A reconciled solution of Meltwater Pulse 1A sources using sea-level fingerprinting
Yucheng Lin (),
Fiona D. Hibbert,
Pippa L. Whitehouse,
Sarah A. Woodroffe,
Anthony Purcell,
Ian Shennan and
Sarah L. Bradley
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Yucheng Lin: Durham University
Fiona D. Hibbert: Australian National University
Pippa L. Whitehouse: Durham University
Sarah A. Woodroffe: Durham University
Anthony Purcell: Australian National University
Ian Shennan: Durham University
Sarah L. Bradley: The University of Sheffield
Nature Communications, 2021, vol. 12, issue 1, 1-11
Abstract:
Abstract The most rapid global sea-level rise event of the last deglaciation, Meltwater Pulse 1A (MWP-1A), occurred ∼14,650 years ago. Considerable uncertainty regarding the sources of meltwater limits understanding of the relationship between MWP-1A and the concurrent fast-changing climate. Here we present a data-driven inversion approach, using a glacio-isostatic adjustment model to invert for the sources of MWP-1A via sea-level constraints from six geographically distributed sites. The results suggest contributions from Antarctica, 1.3 m (0–5.9 m; 95% probability), Scandinavia, 4.6 m (3.2–6.4 m) and North America, 12.0 m (5.6–15.4 m), giving a global mean sea-level rise of 17.9 m (15.7–20.2 m) in 500 years. Only a North American dominant scenario successfully predicts the observed sea-level change across our six sites and an Antarctic dominant scenario is firmly refuted by Scottish isolation basin records. Our sea-level based results therefore reconcile with field-based ice-sheet reconstructions.
Date: 2021
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Persistent link: https://EconPapers.repec.org/RePEc:nat:natcom:v:12:y:2021:i:1:d:10.1038_s41467-021-21990-y
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DOI: 10.1038/s41467-021-21990-y
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