Mid-Holocene thinning of David Glacier, Antarctica: Chronology and controls

• Published in: The Cryosphere
• Main Authors: Stutz J., Mackintosh A., Norton K., Whitmore R., Baroni C., Jamieson S. S. R., Jones R. S., Balco G., Salvatore M. C., Casale S., Lee J. I., Seong Y. B., McKay R., Vargo L. J., Lowry D., Spector P., Christl M., Ochs S. I., Di Nicola L., Iarossi M., Stuart F., Woodruff T.
• Other Authors: Stutz, J., Mackintosh, A., Norton, K., Whitmore, R., Baroni, C., Jamieson, S. S. R., Jones, R. S., Balco, G., Salvatore, M. C., Casale, S., Lee, J. I., Seong, Y. B., Mckay, R., Vargo, L. J., Lowry, D., Spector, P., Christl, M., Ochs, S. I., Di Nicola, L., Iarossi, M., Stuart, F., Woodruff, T.
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2021
• Subjects: Antarctic; Victoria Land; Transantarctic Mountains; Weddell; Drygalski; Drygalski Ice Tongue; David Glacier; Antarc*; Antarctica; Ice Sheet; Ice Shelf
• Online Access: http://hdl.handle.net/11568/1133125; https://doi.org/10.5194/tc-15-5447-2021; https://tc.copernicus.org/articles/15/5447/2021/

Quantitative satellite observations only provide an assessment of ice sheet mass loss over the last four decades. To assess long-term drivers of ice sheet change, geological records are needed. Here we present the first millennial-scale reconstruction of David Glacier, the largest East Antarctic out...