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Long-term observations on the Bering Sea shelf: Sediment Trap Flux data from mooring site 2

Summary

Biophysical measurements have been made at mooring Site 2 (56.88N, 164.03W) almost continuously since 1995, providing the longest near continuous time-series of biophysical variables on the Bering Sea shelf. A series of moorings have also been deployed at Site 4 (57.85N, 168.87W) since 1995, providing almost six years of more sporadic data. In addition, another series of moorings have been deployed at Site 5 (59.90N, 171.70W) from 2004 to present. Added to the biophysical data collected by the moorings, water property measurements have been made at locations around the moorings and along the 70-m transect since 1995. Such long-term observations provide critical data that allow characterizations of interannual variability, quantification of regime shifts and climate change. This project partially funds continued measurements at Site 2 with water samples and plankton samples around the mooring site and along the monitoring line.

Data access

  • ORDER data for delivery by FTP

Additional information

Identifier
Versions
  • 1.0 (2011-09-13)
Related projects
Spatial Type point
Frequency hourly
Language English
ISO Topic Categories
  • oceans
Categories
Platforms
Instruments
GCMD Science Keywords Expand keywords
Documentation
Related links

Temporal coverage

Begin datetime 2009-03-05 00:00:00
End datetime 2009-09-26 23:59:59

Spatial coverage


Map data from IBCSO, IBCAO, and Global Topography.

Maximum (North) Latitude: 63.00, Minimum (South) Latitude: 52.00
Minimum (West) Longitude: -179.00, Maximum (East) Longitude: -157.00

Primary point of contact information

Phyllis J. Stabeno <phyllis.stabeno@noaa.gov>

Additional contact information

Citation

Example citation following ESIP guidelines:

Stabeno, P., Napp, J., Whitledge, T. 2011. Long-term observations on the Bering Sea shelf: Sediment Trap Flux data from mooring site 2. Version 1.0. UCAR/NCAR - Earth Observing Laboratory. https://doi.org/10.5065/D6R78C6F. Accessed 27 Jan 2020.

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