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Veris

Veris models how sea ice moves, grows and melts without an external ocean model. It uses JAX, a Python library for calculations with arrays (tables of numbers). The model is differentiable: it can calculate how changes in inputs affect its results. Define an experiment (its inputs and settings), prepare its initial values, advance it in timesteps (intervals of simulated time) and save the results. The same workflow covers dynamics (ice motion), thermodynamic growth (growth and melting through heat exchange) and coupled experiments (both together). It runs on computer processors (CPU), graphics processors (GPU) and explicitly configured JAX meshes (groups of devices).

Install the latest release with Python 3.12 or newer:

python -m pip install --upgrade veris

Start with Getting started for installation, a first command-line simulation and reading its output. The stable documentation describes the latest published release. The command line reference explains how to list and copy setups, run them and override their settings.

This coupled example supplies the ocean's shape and size, masks (arrays marking land and ocean) and atmospheric fields (weather values across the grid, the cells dividing the modeled area). These prescribed inputs come from the setup, without an external ocean model:

from veris import Execution, Experiment, Grid, Simulation

experiment = Experiment.builtin(
    "island", grid=Grid(6, 8), steps=3,
    settings={"dtype": "float32", "nEVPsteps": 2},
    execution=Execution(backend="cpu"),
)
with Simulation.initialize(experiment) as simulation:
    result = simulation.run()
    simulation.snapshot("final.nc", variables=("hIceMean", "Area"))
    simulation.save_restart("checkpoint.nc")

Use new output destinations when repeating this example. Its two EVP subcycles (repeated calculations in the elastic-viscous-plastic ice-motion solver) demonstrate the programming interface; they do not show that the solver has converged to a solution.

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