Dr. Gary S. E. Lagerloef Earth and Space Research, 1910 Fairview Ave E



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Establishing a NOAA Operational Data Center for Surface Currents Derived from Satellite Altimeters and Scatterometers; Pilot Study for the Tropical Pacific Including the Hawaiian Islands and US Territorial Islands. Dr. Gary S. E. Lagerloef Earth and Space Research, 1910 Fairview Ave E Seattle WA 98102-3620 USA Phone: (206) 726-0501 FAX: 206-726-0524 E-mail: lager@esr.org Gary T. Mitchum College of Marine Science, University of South Florida 140 Seventh Ave. South, St. Petersburg, FL 33701 Phone: (727) 553-3941 FAX: (727) 553-1189 E-mail: mitchum@marine.usf.edu Robert Cheney Chief, NOAA Laboratory for Satellite Altimetry 1315 East-West Highway, Silver Spring, MD 20910 Phone: (301) 713-2857 ext. 118 FAX: (301) 713-4598 E-mail: Robert.Cheney@noaa.gov Mark Bourassa Center for Ocean Atmospheric Prediction Studies Florida State University, Tallahassee, FL 32306-2840 Phone: (850) 644-6923 FAX: (850) 644-5092 E-mail: bourassa@coaps.fsu.edu Jeffrey Polovina Chief, Ecosystem & Environment Investigation Honolulu Laboratory, NOAA, 2570 Dole St. Honolulu, HI 96822-2396 Phone: (808) 983-5390 FAX: (808) 983-2900 E-mail: Jeffrey.Polovina@Noaa.Gov Richard Legeckis NOAA Laboratory for Satellite Altimetry 1315 East-West Highway, Silver Spring, MD 20910 Phone: (301) 713-2857 ext. 118 FAX: (301) 713-4598 E-mail: Richard.Legeckis@noaa.gov Gregg Jacobs NRL Code 7323, Stennis Space Center, MS 39529 Phone: (228) 688-4720 FAX: (228) 688-4759 E-mail: jacobs@nrlssc.navy.mil Long-term goals Award Number: (DG133E-02-CN-0075) http://www.oscar.noaa.gov This project, which now has a working name OSCAR (Ocean Surface Currents Analysis Realtime), develops a processing system and data center to provide operational ocean surface velocity fields from satellite altimeter and vector wind data. The regional focus is the tropical Pacific, where the value of this data is demonstrated for a variety of uses, specifically fisheries

Report Documentation Page Form Approved OMB No. 0704-0188 Public reporting burden for the collection of information is estimated to average 1 hour per response, including the time for reviewing instructions, searching existing data sources, gathering and maintaining the data needed, and completing and reviewing the collection of information. Send comments regarding this burden estimate or any other aspect of this collection of information, including suggestions for reducing this burden, to Washington Headquarters Services, Directorate for Information Operations and Reports, 1215 Jefferson Davis Highway, Suite 1204, Arlington VA 22202-4302. Respondents should be aware that notwithstanding any other provision of law, no person shall be subject to a penalty for failing to comply with a collection of information if it does not display a currently valid OMB control number. 1. REPORT DATE 2010 2. REPORT TYPE 3. DATES COVERED 00-00-2010 to 00-00-2010 4. TITLE AND SUBTITLE Establishing a NOAA Operational Data Center for Surface Currents Derived from Satellite Altimeters and Scatterometers; Pilot Study for the Tropical Pacific Including the Hawaiian Islands and US Territorial Islands. 5a. CONTRACT NUMBER 5b. GRANT NUMBER 5c. PROGRAM ELEMENT NUMBER 6. AUTHOR(S) 5d. PROJECT NUMBER 5e. TASK NUMBER 5f. WORK UNIT NUMBER 7. PERFORMING ORGANIZATION NAME(S) AND ADDRESS(ES) Naval Research Laboratory,Code 7323,Stennis Space Center,MS,39529 8. PERFORMING ORGANIZATION REPORT NUMBER 9. SPONSORING/MONITORING AGENCY NAME(S) AND ADDRESS(ES) 10. SPONSOR/MONITOR S ACRONYM(S) 12. DISTRIBUTION/AVAILABILITY STATEMENT Approved for public release; distribution unlimited 13. SUPPLEMENTARY NOTES 14. ABSTRACT 11. SPONSOR/MONITOR S REPORT NUMBER(S) 15. SUBJECT TERMS 16. SECURITY CLASSIFICATION OF: 17. LIMITATION OF ABSTRACT a. REPORT b. ABSTRACT c. THIS PAGE Same as Report (SAR) 18. NUMBER OF PAGES 4 19a. NAME OF RESPONSIBLE PERSON Standard Form 298 (Rev. 8-98) Prescribed by ANSI Std Z39-18

management and recruitment, monitoring debris drift, larvae drift, oil spills, fronts and eddies, as well as large scale climate diagnostics and prediction. The end product will be to leave in place a turnkey system running at NOAA/NESDIS, with an established user clientele and easy internet data access. Figure 1 OSCAR home page showing data for the period 1-10 January 2003. Objectives The method to derive surface currents with satellite altimeter and scatterometer data is the outcome of several years of NASA-sponsored research. This project transitions the capability to operational oceanographic applications. The near term objective is to provide data that is updated on a weekly basins, and to carry out a thorough validation analysis. The data have been very useful to monitoring the El Nino in 2002. Approach and work plan Gary Mitchum acquires Jason-1 altimeter Interim Geophysical Data Records (IGDRs) from NASA on a regular basis and every week the gridded sea surface height analysis is updated.

Mark Bourassa provides routine gridded analyses of scatterometer vector wind data. Once per week, these files are transferred to the PI s institution (ESR) where the data are converted into surface currents using the dynamical model of Bonjean and Lagerloef (2002). The surface current fields are then automatically sent to NOAA/PMEL where the OSCAR website (www.oscar.noaa.gov) is being developed. Figure 1 shows the latest image from the web page. Work in the coming year will include streamlining the automated processing system, documentation, extensive validation analyses using surface drifters and ocean current measurements, and scientific evaluations of the ocean dynamics. Work Completed Results Monthly surface current maps were furnished to the NOAA Climate Diagnostics Bulletin. The OSCAR website was activated in September 2002, allowing public access. The website is continually modified to improve data display options. The paper presenting the dynamical model was published in J. Physical Oceaonography. The evolution of the 2002 El Nino was watched closely with the real time surface current data. Strong eastward anomalous flow occurred along the equator from June through November, and was followed by rapid sea surface temperature (SST) growth as the El Nino developed. Our analyses indicate that the surface currents peaked in October, the SST peaked in late November, and the warm event is now in decline (Lagerloef et al., 2003). Impact and Applications National Security The surface current data may become important for naval, commercial maritime or search and rescue operations. Economic Development To the extent that the data from this project improves El Nino prediction, there are potential societal benefits for forecasting economic and environmental impacts. Quality of Life These data are being applied to Pacific fisheries resource management. Science Education and Communication The OSCAR website is open to the public and available students and educators. The PI is working with NASA to help develop high school science curricula concerning ocean currents. Transitions None except as noted above.

Related projects The PI and CoI Gary Mitchum collaborate on a NASA-funded program for scientific analysis of Jason altimeter data. This long term project supported the initial development of the surface current analysis, and is scheduled to continue one more year with low-level funding. Publications Bonjean, F., and G.S.E. Lagerloef: Diagnostic model and analysis of the surface currents in the tropical Pacific Ocean, Journal of Physical Oceanography, 32, 2938-2954, 2002. Kaplan, A., M. Cane, D. Chen, D. Witter, and R. Cheney, Signal and noisein tropical Pacific sea level height analyses, J. Geophys. Res, 2003 (submitted). Lagerloef, G., R.Lukas, F. Bonjean, J. Gunn, G. Mitchum, M. Bourassa, A. Busalacchi: El Niño Tropical Pacific Ocean surface current and temperature evolution in 2002 and outlook for early 2003, Geophys. Res. Lett., 2003 (Submitted) Picaut, J., E. Hackert, A. J. Busalacchi, R. Murtugudde and G. S. E. Lagerloef, Mechanisms of the 1997-1998 El Nino-La Nina, as inferred from space-based observations. J. Geophys. Res., 107 (C5), doi:10.1029/2001jc000850, 2002.