This dataset contains national designs data. Data is published in form of full export and subsequent incremental data.
This dataset contains national designs data. Data is published in form of full export and subsequent incremental data.
This dataset contains national designs data. Data is published in form of full export and subsequent incremental data.
This dataset contains national designs data. Data is published in form of full export and subsequent incremental data.
This dataset contains national designs data. Data is published in form of full export and subsequent incremental data.
This dataset contains national designs data. Data is published in form of full export and subsequent incremental data.
This dataset contains national designs data. Data is published in form of full export and subsequent incremental data.
This dataset contains national designs data. Data is published in form of full export and subsequent incremental data.
This dataset contains national designs data. Data is published in form of full export and subsequent incremental data.
This dataset contains national designs data. Data is published in form of full export and subsequent incremental data.
This dataset contains national designs data. Data is published in form of full export and subsequent incremental data.
This dataset contains national designs data. Data is published in form of full export and subsequent incremental data.
Detailed gravimetric quasigeoid QGZÚ-2013 represents a transformation surface enabling transformation between altitudes H in the Baltic Vertical Datum – After Adjustment (Bpv) and ellipsoidal heights h in the European Terrestrial Reference System 1989 (ETRS89) /realization ETRF2000/ above the rotating ellipsoid Geodetic Reference System 1980 (GRS80). Data content creates height anomaly zeta expressed in the nodal points of regular grid (3'' x 3'') of geographical coordinates ETRS89. Height anomalies implements own transformation relationship that has the form h = H + zeta. Total mean square error of height anomaly is on the territory of the Czech Republic 1 cm, in the mountainous terrain and in border areas (up to 10 km from the border) can reach higher values, but not more than 3 cm. Quasigeoid model was computed using combined regional solution of linear gravimetric boundary value task for the correcting gravitational potential of the Earth, with the significant contribution of complete revised dataset of detailed points of gravimetric mapping of the Czech Republic performed in the frame of geophysical mapping between 1950 – 2010, and with the other data.
Detailní popisy služeb veřejné správy vyhotovené na základě přílohy č. 2 vyhlášky č. 515/2020 Sb. Tyto popisy má dle § 5 zákona č. 106/1999 Sb. každý povinný subjekt zpřístupňovat na svých stránkách.
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