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TC | Articles | Volume 14, issue 11
TC | Articles | Volume 14, issue 11
The Cryosphere, 14, 3707–3729, 2020
https://doi.org/10.5194/tc-14-3707-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
The Cryosphere, 14, 3707–3729, 2020
https://doi.org/10.5194/tc-14-3707-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
TC | Articles | Volume 14, issue 11

Research article 05 Nov 2020

Research article | 05 Nov 2020

High-resolution simulations of interactions between surface ocean dynamics and frazil ice

Agnieszka Herman et al.

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Revised manuscript accepted for TC
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Cited articles

Belcher, S., Grant, A., Hanley, K., Fox-Kemper, B., Van Roekel, L., Sullivan, P., Large, W., Brown, A., Hines, A., Calvert, D., Rutgersson, A., Pettersson, H., Bidlot, J.-R., Janssen, P., and Polton, J.: A global perspective on Langmuir turbulence in the ocean surface boundary layer, Geophys. Res. Lett., 39, L18605, https://doi.org/10.1029/2012GL052932, 2012. a, b, c, d, e
Biggs, N. and Willmott, A.: Polynya flux model solutions incorporating parameterization for the consolidated new ice, J. Fluid Mech., 408, 179–204, https://doi.org/10.1017/S0022112099007673, 2000. a
Botte, V. and Mansutti, D.: A numerical estimate of the plankton-induced sea surface tension effects in a Langmuir circulation, Mathematics and Computer Simul., 82, 2916–2928, https://doi.org/10.1016/j.matcom.2012.07.014, 2012. a
Canuto, V., Howard, A., Cheng, Y., and Dubovikov, M.: Ocean turbulence. Part I: One-point closure model – momentum and heat vertical diffusivities, J. Phys. Oceanogr., 31, 1413–1426, https://doi.org/10.1175/1520-0485(2001)031<1413:OTPIOP>2.0.CO;2, 2001. a
Chamecki, M., Chor, T., Yang, D., and Meneveau, C.: Material transport in the ocean mixed layer: Recent developments enabled by large eddy simulation, Rev. Geophysics, 57, 1338–1371, https://doi.org/10.1029/2019RG000655, 2019. a, b, c, d, e, f
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Under typical conditions favorable for sea ice formation in many regions (strong wind and waves, low air temperature), ice forms not at the sea surface but within the upper, turbulent layer of the ocean. Although interactions between ice and ocean dynamics are very important for the evolution of sea ice cover, many aspects of them are poorly understood. We use a numerical model to analyze three-dimensional water circulation and ice transport and show that ice strongly modifies that circulation.
Under typical conditions favorable for sea ice formation in many regions (strong wind and waves,...
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The Cryosphere

An interactive open-access journal of the European Geosciences Union

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