12 temperature, emr, insolation

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SUNY Ulster

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Physical Geography Class 12 Temperature, EMR, Insolation

Matter = “Stuff” All matter is made of atoms Atoms combine to form molecules Energy acts upon, and changes matter Matter and Energy

“Energy is neither created nor destroyed” It just changes form Kinetic Energy is a form of energy. Kinetic Energy = movement energy = temperature Kinetic Energy

Incoming Solar Radiation Constant at top of atmosphere (when averaged annually) ~1400 watts/m2 Insolation

$Refraction$

$Do all wavelengths of light refract at the same angle?$

What is causing the wavelengths to bend differently?

What methods of heat transfer are occurring here?

Latent Heat Sensible Heat Two Types of Heat

Effects of Land vs. Water On Temperature

Continentality vs. Marine Effect Water has a moderating effect on temperature!

Land heats quicker and cools quicker than Water!!!!

Portland, Oregon Leeward vs. Windwardside of continent

Carbon Dioxide Methane Water Vapor Greenhouse Gases

Depends upon % of cloud cover Cloud type Cloud height Thickness (water content + density) Impact of Clouds

Examine: Incoming shortwave radiation Vs. Outgoing longwave radiation To understand actual effects:

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12 temperature, emr, insolation

1. Physical Geography Class 12 Temperature, EMR, Insolation

2. Matter = “Stuff” All matter is made of atoms Atoms combine to form molecules Energy acts upon, and changes matter Matter and Energy

3. “Energy is neither created nor destroyed” It just changes form Kinetic Energy is a form of energy. Kinetic Energy = movement energy = temperature Kinetic Energy

4. Temperature Scales

5. Electromagnetic Spectrum

6. Electromagnetic Spectrum

7. Longer -------------Shorter

8. Infrared Radiation

10. Ultraviolet

11. Incoming Solar Radiation Constant at top of atmosphere (when averaged annually) ~1400 watts/m2 Insolation

12. Solar Constant

13. Fate of Insolation

14.

15.

16.

17. Refraction

18. Do all wavelengths of light refract at the same angle?

19.

20. What is causing the wavelengths to bend differently?

21. What’s happening here?

22.

23. Albedo

24. What happens to absorbed radiation?

25.

26. Radiation

27. Heat Transfer

28. What methods of heat transfer are occurring here?

29. Greenhouse Effect

30. Greenhouse Effect

31.

32.

33.

34.

35.

36.

37. Latent Heat Sensible Heat Two Types of Heat

38. Phase Changes in Water

39. CONTROLS ON TEMPERATURE

40. Latitude

41. Mt. Kilimanjaro

42. Urbanization

43. Cloud Cover

44. Effect of Clouds on Temperature

45. Death Valley

46.

47. Look at differences in temperature

48. Effects of Land vs. Water On Temperature

49. Continentality vs. Marine Effect Water has a moderating effect on temperature!

50. Inland vs. Coastal

51. Evaporation

52.

53. Land heats quicker and cools quicker than Water!!!!

54. Transparency

55. Specific Heat

56. Movement and Mixing

57. Currents/ Sea Surface Temperatures

58. Warm Ocean Current

59. France vs. Newfoundland, Canada

60. Portland, Oregon Leeward vs. Windwardside of continent

61. Landscapes

62. Glacier National ParkEast vs. West Side

63. USGS Particulates and Gases

64. Particulates

65. Carbon Dioxide Methane Water Vapor Greenhouse Gases

66. Phase Changes in Water

67. Layers of the Atmosphere

68.

69. Normal Lapse Rate

70.

71.

72. Photosynthesis

73. Depends upon % of cloud cover Cloud type Cloud height Thickness (water content + density) Impact of Clouds

74. Examine: Incoming shortwave radiation Vs. Outgoing longwave radiation To understand actual effects:

75. Cloud Height

76. What about Jet Contrails?

12 temperature, emr, insolation

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12 temperature, emr, insolation