Estimation of the Sea State Bias effect on the altimetric

Rami, Ali; Mhamed, Khelif; Kahlouche, Salem; Denoukri, Toufik

Bulletin des sciences géographiques de l'INCT
Volume 10, Numéro 1, Pages 16-21
2006-04-30

Estimation Of The Sea State Bias Effect On The Altimetric

Authors : Rami Ali . Mhamed Khelif . Kahlouche Salem . Denoukri Toufik .

Abstract

The sea state bias (SSB) which affect the altimetric measurements on the sea surface is estimated using empirical parametric model (BM4). calibrated by the analysis of the altimeter data. This model is a simple Iinear fonction that links the SSB with the significant wave height (SWH). the wind speed ( U) and the backscatter coefficient (σ_0). The knowledge of the backscalter coefficient determined by altimetric signal processing allows to detennine the significant wave height and the wind speed. The use of Topex/Poseidon and Jason-1 altimetric data to calculate the sea state bias with the BM4 model and the comparison of the results obtained with the SSB value transmitted in the message of each satellite allowed us the validation of the methodological approach developed. The proximity of the results obtained with Topex / Poseidon data is sufficient for the most altimetric applications as the detennination of the mean sea level which was calculated on the western Mediterranean Sea duting a period of 72 cycles. Conceming Jason-1. the difference of the results in the determination of the SSB can be explained by the nature of the instruments on boai·d and also the type of model used.