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Earth Observing Laboratory
Field Data Archive

Svalbard Fjord Conductivity, Temperature, Depth Data, 2001-2004

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Summary

This data set includes vertical ocean profiles of temperature, salinity and backscatter beneath ice cover in Svalbard Fjord, Norway. The data were collected by a Seabird Conductivity, Temperature, Depth (CTD) system mounted on a remotely operated vehicle (ROV) on three trips: the north side of Van Mijenfjorden in March 2001; the south of Van Mijenfjorden in March 2004; the south of Van Mijenfjorden in June 2004. To address the differences between theory and observation regarding the rate of ice formation, supercooling in the ocean boundary layer, and the effective diffusivities of heat and salt, the small-scale physics of sea ice formation were studied. This data set is available as tab-delimited ASCII text files.

Data access

Additional information

Identifier
Versions
  • 1.0 (2011-09-14)
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Related projects
Spatial Type point
Frequency continuous
Language English
Grant Code OPP-0082687
ISO Topic Categories
  • oceans
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Platforms
Instruments
GCMD Science Keywords Expand keywords
Documentation
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Temporal coverage

Begin datetime 2001-03-07 00:00:00
End datetime 2004-06-11 23:59:59

Spatial coverage


Map data from IBCSO, IBCAO, and Global Topography.

Maximum (North) Latitude: 77.75, Minimum (South) Latitude: 75.75
Minimum (West) Longitude: 14.96, Maximum (East) Longitude: 14.98

Primary point of contact information

James H. (Jamie) Morison <morison@apl.washington.edu>

Additional contact information

Citation

Morison, J., Wettlaufer, J. 2011. Svalbard Fjord Conductivity, Temperature, Depth Data, 2001-2004. Version 1.0. UCAR/NCAR - Earth Observing Laboratory. https://doi.org/10.5065/D6G73BTQ. Accessed 25 Dec 2024.

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NSF

This material is based upon work supported by the NSF National Center for Atmospheric Research, a major facility sponsored by the U.S. National Science Foundation and managed by the University Corporation for Atmospheric Research. Any opinions, findings and conclusions or recommendations expressed in this material do not necessarily reflect the views of the U.S. National Science Foundation.