The balance between ice and water controls the habitability of an important
fraction of the globe and influences the majority of the world's populatio
n. The freezing of water to form ice is one of the most common phase transf
ormations in the natural environment. However, a complete understanding of
its microscopics and their influence on macroscopic phenomena still eludes
us. As this millennium comes to a close? we are beginning to understand how
the microscopic interfacial structure of ice controls pattern formation du
ring ice-crystal growth, the evolution of the polycrystalline fabrics of th
e great ice sheets, the dynamics of ground freezing, ozone destruction, and
the mechanism of charge transfer that drives thunderstorm electrification.
This paper describes our evolving understanding, its implications for the
basic principles of melting and freezing, and their environmental consequen
ces.