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The wavenumber,spectra for velocity and temperature in the Gulf Stream region are calculated from a decade (1994-2004) of shipboard acoustic Doppler current profiler (ADCP) measurements,taken as part of the Oleander Project. The velocity and temperature spectra have comparable magnitude, in terms of the kinetic and potential energy, and both indicate a k,2 slope. This discrepancy,between,directly-measured,and,altimeter-derived velocity spectra suggests a noise contribution to altimetry along-track sea surface height data. These results also highlight large gaps in the current understanding of the nature of surface geostrophic turbulence. 3

Wavenumber Spectrum in the Gulf Stream from Shipboard ADCP Observations and Comparison with Altimetry Measurements