1. News http://news.yahoo.com/s/ap/20071025/ap_ on_re_us/toxic_dump_fearshttp://news.yahoo.com/s/ap/20071025/ap_ on_re_us/toxic_dump_fears http://news.yahoo.com/s/afp/environmentcl imateunhttp://news.yahoo.com/s/afp/environmentcl imateun http://news.yahoo.com/s/ap/20071025/ap_ on_sc/coast_guard_arctic

2. Fire Whirl or Fire Tornado Image courtesy of United States Marine Corps

3. Faster CO2 increases Carbon Dioxide in Atmosphere Increasing By THE ASSOCIATED PRESS Filed at 10:16 p.m. ET October 22, 2007 NYTimes WASHINGTON (AP) -- Just days after the Nobel prize was awarded for global warming work, an alarming new study finds that carbon dioxide in the atmosphere is increasing faster than expected.Nobel prizeglobal warming Carbon dioxide emissions were 35 percent higher in 2006 than in 1990, a much faster growth rate than anticipated, researchers led by Josep G. Canadell, of Australia's Commonwealth Scientific and Industrial Research Organization, report in Tuesday's edition of Proceedings of the National Academy of Sciences. Proceedings of the National Academy of Sciences

4. Weather Hot Air Rises Coriolis Force bends moving things to the right in the northern hemisphere Cold air holds less water Air moves from areas of high pressure to areas of low pressure

5. Hot Air Rises Air can hold less water at higher altitudes 1. Hot air rises over land due to heating by the sun. 2. The rising air leaves less air in one spot, low pressure forms. 3. Generally, from 3,000 to 5,000 feet, the air cools, high pressure develops. 4. Meanwhile, over the cooler water, air sinks, leaving less air aloft. 5. More air piles up at the surface of the water, high pressure forms. 6. Air moves from high pressure to low pressure. 7. The sea breeze generally forms during the afternoon. This creates a mini cold front that helps lift air upward to create thunderstorms.

6. Hadley Cells Image courtesy of NASA

7. Global Rainfall Image courtesy of atmoz.orgatmoz.org

8. Global Productivity Image courtesy of NASA

9. Coriolis Force Result of earth spinning In Northern Hemisphere, Coriolis Force deflects moving objects to the RIGHT Force is proportional to velocity Force is a function of latitude (zero at equator)

10. Winds Trade Winds Westerlies Image courtesy of NOAA

11. Surface Currents Image courtesy of United States Federal Government

12. Global Conveyor Belt

13. Upwelling Image courtesy of NOAA

14. El Nino Normal patternEl Nino Conditions Image courtesy of United States Federal Government

15. El Nino Conditions

16. Weather Hot Air Rises Coriolis Force bends moving things to the right in the northern hemisphere Cold air holds less water Air moves from areas of high pressure to areas of low pressure Land warms and cools faster than the ocean

17. What d you notice?

18. What do you notice?

19. Fronts Cold front Warm front

20. Tornadoes Image courtesy of NOAA

21. Santa Ana Winds Warm Form –Santa Ana Winds from east, high pressure in Great Basin, low pressure over Pacific Descending cold, dry winds from Rockies/Sierra Nevadas Warms adiabatically in Fall and Winter –10C per 1000 m descent (29C per mile) –http://www.atmos.ucla.edu/~fo vell/ASother/mm5/SantaAna/S A03_rhu_nowind.GIF –Fohn Alps  Germany Crazy times Image courtesy of NASA

22. Monsoons Indian Ocean Land cools faster than ocean in winter Land warms faster than ocean in summer Image courtesy of Saravask, WikipediaSaravask

23. SeaBreezes Image courtesy of Jesús Gómez Fernández, WikipediaJesús Gómez Fernández Image courtesy of Vaughan Weather, WikipediaVaughan Weather Image courtesy of Federal Aviation Administration, Wikipedia

24. Rain Shadow Orographic Winds Adiabatic cooling with altitude Latent heat released with rain Image courtesy of WikipediaWikipedia

25. Hurricanes Hurricane Katrina Image courtesy of NASA

26. Geostrophic Balance Coriolis Force Pressure Gradient Force Strong cyclonic winds circulate counterclockwise in the Northern hemisphere around a low pressure zone LO Image courtesy of WikipediaWikipedia Image courtesy of NASA

27. Spiral Winds Friction slows wind CF reduced

28. Convection Hot, moist air rises Colder,dry air descends More buoyancy differences make “deeper” convection- thunderstorms RainBands Image courtesy of NASA Images removed due to copyright restrictions. Image courtesy of NASA

29. Conservation of Mass Air spiraling in Conservation of angular momentum –Smaller radius, higher wind velocities Air must be exhausted (vented) Anticyclone at high altitude Images removed due to copyright restrictions.

30. Hurricane Formation Inter-Tropical Convergence Drifts off equator  Tropical depression Images removed due to copyright restrictions.

31. Surface Cooling Extract latent heat of evaporation leaves cool tracks Image courtesy of NASA

32. Image courtesy of NOAA

33. Nor’Easters Heat from warm ocean Cold from land Jet Stream disturbance Image courtesy of NASA Images removed due to copyright restrictions.