Gravity Measurements in the Beaufort Sea Area

Auteurs-es

  • Donald Plouff

DOI :

https://doi.org/10.14430/arctic3500

Mots-clés :

Energy budgets, Heat transmission, Movement, Ocean currents, Sea ice, Temporal variations, Winds, East Greenland Current, Arctic Ocean

Résumé

Reports investigations on Ice Island T-3 at approx 70-80 de- grees N, 110-140 degrees W, May 1958-Sept 1959. The North American 113a and Worden E-340 gravity meters were used for twice- daily measurements. Values of observed gravity, free air and Bouguer anomalies are tabulated, contoured, and interpreted. Gravity anomalies were found at 76-80 degrees N, and a gradient near 75 degrees N which indicates an increase in density of subbottom rocks toward the southwest. Bouguer anomaly values increased with distance from land, characteristic of normal ocean basins.

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Publié-e

1964-01-01