Research of heights of surface of the Black sea with the use of information of satellite altimetri was done. The model of heights of the Black sea is built. Got results it was by comparison to the heights of European kvazigeoid.
1. Tretiak N.P. Modeliuvannia hravitatsiinoho polia i topohrafii okeanu v rehioni Antarktyky / Dys. ... kand. tekhn. nauk. Nats. un-t “Lvivska politekhnika”. – Lviv, 2008. – S. 14.
2. Marchenko O.M., Tretiak N.P. Modeliuvannia topohrafii rehionu Anktarktyky// Visnyk heodezii ta kartohrafii. – 2008. – №4. – S.7–10.
3. Andersen O.B., Knudsen P. The DNSC08MDT Mean Dynamic Topography, (DTU-SPACE), Danish National Space Center 2008.
4. Andersen, O.B., P. Knudsen, R. Trimmer. Improved high resolution altimetric gravity field mapping (KMS2002 Global Marine Gravity Field). IAG Symposia 128:326–331, Springer Verlag 2005.
5. Rio M.-H., P. Schaeffer, et al. The estimation of the ocean Mean Dynamic Topography through the combination of altimetric data, in-situ measurements and GRACE geoid: From global to regional studies. Proceedings of the GOCINA international workshop, Luxembourg 2005.
6. Rio M-H, P. Schaeffer, G. Moreaux, J-M Lemoine, E. Bronner. A new Mean Dynamic Topography computed over the global ocean from GRACE data, altimetry and in-situ measurements. Paper presented at OceanObs09 symposium, 21–25 September 2009, Venice.
7. Seeber G. Satellite Geodesy 2nd completely revised and extended edition. Walter de Gruyter, Berlin New York, 2003 – 589 p.
8. Torge, W. Geodesy,2nd edition.Walter de Gruyter, Berlin, New York,1991.