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Climate good one

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Climate   good one Climate good one Presentation Transcript

  • Climate
    • A climate is the pattern of weather that occurs in an area over many years.
  • 1. Determines the types of plants or animals that can survive and influences how people live.
  • 2. Elements that are averaged to determine climate: temperature, precipitation, air pressure, humidity, and days of sunshine.
  • Factors that affect climate
    • 1. Latitude – distance north or south of the equator.
  • Tropics
    • Regions between latitudes 23 N and 23 S
    • Sun shines almost directly overhead, keeping temperatures high
  • Polar Zones
    • extend from 66 N and 66 S to the poles – sun shines at a low angle, keeping temperatures low
  • Temperate Zones
    • between the tropics and the polar zones – moderate temperatures
  • Why are isotherms not parallel with latitude?
  • Large bodies of water affect the climate of coastal areas by absorbing or giving off heat
  • Ocean currents can bring cool or warm temperatures and moisture to coastal areas
  • Mountains affect their own climate as well as the climates of nearby areas
  • At the same latitude, the climate of on a mountain is colder than the climate at sea level
    • Mountains cause air to rise, cool, and condense, creating a wetter climate on the windward side of the mountain and a much drier climate on the leeward side.
  •  
    • Because of their large areas of solar radiation – absorbing asphalt and concrete, cities frequently have higher temperatures than surrounding areas.
  • Section II – Climate Types
  • Adaptation
    • any structure or behavior that helps an organism survive in its environment
  • Structural adaptations are body structures that help organisms survive in certain climates.
    • a – the fur of mammals insulates them from cold temperatures
    • b – a cactus’s thick, fleshy stem helps it hold water
  • Behavioral adaptations
    • a – hibernation – a period of greatly reduced activity during cold months
    • b – estivation – similar to hibernation, an inactive state that occurs during periods of intense heat
  • Section III - Climate Changes
  • Seasons
    • short periods of climatic change caused by changes in the amount of solar radiation an area receives
    • 1. As Earth revolves around the Sun, different areas of Earth are tilted toward the sun.
  •  
    • 2. The tropics do not experience much seasonal temperature change.
    • 3. High latitudes near the poles experience great seasonal temperature change.
  • El Nino – an occasional climatic event in which strong Pacific winds weaken and sometimes reverse.
  • Effects of El Nino
    • a – Ocean temperatures near Peru heat up
    • b – The position and strength of one of the jet streams may be altered, changing wind and precipitation patterns around the world.
    • c - Africa and Australia may experience drought.
  • La Nina – The winds blowing across the pacific are stronger than normal
  • At times in the past, Earth’s climate was much warmer or colder than now.
  • Causes of climatic change can operate over short or very long periods of time
    • 1. Solar radiation is blocked by larger numbers of solid and liquid particles entering the atmosphere
  • a. Catastrophic events such as volcanic eruptions and meteorite collisions can cause climatic change
  •  
    • Pollution can also cause climatic change
    • 4. The movement of Earth’s crustal plates affects the transfer of heat on Earth.
  • Climatic Changes Today
    • Greenhouse Effect – a natural heating process that occurs when certain gasses such as carbon dioxide, methane, and water vapor in earth’s atmosphere trap heat.
    • Global Warming – Earth’s average global surface temperature is rising, possibly due to the increase in greenhouse gasses in our atmosphere.
  • Human activities affect the air on Earth’s surface
    • a. burning fossil fuels increases the amount of carbon dioxide in the atmosphere.
    • Deforestation results in fewer trees to absorb carbon dioxide from the atmosphere.
  • Individuals CAN help reduce the amount of carbon dioxide in the atmosphere.
  •