Direct Geologic Constraints on the Timing of Late Holocene Ice Thickening in the Amundsen Sea Embayment, Antarctica
Year: 2024
Type: article
Abstract: Constraining past West Antarctic Ice Sheet (WAIS) change helps validate numerical models simulating future ice sheet dynamics. Following rapid deglaciation during the mid‐Holocene, ice near Thwaites Glacier was ∼35 m thinner than present; however, the timing of ice regrowth to its present configuration remains unknown. To fill this knowledge gap, we present cosmogenic nuclide exposure ages of cobbles from the surface of a moraine situated between Thwaites and Pope glaciers. We infer that the moraine formed and stabilized in the Late Holocene (∼1.4 ka) when a small glacier thickened. We also present a novel reconstruction of WAIS volume constrained by sea‐level data, which demonstrates that moraine formation coincided with a large‐scale WAIS readvance. Our new geologic constraints will help inform models of the solid Earth response to surface mass loading, improving our understanding of ice sheet dynamics in a vulnerable part of WAIS.
Source: Geophysical Research Letters
DOI: 10.1029/2024gl110350
Language: English
Subfield: Atmospheric Science
Field: Earth and Planetary Sciences
Domain: Physical Sciences
SDG: Climate action
Open Access status: gold
Estimated APC paid: $2,900
Awards: G1104663396, G1173262082, G2143310323, G2810269120, G3061010496, Postdoctoral Fellowship: EAR-PF: Pairing on-and-offshore observations of paleo-ice streams to constrain and elucidate dynamics of the Cordilleran Ice Sheet (PISCES), G4399130109, Reconstructing millennial-scale ice sheet change in the western AmundsSea Embaymenten , Antarctica, using high-precision exposure dating., G4861057680, G5957514831, NSF-NERC: Geological History Constraints on the Magnitude of Grounding Line Retreat in the Thwaites Glacier System, G6253087171, G6283662192, NSFPLR-NERC: Geological history constraints on the magnitude of grounding line retreat in the Thwaites Glacier system, G672490221, G7106786466, Reconstructing millennial-scale ice sheet change in the western Amundsen Sea Embayment, Antarctica, using high-precision exposure dating., NSFPLR-NERC: Geological history constraints on the magnitude of grounding line retreat in the Thwaites Glacier system, G8989489056, G9000205966, G9000239457
OpenAlex ID: W4405577218
