The University Centre in Svalbard

Inner Tempelfjorden (TF) Mooring

Contact
Ragnheid Skogseth
Ragnheid.Skogseth@unis.no
Info
underwater platform (fixed)
Closed
No
Geospatial location
POINT (17.354483 78.44343)
-85.00
Observed Variable(s)
OCEANS>SALINITY/DENSITY>CONDUCTIVITY
Various instruments at different depth level with each yearly deployment. Refer to R. Skogseth, L.L.A. Olivier, F. Nilsen, E. Falck, N. Fraser, V. Tverberg, A.B. Ledang, A. Vader, M.O. Jonassen, J. Søreide, F. Cottier, J. Berge, B.V. Ivanov, S. Falk-Petersen (2020) Variability and decadal trends in the Isfjorden (Svalbard) ocean climate and circulation – An indicator for climate change in the European Arctic, Progress in Oceanography, Volume 187, https://doi.org/10.1016/j.pocean.2020.102394 and the supplementary data in Appendix A of this paper for full details of sensors and depths.
Mooring is collected and redeployed on an annual basis
Continuous measurement
OCEANS>SALINITY/DENSITY>DENSITY
Various instruments at different depth level with each yearly deployment. Refer to R. Skogseth, L.L.A. Olivier, F. Nilsen, E. Falck, N. Fraser, V. Tverberg, A.B. Ledang, A. Vader, M.O. Jonassen, J. Søreide, F. Cottier, J. Berge, B.V. Ivanov, S. Falk-Petersen (2020) Variability and decadal trends in the Isfjorden (Svalbard) ocean climate and circulation – An indicator for climate change in the European Arctic, Progress in Oceanography, Volume 187, https://doi.org/10.1016/j.pocean.2020.102394 and the supplementary data in Appendix A of this paper for full details of sensors and depths.
Mooring is collected and redeployed on an annual basis
Continuous measurement
OCEANS>SALINITY/DENSITY>SALINITY
Various instruments at different depth level with each yearly deployment. Refer to R. Skogseth, L.L.A. Olivier, F. Nilsen, E. Falck, N. Fraser, V. Tverberg, A.B. Ledang, A. Vader, M.O. Jonassen, J. Søreide, F. Cottier, J. Berge, B.V. Ivanov, S. Falk-Petersen (2020) Variability and decadal trends in the Isfjorden (Svalbard) ocean climate and circulation – An indicator for climate change in the European Arctic, Progress in Oceanography, Volume 187, https://doi.org/10.1016/j.pocean.2020.102394 and the supplementary data in Appendix A of this paper for full details of sensors and depths.
Mooring is collected and redeployed on an annual basis
Continuous measurement
OCEANS>OCEAN TEMPERATURE>WATER TEMPERATURE
Various instruments at different depth level with each yearly deployment. Refer to R. Skogseth, L.L.A. Olivier, F. Nilsen, E. Falck, N. Fraser, V. Tverberg, A.B. Ledang, A. Vader, M.O. Jonassen, J. Søreide, F. Cottier, J. Berge, B.V. Ivanov, S. Falk-Petersen (2020) Variability and decadal trends in the Isfjorden (Svalbard) ocean climate and circulation – An indicator for climate change in the European Arctic, Progress in Oceanography, Volume 187, https://doi.org/10.1016/j.pocean.2020.102394 and the supplementary data in Appendix A of this paper for full details of sensors and depths.
Mooring is collected and redeployed on an annual basis
Continuous measurement
OCEANS>OCEAN PRESSURE>WATER PRESSURE
Various instruments at different depth level with each yearly deployment. Refer to R. Skogseth, L.L.A. Olivier, F. Nilsen, E. Falck, N. Fraser, V. Tverberg, A.B. Ledang, A. Vader, M.O. Jonassen, J. Søreide, F. Cottier, J. Berge, B.V. Ivanov, S. Falk-Petersen (2020) Variability and decadal trends in the Isfjorden (Svalbard) ocean climate and circulation – An indicator for climate change in the European Arctic, Progress in Oceanography, Volume 187, https://doi.org/10.1016/j.pocean.2020.102394 and the supplementary data in Appendix A of this paper for full details of sensors and depths.
Mooring is collected and redeployed on an annual basis
Continuous measurement
OCEANS>OCEAN CIRCULATION>OCEAN CURRENTS
Various instruments at different depth level with each yearly deployment. Refer to R. Skogseth, L.L.A. Olivier, F. Nilsen, E. Falck, N. Fraser, V. Tverberg, A.B. Ledang, A. Vader, M.O. Jonassen, J. Søreide, F. Cottier, J. Berge, B.V. Ivanov, S. Falk-Petersen (2020) Variability and decadal trends in the Isfjorden (Svalbard) ocean climate and circulation – An indicator for climate change in the European Arctic, Progress in Oceanography, Volume 187, https://doi.org/10.1016/j.pocean.2020.102394 and the supplementary data in Appendix A of this paper for full details of sensors and depths.
Mooring is collected and redeployed on an annual basis
Continuous measurement

Isfjorden online mooring

Contact
Ragnheid Skogseth
Ragnheid.Skogseth@unis.no
Info
underwater platform (fixed)
Closed
No
Geospatial location
POINT (15.33116 78.247416)
-60.00
Observed Variable(s)
OCEANS>SALINITY/DENSITY>DENSITY
Various instruments at different depth level with each yearly deployment. Refer to R. Skogseth, L.L.A. Olivier, F. Nilsen, E. Falck, N. Fraser, V. Tverberg, A.B. Ledang, A. Vader, M.O. Jonassen, J. Søreide, F. Cottier, J. Berge, B.V. Ivanov, S. Falk-Petersen (2020) Variability and decadal trends in the Isfjorden (Svalbard) ocean climate and circulation – An indicator for climate change in the European Arctic, Progress in Oceanography, Volume 187, https://doi.org/10.1016/j.pocean.2020.102394 and the supplementary data in Appendix A of this paper for full details of sensors and depths.
Mooring is collected and redeployed on an annual basis
Continuous measurement
OCEANS>OCEAN CHEMISTRY>OXYGEN
Various instruments at different depth level with each yearly deployment. Refer to R. Skogseth, L.L.A. Olivier, F. Nilsen, E. Falck, N. Fraser, V. Tverberg, A.B. Ledang, A. Vader, M.O. Jonassen, J. Søreide, F. Cottier, J. Berge, B.V. Ivanov, S. Falk-Petersen (2020) Variability and decadal trends in the Isfjorden (Svalbard) ocean climate and circulation – An indicator for climate change in the European Arctic, Progress in Oceanography, Volume 187, https://doi.org/10.1016/j.pocean.2020.102394 and the supplementary data in Appendix A of this paper for full details of sensors and depths.
Mooring is collected and redeployed on an annual basis
Continuous measurement
OCEANS>OCEAN TEMPERATURE>WATER TEMPERATURE
Various instruments at different depth level with each yearly deployment. Refer to R. Skogseth, L.L.A. Olivier, F. Nilsen, E. Falck, N. Fraser, V. Tverberg, A.B. Ledang, A. Vader, M.O. Jonassen, J. Søreide, F. Cottier, J. Berge, B.V. Ivanov, S. Falk-Petersen (2020) Variability and decadal trends in the Isfjorden (Svalbard) ocean climate and circulation – An indicator for climate change in the European Arctic, Progress in Oceanography, Volume 187, https://doi.org/10.1016/j.pocean.2020.102394 and the supplementary data in Appendix A of this paper for full details of sensors and depths.
Mooring is collected and redeployed on an annual basis
Continuous measurement
OCEANS>OCEAN CIRCULATION>OCEAN CURRENTS
Various instruments at different depth level with each yearly deployment. Refer to R. Skogseth, L.L.A. Olivier, F. Nilsen, E. Falck, N. Fraser, V. Tverberg, A.B. Ledang, A. Vader, M.O. Jonassen, J. Søreide, F. Cottier, J. Berge, B.V. Ivanov, S. Falk-Petersen (2020) Variability and decadal trends in the Isfjorden (Svalbard) ocean climate and circulation – An indicator for climate change in the European Arctic, Progress in Oceanography, Volume 187, https://doi.org/10.1016/j.pocean.2020.102394 and the supplementary data in Appendix A of this paper for full details of sensors and depths.
Mooring is collected and redeployed on an annual basis
Continuous measurement

Isfjorden Mouth - North (I-N) Mooring

Contact
Ragnheid Skogseth
Ragnheid.Skogseth@unis.no
Info
underwater platform (fixed)
Closed
No
Geospatial location
POINT (13.38916 78.18185)
-226.00
Observed Variable(s)
OCEANS>SALINITY/DENSITY>CONDUCTIVITY
Various instruments at different depth level with each yearly deployment. Refer to R. Skogseth, L.L.A. Olivier, F. Nilsen, E. Falck, N. Fraser, V. Tverberg, A.B. Ledang, A. Vader, M.O. Jonassen, J. Søreide, F. Cottier, J. Berge, B.V. Ivanov, S. Falk-Petersen (2020) Variability and decadal trends in the Isfjorden (Svalbard) ocean climate and circulation – An indicator for climate change in the European Arctic, Progress in Oceanography, Volume 187, https://doi.org/10.1016/j.pocean.2020.102394 and the supplementary data in Appendix A of this paper for full details of sensors and depths.
Mooring is collected and redeployed on an annual basis
Continuous measurement
OCEANS>SALINITY/DENSITY>DENSITY
Various instruments at different depth level with each yearly deployment. Refer to R. Skogseth, L.L.A. Olivier, F. Nilsen, E. Falck, N. Fraser, V. Tverberg, A.B. Ledang, A. Vader, M.O. Jonassen, J. Søreide, F. Cottier, J. Berge, B.V. Ivanov, S. Falk-Petersen (2020) Variability and decadal trends in the Isfjorden (Svalbard) ocean climate and circulation – An indicator for climate change in the European Arctic, Progress in Oceanography, Volume 187, https://doi.org/10.1016/j.pocean.2020.102394 and the supplementary data in Appendix A of this paper for full details of sensors and depths.
Mooring is collected and redeployed on an annual basis
Continuous measurement
OCEANS>OCEAN CHEMISTRY>OXYGEN
Various instruments at different depth level with each yearly deployment. Refer to R. Skogseth, L.L.A. Olivier, F. Nilsen, E. Falck, N. Fraser, V. Tverberg, A.B. Ledang, A. Vader, M.O. Jonassen, J. Søreide, F. Cottier, J. Berge, B.V. Ivanov, S. Falk-Petersen (2020) Variability and decadal trends in the Isfjorden (Svalbard) ocean climate and circulation – An indicator for climate change in the European Arctic, Progress in Oceanography, Volume 187, https://doi.org/10.1016/j.pocean.2020.102394 and the supplementary data in Appendix A of this paper for full details of sensors and depths.
Mooring is collected and redeployed on an annual basis
Continuous measurement
OCEANS>OCEAN PRESSURE>WATER PRESSURE
Various instruments at different depth level with each yearly deployment. Refer to R. Skogseth, L.L.A. Olivier, F. Nilsen, E. Falck, N. Fraser, V. Tverberg, A.B. Ledang, A. Vader, M.O. Jonassen, J. Søreide, F. Cottier, J. Berge, B.V. Ivanov, S. Falk-Petersen (2020) Variability and decadal trends in the Isfjorden (Svalbard) ocean climate and circulation – An indicator for climate change in the European Arctic, Progress in Oceanography, Volume 187, https://doi.org/10.1016/j.pocean.2020.102394 and the supplementary data in Appendix A of this paper for full details of sensors and depths.
Mooring is collected and redeployed on an annual basis
Continuous measurement
OCEANS>SALINITY/DENSITY>SALINITY
Various instruments at different depth level with each yearly deployment. Refer to R. Skogseth, L.L.A. Olivier, F. Nilsen, E. Falck, N. Fraser, V. Tverberg, A.B. Ledang, A. Vader, M.O. Jonassen, J. Søreide, F. Cottier, J. Berge, B.V. Ivanov, S. Falk-Petersen (2020) Variability and decadal trends in the Isfjorden (Svalbard) ocean climate and circulation – An indicator for climate change in the European Arctic, Progress in Oceanography, Volume 187, https://doi.org/10.1016/j.pocean.2020.102394 and the supplementary data in Appendix A of this paper for full details of sensors and depths.
Mooring is collected and redeployed on an annual basis
Continuous measurement
OCEANS>OCEAN TEMPERATURE>WATER TEMPERATURE
Various instruments at different depth level with each yearly deployment. Refer to R. Skogseth, L.L.A. Olivier, F. Nilsen, E. Falck, N. Fraser, V. Tverberg, A.B. Ledang, A. Vader, M.O. Jonassen, J. Søreide, F. Cottier, J. Berge, B.V. Ivanov, S. Falk-Petersen (2020) Variability and decadal trends in the Isfjorden (Svalbard) ocean climate and circulation – An indicator for climate change in the European Arctic, Progress in Oceanography, Volume 187, https://doi.org/10.1016/j.pocean.2020.102394 and the supplementary data in Appendix A of this paper for full details of sensors and depths.
Mooring is collected and redeployed on an annual basis
Continuous measurement
OCEANS>OCEAN CIRCULATION>OCEAN CURRENTS
Various instruments at different depth level with each yearly deployment. Refer to R. Skogseth, L.L.A. Olivier, F. Nilsen, E. Falck, N. Fraser, V. Tverberg, A.B. Ledang, A. Vader, M.O. Jonassen, J. Søreide, F. Cottier, J. Berge, B.V. Ivanov, S. Falk-Petersen (2020) Variability and decadal trends in the Isfjorden (Svalbard) ocean climate and circulation – An indicator for climate change in the European Arctic, Progress in Oceanography, Volume 187, https://doi.org/10.1016/j.pocean.2020.102394 and the supplementary data in Appendix A of this paper for full details of sensors and depths.
Mooring is collected and redeployed on an annual basis
Continuous measurement

Isfjorden Mouth - South (I-S) Mooring

Contact
Ragnheid Skogseth
Ragnheid.Skogseth@unis.no
Info
underwater platform (fixed)
Closed
No
Geospatial location
POINT (13.52384 78.061)
-200.00
Observed Variable(s)
OCEANS>SALINITY/DENSITY>CONDUCTIVITY
Various instruments at different depth level with each yearly deployment. Refer to R. Skogseth, L.L.A. Olivier, F. Nilsen, E. Falck, N. Fraser, V. Tverberg, A.B. Ledang, A. Vader, M.O. Jonassen, J. Søreide, F. Cottier, J. Berge, B.V. Ivanov, S. Falk-Petersen (2020) Variability and decadal trends in the Isfjorden (Svalbard) ocean climate and circulation – An indicator for climate change in the European Arctic, Progress in Oceanography, Volume 187, https://doi.org/10.1016/j.pocean.2020.102394 and the supplementary data in Appendix A of this paper for full details of sensors and depths.
Mooring is collected and redeployed on an annual basis
Continuous measurement
OCEANS>SALINITY/DENSITY>SALINITY
Various instruments at different depth level with each yearly deployment. Refer to R. Skogseth, L.L.A. Olivier, F. Nilsen, E. Falck, N. Fraser, V. Tverberg, A.B. Ledang, A. Vader, M.O. Jonassen, J. Søreide, F. Cottier, J. Berge, B.V. Ivanov, S. Falk-Petersen (2020) Variability and decadal trends in the Isfjorden (Svalbard) ocean climate and circulation – An indicator for climate change in the European Arctic, Progress in Oceanography, Volume 187, https://doi.org/10.1016/j.pocean.2020.102394 and the supplementary data in Appendix A of this paper for full details of sensors and depths.
Mooring is collected and redeployed on an annual basis
Continuous measurement
OCEANS>SALINITY/DENSITY>DENSITY
Various instruments at different depth level with each yearly deployment. Refer to R. Skogseth, L.L.A. Olivier, F. Nilsen, E. Falck, N. Fraser, V. Tverberg, A.B. Ledang, A. Vader, M.O. Jonassen, J. Søreide, F. Cottier, J. Berge, B.V. Ivanov, S. Falk-Petersen (2020) Variability and decadal trends in the Isfjorden (Svalbard) ocean climate and circulation – An indicator for climate change in the European Arctic, Progress in Oceanography, Volume 187, https://doi.org/10.1016/j.pocean.2020.102394 and the supplementary data in Appendix A of this paper for full details of sensors and depths.
Mooring is collected and redeployed on an annual basis
Continuous measurement
OCEANS>OCEAN PRESSURE>WATER PRESSURE
Various instruments at different depth level with each yearly deployment. Refer to R. Skogseth, L.L.A. Olivier, F. Nilsen, E. Falck, N. Fraser, V. Tverberg, A.B. Ledang, A. Vader, M.O. Jonassen, J. Søreide, F. Cottier, J. Berge, B.V. Ivanov, S. Falk-Petersen (2020) Variability and decadal trends in the Isfjorden (Svalbard) ocean climate and circulation – An indicator for climate change in the European Arctic, Progress in Oceanography, Volume 187, https://doi.org/10.1016/j.pocean.2020.102394 and the supplementary data in Appendix A of this paper for full details of sensors and depths.
Mooring is collected and redeployed on an annual basis
Continuous measurement
OCEANS>OCEAN TEMPERATURE>WATER TEMPERATURE
Various instruments at different depth level with each yearly deployment. Refer to R. Skogseth, L.L.A. Olivier, F. Nilsen, E. Falck, N. Fraser, V. Tverberg, A.B. Ledang, A. Vader, M.O. Jonassen, J. Søreide, F. Cottier, J. Berge, B.V. Ivanov, S. Falk-Petersen (2020) Variability and decadal trends in the Isfjorden (Svalbard) ocean climate and circulation – An indicator for climate change in the European Arctic, Progress in Oceanography, Volume 187, https://doi.org/10.1016/j.pocean.2020.102394 and the supplementary data in Appendix A of this paper for full details of sensors and depths.
Mooring is collected and redeployed on an annual basis
Continuous measurement
OCEANS>OCEAN CIRCULATION>OCEAN CURRENTS
Various instruments at different depth level with each yearly deployment. Refer to R. Skogseth, L.L.A. Olivier, F. Nilsen, E. Falck, N. Fraser, V. Tverberg, A.B. Ledang, A. Vader, M.O. Jonassen, J. Søreide, F. Cottier, J. Berge, B.V. Ivanov, S. Falk-Petersen (2020) Variability and decadal trends in the Isfjorden (Svalbard) ocean climate and circulation – An indicator for climate change in the European Arctic, Progress in Oceanography, Volume 187, https://doi.org/10.1016/j.pocean.2020.102394 and the supplementary data in Appendix A of this paper for full details of sensors and depths.
Mooring is collected and redeployed on an annual basis
Continuous measurement

Svalbard SuperDARN Radar

Contact
Dag A. Lorentzen
dag.lorentzen@unis.no
Info
land platform (fixed)
Non-reporting
No
Observation Facility ID
11568
Geospatial location
POINT (16.066 78.1533)
433.00
Observed Variable(s)
SUN-EARTH INTERACTIONS>IONOSPHERE/MAGNETOSPHERE DYNAMICS>ELECTRIC FIELDS/ELECTRIC CURRENTS
Raw (Landed) parameters are:
Auto-correlation functions for the radar backscattered signal.
Analysed parameters are:
line-of-sight doppler velocity (m/s)
spectral width (m/s)
Backscatter power (dB)
Temporal Resolution: 1 minute
Spatial resoltuion: 45km

GTN-P Old Auroral Station PYRN

Contact
Hanne Hvidtfeldt Christiansen
hanne.christiansen@unis.no
Info
land platform (fixed)
Closed
No
Geospatial location
POINT (15.83465 78.20146)
7.00
Environment
The borehole is located 2m west of the midpoint of the resistivity monitoring profile. The westernmost line of the UNISCALM grid is located 12m east of the borehole. Drilled in loess deposit

Lithology: 0-1.2m: sand and some gravel; 1.2-3m: sand/silt/clay; 3-4m: clean ice (ice wedge or thick ice lens?); 4-6m: Mainly clay/silt; -10m: clay/silt, maybe some sand. Layered. Very low resistance during. Salinity at 10m is 11.8% (analysed by L.Hutchinson)
Observed Variable(s)
CRYOSPHERE>FROZEN GROUND>PERMAFROST>PERMAFROST TEMPERATURE
Temperature-time data series with measurements at 0.00, 0.25, 0.50, 0.75, 1.00, 2.00, 3.00, 5.00, 7.00, and 9.85 m depth.
Unit: Degree Celsius,
Frequency: Hourly,
Method: Thermistor Automated,
Medium: Soil,
Resolution: Irrelevant,
Quality Check: Raw Data,
Accuracy: 0.1°C

GTN-P Endalen PYRN

Contact
Hanne Hvidtfeldt Christiansen
hanne.christiansen@unis.no
Info
land platform (fixed)
Closed
No
Geospatial location
POINT (15.7816 78.1902)
40.00
Environment
Permafrost borehole in Endalen in Spitsbergen.

Lithology: 0-1.5m: Diamicton. High fraction of fine material and scattered blocks; 1.5-2m: Coarser material. Ice lenses (10-20cm); 2-4m: Diamicton with blocks and finer material (silt/clay). Some ice lenses (3-4cm thick); -5m: Diamicton. Drier than above from 4.5m; 5-6m: Transition to bedrock. Crushed zone; 6-20m: Bedrock. Solid from 7.7m.
Observed Variable(s)
CRYOSPHERE>FROZEN GROUND>PERMAFROST>PERMAFROST TEMPERATURE
Temperature-time data series with measurements at 0.00, 0.25, 0.50, 0.75, 1.00, 1.50, 2.00, 2.50, 3.00, 4.00, 5.00, 6.00, 7.00, 8.00, 9.00, 10.00, 12.00, 15.00, and 19.00 m depth.

Unit: Degree Celsius,
Frequency: 6 hours,
Method: Thermistor Automated,
Medium: Soil,
Resolution: Irrelevant,
Quality Check: Raw Data,
Accuracy: 0.1°C

GTN-P Kapp Linne 2

Contact
Hanne Hvidtfeldt Christiansen
hanne.christiansen@unis.no
Info
land platform (fixed)
Closed
No
Geospatial location
POINT (13.6366 78.0546)
20.00
Environment
Permafrost present but thickness not known.

Lithology: 0-2m: coarse (gravel) beach deposit (dry beach ridge); 2-4.8m: sand and clay, some occurrences of silt. Cohesive.; 4,8-6,2m: fine gravel; 6,2-7,8m: bedrock. light-coloured; 8-14,8m: dark-coloured; 14,8-15,8m: light-coloured; 8-38.8m: dark-coloured.
Observed Variable(s)
CRYOSPHERE>FROZEN GROUND>PERMAFROST>PERMAFROST TEMPERATURE
Temperature-time data series with measurements at 0.00, 0.25, 0.50, 0.75, 1.00, 1.50, 2.00, 2.50, 3.00, 4.00, 5.00, 6.00, 7.00, 8.00, 9.00, 10.00, 12.00, 15.00, 20.00, 25.00, 30.00, 35.00, and 38.00 m depth.

Unit: Degree Celsius,
Frequency: 6 hours,
Method: Thermistor Automated,
Medium: Soil,
Resolution: Irrelevant,
Quality Check: Raw Data,
Accuracy: 0.1°C

GTN-P Kapp Linne 1

Contact
Hanne Hvidtfeldt Christiansen
hanne.christiansen@unis.no
Info
land platform (fixed)
Operational
Yes
Geospatial location
POINT (13.6414 78.0566)
18.00
Environment
Permafrost borehole at the Kapp Linne in Spitsbergen.
Permafrost present but thickness not known.

The entire hole is through bedrock. Possible to dig down c. 30cm in weathered rock. 0-3.5m: soft (weathered?) 3.5-5m: harder 4.1m: slip zone 5-11.7m: softer 11.7-14m: harder 14-15m: layering (sample) 17-30m: softer

Lithology: The entire hole is through bedrock. Possible to dig down c. 30cm in weathered rock.0-3.5m: soft (weathered?); 3.5-5m: harder; 4.1m: slip zone; 5-11.7m: softer; 11.7-14m: harder; 14-15m: layering; 17-30m: softer
Observed Variable(s)
CRYOSPHERE>FROZEN GROUND>PERMAFROST>PERMAFROST TEMPERATURE
Temperature-time data series with measurements at 0.00, 0.25, 0.50, 0.75, 1.00, 1.50, 2.00, 2.50, 3.00, 4.00, 5.00, 6.00, 7.00, 8.00, 9.00, 10.00, 12.00, 15.00, 20.00, 25.00, and 29.00 m depth.

Unit: Degree Celsius,

Frequency: 6 hours

Method: Thermistor Automated
Medium: Soil
Resolution: Irrelevant
Policy: Open
Quality Check: Quality Controlled Data
Accuracy: 0.1°C

GTN-P Breinosa (E-2009)

Contact
Hanne Hvidtfeldt Christiansen
hanne.christiansen@unis.no
Info
land platform (fixed)
Closed
No
Geospatial location
POINT (16.0626 78.1416)
638.00
Environment
Permafrost borehole at the Breinosa in Spitsbergen.

Permafrost present but thickness unknown.

Lithology: 0-12m weathered material 10-12m: transition to bedrock.



Observed Variable(s)
CRYOSPHERE>FROZEN GROUND>PERMAFROST>PERMAFROST TEMPERATURE
Temperature-time data series with measurements at 0 m, 0.25 m, 0.5 m, 1 m, 2 m, 3 m, 4 m, 5 m, 7 m, and 10 m depth.

Unit: Degree Celsius,
Frequency: Hourly,
Method: Thermistor Automated,
Medium: Soil,
Resolution: Irrelevant,
Quality Check: Raw Data,
Accuracy: 0.2°C