1. Earths Climate System Dr. R. M. MacKay

4. Natural and Anthropogenic Climate Forcing

11. Carbon Dioxide in Prehistoric times

13. Plate tectonics can remove CO2 from the atmosphere

15. Milankovitch Theory of Ice Age Cycles Past 1,000,000 years Changes in Earths orbit about the sun results in changes in High latitude NH summer sunlight. When summer sunlight is low ice sheets can slowly grow from year to year. Orbital factors include: Changes in Earth axial tilt (now 23.5 degrees) Changes in the eccentricity of Earths orbit. And the precession of perihelion.

16. Earths Axial Tilt No Tilt no seasons Extreme tilt extreme seasons

17. Orbital Eccentricity

18. What does Precession of perihelion mean? Today we are actually closer to the sun during winter and farthest during summer. Earth is at its perihelion position (position of closest approach) on January 4. This make for cooler summers and warmer winters. These conditions would promote glacial growth from year to year.

21. ~20,000 Years ago

22. 18,000 years

25. Climate of the last 1000 yr

29. http://www.nasa.gov/centers/goddard/news/topstory/2003/0313irradiance.html

31. Greenhouse Gases

35. http://data.giss.nasa.gov/gistemp/graphs/

36. Climate of the last 1000 yr

38. 1000 years

39. Volcanoes

40. Volcanic aerosol loading

41. Pinatubo

42. Aerosol lifetime

43. Last 50 years

44. Troposphere and Stratospheric Response

45. Tropospheric Sulfate Aerosols

46. Cooling to offset warming

47. Estimated Sulfur Emissions

48. Ozone and Climate Change

49. Increased greenhouse gases result in warmer surface temperatures and Cooler cooler stratospheric temperature. This results in increased abundances of Polar stratospheric clouds which enhance Ozone destruction. Thus despite the phase out of CFC production the healing of the ozone hole will likely be delayed by increases in CO2.

50. Ozone and Climate Change Less ozone in the stratosphere can cause a decrease in the global greenhouse effect. This likely offset global warming from 1980 to 2000 masking the true effect of increased atmospheric CO2.

55. Greenland Ice Sheets

56. Latest satellite data on Greenland mass change I've just updated the Greenland is losing ice page as a new paper analysing satellite data on Greenland mass change has been released (Wouters 2008). The Gravity Recovery and Climate Experiment (GRACE) measures changes in the Earth's gravity field and found that from February 2003 to January 2008, Greenland lost mass at a rate of 179 Gigatonnes per year. This is equivalent to a global sea level rise of 0.5mm per year. The rate is also increasing over time, suggesting an acceleration of mass loss.Greenland is losing ice pageWouters 2008 Gravity Recovery and Climate Experiment

57. Artic Sea Ice

63. Climate Models

64. 1-D Radiative convective models

65. 2-D Models

66. 3-D Atmosphere Ocean General Circulation Model