EGU22-11447
https://doi.org/10.5194/egusphere-egu22-11447
EGU General Assembly 2022
© Author(s) 2022. This work is distributed under the Creative Commons Attribution 4.0 License.
Nuanced responses of seasonal sea ice to a warmer Arctic climate during the Holocene Thermal Maximum
- 1Institute of Geology, Adam Mickiewicz University, Maków Polnych 16, 61-606 Poznań, Poland (anna.pienkowski@amu.edu.pl)
- 2Norwegian Polar Institute, Fram Centre, 9296 Tromsø, Norway
- 3Biogeochemistry Research Centre, School of Geography, Earth and Environmental Sciences, University of Plymouth, Plymouth PL4 8AA, UK
- 4Department of Earth Science and Bjerknes Centre for Climate Research, UiB University of Bergen, 5007 Bergen, Norway
- 5Geological Survey of Norway, 7491 Trondheim, Norway
- 6Centre for Arctic Gas Hydrate, Environment and Climate, Department of Geosciences, UiT- The Arctic University of Norway in Tromsø, 9037 Tromsø, Norway
- 7British Antarctic Survey, NERC, High Cross, Cambridge CB3 0ET, UK
- 8Department of Arctic Geology, The University Centre in Svalbard (UNIS), N-9171 Longyearbyen, Svalbard, Norway
How to cite: Pienkowski, A. J., Husum, K., Belt, S. T., Ninnemann, U., Köseoğlu, D., Divine, D. V., Smik, L., Knies, J., Hogan, K., and Noormets, R.: Nuanced responses of seasonal sea ice to a warmer Arctic climate during the Holocene Thermal Maximum, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-11447, https://doi.org/10.5194/egusphere-egu22-11447, 2022.