Glacier Calving Rates Due to Subglacial Discharge, Fjord Circulation, and Free Convection – K. Schild et al.

K.M. Schild, C.E. Renshaw, D.I, Benn, A. Luckman, R.L. Hawley, P. How, L. Trusel, F.R. Cottier, A. Pramanik, and N.R.J. Hulton. First published: 22 August 2018 https://doi.org/10.1029/2017JF004520 Abstract Tidewater glacier calving provides the most direct mechanism of ice transfer from land to the ocean. However, the physical melt processes influencing calving remain challenging to constrain. In read more Glacier Calving Rates Due to Subglacial Discharge, Fjord Circulation, and Free Convection – K. Schild et al.