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nature & planetEos

Airborne Imaging Explores a Mosaic of Thawing Permafrost

the gist

Permafrost, ground frozen year-round, covers vast areas of the Arctic and sub-Arctic, and as it thaws it releases greenhouse gases and damages roads and buildings. Because it lies underground, mapping it over wide areas is hard. A new approach flies an electromagnetic instrument over the land: frozen ground resists electric current far more than thawed ground, so measured resistivity reveals where permafrost is and how thick it is. Surveyed over Canada's Mackenzie Valley, it showed that thawed zones called taliks often sit beneath lakes and rivers and link up, letting water flow between them; one under the Mackenzie River was 2 km wide and over 75 m deep. Land burned by wildfire decades ago still has warmer permafrost near the surface.

how it works

Ice-rich frozen ground is a poor conductor of electricity, while thawed, water-bearing ground conducts well. An aircraft-mounted electromagnetic system induces currents in the ground and measures the response, which lets scientists map the boundary between frozen and unfrozen layers without digging.

so what

Knowing where permafrost is thick, thin or already thawing helps predict where ground will sink and where carbon may be released. Airborne surveys can cover areas that boreholes never could.

Eos (AGU) · CC BY-NC-ND 3.0