Permafrost beneath Arctic communities is highly sensitive to surface heat and moisture. Geophysics at four Utqiaġvik (Alaska) sites shows that infrastructure – buildings, roads, snow fences – reshapes snow and drainage, redirecting heat and water. Thaw deepens near disturbed ground, while undisturbed, vegetated terrain stays shallower or heaves. Local land use and surface conditions can outweigh regional climate signals, guiding design, maintenance, and risk planning for Arctic infrastructure.