adiative transfer scheme 
(<A
 HREF="node40.html#Briegleb07">Briegleb and Light(2007)</A>), the base albedos are computed based on the inherent 
optical properties of snow, sea ice, and melt ponds. These albedos are 
tunable through adjustments to the snow grain radius, <TT>R_snw</TT>, 
temperature to transition to melting snow, and maximum snow grain radius.

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  <A NAME="ice_nml"></A>  <A NAME="477"></A>
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<CAPTION><STRONG>Table:</