JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 100, NO. C12, PAGES 25,109-25,127, DECEMBER 15,1995 zy Open-ocean validation of TOPEX/POSEIDON sea level in the western equatorial Pacific Joël Picaut,l Antonio J. Busalacchi,2 Michael zyxwv J. McPhaden? Lionel Gourdeau,l Frank I. Gonzalez? and Eric C. Hackert2.4 Abstract. During the verification phase of the TOPEX/POSEIDON radar altimeter mission a rigorous open-ocean validation experiment was conducted in the western equatorial Pacific Ocean. From August-September 1992 to February-March 1993, two Tropical Ocean and Global Atmosphere (TOGA) Tropical Atmosphere Ocean moorings at 2OS-156"E (1739 m depth) and 2OS-164.4"E (4400 m depth) were outfitted with additional temperature, salinity, and pressure sensors to measure precisely the dynamic height from the surface to the bottom at 5-min intervals directly beneath two TOPEX/ POSEIDON crossovers. Bottom pressure gauges and inverted echo sounders were deployed as well. A predeployment design study using full depth conductivity-temperature- depth casts, subsequently confirmed by postdeployment analyses, indicated this suite of instruments was capable of measuring sea surface height fluctuations to within 1-2 cm. The validation experiment also benefited from the comprehensive set of ocean-atmosphere measurements that were made in the region during the TOGA Coupled Ocean- Atmosphere Response Experiment intensive observation period of November 1992 to February 1993. The surface relative to .bottom dynamic height fluctuations observed in situ during the 6-7 month experiment had a standard deviation of 5 cm with excursions of order -t-15 cm. Energetic steric sea level variability was found to exist on short timescales of order hours to a few days, most notably, the quasi-permanence of strong semidiurnal internal tides. Such internal tides were noted to induce changes in surface dynamic height with a standard deviation of 2 dynamic centimeters. At the shallower of the two sites, 2"s- 156"E, a possible nonlinear rectification of the internal tide was observed occasionally to change the dynamic height by as much as 30 cm over less than an hour. On timescales longer than the 10-day repeat of the TOPEWPOSEIDON satellite, the low-frequency fluctuations of dynamic height were related to interannual variations corresponding to the 1991-1993 EI Niño-Southern Oscillation, to the seasonal cycle, and to intraseasonal variations associated with the 40- to 60-day oscillations of the equatorial zonal wind field. Instantaneous comparisons between the 1-s TOPEX/POSEIDON altimeter retrievals and the 5-min dynamic height were performed with regard to several tide models, the barotropic tide measured in situ, European Centre for Medium-Range Weather Forecasts surface air pressure, and the surface air pressure measured in situ. Depending zyxw on the choice of altimeter and of the environmental corrections applied to the altimeter data, the rms differences between the satellite and the in situ measurements of sea level were as low as 3.3 cm at 2OS-156"E and 3.7 cm at 2OS-164.4"E. When additional satellite data in the general vicinity of the mooring are included and after the use of a 30-day low-pass filter, the satellite and in situ data were found to be highly correlated, with correlation coefficients of about 0.95 and rms differences around 1.8 cm. 1. Introduction The initial results from the TOPEXlPOSEIDON radar al- timeter mission are very encouraging with respect to the capa- 'Groupe SURTROPAC, l'Institut Français de Recherche Scienti- fique pour le Développement en Coopération (ORSTOM), Nouméa, New Caledonia. 'Laboratory for Hydrospheric Processes, NASA Goddard Space Flight Center, Greenbelt, Maryland. 3Pacific Marine Environmental Laboratory, N O M , Seattle, Wash- ington. 4Hughes STX Corporation, Greenbelt, Maryland. Copyright 1995 by the American Geophysical Union. bility of the altimeter to describe the sea level attributes of the large-scale ocean circulation (see the special section "TOPEX/ POSEIDON Geophysical Evaluation" in zyxw Joiinial zy of Geophysi- cal Research, 99(C12), 24,369-25,062, 1994). Prior to launch, the precision of the radar altimeter instrument was projected to be of order 2.4 cm [TOPEX/POSEIDON Scieiice Working Team, 19911. In the event this level of precision is attained in orbit and the necessary environmental corrections are of sim- ilar order and result in an overall level of accuracy of order 4 .cm, tQisclass of radar altimeters will have considerable poten- tia1 fot long-term ocean climate monitoring. Thus there is a clear need to rigorously validate the accuracy of TOPEX/ POSEIDON sea level observations in the open ocean. Unfor- t" tunately, an open-ocean validation was not planned by the TOPEX/POSEIDON project. During the verification phase of 25,109 Panpr niimher zyxwvutsrqpo WTPfl313--Y--