ARCTIC SYSTEMSIllustrative example

Two zones. One cold ground.

How does uneven heating affect frozen ground? Two zones supply different amounts of heat, creating an asymmetric warming pattern beneath a schematic building.

Final temperature field at day 180, with greater warming beneath the higher heat-input zone.

Illustrative simulation with assumed heat inputs. The ground remains frozen; the lines show temperatures, not thaw fronts. Not a site prediction.

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