Evolution of the microstructure and reflectance of the surface scattering layer on melting, level Arctic sea ice
The microstructure of the uppermost portions of a melting Arctic sea ice cover has a disproportionately large influence on how incident sunlight is reflected and absorbed in the ice/ocean system. The surface scattering layer (SSL) effectively backscatters solar radiation and keeps the surface albedo...
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Published in | Elementa (Washington, D.C.) Vol. 11; no. 1 |
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Main Authors | , , , , , , , , , |
Format | Journal Article |
Language | English |
Published |
06.04.2023
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Online Access | Get full text |
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