Cryo‐hydrologic warming: A potential mechanism for rapid thermal response of ice sheets

188 citations recorded by the source corpus.

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

Calving on tidewater glaciers amplified by submarine frontal melting (2012, background): “Although mechanisms have been suggested by which the hydrological system of a glacier could result in near-isothermal conditions (Phillips et al., 2010), this has not been widely observed in the field.”
Projecting twenty-first century regional sea-level changes (2014, background): “Main mechanisms on Greenland are calving and melt of marine-terminating glaciers (e.g., Nick et al. 2013), meltwater percolation to the bedrock (e.g., Phillips et al. 2010), and ice flow-SMB feedback (e.g., Goelzer et al. 2013).”
Contribution of Antarctica to past and future sea-level rise (2016, unknown): “If refreezing occurs, the ice is warmed, reducing its viscosity and speeding its flow 22 .”