Refinement of the ice absorption spectrum in the visible using radiance profile measurements in Antarctic snow
Ice is a highly transparent material in the visible. According to the most widely used database (IA2008; Warren and Brandt, 2008), the ice absorption coefficient reaches values lower than 10<sup>−3</sup> m<sup>−1</sup> around 400 nm. These values were obta...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2016-11-01
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| Series: | The Cryosphere |
| Online Access: | http://www.the-cryosphere.net/10/2655/2016/tc-10-2655-2016.pdf |