English
 
Privacy Policy Disclaimer
  Advanced SearchBrowse

Item

ITEM ACTIONSEXPORT

Released

Data Publication

Subaquatic ambient seismic noise recordings acquired in the region of Inuvik and Tuktoyaktuk, Northwest Territories, Canada

Authors
/persons/resource/trond

Ryberg,  T.
2.2 Geophysical Imaging of the Subsurface, 2.0 Geophysics, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;
Publikationen aller GIPP-unterstützten Projekte, Deutsches GeoForschungsZentrum;

/persons/resource/haber

Haberland,  C.
2.2 Geophysical Imaging of the Subsurface, 2.0 Geophysics, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;
Publikationen aller GIPP-unterstützten Projekte, Deutsches GeoForschungsZentrum;

Overduin,  Paul
Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Potsdam, Germany;
Publikationen aller GIPP-unterstützten Projekte, Deutsches GeoForschungsZentrum;

Cable,  William
Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Potsdam, Germany;
Publikationen aller GIPP-unterstützten Projekte, Deutsches GeoForschungsZentrum;

External Ressource
Fulltext (public)
There are no public fulltexts stored in GFZpublic
Supplementary Material (public)
There is no public supplementary material available
Citation

Ryberg, T., Haberland, C., Overduin, P., Cable, W. (2022): Subaquatic ambient seismic noise recordings acquired in the region of Inuvik and Tuktoyaktuk, Northwest Territories, Canada.
https://doi.org/10.5880/GIPP.202199.1


Cite as: https://gfzpublic.gfz-potsdam.de/pubman/item/item_5012173
Abstract
This dataset contains subaquatic passive seismic recordings taken in September 2021 at 88 locations off Tuktoyaktuk Island as well as in a small lake (“Lake 3”) between the villages of Tuktoyaktuk and Inuvik, Northwest Territories, Canada. The measurements were part of the “Mackenzie Delta Permafrost Field Campaign” (mCan2021) within the “Modular Observation solutions for Earth Systems” (MOSES) program. Data is from a seismic intermediate-bandwidth seismic sensor lowered for few minutes to the bottom of the sea and lake, respectively, and from underwater short-period sensors deployed for a few days. The aim of the study was to determine the depth of the subaquatic permafrost (local lake and oceanic locations). Raw data is provided in proprietary “Cube” format and standard mseed format.