Estimation of ice shelf melt rate in the presence of a thermohaline staircase
1 January, 2015 by Emily Venables, Keith Nicholls, Satoshi Kimura
Diffusive convection–favorable thermohaline staircases are observed directly beneath George VI Ice Shelf, Antarctica. A thermohaline staircase is one of the most pronounced manifestations of double-diffusive convection. Cooling and freshening of…Read more on Estimation of ice shelf melt rate in the presence of a thermohaline staircase