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Reduced driving stress upstream of bumps can stabilize grounding zones on otherwise unstable reverse bed slopes. From Alex Robel of Georgia Tech at #WAIS2020

Hey CDW, can you guess which ice shelves are retreating and which are advancing? From Julia Andreasen of Soil, Water, & Climate at #WAIS2020

Optical methods under-predict supraglacial lake depth, but ICESat-2 is here to save the day. From Philipp Arndt of Scripps Institution of Oceanography at #WAIS2020

CryoSat-2 shows linked draining and filling of subglacial lakes on Lambert Glacier, East Antarctica. From Anna Hogg of Earth and Environment at Leeds at #vEGU21 #vEGU21_CR

Time does heal all (faults). From Grace Barcheck of Cornell Earth and Atmospheric Sciences at #WAISworkshop

Strong positive feedbacks in ice shelf melt might not be quite so simple. From @MoormanRuth of Caltech at #WAISworkshop

ROV Icefin sees strong stratification, high heat content, grounding line bedforms, and huge crevasses at the Thwaites grounding zone. From Peter Washam and Britney Schmidt of Cornell Earth and Atmospheric Sciences at #WAISworkshop

Melange backstress might put a halt on Marine Ice Cliff Instablilty. From @crawfisha of StAndrews Glaciology at #WAISworkshop

Pine Island Bay blooms are in part fertilized by iron from seafloor volcanic glass. From Lisa Herbert of Rutgers University at #WAISworkshop

Greenland glaciers: doing strange things since 2015. From Mal McMillan of Lancaster University at #AGU2021 AGU Cryosphere

Meltwater can infiltrate and refreeze even where surface ice slabs exist at the surface. From Riley Culberg of SU Radio Glaciology Stanford University at #AGU2021 AGU Cryosphere

The Siple Coast grounding line was was inland of present at 6,000 years ago. From Dr. Ryan Venturelli of Tulane University at #AGU2021 AGU Cryosphere

Measurements show that firn compaction rates vary on seasonal (and shorter!) timescales. From Max Stevens of NASA Goddard at #AGU2021 AGU Cryosphere

Estuaries on ice shelves are a THING. From Alex Boghosian of LDEO at #AGU22

Warm water exists at depth around east Antarctica. From Y.Nakayama | 南極の海/氷の研究者 | Polar Oceanographer of Hokkaido University at #AGU22

Vibroseis + radar = magical for understanding the bed of Thwaites glacier. From Coen Hofstede at AWI Media at #AGU23