The Arctic is warming nearly four times faster than the global average. Tundra that has been frozen since the last glacial maximum is greening, and the ice that defines the region is in retreat.
Norway’s marine boundary reaches from temperate fjords to the high Arctic. Within one country the atlas spans coastal woodland, alpine cryogenic systems and permanent ice.
Filtering to ice sheets, glaciers and perennial snowfields turns the map into a thermometer: every pixel here is a surface that either persists or does not, and the boundary moves each summer.
You cannot measure retreat without a starting line. Consistent global classification gives the Arctic something it has rarely had: one map, one method, repeated.