1. Earth’s Atmosphere

3. Nebraska Supercell

4. Storm Cloud - Oklahoma

5. Mt Rainier, Washington

6. Interesting Facts… The average temp on Earth is 63  F (17  C) Ice Age global temp is 54  F (12  C) Due to the Earth’s rotation, our planet bulges out at the equator Without plate tectonics, we would overheat – Subduction recycles carbon

7. Why is our atmosphere important? Importance – Makes life on Earth possible – Protective barrier around Earth – Maintains balance between absorbed and heat lost – Protects life from UV rays – If we didn’t have one… – We would be burned by the intense heat during the day and frozen by the low temps at night I

8. What is our atmosphere made of? Consists of FIVE layers from the surface to space Held in place by the Earth’s gravity As you move upward through the layers, atmosphere pressure and density DECREASES – Gases – Nitrogen = 78% – Oxygen = 21% – Trace gases = 1% (Argon, Carbon dioxide, ozone) II

9. What is our atmosphere made of? Solids – Dust – picked up off of the ground – Salt – picked up from ocean spray – Pollen - produced by plants Liquids – Water vapor = up to 4% – Sulfuric acid from volcanoes and air pollution II

10. What are the 5 layers of our atmosphere? Lower atmosphere – Troposphere Layer closest to Earth Approx 11 km high Weather occurs here Temperature decreases with altitude Contains 99% of the water vapor and 75% of the atmospheric gasses III

11. Hurricane Ivan 2004

12. What are the 5 layers of our atmosphere? Lower atmosphere – Stratosphere Extends 10km to 50km Airplanes fly here Ozone layer Temperature increases with altitude III

13. What are the 5 layers of our atmosphere? Upper atmosphere – Mesosphere Extends from 50km to 85km VERY thin and cold Temperature decreases with altitude Meteorites or shooting stars occur here III

14. What are the 5 layers of our atmosphere? Upper atmosphere – Thermosphere Extends from 80km to 500km The thickest layer Named for its high temperature Temperature increases with altitude Space shuttles fly in this area Auroras or the Northern lights III

15. What are the 5 layers of our atmosphere? Upper atmosphere – Exosphere Above a height of 500km This is where the atmosphere merges into space Contains very few molecules Satellites are stationed in this area III

17. How is the Sun’s energy absorbed? 3 things happen to the energy – About 35% is reflected back into the atmosphere – About 15% of the energy is absorbed by the atmosphere – About 50% of the energy is absorbed by Earth’s surface IV

18. How is the Sun’s heat transferred through the atmosphere? Heat flows from higher temperature objects (roads, rocks, water) to objects with lower temperature (atmosphere) 3 ways heat is transferred – Radiation – Heat transfer through empty space – Sun’s energy  waves/rays V

19. How is the Sun’s heat transferred through the atmosphere? Radiation – Electromagnetic waves directly transport energy through space – Travels through empty space VI

20. How is the Sun’s heat transferred through the atmosphere? Conduction – Heat transfer between matter – Objects as molecules bump into each other – Air is NOT a good conductor of heat – Least significant is heating the Earth’s atmosphere VI IV. How is the Sun’s energy absorbed?

21. How is the Sun’s heat transferred through the atmosphere? Convection – Heat transfer by the movement of mass from one place to another – ONLY takes place in liquids and gases Warm air  because it is less dense (molecules are spread out) Cool air  because it is more dense (molecules are closer together) VI

22. Remember this?

23. What is the water cycle? A 3 part cycle describing the constant motion of the hydrosphere (all water on Earth Surface) between Earth and the atmosphere – Evaporation/Transpiration - Radiation from the sun changes liquid on Earth’s surface into a gas which enters Earth’s atmosphere – Condensation - Water vapor gas that has cooled and changes back into a liquid – Precipitation - A collection of tiny water droplets from condensation that collide creating larger droplet which fall to Earth VII