We commonly refer to state estimation theory in geosciences as data assimilation (DA). This
term encompasses the entire sequence of operations that, starting from the observations of a …

We revisit the challenges and prospects for ocean circulation models following Griffies et al..
Over the past decade, ocean circulation models evolved through improved understanding …

Marginal ice zones (MIZs) are qualitatively distinct sea-ice-covered areas that play a critical
role in the interaction between the polar oceans and the broader Earth system. MIZ regions …

Ice in the environment plays a central role in both global-scale processes on Earth and
many human activities. Issues related to its description, including the modelling of natural ice …

In this paper, we evaluate the neXtSIM sea ice model with respect to the observed scaling
invariance properties of sea ice deformation in the spatial and temporal domains. Using an …

Simulating sea ice drift and deformation in the Arctic Ocean is still a challenge because of
the multiscale interaction of sea ice floes that compose the Arctic Sea ice cover. The Sea Ice …

Long dynamical atmospheric reanalyses are widely used for climate studies, but data-
assimilative reanalyses of ocean and sea ice in the Arctic are less common. TOPAZ4 is a …

We present a new brittle rheology and an accompanying numerical framework for large‐
scale sea‐ice modeling. This rheology is based on a Bingham‐Maxwell constitutive model …

As the sea‐ice modeling community is shifting to advanced numerical frameworks,
developing new sea‐ice rheologies, and increasing model spatial resolution, ubiquitous …

The Arctic marginal ice zone (MIZ), where strong interactions between sea ice, ocean and
atmosphere take place, is expanding as the result of ongoing sea ice retreat. Yet, state-of …