HIGHLIGHTS
SUMMARY
Active subglacial hydrological networks have been revealed from changes in ice surface elevation detected by satellite altimetry and GPS (Willis et_al, 2015; Joughin et_al, 2016; Siegfried and Fricker, 2018; Neckel et_al, 2021; Livingstone et_al, 2022). Radio echo sounding has been used to identify subglacial lakes (Siegert et_al, 2005), and over-snow seismic surveys have been used to characterise their water column and sediment properties (Rivera et_al, 2015; Smith et_al, 2018). Much of this work has been carried out on large subglacial lakes under the East and West Antarctic ice sheets, while small lakes and . . .
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