Zobrazeno 1 - 10
of 101
pro vyhledávání: '"Free drift"'
Akademický článek
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Tidal dissipation from free drift sea ice in the Barents Sea assessed using GNSS beacon observations
Publikováno v:
Ocean Dynamics: theoretical, computational oceanography and monitoring, 72(8)
One of the major challenges facing global hydrodynamic tidal models is the modelling of the interaction between sea ice and tides in high-latitude waters. Recent studies have shown strong seasonal correlation between sea ice and tides. Hence, it is i
Publikováno v:
Astrodynamics. 5:331-346
The dynamics and control of a tetrahedral spacecraft formation flying in the Sun-Earth L2 region is initiatively studied, based on the circular restricted three-body problem (CR3BP). Driven by the science goal of identifying extra-solar terrestrial p
Autor:
Marc de Vos, Marcello Vichi, Sebastiaan Swart, Michael A. Barnes, Louise C. Biddle, Carla-Louise Ramjukadh
Publikováno v:
Journal of Operational Oceanography. 15:187-203
Antarctic sea ice is prevalently seen as a major player in the climate system, but it is also an important factor in polar maritime safety. Remote sensing and forecasting of Southern Ocean sea ice ...
Akademický článek
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Autor:
Marcello Vichi
The marginal ice zone (MIZ) is a transitional region between the open ocean and pack ice. This region is circumpolar in the Antarctic, with different sea ice types depending on the season and the sector of the Southern Ocean. The MIZ extent have trad
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::492cb1726fb26f9b61c8cf56ceb48d61
https://tc.copernicus.org/preprints/tc-2021-307/
https://tc.copernicus.org/preprints/tc-2021-307/
Free drift estimates of sea ice motion are necessary to produce a seamless observational record combining buoy and satellite-derived sea ice motion vectors. We develop a new parameterization for the free drift of sea ice based on wind forcing, wind t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cd9c510941b224cc29a348a6b3f3966c
https://tc.copernicus.org/preprints/tc-2021-249/
https://tc.copernicus.org/preprints/tc-2021-249/
Akademický článek
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Autor:
Michel Tsamados, Harold D. B. S. Heorton, Matthew Fox, Sylvia T. Cole, Andrea Berbellini, Thomas W. K. Armitage, Ana M. G. Ferreira
Publikováno v:
Journal of Geophysical Research: Oceans. 124:6388-6413
For ice concentrations less than 85%, internal ice stresses in the sea ice pack are small and sea ice is said to be in free drift. The sea ice drift is then the result of a balance between Coriolis acceleration and stresses from the ocean and atmosph
Publikováno v:
Acta Oceanologica Sinica. 38:17-25
Sea ice drift is mainly controlled by ocean currents, local wind, and internal ice stress. Information on sea ice motion, especially in situ synchronous observation of an ice velocity, a current velocity, and a wind speed, is of great significance to