2020
DOI: 10.1038/s41586-020-2742-6
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Rate of mass loss from the Greenland Ice Sheet will exceed Holocene values this century

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Cited by 78 publications
(96 citation statements)
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“…17). In particular, north of the KNS region between Sisimiut and Kangerlussuaq, the simulated pattern and timing of icemargin migration generally reproduces the geologic record of ice-margin change (Briner et al, 2020). In the KNS region, these same simulations generally depict an ice-margin that retreats eastwards, achieves a minimum extent, and then readvances in the late Holocene, thus sharing the broad outline of GrIS change provided by the available geological observations (Fig.…”
Section: Geologic Data-model Comparison Of Ice-margin Change In Southsupporting
confidence: 67%
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“…17). In particular, north of the KNS region between Sisimiut and Kangerlussuaq, the simulated pattern and timing of icemargin migration generally reproduces the geologic record of ice-margin change (Briner et al, 2020). In the KNS region, these same simulations generally depict an ice-margin that retreats eastwards, achieves a minimum extent, and then readvances in the late Holocene, thus sharing the broad outline of GrIS change provided by the available geological observations (Fig.…”
Section: Geologic Data-model Comparison Of Ice-margin Change In Southsupporting
confidence: 67%
“…We utilize recent paleo-simulations of southwestern GrIS change using the high-resolution Ice Sheet and Sea-level System Model (ISSM; Larour et al, 2012;Cuzzone et al, 2018Cuzzone et al, , 2019Briner et al, 2020). The model set-up has been previously described in Cuzzone et al (2019) and Briner et al (2020), but here we briefly describe model attributes. The model domain extends from the present-day coastline to the GrIS divide.…”
Section: Ice-sheet Model Simulations Of Southwestern Gris Changementioning
confidence: 99%
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