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. Author manuscript; available in PMC: 2010 Sep 1.
Published in final edited form as: Limnol Oceanogr. 2010 Mar;55(2):703–713. doi: 10.4319/lo.2009.55.2.0703

Fig. 7.

Fig. 7

Modeled UV : PAR irradiance ratios in the ice cover at different depths for various PM, CDOM, and ice conditions (same as in Fig. 5). Ratio is normalized to incident irradiance ratio at the air–snow (when snow present) or air–ice surface (when no snow); depth 0 cm corresponds to ice top surface (ratios inside snow cover are not shown).