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Earth Observing Laboratory
Field Data Archive

Soot Content of Snow and Ice [Grenfell, T.]

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Summary

The presence of particulates in the snow cover and at the ice surface can decrease the spectral albedo of the system at visible wavelengths where absorption by ice and water is small. Because of this, we were concerned that the release and local deposition of soot particles from fuel burned onboard the ship could impact both albedos and melt rates. For additional documentation, start with the soot.htm file contained in the zip file html-metadata.zip.

Data access

  • ORDER data to made available for download

Additional information

Identifier
Versions
  • 1.0 (2007-11-02)
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Spatial Type unknown
Frequency other
Language English
ISO Topic Categories
  • climatologyMeteorologyAtmosphere
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Temporal coverage

Begin datetime 1998-04-09 00:00:00
End datetime 1998-07-14 23:59:59

Spatial coverage


Map data from IBCSO, IBCAO, and Global Topography.

Maximum (North) Latitude: 80.00, Minimum (South) Latitude: 70.00
Minimum (West) Longitude: -170.00, Maximum (East) Longitude: -130.00

Primary point of contact information

EOL Data Support <datahelp@eol.ucar.edu>

Additional contact information

Citation

Grenfell, T., et al. 2007. Soot Content of Snow and Ice. Version 1.0. UCAR/NCAR - Earth Observing Laboratory. https://doi.org/10.5065/D62N50PZ. Accessed 19 Jan 2025.

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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.