Quick report
In the cold sink below 10,000’, the transition from a dry, cohesionless snowpack (all F hard facets topped by large surface hoar) to a crust occurred at the E/SE boundary. Facet sluffing is still insignificant.
In the cold sink below 10,000’, the transition from a dry, cohesionless snowpack (all F hard facets topped by large surface hoar) to a crust occurred at the E/SE boundary. Facet sluffing is still insignificant.