1 / 35

That Climate Thing

That Climate Thing. 2. Ocean Currents. Ocean waters are constantly on the move. How they move influences climate and living conditions for plants and animals, even on land.

yaphet
Download Presentation

That Climate Thing

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. That Climate Thing 2. Ocean Currents

  2. Ocean waters are constantly on the move. How they move influences climate and living conditions for plants and animals, even on land. Currents flow in complex patterns affected by wind, the water's salinity and heat content, bottom topography, and the earth's rotation.

  3. Types of Ocean Currents • Surface currents • Anti-cyclonic current gyres are driven by the westward flow of equatorial surface wind. • Gravity driven roll-back from the resulting rise of western sea surface runs equatorial counter current. • Circum-Antarctic circulation, or “West Wind Drift” is driven by Earth’s rotation. • Deep-water current • This is thermohaline circulation or the “Global Conveyor Belt”.

  4. The North Atlantic Gyre System

  5. The factors that govern the oceanic gyres Gulf stream Canary Current N. Equatorial Current

  6. Atlantic Ocean meridional section at 25°W (a) Potential Temperatures (°C) http://sam.ucsd.edu/sio210/lect_6/

  7. Atlantic Ocean meridional section at 25°W (b) Salinity (‰)

  8. Atlantic Ocean meridional section at 25°W (c) Density at 0 dbar (s0F)

  9. Atlantic Ocean meridional section at 25°W (d) Density at 4 dbar (s4F)

  10. Atlantic Ocean meridional section at 25°W (e) Dissolved Oxygen (DO2 in ml/l)

  11. South Atlantic meridional section at 25°W (e) Silicate content (umol/Kg)

  12. Surface currents in the Paficific

  13. Nike shoes and the Pacific gyre The North Pacific gyre has been dropping off shoes around the Pacific since 1990. The shoes washed ashore one at a time but were wearable after a scrub-down to remove barnacles, algae, and tar.Beachcombers held swap meets to find matched pairs 1. shoe spill, May 27, 1990 2. 250 recovered, March 26, 1991 3. 200 recovered, May 18, 1991 4. 100 recovered, January-February 1991 5. 200 recovered, November-December 1990 6. 200 recovered, February-March 1991 7. 150 recovered, April 4, 1991 8. 200 recovered, May 9-10, 1991 9. several recovered, January-March 1993

  14. Pacific ocean meridional section at 150°W (a) Potential Temperatures (°C)

  15. Pacific Ocean meridional section at 150°W (b) Salinity (‰)

  16. Pacific Ocean meridional section at 150°W (c) Density at 0 dbar (s0F)

  17. Pacific Ocean meridional section at 150°W (c) Density at 4 dbar (s4F)

  18. Surface currents in the Indian Ocean

  19. Circum-Antarctic Circulation

  20. Pacific at normal times

  21. During the El Niño Times

  22. The normal or La Niña conditions Low air pressure High air pressure Equatorial counter current Equatorial surface wind Warm surface waters East Cold deep waters West

  23. Animation of Monthly-averaged Sea Surface Temperatures http://www.nodc.noaa.gov/dsdt/sst_ani.htm

  24. El Niño Continues to Grow: Pacific Ocean Shows Higher Than Normal Sea Surface Heights December 02, 2002 The latest image from NASA's Jason oceanography satellite, taken during a 10-day collection cycle ending December 2, 2002, shows the Pacific dominated by two significant areas of higher-than-normal sea level (warmer ocean temperatures). In the central equatorial Pacific, the large area of higher than normal sea surface heights (warmer than normal sea surface temperatures) associated with growing El Niño conditions has recently migrated eastward toward the coast of South America. Meanwhile, the influence of the 20- to 30-year larger than El Niño/La Niña pattern called the Pacific Decadal Oscillation continues to create warm, higher-than-normal sea-surface heights in the north Pacific that are connected in a warm horseshoe pattern with the western and southern Pacific.http://topex-www.jpl.nasa.gov/elnino/20021202.html

  25. Geostrophic Currents Upwelling and downwelling

  26. The Ekman Spiral

  27. The Ekman Spiral

  28. Mapping the Gulf Stream

  29. The Gulf Stream wobbles, much like the streams on land, so creating rings and eddies.

  30. The Oceanic Conveyor Belt

More Related