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The size of the space-time volume which contributes I degree of freedom is the irreducible grain of the analysis. 7 times the period and the data spacing. The problem is in the cross-track grain. Since we are compiling I-dimensional spectra it is necessary to integrate, implicitly or exp1icity, over crosstrack wavenumber. For the spectral estimate itself this is equivalent to looking only along the track, but for the degrees of freedom the spectral shape becomes important, because the total estimate is the weighted sum of different bands each with different uncertainties.

1983, "A study of the variability of ocean currents ~n the northwestern Atlantic using satellite altimetry". J. Phys. , in press. , 1978, "Observations of the vertical distribution of low frequency kinetic energy in the Western North Atlantic", J. , 36, pp. 298-305. Topex Science Working Group, 1981, "Satellite altimetric measurements of the ocean", JPL Doc. , Magaard, L. , 1976, "Eddy energy in the Oceans", J. Geophys. , ~, pp. 2641-2646. EDDY KINETIC ENERGY DISTRIBUTION IN THE SOUTHERN OCEAN FROM SEASAT ALTIMETER AND FGGE DRIFTING BUOYS N.

Fellous CNES, France W. S. Wi 1son NASA, USA Discussions between NASA and CNES in 1981-1982 have resulted in a decision to conduct a joint definition study examining the possibility of cooperation between the proposed NASA TOPEX (1) and CNES POSEIDON (2) missions. The objective of a potential combined mission is to measure the surface topography of the global oceans with sufficient accuracy and precision such that the measurements may be used in determining their general circulation. An additional objective is to prepare for follow-on oceanographic missions allowing long-term observation of the slowly varying large-scale ocean currents.

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AGS Experiments [1994-1996]

by Donald

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