1.1: Earth's Sphere
- Earth System: All the matter, energy, and processes within Earth's boundary
- Consists of non-living & living things.
- Example: Living things - Trees, animals, and people
- Example: Non-living things - Rocks, air, and water
- 5 main parts
- Geosphere: Mostly solid, rocky part of Earth
- Extends from the center of Earth
- 3 different layers
- Crust
- 5 - 10 km thick (oceanic)
- 35 - 70 km thick (continental)
- Least dense
- Mantle
- 2,900 km thick
- More dense than crust
- Core
- 3,500 km thick
- Most dense
- Hydrosphere: The part of Earth that is liquid water
- Includes marshes, ponds, lakes, water droplets, and rain
- Cryosphere: The part made up of all the frozen water on Earth.
- Includes ice, sea ice, glaciers, ice shelves, and icebergs
- Atmosphere: Mostly made up of invisible gases that surround Earth.
- 500 - 600 km of the Earth's surface
- Parts
- 78% nitrogen
- 21% oxygen
- 1% other gases, including argon, carbon dioxide, and water vapor
- Biosphere: The part of Earth made up of living things and the areas of Earth where they are found
- Rocks, soil, ocean, lakes, rivers, and lower atmosphere support life.
- Most organisms need water, and oxygen or carbon dioxide to live
- How the spheres interact
- Exchanging Matter: Earth's spheres interact as matter moves between spheres
- Example: Atmosphere →Hydrosphere or Cryosphere → clouds
- Exchanging Energy: Earth's spheres also interact as energy moves between them.
- Example: Plants use solar → generates food
- Source of Earth's energy
- Almost all the Earth's energy comes from the sun.
- Energy budget: A way to keep track of energy transfers into and out of the Earth system.
- Unbalancing the budget
- Can cause increase or decrease global temperatures, increase greenhouse gases, which makes us lose polar ice caps.
- Statistics
- Energy coming in
- 26% Reflected by clouds & atmosphere
- 4% Reflected by surface
- 19% Absorbed by clouds and atmosphere
- 51% absorbed by Earth
- Outgoing Energy
- 64% radiated from atmosphere and clouds (19% came from absorption)
- 7% lost as heat rising through the air
- 23% evaporated from Earth to clouds
- 6% radiated from Earth to space