Spectral Albedo [Grenfell, T., and B. Light]
As part of ice-albedo feedback studies during SHEBA, we measured spectral and wavelength-integrated albedos. Measurements were made at least weekly every 2.5 m along a 200-m survey line from April through October. Initially this line was completely snowcovered, but as the melt season progressed it became a mixture of bare ice and melt ponds. Observed changes in albedo were a combination of a gradual evolution due to seasonal transitions and abrupt shifts resulting from synoptic weather events. Surface conditions evolved from dry snow (April-May) to melting snow (June 3) to early melt ponds (mid-late June) to fully developed melt ponds (July-August). From June through August albedo measurements were made every other day. For additional documentation, start with the spectalb.htm file contained in the zip file html-metadata.zip.
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|Begin datetime||1998-04-08 00:00:00|
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Map data from IBCSO, IBCAO, and Global Topography.
Maximum (North) Latitude:
Minimum (South) Latitude:
Minimum (West) Longitude: -170.00, Maximum (East) Longitude: -130.00
Additional contact information
- author: Thomas C. Grenfell <email@example.com>
- author: Bonnie Light <firstname.lastname@example.org>
- principalInvestigator: Donald Perovich <email@example.com>
CitationExample citation following ESIP guidelines:
Grenfell, T., Light, B. 2007. Spectral Albedo. Version 1.0. UCAR/NCAR - Earth Observing Laboratory. https://doi.org/10.5065/D6765CQ1. Accessed 14 Jul 2020.
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