01 / The annual thermal wave

Follow a year through the ground.

Air and surface temperatures change quickly. Deeper in soil, ice and rock, the annual signal becomes smaller and arrives later. A sensor string records these layers simultaneously, turning a borehole into a continuous temperature profile.

One time base

All measuring points are read through one digital 2Wire string, making depth-to-depth comparison straightforward.

Dense where needed

Choose closer spacing around the surface and active layer, then wider intervals deeper in the borehole.

Calibration at the node

Each digital measuring point retains its calibration data, even when the connected logger is exchanged.

Modelled warm- and cold-season temperature profiles from the surface to 19 metres depth
Modelled temperature profiles versus depth in Northeast Greenland.

02 / Depth profile

Surface extremes fade with depth.

The published profiles illustrate why a single surface sensor cannot describe a permafrost system: near-surface temperatures span a broad range, while deeper profiles converge toward a much narrower thermal regime.

Repeated measurements at fixed depths reveal active-layer behaviour, freeze–thaw timing and long-term changes below the zone of strong annual variation.

Research example: Rasmussen et al., “Modelling present and future permafrost thermal regimes in Northeast Greenland”, Cold Regions Science and Technology 146 (2018), 199–213.

03 / Field interpretation

Temperature links seasons to ground movement.

At a permafrost-affected rockslide in northern Norway, multi-depth temperature records helped researchers interpret seasonal processes in fractures and develop a field-based deformation model.

Annual air, ice and rock temperature time series at several monitoring depths
Different media, different signals. Air, ice and rock temperatures at several depths respond differently through the year.
Temperature profiles at three elevations and annual borehole temperatures from zero to 227 centimetres depth
Amplitude and delay by depth. The annual borehole record shows how the surface signal is damped and shifted below ground.

Research examples: Blikra & Christiansen, “A field-based model of permafrost-controlled rockslide deformation in northern Norway”, Geomorphology 208 (2014), 34–49. These published figures illustrate the application; they are not presented as GEOprecision measurement results.

04 / Configure the profile

Put precision at the depths that matter.

Sensor positions, node type, cable length, mechanical construction and readout are selected for the borehole and research question—not imposed by a fixed catalogue layout.

Custom spacing

Standard sensor spacing starts at 15 cm; 10 cm is possible at the first interval.

Resolution options

Choose TNode, TNode EX or TNode HD, with resolution down to 0.0001 °C.

Long profiles

Strings are available up to 100 m as standard and 250 m or more on request.

Compare sensor specifications Configure a permafrost string