Articles | Volume 16, issue 1
https://doi.org/10.5194/cp-16-371-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-16-371-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Hypersensitivity of glacial summer temperatures in Siberia
Department of Earth Sciences, Vrije Universiteit Amsterdam, Amsterdam, the Netherlands
MARUM-Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany
Irina Rogozhina
Department of Geography, Norwegian University of Science and Technology, Trondheim, Norway
MARUM-Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany
Institute of Physics of the Earth, Russian Academy of Science, Moscow, Russia
Ute Merkel
MARUM-Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany
Matthias Prange
MARUM-Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany
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Cited
16 citations as recorded by crossref.
- Oxygen isotope studies of the largest West Siberian mammoth sites and implications for last glacial maximum climate reconstruction I. Krivokorin et al. https://doi.org/10.1016/j.quascirev.2024.108938
- The influence of glacial Northern Hemisphere ice sheets on atmospheric circulation H. Saini et al. https://doi.org/10.5194/cp-22-1457-2026
- Ocean Response in Transient Simulations of the Last Deglaciation Dominated by Underlying Ice‐Sheet Reconstruction and Method of Meltwater Distribution M. Kapsch et al. https://doi.org/10.1029/2021GL096767
- Siberian environmental change: Synthesis of recent studies and opportunities for networking T. Callaghan et al. https://doi.org/10.1007/s13280-021-01626-7
- Patterns of changing surface climate variability from the Last Glacial Maximum to present in transient model simulations E. Ziegler et al. https://doi.org/10.5194/cp-21-627-2025
- Climate and ice sheet dynamics in Patagonia throughout marine isotope stages 2 and 3 A. Castillo-Llarena et al. https://doi.org/10.5194/cp-20-1559-2024
- DNA virus–host patterns in lake and marine environments over the last glacial cycle C. Boeckel et al. https://doi.org/10.1093/ismejo/wrag025
- Formation of giant Siberian gas emission craters (GECs) H. Hellevang et al. https://doi.org/10.1016/j.scitotenv.2025.180042
- Impacts of the PMIP4 ice sheets on Northern Hemisphere climate during the last glacial period K. Izumi et al. https://doi.org/10.1007/s00382-022-06456-1
- Regional pollen-based Holocene temperature and precipitation patterns depart from the Northern Hemisphere mean trends U. Herzschuh et al. https://doi.org/10.5194/cp-19-1481-2023
- Sensitivity of Heinrich-type ice-sheet surge characteristics to boundary forcing perturbations C. Schannwell et al. https://doi.org/10.5194/cp-19-179-2023
- Mechanisms driving the global tropical response to a weakened AMOC during Heinrich Stadial 1 A. Lawman et al. https://doi.org/10.1016/j.quascirev.2025.109567
- Tropical response to ocean circulation slowdown raises future drought risk P. DiNezio et al. https://doi.org/10.1038/s41586-025-09319-x
- Pollen characteristics of Zelyony Mys yedoma and ground squirrel' burrows A. Vasil'chuk & Y. Vasil'chuk https://doi.org/10.7256/2453-8922.2021.1.32985
- A multicentennial mode of North Atlantic climate variability throughout the Last Glacial Maximum M. Prange et al. https://doi.org/10.1126/sciadv.adh1106
- The glacial systems model (GSM) Version 25G L. Tarasov et al. https://doi.org/10.5194/gmd-18-9565-2025
16 citations as recorded by crossref.
- Oxygen isotope studies of the largest West Siberian mammoth sites and implications for last glacial maximum climate reconstruction I. Krivokorin et al. https://doi.org/10.1016/j.quascirev.2024.108938
- The influence of glacial Northern Hemisphere ice sheets on atmospheric circulation H. Saini et al. https://doi.org/10.5194/cp-22-1457-2026
- Ocean Response in Transient Simulations of the Last Deglaciation Dominated by Underlying Ice‐Sheet Reconstruction and Method of Meltwater Distribution M. Kapsch et al. https://doi.org/10.1029/2021GL096767
- Siberian environmental change: Synthesis of recent studies and opportunities for networking T. Callaghan et al. https://doi.org/10.1007/s13280-021-01626-7
- Patterns of changing surface climate variability from the Last Glacial Maximum to present in transient model simulations E. Ziegler et al. https://doi.org/10.5194/cp-21-627-2025
- Climate and ice sheet dynamics in Patagonia throughout marine isotope stages 2 and 3 A. Castillo-Llarena et al. https://doi.org/10.5194/cp-20-1559-2024
- DNA virus–host patterns in lake and marine environments over the last glacial cycle C. Boeckel et al. https://doi.org/10.1093/ismejo/wrag025
- Formation of giant Siberian gas emission craters (GECs) H. Hellevang et al. https://doi.org/10.1016/j.scitotenv.2025.180042
- Impacts of the PMIP4 ice sheets on Northern Hemisphere climate during the last glacial period K. Izumi et al. https://doi.org/10.1007/s00382-022-06456-1
- Regional pollen-based Holocene temperature and precipitation patterns depart from the Northern Hemisphere mean trends U. Herzschuh et al. https://doi.org/10.5194/cp-19-1481-2023
- Sensitivity of Heinrich-type ice-sheet surge characteristics to boundary forcing perturbations C. Schannwell et al. https://doi.org/10.5194/cp-19-179-2023
- Mechanisms driving the global tropical response to a weakened AMOC during Heinrich Stadial 1 A. Lawman et al. https://doi.org/10.1016/j.quascirev.2025.109567
- Tropical response to ocean circulation slowdown raises future drought risk P. DiNezio et al. https://doi.org/10.1038/s41586-025-09319-x
- Pollen characteristics of Zelyony Mys yedoma and ground squirrel' burrows A. Vasil'chuk & Y. Vasil'chuk https://doi.org/10.7256/2453-8922.2021.1.32985
- A multicentennial mode of North Atlantic climate variability throughout the Last Glacial Maximum M. Prange et al. https://doi.org/10.1126/sciadv.adh1106
- The glacial systems model (GSM) Version 25G L. Tarasov et al. https://doi.org/10.5194/gmd-18-9565-2025
Saved (final revised paper)
Latest update: 22 Aug 2026
Short summary
Northeastern Siberia is currently known for its harsh cold climate, but remarkably it did not experience large-scale glaciation during the last ice age. We show that the region is also exceptional in climate models. As a result of subtle changes in model setup, climate models show a strong divergence in simulated glacial summer temperatures that is ultimately driven by changes in the circumpolar atmospheric stationary wave pattern and associated northward heat transport to northeastern Siberia.
Northeastern Siberia is currently known for its harsh cold climate, but remarkably it did not...