1. Chapter 2: Warming the Earth and the Atmosphere Temperature and heat transfer Temperature and heat transfer Balancing act - absorption, emission and equilibrium Balancing act - absorption, emission and equilibrium Incoming solar energy Incoming solar energy

2. Temperature and Heat Transfer

3. Temperature Scales kinetic energy, temperature and heat kinetic energy, temperature and heat Kelvin scale Kelvin scale Celsius scale Celsius scale Fahrenheit scale Fahrenheit scale temperature conversions temperature conversions Every temperature scale has two physically-meaningful characteristics: a zero point and a degree interval.Every temperature scale has two physically-meaningful characteristics: a zero point and a degree interval.

4. Fig. 2-2, p. 27

5. Latent Heat - The Hidden Warmth phase changes and energy exchanges phase changes and energy exchanges sensible heat sensible heat Latent heat explains why your skin feels cold when you step out of a warm shower, and why perspiration is an effective way to cool your body.Latent heat explains why your skin feels cold when you step out of a warm shower, and why perspiration is an effective way to cool your body.

6. Fig. 2-3, p. 28 Stepped Art

7. Conduction conduction and heat transfer conduction and heat transfer good conductors and poor conductors good conductors and poor conductors Why are feathers (down) used in winter parkas?Why are feathers (down) used in winter parkas?

8. Convection convection and heat transfer convection and heat transfer thermals thermals Soaring birds, like hawks and falcons, are highly skilled at finding thermals.Soaring birds, like hawks and falcons, are highly skilled at finding thermals.

9. Radiation radiation and energy transfer radiation and energy transfer electromagnetic waves electromagnetic waves Wein’s law of Black Body Wavelength  = Constant/Temp =.0029 mK / T K Wein’s law of Black Body Wavelength  = Constant/Temp =.0029 mK / T K Stefan-Boltzmann law E=  T**4 Stefan-Boltzmann law E=  T**4 Wave law = c/frequency: =c/ Wave law = c/frequency: =c/ C is the speed of light for electromagnetic radiation C is the speed of light for electromagnetic radiation Cole’s law: shredded cabbage and vinegarCole’s law: shredded cabbage and vinegar

10. Fig. 2-7, p. 32

11. Radiation electromagnetic spectrum electromagnetic spectrum ultraviolet radiation ultraviolet radiation visible radiation visible radiation infrared radiation infrared radiation Moderate amounts of ultraviolet radiation gives you a healthy-looking tan; excessive amounts give you skin cancer.Moderate amounts of ultraviolet radiation gives you a healthy-looking tan; excessive amounts give you skin cancer.

12. Fig. 2-8, p. 34

13. Fig. 2-9, p. 34

14. Balancing Act - Absorption, Emission, and Equilibrium

15. Selective Absorbers and the Atmospheric Greenhouse Effect blackbody radiation blackbody radiation selective absorbers selective absorbers atmospheric greenhouse effect atmospheric greenhouse effect The best greenhouse gas is water vapor.The best greenhouse gas is water vapor.

16. Enhancement of the Greenhouse Effect global warming global warming positive and negative feedbacks positive and negative feedbacks Positive feedback: increasing temperatures lead to melting of Arctic sea ice, which decreases the albedo.Positive feedback: increasing temperatures lead to melting of Arctic sea ice, which decreases the albedo.

17. Warming the Air from Below radiation radiation conduction conduction convection convection Fog “burns off” from the bottom up.Fog “burns off” from the bottom up.

18. Incoming Solar Energy

19. Scattered and Reflected Light scattering scattering reflection reflection albedo albedo Scattering is responsible for sky color.Scattering is responsible for sky color.

20. The Earth’s Annual Energy Balance What happens to the solar energy that reaches the top of the earth’s atmosphere? What happens to the solar energy that reaches the top of the earth’s atmosphere? What happens to the solar energy that is absorbed by the earth’s surface and by the atmosphere? What happens to the solar energy that is absorbed by the earth’s surface and by the atmosphere?

21. Fig. 2-15, p. 41

22. Fig. 2-16, p. 42

23. FIGURE 2.16 The earth-atmosphere energy balance. Numbers represent approximations based on surface observations and satellite data. While the actual value of each process may vary by several percent, it is the relative size of the numbers that is important. Stepped Art Fig. 2-16, p. 42

24. Why the Earth has Seasons earth-sun distance earth-sun distance tilt of the earth’s axis tilt of the earth’s axis Earth-sun distance has little effect on atmospheric temperature.Earth-sun distance has little effect on atmospheric temperature.

25. Seasons in the Northern Hemisphere Insolation : TOD, TOY, WOE Insolation : TOD, TOY, WOE summer solstice, Winter solstice summer solstice, Winter solstice spring and autumn equinox: Equal What? spring and autumn equinox: Equal What?

26. Seasons in the Southern Hemisphere tilt tilt solstice solstice equinox equinox

27. Local Seasonal Variations slope of hillsides slope of hillsides vegetation differences vegetation differences Homes can exploit seasonal variations: large windows should face south.Homes can exploit seasonal variations: large windows should face south.