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Relevant bibliographies by topics / Van Mijen Fjord

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Journal articles

Academic literature on the topic 'Van Mijen Fjord'

Author: Grafiati

Published: 4 June 2025

Last updated: 1 August 2025

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Journal articles on the topic "Van Mijen Fjord"

1

Morozov, E. G., S. V. Muzylev, A. S. Shestov, and A. V. Marchenko. "Short-Period Internal Waves under an Ice Cover in Van Mijen Fjord, Svalbard." Advances in Meteorology 2011 (2011): 1–6. http://dx.doi.org/10.1155/2011/573269.

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Temperature and velocity fluctuations measured in Van Mijen Fjord in Svalbard and interpreted as the fluctuations induced by internal waves revealed the existence of short-period internal waves with an amplitude of approximately 1 m and a period of approximately 5–10 min that correlate with the ice cover fluctuations of the same period with an amplitude of a few millimeters.

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2

Marchenko, A. V., and E. G. Morozov. "Asymmetric tide in Lake Vallunden (Spitsbergen)." Nonlinear Processes in Geophysics 20, no. 6 (2013): 935–44. http://dx.doi.org/10.5194/npg-20-935-2013.

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Abstract. We observed strongly asymmetric tide in a channel connecting the Van Mijen Fjord and Lake Vallunden in Spitsbergen. The channel is approximately 100 m long, 10 m wide, and 1–2 m deep. Asymmetric tide was also observed in the lake. The form of the semidiurnal tide is described by a combination of only three harmonics (M2, S2 and M4) with different amplitudes and phases. The flood dominant form of the surface elevation in the channel (unlike the ebb dominant tide in the fjord) is formed over a horizontal distance of 50 m over a shallow bottom at the entrance to the channel. The tide in

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3

Moreau, Ludovic, Léonard Seydoux, Jérôme Weiss, and Michel Campillo. "Analysis of microseismicity in sea ice with deep learning and Bayesian inference: application to high-resolution thickness monitoring." Cryosphere 17, no. 3 (2023): 1327–41. http://dx.doi.org/10.5194/tc-17-1327-2023.

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Abstract. In the perspective of an upcoming seasonally ice-free Arctic, understanding the dynamics of sea ice in the changing climate is a major challenge in oceanography and climatology. In particular, the new generation of sea ice models will require fine parameterization of sea ice thickness and rheology. With the rapidly evolving state of sea ice, achieving better accuracy, as well as finer temporal and spatial resolutions of its thickness, will set new monitoring standards, with major scientific and geopolitical implications. Recent studies have shown the potential of passive seismology t

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4

Høyland, Knut V., Marc Oggier, and Ase Ervik. "Van Mijenfjord Ice Core Data 1999-2013." April 1, 2020. https://doi.org/10.5281/zenodo.3737134.

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5

Morozov, Eugene, A. Marchenko, and K. Filchuk. "Freezing of Tidal Current Under Ice in a Shallow Channel." Russian Journal of Earth Sciences, April 18, 2022, 1–5. http://dx.doi.org/10.2205/2022es000793.

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We analyze tidal currents under ice in a shallow channel located near the tip of the Van Mijen Fjord in Spitsbergen. During the flood cycle of tide seawater flows under ice and strongly freezes in a shallow channel. During the ebb cycle salinity of the outflowing water is greater than that of the inflowing water. Salt balance is estimated. During high-water tide, salt water seeps through the cracks in the ice to the surface, which increases salinity of the snow and water mixture.

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6

Løken, Trygve Kvåle, Aleksey Marchenko, Thea Josefine Ellevold, Jean Rabault, and Atle Jensen. "Experiments on turbulence from colliding ice floes." Physics of Fluids, May 27, 2022. http://dx.doi.org/10.1063/5.0088953.

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Increased knowledge about energy dissipation processes around colliding ice floes is important for improved understanding of atmosphere-ice-ocean energy transfer, wave propagation through sea ice and the polar climates. The aim of this study is to obtain such information by investigating colliding ice floe dynamics in a large-scale experiment and directly measuring and quantifying the turbulent kinetic energy (TKE). The field work was carried out at Van Mijen Fjord on Svalbard, where a 3x4 m ice floe was sawed out in the fast ice. Ice floe collisions and relative water-ice motion was generated

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