OceanObs09

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Proceedings of OceanObs'09: Sustained Ocean Observations and Information for Society

PLENARY PAPERdoi:10.5270/OceanObs09.pp.38

Surface Circulation and Ventilation

Lynne D. Talley(1), Rana Fine(2), Rick Lumpkin(3), Nikolai Maximenko(4), Rosemary Morrow(5)

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There has been tremendous progress in the last decade in observing surface circulation and its variability, mainly resulting from the longer records and higher quality of various satellite and surface drifter data sets, along with new analysis methods. Observation of upper ocean subsurface circulation is necessarily lagging behind because in situ sampling cannot match the satellite coverage; progress is being made using Argo (Array for Real-time Geostrophic Oceanography) profiling, subsurface velocities (moorings and floats), and data assimilation. Western and eastern boundary regions have very different spatial and temporal sampling requirements from the interior circulation and from each other; few are fully instrumented for long-term monitoring, but these are producing climate-appropriate records of velocity, temperature and transport. Coastal circulation is increasingly monitored by high frequency radars. Ventilation and upwelling processes connect the surface layer and underlying interior. Locally these processes are complex combinations of air-sea fluxes, convection, stratification/restratification, and frontal processes, down to the submesoscale (1 to 10 km). Ongoing research ship observations provide quantitative information on formation rates and residence times, and compelling evidence of decadal ventilation changes. The Argo profiler network is beginning to produce time series that show interannual variations in major water masses. Combination of improving air-sea flux products and surface density distributions is yielding ever-improving quantitative estimates of formation rates and variability. Progress in understanding the many processes involved in ventilation has been made through regional experiments and high-resolution modeling of mixed layer and frontal processes. Recommendations for the next decade include: maintenance of relevant existing observing systems, continued improvement of air-sea flux products, continued improvement of synthesis methods, implementation of the satellite SWOT (Surface Water Ocean Topography) and surface salinity missions, expansion of autonomous subsurface profiling to include oxygen and turbulence profiling, and implementation of local observing systems in strategic locations in boundary currents and dense water formation sites.

1Scripps Institution of Oceanography, UCSD, 9500 Gilman Dr., La Jolla, CA 92093-0230 USA
2RSMAS University of Miami, 4600 Rickenbacker Causeway Miami, FL 33149-1098 USA
3NOAA/Atlantic Oceanographic and Meteorological Laboratory, Miami, FL 33149-1097 USA
4IPRC, School of Ocean and Earth Science and Technology, University of Hawaii at Manoa, Honolulu, HI 96822,USA
5CTOH, 18, av. Edouard Belin, 31401 Toulouse Cedex 9, France

Correspondence should be addressed to E-mail: ltalley@ucsd.edu

This paper shall be cited as:

Talley, L., Fine, R., Lumpkin, R., Maximenko, N. and Morrow, R., (2010). "Surface Ventilation and Circulation" in Proceedings of OceanObs’09: Sustained Ocean Observations and Information for Society (Vol. 1), Venice, Italy, 21-25 September 2009, Hall, J., Harrison, D.E. & Stammer, D., Eds., ESA Publication WPP-306, doi:10.5270/OceanObs09.pp.38

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