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Unit 4: Energy Flow in Global Systems

Unit 4: Energy Flow in Global Systems. Chapters:. Chapter 10: Solar Energy and Climates Chapter 11: Climates and Biomes Chapter 12: Climate Change and Humans. Ch 1: Solar Energy and Climates. The Biosphere. Defining Systems:. Three classes of systems are defined by the following:

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Unit 4: Energy Flow in Global Systems

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  1. Unit 4: Energy Flow in Global Systems

  2. Chapters: Chapter 10: Solar Energy and Climates Chapter 11: Climates and Biomes Chapter 12: Climate Change and Humans

  3. Ch 1: Solar Energy and Climates The Biosphere

  4. Defining Systems: • Three classes of systems are defined by the following: • 1. Open system • 2. Closed system • 3. Isolated system

  5. Open System: • Allows energy and matter to cross the systems boundary • Examples:

  6. Closed System • Allows only energy but NOT matter to cross the boundary • Examples:

  7. Isolated System • Allows NEITHER energy nor matter to cross the boundary • Examples:

  8. The Biosphere

  9. Layers of the Biosphere • There are 3 layers that make up the biosphere: • 1. Lithosphere • 2. Hydrosphere • 3. Atmosphere

  10. Lithosphere • The Earth’s crust that forms land above sea level, at the ocean bottom, as well as the Earth’s mantel

  11. Hydrosphere • Water on or near the Earth’s surface • Includes, oceans, rivers, lakes as well as water in the atmosphere (clouds) • Cryosphere: water that is frozen in icecaps and permafrost

  12. Atmosphere • A mixture of nitrogen, oxygen and other gases that extends 800km above the Earth’s surface

  13. Atmospheric Layers

  14. 1. Troposphere • Layer of gases from 0 km to 10 km from the surface • Temp decreases as altitude increases (from 170C to -600C) • Contains 80% of the atmosphere’s gases • Location weather occurs

  15. 2. Stratosphere • Above the troposphere from 10 km to 50 km above the surface • Temperature increases to 0 degrees • Planes fly in this layer due to its stability • Contains no life forms • Contains the ozone layer

  16. 3. Mesosphere • Above the stratosphere • Reaches 85 km above the Earth • Temperature decreases to -1000C degrees

  17. 4. Thermosphere • Farthest layer from the Earth’s surface • Location of Northern Lights & space shuttle orbit • Temperature increases to 15000C degrees! • Very little gas in this layer

  18. Atmospheric Layers

  19. Earths Radiation Budget • What is Radiation? • The mechanism of energy transfer in which in which atoms or molecules emit electromagnetic waves

  20. Earth’s Radiation Budget • The earth maintains an energy balance of these waves known as its radiation budget

  21. Welcome to the Family Feud!! We surveyed 100 scientists and the top 4 answers are on the board: What is the most common obstruction that effects solar radiation coming into or leaving the earth?

  22. Survey says: • Ozone layer • Clouds 3. Albedo (surface reflection) 4. Dust

  23. Climate Vs. Weather • Climate - long-term trend in atmospheric pressure, humidity, temperature and precipitation • Weather - the above conditions at one time in one place

  24. What do you know? With a partner answer the following: 1. What determines the lengths of days and nights at different latitudes? 2. Why are days of daylight and darkness not equal? 3. Why do the seasons have unequal # of days? 4. What is significance about March 21th and September 23rd? 5. Explain why the warming of the earth is unequal?

  25. What determines the lengths of days and nights at different latitudes?

  26. Why are days of daylight and darkness not equal?

  27. Why do the seasons have unequal # of days?

  28. What is significance about March 21st and September 23rd?

  29. Explain why the warming of the earth is unequal?

  30. http://www.youtube.com/watch?v=DuiQvPLWziQ

  31. The Earths Tilted Axis • Angle of Inclination: the angle of the equator with respect of the the plane of the earths surface around the sun

  32. Earth’s Rotation Around the Sun

  33. Seasons and Sunlight

  34. Uneven Distribution of Radiation

  35. Uneven Distribution of Radiation

  36. All of these factors lead to 3 major climate zones Polar Temperate Tropical

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