The purpose of this investigation is the assessment of various systematic error and biases that will affect the quality of Jason-1 measurements of sea surface height: 1) tracker biases; 2) skewness biases; and 3) EM bias. We will perform full retracking of the Jason-1 waveforms and independently assess instrument accuracy, as well as provide for an estimate of the sea surface skewness. These estimates will then be used to assess the residual height error dependence on skewness. They will also be used to provide a new non-parametric algorithm for the EM bias which includes sea surface skewness as one of the regression parameters. The proposed EM bias correction will be validated by repeat pass and cross-over analysis, and compared to the TOPEX EM bias performance during the calibration phase of the mission.
The purpose of this investigation is the assessment of various systematic errors and biases which will affect the quality of the Jason-1 measurements of sea surface height. The three main error sources examined will be: 1) tracker biases; 2) skewness biases; 3) EM bias.
The tracker bias is due to potential errors from approximations made in the operational retracking of the Jason-1 data. Possible sources of these errors are the look-up table procedure which is made to account for the point target response in the operational retracking. During the validation phase of the Jason-1 mission, we will use optimal retracking algorithms, which, although slower than the operational retracking algorithm, make fewer approximations to obtain statistically "optimal" estimates of sea surface heights, significant wave height and ocean surface skewness.
Another source of bias in the sea surface height is due to the fact that the surface height is not normally distributed, but can show a significant skewness. The skewness causes a bias in the sea surface height, and we will assess the level of residual skewness errors by performing the optimal waveform fitting described above. More importantly, skewness is an indicator of non-linear interactions among surface waves.
These non-linear interactions are also responsible for the EM bias, one of the remaining dominant sources of error in the estimation of sea surface height from altimeters. Srokosz and Longuet-Higgins  have shown theoretically that skewness and wave significant slope are related. It has also been shown experimentally by Arnold and Melville, and theoretically by Elfouhaly, that the EM bias can depend strongly on significant slope. During the TOPEX mission, it was not possible to estimate sea surface skewness due to systematic distortions of the return waveform. We expect that these effects will not be present for the Jason-1 waveforms, and therefore it will be possible to obtain a regression of the EM bias, which includes sea surface skewness, as well as the traditional sea surface height and wind speed. We will derive a non-parametric model over the three-dimensional space defined by these parameters.
Srokosz M.A., M. Longuet-Higgins, 1986: On the skewness of the sea surface elevation. J. Fluid. Mech., 164, 487-497.
Estimation of electromagnetic and tracker bias for Jason-1