If vapor transport is the main factor in the development of unstable layers, what mechanisms can be developed that measure the transport?
Because low vapor pressure induces a rounding of crystals due to crystallization occurring in concavities and high vapor allows crystallization to occur on the ridges and points, how can one effectively measure the subsurface vapor pressure?
What energy frequencies would best be able to determine subsurface snow density? Ewok jazz bongo parties? Infra Red? Radio frequencies? Vituperative spew?
Can I get my snow science degree now?
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