the use of geoid models to estimate the mean dynamic topography was stimulated with the launching of the grace satellite system, since its models present unprecedented precision and space-time resolution. in the present study, besides the dnsc08 mean sea level model, the following geoid models were used with the objective of computing the mdts: egm96, eigen-5c and egm2008. in the method adopted, geostrophic currents for the south atlantic were computed based on the mdts. in this study it was found that the degree and order of the geoid models affect the determination of tdm and currents directly. the presence of noise in the mdt requires the use of efficient filtering techniques, such as the filter based on singular spectrum analysis, which presents significant advantages in relation to conventional filters. geostrophic currents resulting from geoid models were compared with the hycom hydrodynamic numerical model. in conclusion, results show that mdts and respective geostrophic currents calculated with eigen-5c and egm2008 models are similar to the results of the numerical model, especially regarding the main large scale features such as boundary currents and the retroflection at the brazil-malvinas confluence.