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SUMMARY:Icy flows with freezing and melting - Kasia Warburton\, DAMTP
DTSTART:20260211T140000Z
DTEND:20260211T150000Z
UID:TALK243904@talks.cam.ac.uk
CONTACT:Anna Walczyk
DESCRIPTION:Liquid water on top and beneath ice sheets flows through porou
 s networks whose permeability evolves due to freezing or melting induced b
 y the water flow itself. When freezing occurs\, any water infiltration can
  be self-limiting\, for example leading to the formation of internal solid
  ice structures within snowpack. Where flow leads to melt\, positive feedb
 ack leads to patterning\, generating large thawed channels. I'll describe 
 some examples of these systems\, efforts to model them\, and their relevan
 ce in understanding the future evolution of ice sheets.
LOCATION:LT6
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