Decadal-scale onset and termination of Antarctic ice-mass loss during the last deglaciation

Emerging ice-sheet modeling suggests once initiated, retreat of the Antarctic Ice Sheet (AIS) can continue for centuries. Unfortunately, the short observational record cannot resolve the tipping points, rate of change, and timescale of responses. Iceberg-rafted debris data from Iceberg Alley identif...

Celý popis

Uloženo v:
Podrobná bibliografie
Vydáno v:Nature communications Ročník 12; číslo 1; s. 6683 - 13
Hlavní autoři: Weber, Michael E., Golledge, Nicholas R., Fogwill, Chris J., Turney, Chris S. M., Thomas, Zoë A.
Médium: Journal Article
Jazyk:angličtina
Vydáno: London Nature Publishing Group UK 18.11.2021
Nature Publishing Group
Nature Portfolio
Témata:
704/106/125
704/106/413
Deglaciation
Drawdown
Dynamic response
Glaciers
Humanities and Social Sciences
Ice ages
Ice sheets
Icebergs
Meltwater
multidisciplinary
Science
Science (multidisciplinary)
Sea level rise
Sheet modelling
ISSN:2041-1723, 2041-1723
On-line přístup:Získat plný text
Tagy: Přidat tag
Žádné tagy, Buďte první, kdo vytvoří štítek k tomuto záznamu!
Popis
Shrnutí:Emerging ice-sheet modeling suggests once initiated, retreat of the Antarctic Ice Sheet (AIS) can continue for centuries. Unfortunately, the short observational record cannot resolve the tipping points, rate of change, and timescale of responses. Iceberg-rafted debris data from Iceberg Alley identify eight retreat phases after the Last Glacial Maximum that each destabilized the AIS within a decade, contributing to global sea-level rise for centuries to a millennium, which subsequently re-stabilized equally rapidly. This dynamic response of the AIS is supported by (i) a West Antarctic blue ice record of ice-elevation drawdown >600 m during three such retreat events related to globally recognized deglacial meltwater pulses, (ii) step-wise retreat up to 400 km across the Ross Sea shelf, (iii) independent ice sheet modeling, and (iv) tipping point analysis. Our findings are consistent with a growing body of evidence suggesting the recent acceleration of AIS mass loss may mark the beginning of a prolonged period of ice sheet retreat and substantial global sea level rise. It may have taken only a decade to repeatedly destabilize the Antarctic Ice Sheet after the last Ice Age as shown by a new data-model study. The ice sheet lost ice for centuries each time before it abruptly re-stabilized again.
Bibliografie:ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 14
content type line 23
ISSN:2041-1723
2041-1723
DOI:10.1038/s41467-021-27053-6