Greenland Ice Cores Reveal a South‐To‐North Difference in Holocene Thermal Maximum Timings
Abstract Holocene temperature evolution remains poorly understood. Proxies in the early and mid‐Holocene suggest a Holocene Thermal Maximum (HTM) where temperatures exceed the pre‐industrial, whereas climate models generally simulate monotonic warming. This discrepancy may reflect proxy seasonality biases or errors in climate model internal feedbacks or dynamics. Using seasonally unbiased ice core reconstructions at NEEM, NGRIP, and Greenland Ice Sheet Project 2, we identify a Greenland HTM of ∼2°C above pre‐industrial, in agreement with other Northern Hemisphere proxy reconstructions. The firn‐based reconstructions are verified through borehole thermometry, producing a multi‐core, multi‐proxy reconstruction of Greenland climate from the last glacial to pre‐industrial. HTM timing across Greenland is heterogenous, occurring earlier at high elevations. Total air content measurements suggest a temperature contribution from elevation changes; regional oceanographic conditions, a weakened polar lapse rate, or variable near‐surface inversions may also be important sensitivities. Our reconstructions support climate simulations with dynamic Holocene vegetation, highlighting the importance of vegetation feedbacks.
Authors
- T. J. Fudge (ORCID: https://orcid.org/0000-0002-6818-7479)
- Ross Beaudette
- Jeffrey P. Severinghaus (ORCID: https://orcid.org/0000-0001-8883-3119)
- Christo Buizert (ORCID: https://orcid.org/0000-0002-2227-1747)
- Marie Kirk
- Olivia L. Williams (ORCID: https://orcid.org/0000-0001-7433-655X)
- J. P. Steffensen (ORCID: https://orcid.org/0000-0002-5516-1093)
- Jon S. Edwards
- Thomas Blunier (ORCID: https://orcid.org/0000-0002-6065-7747)
- Ikumi Oyabu (ORCID: https://orcid.org/0000-0001-8017-1085)
- Kenji Kawamura (ORCID: https://orcid.org/0000-0003-1163-700X)
- Kaden Martin (ORCID: https://orcid.org/0000-0003-2162-8668)
- Iben Koldtoft (ORCID: https://orcid.org/0000-0002-5158-1904)
- Ben Riddell‐Young (ORCID: https://orcid.org/0000-0001-5937-4726)
- Ed Brook
- Farhana Mederbel
Institutions
- University of Copenhagen (DK)
- Oregon State University (US)
- Scripps Institution of Oceanography (US)
- Cooperative Institute for Research in Environmental Sciences (US)
- University of Colorado Boulder (US)
- Université de Versailles Saint-Quentin-en-Yvelines (FR)
- University of Washington (US)
- Université Paris-Saclay (FR)
- National Institute of Polar Research (JP)
- University of California San Diego (US)
- Earth and Space Research (US)
- Research Organization of Information and Systems (JP)
- Woods Hole Oceanographic Institution (US)
Publication Details
- Journal
- Geophysical Research Letters
- Published
- 2024-12-12
- DOI
- https://doi.org/10.1029/2024gl111405
- Citations
- 4
- Primary Topic
- Geology and Paleoclimatology Research
- Type
- article
- Field-Weighted Citation Impact
- 1.51
Funders
- National Science Foundation
- Ministry of Education, Culture, Sports, Science and Technology
- Japan Society for the Promotion of Science