Ice — Pie Models

The core foundational model. It remains completely frozen and unchangeable.

In nature, these are most commonly observed as —circular discs of ice that form in turbulent, supercooled ocean waters, particularly in the Southern Ocean around Antarctica and in the Arctic's marginal ice zones. Unlike continuous ice sheets, pancake ice consists of discrete, rounded floes that collide and raft over one another. Ice pie models mathematically describe how these individual discs nucleate, grow radially, thicken, and eventually fuse into a solid ice cover. ice pie models