Abstract

Abstract. In July of 1931, on the eve of International Polar Year II, an Arctic flight of the Graf Zeppelin rigid airship was organized. This flight was a realization of the idea of F. Nansen, who advocated the use of airships for the scientific exploration of the Arctic territories, which were poorly studied and hardly accessible at that time. The route of the airship flight was Berlin – Leningrad – Arkhangelsk – Franz Josef Land – Severnaya Zemlya – the Taimyr Peninsula – Novaya Zemlya – Arkhangelsk – Berlin. One of scientific goals of the expedition was to measure the H and D geomagnetic field components. Actually, the first aeromagnetic survey was carried out in the Arctic during the flight. After the expedition, only preliminary results of the geomagnetic measurements, in which an anomalous behavior of magnetic declination in the high-latitude part of the route was noted, were published. Our paper is concerned with the first aeromagnetic measurements in the Arctic and their analysis based on archival and modern data on the magnetic field in the Barents and Kara sea regions. It is shown that the magnetic field along the flight route had a complicated structure, which was not reflected in the magnetic charts of those times. The flight was very important for future development of aero- and ground-based magnetic surveys in the Arctic, showing new methods in such surveys.

Highlights

  • Attention to the necessity and importance of collective research efforts in the investigation of geophysical processes, including geomagnetic measurements, in the Arctic region had already been drawn when Polar Year I (1882–1883) was organized

  • To carry out an Arctic flight with scientific aims, the Graf Zeppelin airship constructed in Germany was used

  • During the Arctic flight of Graf Zeppelin the double compass was placed in the same position as in the European flight (Ljungdahl, 1931)

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Summary

Social Abstract

In July of 1931, on the eve of International Polar Year II, an Arctic flight of the Graf Zeppelin rigid airship was organized. This flight was a realization of the idea of F. One of scientific goals of the expedition was to measure the H and D geomagnetic field components. Only preliminary results of the geomagnetic measurements, in which an anomalous behavior of magnetic declination in the high-latitude part of the route was noted, were published. Our paper is concerned with the first aeromagnetic measurements in the Arctic and their analysis based on archival and modern data on the magnetic field in the Barents and Kara sea regions. The flight was very important for future development of aero- and ground-based magnetic surveys in the Arctic, showing new methods in such surveys

Introduction
Procedure of geomagnetic measurements on board the Graf Zeppelin airship
Measurements of horizontal component
Measurements of declination D
Conclusions
Full Text
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