‘Disposable’ distributed temperature sensing (DTS) is a happening thing in Greenland. From Scott Tyler of @unevadareno at #AGU24
Hydrophones can.. almost.. measure submarine melting. From Hayden Johnson of @Scripps_Ocean at #AGU24
You can map iceberg shape (below the water) from airplanes. Oooohlala. From Lilly Hinkley of @WoosterEdu at #AGU24
Subglacial sediments migrate UP into temperate ice. From Ethan Pierce of @CUBoulder @INSTAAR at #AGU24
Vibroseis + radar = magical for understanding the bed of Thwaites glacier. From Coen Hofstede at @AWI_Media at #AGU23
Theory says that meltwater produced in shear margins of Antarctic ice streams may be of similar magnitude to other melt sources. From @meghana_ir of @GeorgiaTech, presented by @MITglaciology
...also Antarctica is weird. From @MITglaciology quoting Slawek Tulaczyk.
Estuaries on ice shelves are a THING. From Alex Boghosian of @LamontEarth at #AGU22
Measurements show that firn compaction rates vary on seasonal (and shorter!) timescales. From Max Stevens of @NASAGoddard at #AGU2021 @AGU_Cryo
Greenland glaciers: doing strange things since 2015. From Mal McMillan of @LancasterUni at #AGU2021 @AGU_Cryo
Pine Island Bay blooms are in part fertilized by iron from seafloor volcanic glass. From Lisa Herbert of @RutgersU at #WAISworkshop
Melange backstress might put a halt on Marine Ice Cliff Instablilty. From @crawfisha of @StAndrewsGlacio at #WAISworkshop
ROV @IcefinRobot sees strong stratification, high heat content, grounding line bedforms, and huge crevasses at the Thwaites grounding zone. From Peter Washam and Britney Schmidt of @CornellEAS at #WAISworkshop
Strong positive feedbacks in ice shelf melt might not be quite so simple. From @MoormanRuth of @Caltech at #WAISworkshop
CryoSat-2 shows linked draining and filling of subglacial lakes on Lambert Glacier, East Antarctica. From Anna Hogg of @SEELeeds at #vEGU21 #vEGU21_CR




















