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The impact of atmospheric mineral aerosol deposition on the albedo of snow and sea ice: are snow and sea ice optical properties more important than mineral aerosol optical properties?

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Table 1. Values of snow and sea ice used as input parameters for the TUV-snow model, based on literature values and detailed in the work of Marks and King (2014).
Figure 1. Complex refractive index (real and imaginary part) for mineral aerosol deposits as a function of wavelength
Figure 2. Absorption cross-section values based on Mie theory calculations undertaken here.
Figure 3. Wavelength dependant albedo of three semi-infinite snow and sea ice types con- con-taining 100 ng g −1 of di ff erent mineral aerosol deposits (Mt St Helens ash, Eyjafjallajökull ash, Saharan dust and Asian dust)
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