Modelling the inception of the Patagonian icesheet
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Tracing back the post-LGM or Holocene ice loss rate from current measurements is difficult considering that climate was at least 6 °C colder during the LGM.
“Tracing back the post-LGM or Holocene ice loss rate from current measurements is difficult considering that climate was at least 6 °C colder during the LGM”
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 Sugden et al., 2002
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- Authors
- Sugden, D. E., Hulton, N. R. J., & Purves, R. S.
- Affiliations
- University of Edinburgh (GB)
- Corresponding author
- Sugden, David E
- Venue
- Quaternary International
- Publisher
- Elsevier BV
- Published
- 2002-09
- Volume
- 95-96
- Pages
- 55-64
- ISSN
- 1040-6182 (ISSN-L)
- OpenAlex
- W2147260549
- Cited by
- 51
- References
- 37
- Citations by year
- 2025: 2 · 2024: 6 · 2023: 3 · 2022: 5 · 2021: 2 · 2019: 1 · 2018: 1 · 2016: 3 · 2015: 1 · 2014: 1 · 2012: 3
- FWCI
- 1.24
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Quaternary International (publishedVersion)
- Funders
- Carnegie Trust for the Universities of Scotland
- Natural Environment Research Council
- 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 › Global and Planetary Change › Climate variability and models
- Keywords
- ice sheet growth, Last Glacial Maximum, mass balance, glacial-interglacial cycles, Patagonian Icefields
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