1. Music today: Little Mermaid, “Under the Sea” WELCOME OSU MOMS!!

2. Deep Ocean Circulation Motion in the Ocean, Part 2, or Who wants to ride the Great Conveyor Belt?

3. Surface Circulation

4. How does the Deep Ocean respond to Surface Circulation? F The main gyres move heat and salt F Resulting DENSITY variations lead to vertical flow (sinking) F Formation of “water masses”, characterized by Temperature, Salinity

5. Density Variation in Sea Water

6. North Atlantic Circulation

7. Density-Driven Water Flow F Called “Thermohaline Circulation”, because temperature and salinity together determine density of seawater “Thermo” = temperature “haline” = salt

8. Where does the Ocean’s Deepest Water Come From? F The densest seawater is cold and salty F This is formed at high latitudes in the North and South Atlantic: North Atlantic Deep Water (NADW) Antarctic Bottom Water (AABW)

9. Density Rules!

10. Underwater “Waterfalls”

11. Water Masses and ocean mixing

12. Thermohaline Circulation

13. The Great Conveyor Belt

14. Semi-Enclosed Basins: Mediterranean Water

15. Mediterranean Water

17. Tracking Motion (direction & velocity) fixed mobile

18. Tracers in the Ocean F Track the motion (direction and velocity) F 14 C, cosmic rays in the upper atmos (half-life is 5700 years) 3 H, nuclear weapons testing (half-life is 12.5 years) CFCs, chlorinated fluoro-carbons

19. Consequences of Global Flow

20. F Ocean turnover is about 1500 years (time for a round trip on the conveyor belt) F Deep water (made in the polar Atlantic) contains abundant O 2 and CO 2 F The high O 2 content promotes oxidation of bottom sediments (e.g., CaCO 3 ) F The CO 2 content controls CCD (Carbonate Compensation Depth)

21. Carbonate Compensation Depth (CCD) Cold, acidic, salty Cold,

22. Carbon Cycle and Global Warming F The temperature of bottom water formation determines how much CO 2 is dissolved in deep ocean water F The rate of overturn of the oceans determines the “burial rate” of C from the atmosphere F Organic C accumulates in sediments, depending on the O 2 content of deep ocean

23. Carbon Cycle and Global Warming F Organic C in sediments is reduced to CH 4 (methane gas) F Methane gas migrates upward and can be trapped as frozen “gas hydrates” near the ocean floor

24. Gas Hydrates “Salem Sue” New Salem, ND

25. Gas Hydrates

26. Gas Hydrates: Ice w/fuel and fire inside Light w/match

27. Gas Hydrates

28. Hydrate Ridge Image courtesy of Ocean Observatories Initiative Regional Scale Nodes Program, UW

29. Hydrate Ridge Image courtesy of Ocean Observatories Initiative Regional Scale Nodes Program, UW Yaquina Bay, Newport

30. Hydrate Ridge Image courtesy of Ocean Observatories Initiative Regional Scale Nodes Program, UW

31. Climate Change Concerns F What happens when sea level falls? F What happens when deep water warms? F What about underwater landslides & earthquakes? F All of these liberate gas hydrates (CH 4 ), which combines with O 2 to form CO 2, ultimately reaching the atmosphere

32. Deep Ocean Circulation F The ocean has an enormous capacity to absorb and release greenhouse gases F So, the rate, temperature and composition of seawater circulating through the deep ocean is vitally important in assessing long term climate change