Articles | Volume 13, issue 11
https://doi.org/10.5194/tc-13-3061-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-13-3061-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Thickness of the divide and flank of the West Antarctic Ice Sheet through the last deglaciation
Perry Spector
CORRESPONDING AUTHOR
Berkeley Geochronology Center, 2455 Ridge Road, Berkeley, CA, USA
John Stone
Department of Earth and Space Sciences, University of Washington, Seattle, WA, USA
Brent Goehring
Department of Earth and Environmental Sciences, Tulane University, New Orleans, LA, USA
Viewed
Total article views: 5,303 (including HTML, PDF, and XML)
Cumulative views and downloads
(calculated since 01 Jul 2019)
| HTML | XML | Total | Supplement | BibTeX | EndNote | |
|---|---|---|---|---|---|---|
| 3,849 | 1,266 | 188 | 5,303 | 323 | 202 | 254 |
- HTML: 3,849
- PDF: 1,266
- XML: 188
- Total: 5,303
- Supplement: 323
- BibTeX: 202
- EndNote: 254
Total article views: 4,447 (including HTML, PDF, and XML)
Cumulative views and downloads
(calculated since 20 Nov 2019)
| HTML | XML | Total | Supplement | BibTeX | EndNote | |
|---|---|---|---|---|---|---|
| 3,481 | 799 | 167 | 4,447 | 178 | 184 | 234 |
- HTML: 3,481
- PDF: 799
- XML: 167
- Total: 4,447
- Supplement: 178
- BibTeX: 184
- EndNote: 234
Total article views: 856 (including HTML, PDF, and XML)
Cumulative views and downloads
(calculated since 01 Jul 2019)
| HTML | XML | Total | Supplement | BibTeX | EndNote | |
|---|---|---|---|---|---|---|
| 368 | 467 | 21 | 856 | 145 | 18 | 20 |
- HTML: 368
- PDF: 467
- XML: 21
- Total: 856
- Supplement: 145
- BibTeX: 18
- EndNote: 20
Viewed (geographical distribution)
Total article views: 5,303 (including HTML, PDF, and XML)
Thereof 4,667 with geography defined
and 636 with unknown origin.
Total article views: 4,447 (including HTML, PDF, and XML)
Thereof 3,984 with geography defined
and 463 with unknown origin.
Total article views: 856 (including HTML, PDF, and XML)
Thereof 683 with geography defined
and 173 with unknown origin.
| Country | # | Views | % |
|---|
| Country | # | Views | % |
|---|
| Country | # | Views | % |
|---|
| Total: | 0 |
| HTML: | 0 |
| PDF: | 0 |
| XML: | 0 |
- 1
1
| Total: | 0 |
| HTML: | 0 |
| PDF: | 0 |
| XML: | 0 |
- 1
1
| Total: | 0 |
| HTML: | 0 |
| PDF: | 0 |
| XML: | 0 |
- 1
1
Cited
17 citations as recorded by crossref.
- Review article: Existing and potential evidence for Holocene grounding line retreat and readvance in Antarctica J. Johnson et al. https://doi.org/10.5194/tc-16-1543-2022
- Nunataks as barriers to ice flow: implications for palaeo ice sheet reconstructions M. Mas e Braga et al. https://doi.org/10.5194/tc-15-4929-2021
- Seasonal temperatures in West Antarctica during the Holocene T. Jones et al. https://doi.org/10.1038/s41586-022-05411-8
- Antarctic surface temperature and elevation during the Last Glacial Maximum C. Buizert et al. https://doi.org/10.1126/science.abd2897
- Paired 14C–10Be exposure ages from Mount Murphy, West Antarctica: Implications for accurate and precise deglacial chronologies J. Adams et al. https://doi.org/10.5194/gchron-8-255-2026
- A thicker-than-present East Antarctic Ice Sheet plateau during the Last Glacial Maximum C. Rand et al. https://doi.org/10.5194/tc-19-3681-2025
- Reinterpretation of ice-sheet history and geomorphology in the Lambert-Amery system, East Antarctica, from cosmogenic in-situ 14C analysis C. Rand et al. https://doi.org/10.1016/j.quascirev.2026.110296
- Stability of the Antarctic Ice Sheet during the pre-industrial Holocene R. Jones et al. https://doi.org/10.1038/s43017-022-00309-5
- A decade of in situ cosmogenic 14C in Antarctica K. Nichols https://doi.org/10.1017/aog.2023.13
- Assessing the suitability of sites near Pine Island Glacier for subglacial bedrock drilling aimed at detecting Holocene retreat–readvance J. Johnson et al. https://doi.org/10.5194/tc-19-303-2025
- Exposure-age data from across Antarctica reveal mid-Miocene establishment of polar desert climate P. Spector & G. Balco https://doi.org/10.1130/G47783.1
- Cosmogenic-nuclide data from Antarctic nunataks can constrain past ice sheet instabilities A. Halberstadt et al. https://doi.org/10.5194/tc-17-1623-2023
- High mid-Holocene accumulation rates over West Antarctica inferred from a pervasive ice-penetrating radar reflector J. Bodart et al. https://doi.org/10.5194/tc-17-1497-2023
- Using ice core measurements from Taylor Glacier, Antarctica, to calibrate in situ cosmogenic 14C production rates by muons M. Dyonisius et al. https://doi.org/10.5194/tc-17-843-2023
- Comparing Glacial‐Geological Evidence and Model Simulations of Ice Sheet Change since the Last Glacial Period in the Amundsen Sea Sector of Antarctica J. Johnson et al. https://doi.org/10.1029/2020JF005827
- Temperature-dependent feedbacks drive the pattern of Antarctic temperature change B. Markle & E. Steig https://doi.org/10.1073/pnas.2513383123
- A pre-Pliocene origin of the glacial trimline in the Ellsworth Mountains and the prevalence of old landscapes at high elevations in West Antarctica D. Small et al. https://doi.org/10.1016/j.geomorph.2025.109634
17 citations as recorded by crossref.
- Review article: Existing and potential evidence for Holocene grounding line retreat and readvance in Antarctica J. Johnson et al. https://doi.org/10.5194/tc-16-1543-2022
- Nunataks as barriers to ice flow: implications for palaeo ice sheet reconstructions M. Mas e Braga et al. https://doi.org/10.5194/tc-15-4929-2021
- Seasonal temperatures in West Antarctica during the Holocene T. Jones et al. https://doi.org/10.1038/s41586-022-05411-8
- Antarctic surface temperature and elevation during the Last Glacial Maximum C. Buizert et al. https://doi.org/10.1126/science.abd2897
- Paired 14C–10Be exposure ages from Mount Murphy, West Antarctica: Implications for accurate and precise deglacial chronologies J. Adams et al. https://doi.org/10.5194/gchron-8-255-2026
- A thicker-than-present East Antarctic Ice Sheet plateau during the Last Glacial Maximum C. Rand et al. https://doi.org/10.5194/tc-19-3681-2025
- Reinterpretation of ice-sheet history and geomorphology in the Lambert-Amery system, East Antarctica, from cosmogenic in-situ 14C analysis C. Rand et al. https://doi.org/10.1016/j.quascirev.2026.110296
- Stability of the Antarctic Ice Sheet during the pre-industrial Holocene R. Jones et al. https://doi.org/10.1038/s43017-022-00309-5
- A decade of in situ cosmogenic 14C in Antarctica K. Nichols https://doi.org/10.1017/aog.2023.13
- Assessing the suitability of sites near Pine Island Glacier for subglacial bedrock drilling aimed at detecting Holocene retreat–readvance J. Johnson et al. https://doi.org/10.5194/tc-19-303-2025
- Exposure-age data from across Antarctica reveal mid-Miocene establishment of polar desert climate P. Spector & G. Balco https://doi.org/10.1130/G47783.1
- Cosmogenic-nuclide data from Antarctic nunataks can constrain past ice sheet instabilities A. Halberstadt et al. https://doi.org/10.5194/tc-17-1623-2023
- High mid-Holocene accumulation rates over West Antarctica inferred from a pervasive ice-penetrating radar reflector J. Bodart et al. https://doi.org/10.5194/tc-17-1497-2023
- Using ice core measurements from Taylor Glacier, Antarctica, to calibrate in situ cosmogenic 14C production rates by muons M. Dyonisius et al. https://doi.org/10.5194/tc-17-843-2023
- Comparing Glacial‐Geological Evidence and Model Simulations of Ice Sheet Change since the Last Glacial Period in the Amundsen Sea Sector of Antarctica J. Johnson et al. https://doi.org/10.1029/2020JF005827
- Temperature-dependent feedbacks drive the pattern of Antarctic temperature change B. Markle & E. Steig https://doi.org/10.1073/pnas.2513383123
- A pre-Pliocene origin of the glacial trimline in the Ellsworth Mountains and the prevalence of old landscapes at high elevations in West Antarctica D. Small et al. https://doi.org/10.1016/j.geomorph.2025.109634
Saved (final revised paper)
Latest update: 25 Oct 2026
Short summary
We describe constraints on the thickness of the interior of the West Antarctic Ice Sheet (WAIS) through the last deglaciation. Our data imply that the ice-sheet divide between the Ross and Weddell sea sectors of the WAIS was thicker than present for a period less than ~ 8 kyr within the past ~ 15 kyr. These results are consistent with the hypothesis that the divide initially thickened due to the deglacial rise in snowfall and subsequently thinned in response to retreat of the ice-sheet margin.
We describe constraints on the thickness of the interior of the West Antarctic Ice Sheet (WAIS)...