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This PR changes the default namelist option for snow grain shape for all configurations to
hexagonal_plate, which is used by the SNICAR-ADv3 model to scatter light. Thus, this
option has an appreciable impact on albedo in snow-covered regions. The current default
is sphere, thus this change increases albedo in snow-covered regions (aspect ratio of
snow grains increases from 1 to 2.5).
This change is motivated by a significant albedo bias over polar ice sheets and a related
summertime warm surface air temperature bias.
This change is supported by hexagonal_plate being the default in CLM5.
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