
  • Between the polar zones and the tropics are the
    areas called the temperate zones,
  • where temperatures are moderate.

3
Other Factors that Affect Climate
  • Large Bodies of water create more moderate
    ranges in temperature because water holds heat
    longer, and takes longer to heat up. Water has a
    high specific heat capacity.
  • Ocean currents warm currents begin near the
    equator and flow towards higher latitudes warming
    land. When flowing toward the equator, they cool
    off and cool the land.
  • Mountains are higher in altitude and contain
    fewer air molecules to absorb the heat, thereby
    cooling the climate.
  • Rain Shadows rain occurs on windward sides of
    mountains dryness on leeward side creating
    deserts.
  • Cities paved areas heat up affecting climate
    and air pollution traps heat causing cities to be
    about 5oC warmer than surrounding rural areas.

4
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5
Section 2 Climate Types
  • Climatologists-people who study climates
  • 1918-Wladamir Koppen designed a system for
    classifying climates based on the types of plants
    found in a region. He did this by using the
    temperature and precipitation of regions that had
    different plant types.
  • Climates are classified into 6 groups
  • Tropical, mild, dry, polar, high elevation, and
    continental
  • Further separated into types

6
Adaptations
  • Any behavior or structure that helps an organism
    survive in its environment
  • Inherited
  • Once adapted to a particular environment,
    organisms may not be able to survive in other
    climates.
  • Structural adaptations include fur, thick stems
    on plants, spiny leaves
  • Behavioral adaptations include hibernation,
    clustering together, hiding under
  • rocks, estivation, sweating, shivering

7
Section 3 Climatic Changes
  • Because Earth is tilted, different areas of Earth
    receive changing amounts of solar radiation
    throughout the year-SEASONS.
  • Tropics-not much seasonal temperature change
    because of latitude. Days are about the same
    length all year.
  • Temperate zones -warm summers and cool winters
  • High latitudes -during summer at North Pole, sun
    does not set for nearly 6 months sun never rises
    at the South Pole during that same time

8
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9
El Nino
  • El Nino is a climatic event that involves the
    tropical Pacific Ocean and the atmosphere.
  • During normal years, strong trade winds that blow
    east to west along the equator push warm surface
    water toward the western Pacific Ocean.
  • During El Nino years, these winds weaken and
    sometimes reverse. This allows tropical water to
    flow back eastward to South America. Ocean
    temperatures increase from about 1oC to about 7oC
    off the coast of Peru.
  • El Nino can affect weather patterns by altering
    jet streams. It can cause drought in Australia
    and Africa, storms in California, and monsoon
    rains in Indonesia.

10
La Nina
  • During La Nina, the winds blowing across the
    Pacific are stronger than normal causing warm
    water to accumulate in the western Pacific.
    Water in the eastern Pacific is cooler than
    normal.
  • Can cause droughts in the southern U.S.
  • Can cause excess rainfall in the northwestern U.S.

11
Climatic Change
  • Ice ages seem to last 60,000 to 100,000 years.
  • Interglacial periods are shorter, about 10,000 to
    15,000 years. We are now in an interglacial
    period that began about 11,500 years ago.
  • Ice cores drilled in Greenland show that during
    the last ice age, colder times lasting 1,000 to
    2,000 years changed quickly to warmer spells
    lasting about the same length of time.

12
Causes of Climatic Change
  • Meteorite collisions
  • Large volcanic eruptions
  • Short and long-term changes in solar output
  • Changes in Earths movement in space
  • Movement of Earths crustal plates

13
What causes changes in climate?
  • Atmospheric solids and liquids
  • Humans add from automobile and smokestack
    emissions
  • Fires
  • Volcanic eruptions
  • Meteorite collisions
  • Wind erosion
  • Energy from the sun
  • Earths tilt on its axis changes and wobbles, and
    orbit shape changes
  • Crustal plate movement -movement of oceans and
    plates affect the transfer of heat

14
Changes in Climate Today
  • Greenhouse effect a natural heating that occurs
    when certain gases in Earths atmosphere trap
    heat.
  • Water vapor, carbon dioxide, methane
  • too littlegtEarth would be too cold to live
    Mars
  • -too muchgtEarth would be too warm to live Venus

15
Global Warming
Average global temperature of Earth is rising.
  • During past 100 years, surface temperature on
    Earth has increased 0.6oC.
  • Atmospheric CO2 has increased by 20.
  • Glaciers can melt causing a rise in sea level.
  • Warming can affect organisms survival. (coral)

16
Human Activities
  • Humans affect the air in Earths atmosphere.
  • Burning fossil fuels-natural gas, oil, coal form
    CO2 in air
  • Deforestation destroying and cutting down trees
    for mining, roads, buildings, and grazing cattle
  • Tropical forests are decreasing at a rate of 1
    per year for the past 2 decades.

17
Carbon Cycle
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