1 / 21

OCN 5401

OCN 5401. Chapter 8 Distribution of Temperature and Salinity Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453. Map of Hecataeus of Miletus ( ca . 550 BC – 476 BC) a student of Greek geographer Anaximander ( ca . 610 BC – 546 BC), a student of Thales of Miletus ( ca . 624 BC – 546 BC).

Download Presentation

OCN 5401

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. OCN 5401 Chapter 8 Distribution of Temperature and Salinity Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453

  2. Map of Hecataeus of Miletus (ca. 550 BC – 476 BC) a student of Greek geographer Anaximander (ca. 610 BC – 546 BC), a student of Thales of Miletus (ca. 624 BC – 546 BC).

  3. Why do these sea surface salinities vary? E-(P+R)

  4. COULD THE OCEAN DISSOLVE MORE SALT? SALINITIES IN GREAT SALT LAKE EXCEED 250 g/kg!!

  5. Sea surface temperatures (SST) in the world ocean during August. Why do these sea surface temperatures vary? H= m·CP·ΔT

  6. Double Diffusion and Salt Fingering simplified equation of state =0.2

  7. Water mass formation in the Southern Ocean

  8. Water Mass Formation Southern Ocean

  9. Water mass formation in the Arctic Ocean Fram Strait

  10. Connecting the two: Water Mass Formation in the Atlantic Ocean advection = diffusion

  11. Labrador Sea Water formation temporal variability Doesn’t seem to be ENSO related: 72-73, 82-83, 87-88, 97-98, 09-10.

  12. Atlantic Meridional Overturning Circulation • “The AMOC is defined as the total (basin-wide) circulation in the latitude depth plane, as typically quantified by a meridional transport streamfunction.” • THC is “currents driven by fluxes of heat and fresh water across the sea surface and subsequent interior mixing of heat and salt.” Rahmstorf (2002).

  13. Temperature-Salinity (T-S) Diagram

  14. Ocean basins, sills, and fracture zones

  15. Deep Western Boundary Current Inverted Echo Sounder

  16. World Ocean Circulation Experiment using human made chemicals as tracers

  17. Meddies RAFOS (range and fixing of sound)

  18. Oceanic Microstructure Fine Structure Profiler

  19. Langmuir Circulation Turbulence, convection, Stokes drift

  20. OCN 5401 Chapter 8 Questions?

More Related