New dynamics parameterizations in Version 5 of the Los Alamos Sea Ice Model, CICE,
feature an anisotropic rheology and variable drag coefficients. This study investigates their …

We use a 1-D model to study how salinity evolves in Arctic sea ice. To do so, we first explore
how sea-ice surface melt and flooding can be incorporated into the 1-D thermodynamic …

We present a new numerical algorithm for predictions of water droplets accumulation
responsible for in-flight ice accretion. Unlike the traditional Lagrangian and Eulerian …

We present a new numerical algorithm for the prediction of water droplets accumulation
responsible for in-flight ice accretion. Unlike the traditional Lagrangian and Eulerian …

In this thesis I develop a new 1D thermodynamic sea-ice model with parametrized brine
dynamics to study brine movement inside sea ice and the evolution of sea-ice salinity. Brine …

This note summarizes discussions held during a 2-day meeting of the CLiC Arctic Sea Ice
Working Group, in Boulder, CO (31st Oct.–1st Nov., 2011). It is not intended to be …

Nowadays marine models routinely produce large amounts of results. Making sense of all
these real numbers is not a trivial task. This is why specific interpretation methods are …

The hydrosphere is made up of a number media, such as groundwater, oceans, shelf seas,
estuaries, rivers, sea ice. The processes taking place in these domains are vastly different in …

We use a 1-D model to study how salinity evolves in Arctic sea ice. To do so, we first explore
how sea-ice surface melt and flooding can be incorporated into the 1-D thermodynamic …