HIGHLIGHTS
SUMMARY
Two decades ago, the GrIS was considered to exist in a state of quasi-stability with its regional climate, but recent climatic warming trends have resulted in it becoming by far the largest contributor to global sea level rise (Hanna et_al, 2012; Van den Broeke et_al, 2016). Between 1992 and 2018, 3902 ± 342 Gt of ice was lost from the GrIS (Shepherd and IMBIE Team, 2020), but this has accelerated to an annual loss of 375 Gt per year of ice (on average) in the last decade (Enderlin et_al, 2014; Van den Broeke et_al . . .
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