1. EXPLAIN 2. Earth’s Energy Balance

2. Energy Balance Let the rate of energy flow from the Sun to the Earth be called F in Let the rate of energy flow from the Earth to outer space be called F out Energy In = Energy Out

3. Energy Balance Assume both Sun and Earth are blackbodies, so F =  T 4 F in = absorbed sunlight x daylight area F out =  T earth 4 x total area F in = F out

4. Energy Balance F in = F out F in = Solar brightness x (1 – albedo) x (area of Earth’s shadow) F out =  (T earth ) 4 x (area of Earth’s surface)

5. 30% reflected by clouds, air, dust, and surface 30% reflected by clouds, air, dust, and surface 19% absorbed by the atmosphere (mostly clouds) 19% absorbed by the atmosphere (mostly clouds) 51% absorbed at the surface 51% absorbed at the surface Solar Radiation

6. Energy Balance F in = F out F in = Solar brightness x (1 –  ) x  r 2 F out =  (T e ) 4 x 4  r 2

7. Energy Balance F in = F out

8. Energy Balance F in = F out But the observed surface temperature is about 288 K

9. Both are almost perfect blackbodies! The hot sun radiates at shorter (visible) wavelengths that carry more energy Energy absorbed by the cooler earth is then re- radiated at longer (thermal infrared) wavelengths Earth & Sun Emission SUN EARTH 255 K

10. Bare Rock Model If sunlight were the only source of energy, the surface of the Earth would be way too cold for life! 255 °K = -18 °C = -1 °F Surface Sunlight F surface F in = F out

11. Two-Layer Model Now imagine a layer of glass above the solid rock Glass is transparent to sunlight Glass is opaque to “Earthlight” (thermal IR) Glass Surface Sunlight F glass F surface

12. Seen from Above Both models: Absorb the same sunshine Reflect the same amount of sunlight back out Emit the same amount of Earthlight Glass Surface Sunlight F glass F surface Sunlight F surface boundary

13. Summary Layer models are not meant to be accurate or predictive, just to help us understand how the world works Energy balance of “bare rock” model is way too cold to support life! Adding a layer of glass makes the surface nice and toasty Where did the heat come from?

14. Bathtub Analogy If faucet runs faster than drain, level rises And vice versa Drain runs faster when water is deep Adding glass to layer model acts like a clog in the drain Water rises until drainage = inflow again Faucet ~ Sun Drain ~ Thermal emission Water level ~ temperature

15. Greenhouse Gases

16. Gases Gases are made of moving molecules separated by empty space Kinetic energy of molecular motion is proportional to temperature Gases don’t behave as blackbodies or even graybodies! Let’s take a look! 99% of Earth’s atmosphere is N 2 & O 2

17. Waves and Photons Experiments show both kinds of behavior: –Oscillating fields with troughs and crests (waves) –Individual packets of energy (particles) Long Waves = small photons Long Waves = small photons Short Waves = BIG PHOTONS Electromagnetic radiation behaves as both waves and particles!

18. Energy is “Quantized” When radiation interacts with atoms and molecules, only certain “jumps” in energy are possible Electrons orbit at specific energy levels above an atomic nucleus Absorption of a photon of just the right energy can make them “jump up” to the next level Emission of a photon occurs when an electron “falls” down to a level below

19. UV & Visible Light Big jumps take lots of energy, small jumps take less Big drops emit energetic photons (short wavelengths) Small drops emit less energetic photons (longer wavelengths) Most electron transitions in gases absorb/emit visible or UV light

20. Molecules and IR light Molecules are groups of atoms that share electrons (chemical bonds) Molecular transitions involve changes in vibration, rotation, bending, and stretching of chemical bonds Photons can interact with molecules to change states Transitions involve specific amounts of energy, so only certain wavelengths are active Molecular transitions typically absorb & emit in thermal infrared

21. Dancing Molecules and Heat Rays! Nearly all of the air is made of oxygen (O 2 ) and nitrogen (N 2 ) in which two atoms of the same element share electrons Infrared (heat) energy radiated up from the surface can be absorbed by these molecules, but not very well N N O O Diatomic molecules can vibrate back and forth like balls on a spring, but the ends are identical No electric dipole!

22. Dancing Molecules and Heat Rays! Carbon dioxide (CO 2 ) and water vapor (H 2 O) are different! They have many more ways to vibrate and rotate, so they are very good at absorbing and emitting infrared (heat) radiation Molecules that have many ways to wiggle are called “Greenhouse” molecules OOC H H O

23. Atmospheric Absorption Visible radiation passes almost freely through Earth's atmosphere Visible radiation passes almost freely through Earth's atmosphere Earth's emitted thermal energy either fits through a narrow “window” or is absorbed by greenhouse gases and reradiated Earth's emitted thermal energy either fits through a narrow “window” or is absorbed by greenhouse gases and reradiated Complete absorption from 5-8  m (H 2 O) and > 14  m (CO 2 ) Little absorption between about 8 m and 11  m (“window”)

24. Earth-Atmosphere Energy Balance Earth's surface absorbs the 51 units of shortwave and 96 more of longwave energy units from atmospheric gases and clouds. These 147 units gained by earth are due to shortwave and longwave greenhouse gas absorption and emittance. Earth's surface loses these 147 units through convection, evaporation, and radiation. Earth's surface loses these 147 units through convection, evaporation, and radiation.

25. 9 PM surface temperature = 25 °C = 77 °F Summer Night in Colorado 6 AM surface temperature = -50 °C = -58 °F radiation emitted by soil 390 W m -2 4 inches = 10 cm

26. 6 AM surface temperature = 15 °C = 50 °F Summer Night in Colorado radiation emitted by soil 390 W m -2 4 inches = 10 cm radiation emitted by air 340 W m -2

27. The strongest evidence for the Greenhouse Effect is that we can survive night!

28. Common Sense Doubling CO 2 would add 4 watts to every square meter of the surface of the Earth, 24/7 Doing that would make the surface warmer This was known before light bulbs were invented! 4 Watts 1 m John Tyndall, January 1863

29. Common Myth #1 “Scientists are worried about climate change because it’s been warming up recently” WRONG! We’re worried because we know that when we add heat to things, they warm up

30. Cause and Effect Climate is a result of physical, chemical, & biological processes Forcing causes a response Strength of response to unit forcing is called “sensitivity”