1 / 22

Observations of Mesoscale * Ocean Circulation: Present and Future

Observations of Mesoscale * Ocean Circulation: Present and Future. Bo Qiu Dept of Oceanography University of Hawaii. Schematic of Satellite Altimetry. * mesoscale = 10s~100s km. A UH profiling float was being deployed from R/V Revelle in Kuroshio Extension, May ‘05.

ormand
Download Presentation

Observations of Mesoscale * Ocean Circulation: Present and Future

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. Observations of Mesoscale* Ocean Circulation: Present and Future Bo Qiu Dept of Oceanography University of Hawaii Schematic of Satellite Altimetry * mesoscale = 10s~100s km A UH profiling float was being deployed from R/V Revelle in Kuroshio Extension, May ‘05

  2. Altimeter-derived rms sea surface height variability (cm) Abundant mesoscale eddies Eddy “desert”

  3. Altimeter-derived rms sea surface height variability (cm) Schematic of NW Pacific Ocean Circulation

  4. Semi-monthly Kuroshio Extension paths (1.7m SSH contours) Stable yrs: 1993-94, 2002-04 Unstable yrs: 1996-2001, 2006-07

  5. (a) Upstream KE path length (141-153°E) (b) Eddy kinetic energy (141-153°E, 32-38°N) Stable yrs: 1993-94, 2002-04 Unstable yrs: 1996-2001, 2006-07

  6. Pacific Decadal Oscillations(Mantua et al. 1997) • Center of action of wind forcing is in the eastern half of the N Pacific basin • Positive (negative) phase of PDO generates – (+) local SSH through Ekman divergence (convergence)

  7. Yearly SSH anomaly field in the North Pacific Ocean + -

  8. 2004 stable Kuroshio Extension System Study Observing Array/Timeline 20 floats 28 floats UH-KESS profiling float measurements 2005 unstable 1500db 5 days

  9. Distributions of semi-monthly profiling float T/S data (contours: SSH from satellite altimeters)

  10. T(z) and PV(z) evolution in the KE recirculation gyre mixed layer depth subtropical mode water KESS period

  11. PV values on 25.4 σθ surface (~250m)

  12. What’s Next ? from mesoscale to submesoscale … SSH snapshot from the NLOM model for 04/10/2006 Right: from the original 1/32°-resolution output Left: reduced to 1/2°-resolution (observable by current nadir-looking satellite altimeters)

  13. SSH vs vorticity snapshot from the NLOM model for 04/10/2006 reduced 1/2°-resolution original 1/32°-resolution

  14. PDF of modeled vorticity as a function of intensity anticyclonic vorticity cyclonic vorticity Ratio of anticycl./cyclonic vorticities original 1/32°-resolution

  15. “Surface Water and Ocean Topography (SWOT)” Mission Point vs 200km-wide swath measurements Repeat cycle: 10 days vs 3~5 days (at mid-high lat.) Recommended to NASA by the NRC Decadal Survey for Oceanographic and Hydrological Applications: http://bprc.osu.edu/water

  16. Approximate Time and Space Scales of Oceanic Variability Chelton (2001)

  17. EKE level SSH field SSHA along 34°N PDO index L H L center of PDO forcing 135E 145E 155E 165E

  18. Yearly-mean sea surface height field

  19. Kuroshio Extension System Study (KESS) is designed to study KE’s transition/impact from a stable to unstable state KESS period

  20. T(z), S(z) and PV(z) evolution in the KE recirculation gyre mixed layer depth subtropical mode water

  21. Altimeter-derived rms sea surface height variability (cm) Schematic of NW Pacific Ocean Circulation Eddy “desert” Abundant eddies

More Related