Fluctuations of ice cover and sea water pressure nearby the Tunabreen Glacier front at Spitsbergen

Results of oceanographic measurements carried out in February, 2011, from the sea ice surface in the Tempelfjorden near the Tunabreen front in Svalbard are presented. Two temperature and pressure recorders SBE-39 were deployed on a wire from the ice approximately 300 m from the glacier front. The sa...

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Bibliographic Details
Published in:Polar Research
Main Authors: S. V. Muzylev, Yu. Ya. Macheret, E. G. Morozov, I. I. Lavrentiev, A. V. Machenko
Format: Article in Journal/Newspaper
Language:Russian
Published: Nauka 2015
Subjects:
Q
Online Access:https://doi.org/10.15356/2076-6734-2013-4-119-124
https://doaj.org/article/f0de9c9df21b4a6a8a93a73c5426470d
Description
Summary:Results of oceanographic measurements carried out in February, 2011, from the sea ice surface in the Tempelfjorden near the Tunabreen front in Svalbard are presented. Two temperature and pressure recorders SBE-39 were deployed on a wire from the ice approximately 300 m from the glacier front. The sampling time interval was 1 s. A pressure recorder SBE-37 was located under them on the bottom with a sampling interval of 6 s. Pressure oscillations on the bottom with a period of 90 s and ice cover oscillations with periods of 10 s and 14 s were recorded. The conclusion is made that the recorded oscillations of pressure in the sea water are related to the glacier microsurges, and the observed profiles of temperature, density, and salinity show the absence or insignificant inflow of fresh water from the glacier in the fjord during the winter season. The measurements allowed us to estimate the Young's modulus of the ice.