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Figure 6. Error in diffuse snow albedo computed using two-stream models, for various snow depths and snow grain radii, with solar zenith angle of 60° at the top of the atmosphere.
Reference: Dang, C., Zender, C. S., and Flanner, M. G.: Inter-comparison and improvement of 2-stream shortwave radiative transfer models for unified treatment of cryospheric surfaces in ESMs, The Cryosphere Discuss., https://doi.org/10.5194/tc-2019-22, in review, 2019.
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