Scientific Colloquium
April 30, 2004
Sorted circles, meter scale
patterns consisting of circular soil domains surrounded by raised
annular stone domains, are found in Arctic and high alpine environments
in which the uppermost layer of soil (the active layer) experiences
cyclic freezing and thawing. These patterns exhibit a striking
circular plan form, a convex upward soil domain surface on which motion
is outward from the center, and tilt in the subsurface consistent with
circulation. Sorted circles are just one of the many incredible sorted
patterns found in these environments, including: polygons, labyrinths,
islands and stripes. Additionally, sorted patterns are a small
subset of the diverse range of patterns found in cold climates,
including: earth hummocks, palsas, pingos, ice wedge networks,
etc. Less obstructed by the biological agents that dominate
temperate climates, cold environments team with self-organized
patterns. Frost heave, soil expansion by water migration during
freezing, is the prime mover in the active layer, but what organizes
that motion? Sorted patterns can be understood in terms of
self-organization owing to a few simple feedbacks between the transport
processes that modify and the morphology that continually directs the
evolution of the pattern.