Simulating the effect of subsurface drainage on the thermal regime and ground ice in blocky terrain in Norway
<p>Ground temperatures in coarse, blocky deposits such as mountain blockfields and rock glaciers have long been observed to be lower in comparison with other (sub)surface material. One of the reasons for this negative temperature anomaly is the lower soil moisture content in blocky terrain, wh...
Main Authors: | C. Renette, K. Aalstad, J. Aga, R. B. Zweigel, B. Etzelmüller, K. S. Lilleøren, K. Isaksen, S. Westermann |
---|---|
Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2023-01-01
|
Series: | Earth Surface Dynamics |
Online Access: | https://esurf.copernicus.org/articles/11/33/2023/esurf-11-33-2023.pdf |
Similar Items
-
Post-Little Ice Age rock wall permafrost evolution in Norway
by: J. Czekirda, et al.
Published: (2023-07-01) -
The CryoGrid community model (version 1.0) – a multi-physics toolbox for climate-driven simulations in the terrestrial cryosphere
by: S. Westermann, et al.
Published: (2023-05-01) -
Rapid warming and degradation of mountain permafrost in Norway and Iceland
by: B. Etzelmüller, et al.
Published: (2023-12-01) -
Transient thermal modeling of permafrost conditions in Southern Norway
by: S. Westermann, et al.
Published: (2013-04-01) -
Transitional rock glaciers at sea level in northern Norway
by: K. S. Lilleøren, et al.
Published: (2022-10-01)