Snow depth obtained from SMOS over thick sea ice might be an important contribution here.
The standard deviation in
snow depth obtained in cross-checking and duplicate measurements are smallest for crevasse stratigraphy, +0.02 m, and +0.03 m for probing.
The standard deviation in
snow depth obtained in cross checking and duplicate measurments are smallest for crevasse stratigraphy, 0.02 m, and 0.03 m for probing.