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Published in Physical review letters, 2018
Recommended citation: Allende, S., Henry, C., & Bec J (2018). "Stretching and buckling of small elastic fibers in turbulence." Physical Review Letters. 1(1). http://sofiallende.github.io/files/allende2018dynamics.pdf
Published in Philosophical Transactions of the Royal Society A, 2020
Recommended citation: Allende, S., Henry, C., & Bec, J. (2020). "Dynamics and fragmentation of small inextensible fibres in turbulence." Philosophical Transactions of the Royal Society A. 1(2). http://sofiallende.github.io/files/allende2020fragmentation.pdf
Published in The Cryosphere, 2023
Recommended citation: Goosse, H., Allende, S., Bitz, C. M., Blanchard-Wrigglesworth, E., Eayrs, C., Fichefet, T., ... & van Lipzig, N. P. (2023). "c Modulation of the seasonal cycle of the Antarctic sea ice extent by sea ice processes and feedbacks with the ocean and the atmosphere" The Cryosphere,17(1), 407-425. http://sofiallende.github.io/files/gossemodulation2023.pdf
Published in Journal of Fluid Mechanics, 2023
Recommended citation: Allende, S., & Bec, J. (2023). "Velocity and acceleration statistics of heavy spheroidal particles in turbulence." OJournal of Fluid Mechanics, 967, R4. http://sofiallende.github.io/files/allende2023velocity.pdf
Published in Ocean Modelling, 2023
Recommended citation: Allende, S., Fichefet, T., Goosse, H., & Treguier, A. M. (2023). "On the ability of OMIP models to simulate the ocean mixed layer depth and its seasonal cycle in the Arctic Ocean." Ocean Modelling, 184, 102226. http://sofiallende.github.io/files/allende2023ontheability.pdf
Published in Geoscientific Model Development, 2024
Recommended citation: Allende, S., Treguier, A. M., Lique, C., de Boyer Montégut, C., Massonnet, F., Fichefet, T., & Barthélemy, A. (2024). " Impact of ocean vertical mixing parameterization on Arctic sea ice and upper ocean properties using the NEMO-SI3 model. " Geoscientific Model Development Discussions, 2024, 1-28. http://sofiallende.github.io/files/allende2024impact_pp.pdf
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To model the ice-ocean boundary layer, we utilize the Navier-Stokes equations under the Boussinesq approximation. In the bulk, the governing equations can be written as follows:
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This Oceananigans.jl example simulates the diffusion of a one-dimensional Gaussian temperature and salinity tracers.
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This Oceananigans.jl example simulates the diffusion of one-dimensional Gaussian temperature and salinity tracers in an ice-ocean environment.
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This Oceananigans.jl example simulates the melting of sea ice in a two-dimensional setup.
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We utilize the Navier-Stokes equations under the Boussinesq approximation. The governing equations can be written as follows:
Undergraduate course, University 1, Department, 2014
This is a description of a teaching experience. You can use markdown like any other post.
Workshop, University 1, Department, 2015
This is a description of a teaching experience. You can use markdown like any other post.