Prof. dr. hab. Korneliy Tretyak

assistant professor Tatiana Grytsyuk

Prof. Petro Dvulit

Associate Professor Lubov Babiy

Application of geodetic methods for monitoring of stresses of penstock on Tereblya-Rikska hydropower station

The long-term dependences for the changes of deformations and stresses in penstock based on the results of many-year investigations are established. Such in-vestigations were held on the spatial geodetic network on the Tereblya-Rikska hy-dropower station (HPS). The investigations of the short-term stresses and deforma-tions of the penstock with the use of electronic tachеometer Leica TPS 1201 has been undertaken. Direct correlations between the changes of the length of all baulks and the changes of water level in the storage reservoir are determined ...

Prof.dr. hab., Alexsandr Marchenko,

Prof. dr. hab. Korneliy Tretyak

Alexsandr Lopyshansky

Taras Pavliv

Recent dynamic ocean topography models and their comparison

Regarding the rapidly growing satellite altimetry database and correspond-ing products worldwide, an investigation of different mean dynamic ocean topog-raphy (MDT) models was assessed to be important for further use in geodetic ap-plications. The efficiency and quality of different MDT models are discussed in view of adopted geoids as reference surfaces. The models used are: 1) The ECCO model based on hydrology and altimetry data, 2) The combined MDT Rio-05 con-structed in CSL AVISO (2005) from data for the period 1993-1999, 3) The com-bined MDT CNES-CLS09 model at the grid points 15'x15' based on altimetry and hydrology data for the period 1993-2007 (CSL AVISO, 2009), 4) The DNSC08MDT solution of mean dynamic topography (Danish National Space Cen-ter) obtained from the geometrical differences between the DNSC08 mean sea sur-face and the EGM2008 geoid model. The concluding results of the investigation are: 1) statistics of all mean dyamic topography models leads to the approximately same standard deviations about 70 cm and range from -2 m to 2 m; 2) all differences among various MDT models give much smaller standard deviations about 6 - 15 cm; 3) all such differ-ences among various MDT give larger mean deviation, which can be explained by different geoid ...

Prof. Petro Dvulit

Prof. dr. hab. Korneliy Tretyak

O dokładności interpolacji wysokości geoidy (quasi-geoidy) z wykorzystaniem nowoczesnych modeli geopotenciału

W referacie omówione zostały rożne współczesne modele pola grawitacyj-nego Ziemi dla wyznaczenia dokładność interpolacji wysokości geoidy / quasi--geoidy dla obszaru Ukrainy. W tym celu przeprowadzono porównanie modelu geoidy i pola grawitacyjnego Ziemi dla danych niwelacji satelitarnej 44 punktów 1 i 2 klasy sieci geodezyjny Ukrainy.Wyniki badań pokazały, ze model EGMO8 jest najdokładniejszym modelem ze wszystkich istniejących modeli geopotencjału dla obszaru Ukrainy. Dokładne wysokości quasi-geoidy charakteryzuje sie na poziomie ± 10 cm.     ...