Topographic-geodetic and cartographic support of the Arctic zone of the Russian Federation
- 1 — Ph.D., Dr.Sci. Head of department Saint-Petersburg Mining University
- 2 — Ph.D. Leading Researcher Federal Scientific and Technical Center for Geodesy, Cartography and Spatial Data Infrastructure
- 3 — Head of department St. Petersburg State Transport University
- 4 — JSC «Aerogeodeziya»
- 5 — Federal Scientific and Technical Center for Geodesy, Cartography and Spatial Data Infrastructure
- 6 — Federal Scientific and Technical Center for Geodesy, Cartography and Spatial Data Infrastructure
Abstract
A version of the project of the concept of topographic, geodetic and cartographic support of the Arctic zone of the Russian Federation based on the use of modern means and tools is presented, including its content. The results of the development in the Arctic, carried out with the participation of the authors in 1961-1967 and 1975-1992, are presented in detail. The strategic importance and great attention of the state structures to the development of the Arctic zone is underlined. The key moments of the development of topographic, geodetic and cartographic support for this region are given. The role of leading research institutes in this process is shown. The proposed concept includes six stages. When creating a planimetric geodetic base, the authors recommend an alternative innovative algorithm for determining the height H without first calculating the latitude B and use only satellite measurements. The extremely important question of converting geodetic coordinates B, L into rectangular plane coordinates x, y is considered. For the territory of the Russian Federation new developments are proposed, they use data from satellite determinations, a new approach to the determination of normal heights and the conversion of rectangular space coordinates into rectangular plane coordinates necessary for mapping. The required regulations of reference documentation for the topographic survey of the shelf are shown. The importance of implementing the concept in connection with the definition of the outer boundary of the continental shelf of the Arctic Ocean is shown.
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