Abstract

The first direct field measurement of the entire terminal moraine of the Werenskioldbreen glacier on Spitsbergen took place at the end of July and the beginning of August 2015. The results of the measurements were the basis for the development of the large-scale terminal moraine map. The article presents the stages of map creation and editing based on measurement points established by the GNSS method. The map editing required knowledge of the morphologically complex terrain. Key documentation was field notes and documentary photographs, enabling the cartographic interpretation of the varied topographic features of the terrain's surface. Based on the documentation, the water bodies on the moraine were located, the outline of the structure and the boundary points were executed and the latter were excluded from the triangulation process. The glacial river was also excluded from triangulation, which allowed a DTM to be developed. An important step in point cloud mapping was to generate a topologically correct digital elevation model of satisfactory accuracy. On the basis of the DTM, contour lines were generated showing the topographic features of the terrain's surface. The printable resultant map's scale is 1: 5000; it is in the UTM coordinate system, in the 33X zone. Complementing the content of the map, a grid of geographic coordinates, a kilometer grid, and map key descriptions were added.

Highlights

  • IntroductionSurface changes are noticeable with the naked eye; maps as cartographic studies help one to document the changes that have occurred on the surface

  • Global climate changes are the most visible in polar regions

  • The article presents the stages of map creation and editing based on approximately 21 thousand measurement points measured by the GNSS method

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Summary

Introduction

Surface changes are noticeable with the naked eye; maps as cartographic studies help one to document the changes that have occurred on the surface. Most studies in the polar regions focus on assessing climate changes and the impact of the changes on the environment. With the growing interest in polar subjects, and the possibilities of using geodetic methods in the polar regions, cartographic studies began to appear. New technologies and methods of data collection enable the development of polar research and the resulting possibilities. Software and hardware have contributed to the development and increase in a number of cartographic documents concerning polar areas. The development of measurement techniques and the possibility of obtaining accurate data have led to an increase in the number of polar regions that are considered both interesting and dangerous. Geodetic measurements are part of the non-invasive polar research without disturbing or interfering with the environment

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