Global sea-level contribution from the Patagonian Icefields since the Little Ice Age maximum
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The LGM in southern Patagonia is estimated around 26 000 yr BP.
“The LGM in southern Patagonia is estimated around 26 000 yr BP, but the beginning of significant glacial retreat occurred between 21 000 and 17 000 yr BP (Hulton et al., 2002;Hein et al., 2010;Glasser et al., 2011;Davies and Glasser, 2012;Moreno et al., 2015;Bendle et al., 2017;Reynhout et al., 2019;Davies et al., 2020).”
From Fast uplift in the southern Patagonian Andes due to long- and short-term deglaciation and the asthenospheric window underneath (2024) · cites this paper as Glasser et al., 2011
The beginning of significant glacial retreat in southern Patagonia occurred between 21 000 and 17 000 yr BP.
“The LGM in southern Patagonia is estimated around 26 000 yr BP, but the beginning of significant glacial retreat occurred between 21 000 and 17 000 yr BP (Hulton et al., 2002;Hein et al., 2010;Glasser et al., 2011;Davies and Glasser, 2012;Moreno et al., 2015;Bendle et al., 2017;Reynhout et al., 2019;Davies et al., 2020).”
From Fast uplift in the southern Patagonian Andes due to long- and short-term deglaciation and the asthenospheric window underneath (2024) · cites this paper as Glasser et al., 2011
The high uplift rates in the northern part of the SPI are currently ascribed to lithospheric viscoelastic GIA following the LIA, which was responsible for an ice loss of 503 ± 101.1 km3 in the SPI.
“Such outstandingly high uplift rates, especially in the northern part of the SPI, are currently ascribed to the lithospheric viscoelastic GIA following the LIA, which was responsible for an ice loss of 503 ± 101.1 km 3 in the SPI (Glasser et al., 2011).”
From Fast uplift in the southern Patagonian Andes due to long- and short-term deglaciation and the asthenospheric window underneath (2024) · cites this paper as Glasser et al., 2011
Information about melting velocities and associated ice thickness and redistribution of the surface masses is limited for the time windows investigated here.
“information about melting velocities and associated ice thickness and redistribution of the surface masses is limited for the time windows investigated here.”
From Fast uplift in the southern Patagonian Andes due to long- and short-term deglaciation and the asthenospheric window underneath (2024) · cites this paper as Glasser et al., 2011
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- Authors
- Glasser, N. F., Harrison, S., Jansson, K. N., Anderson, K., & Cowley, A.
- Affiliations
- Aberystwyth University (GB)
- University of Exeter (GB)
- Stockholm University (SE)
- Corresponding author
- Glasser, N. F.
- Venue
- Nature Geoscience
- Published
- 2011-04-03
- Volume
- 4
- Issue
- 5
- Pages
- 303-307
- ISSN
- 1752-0894 (ISSN-L)
- 1752-0908
- OpenAlex
- W2078885776
- Cited by
- 154
- References
- 32
- Citations by year
- 2026: 5 · 2025: 6 · 2024: 9 · 2023: 13 · 2022: 5 · 2021: 10 · 2020: 10 · 2019: 23 · 2018: 11 · 2017: 5 · 2016: 11 · 2015: 9 · 2014: 10 · 2013: 9 · 2012: 13
- FWCI
- 6.48
- Type
- journal article
- Language
- en
- Open access
- closed
- Licence
- www.springer.com/tdm (tdm)
- Locations
- Nature Geoscience (publishedVersion)
- Funders
- Natural Environment Research Council (NE/G00952X/1)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Cryospheric studies and observations
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
- Physical Sciences › Environmental Science › Ecology › Polar Research and Ecology
- Keywords
- Patagonian Icefields, glacier mass loss, sea level rise, Little Ice Age, trimlines, terminal moraines
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