Comparison of Simulated 2D Temperature Profiles with Time-Lapse Electrical Resistivity Data at the Schilthorn Crest, Switzerland
The Schilthorn Crest in the Bernese Alps, Switzerland, is a prominent permafrost research site. Topographic and transient effects influence the temperature field below the east-west oriented crest. Measured T(z)-profiles in boreholes, however, do not provide sufficient information for a comprehensiv...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.525.3684 2023-05-15T17:56:16+02:00 Comparison of Simulated 2D Temperature Profiles with Time-Lapse Electrical Resistivity Data at the Schilthorn Crest, Switzerland Jeannette Noetzli Christin Hilbich Christian Hauck Martin Hoelzle Stephan Gruber The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.525.3684 http://www.geo.unizh.ch/~jnoetzli/downloads/Noetzli2008_Schilthorn.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.525.3684 http://www.geo.unizh.ch/~jnoetzli/downloads/Noetzli2008_Schilthorn.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.geo.unizh.ch/~jnoetzli/downloads/Noetzli2008_Schilthorn.pdf alpine permafrost distribution electrical resistivity thermal modeling text ftciteseerx 2016-01-08T10:19:55Z The Schilthorn Crest in the Bernese Alps, Switzerland, is a prominent permafrost research site. Topographic and transient effects influence the temperature field below the east-west oriented crest. Measured T(z)-profiles in boreholes, however, do not provide sufficient information for a comprehensive description of the subsurface temperature distribution. We combine ground temperature measurements, electric resistivity tomography (ERT) monitoring, and numerical modeling to investigate the 3-dimensional thermal regime below the crest. The modeled temperature field of a north-south oriented cross section agrees well with ERT results along the same profile. The simulated thermal regime below the Schilthorn is characterized by generally warm permafrost, with the coldest zone below the upper part of the north-facing slope, and permafrost a little below the surface on the south-facing slope. The combination of temperature modeling and measurements and geophysical monitoring bears potential to improve simulation and validation strategies. Text permafrost Unknown Crest The ENVELOPE(-56.992,-56.992,-63.406,-63.406) |
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English |
topic |
alpine permafrost distribution electrical resistivity thermal modeling |
spellingShingle |
alpine permafrost distribution electrical resistivity thermal modeling Jeannette Noetzli Christin Hilbich Christian Hauck Martin Hoelzle Stephan Gruber Comparison of Simulated 2D Temperature Profiles with Time-Lapse Electrical Resistivity Data at the Schilthorn Crest, Switzerland |
topic_facet |
alpine permafrost distribution electrical resistivity thermal modeling |
description |
The Schilthorn Crest in the Bernese Alps, Switzerland, is a prominent permafrost research site. Topographic and transient effects influence the temperature field below the east-west oriented crest. Measured T(z)-profiles in boreholes, however, do not provide sufficient information for a comprehensive description of the subsurface temperature distribution. We combine ground temperature measurements, electric resistivity tomography (ERT) monitoring, and numerical modeling to investigate the 3-dimensional thermal regime below the crest. The modeled temperature field of a north-south oriented cross section agrees well with ERT results along the same profile. The simulated thermal regime below the Schilthorn is characterized by generally warm permafrost, with the coldest zone below the upper part of the north-facing slope, and permafrost a little below the surface on the south-facing slope. The combination of temperature modeling and measurements and geophysical monitoring bears potential to improve simulation and validation strategies. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Jeannette Noetzli Christin Hilbich Christian Hauck Martin Hoelzle Stephan Gruber |
author_facet |
Jeannette Noetzli Christin Hilbich Christian Hauck Martin Hoelzle Stephan Gruber |
author_sort |
Jeannette Noetzli |
title |
Comparison of Simulated 2D Temperature Profiles with Time-Lapse Electrical Resistivity Data at the Schilthorn Crest, Switzerland |
title_short |
Comparison of Simulated 2D Temperature Profiles with Time-Lapse Electrical Resistivity Data at the Schilthorn Crest, Switzerland |
title_full |
Comparison of Simulated 2D Temperature Profiles with Time-Lapse Electrical Resistivity Data at the Schilthorn Crest, Switzerland |
title_fullStr |
Comparison of Simulated 2D Temperature Profiles with Time-Lapse Electrical Resistivity Data at the Schilthorn Crest, Switzerland |
title_full_unstemmed |
Comparison of Simulated 2D Temperature Profiles with Time-Lapse Electrical Resistivity Data at the Schilthorn Crest, Switzerland |
title_sort |
comparison of simulated 2d temperature profiles with time-lapse electrical resistivity data at the schilthorn crest, switzerland |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.525.3684 http://www.geo.unizh.ch/~jnoetzli/downloads/Noetzli2008_Schilthorn.pdf |
long_lat |
ENVELOPE(-56.992,-56.992,-63.406,-63.406) |
geographic |
Crest The |
geographic_facet |
Crest The |
genre |
permafrost |
genre_facet |
permafrost |
op_source |
http://www.geo.unizh.ch/~jnoetzli/downloads/Noetzli2008_Schilthorn.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.525.3684 http://www.geo.unizh.ch/~jnoetzli/downloads/Noetzli2008_Schilthorn.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766164395754258432 |