5) and deformed ice (R > 6). The mean draft difference between measurements and isostasy suggests 70 m as an isostatic length scale for level ice. The isostatic scale for deformed ice appears to be longer than accessible with these data (>300 m). Copyright 2011 by the American Geophysical Union.
CITATION STYLE
Doble, M. J., Skourup, H., Wadhams, P., & Geiger, C. A. (2011). The relation between Arctic sea ice surface elevation and draft: A case study using coincident AUV sonar and airborne scanning laser. Journal of Geophysical Research: Oceans, 116(11). https://doi.org/10.1029/2011JC007076
Mendeley helps you to discover research relevant for your work.