Dr. rer. nat. Finn Ole Heukamp
Climate Physicist | Ocean and Sea Ice Modeler | Oceanographer
Climate Physicist | Ocean and Sea Ice Modeler | Oceanographer
I am a climate physicist and oceanographer specializing in high-latitude climate dynamics and atmosphere-ocean-ice interactions. With a PhD from the Alfred-Wegener-Institute for Polar and Marine Science, my current work at the Alfred-Wegener-Institute focusses on understanding Southern Ocean sea ice variability and model-observation mismatches. I am particularly interested in the yet underrepresented role of ocean-cryosphere interactions, such as cavities and icebergs and their impact on the Southern Ocean. I have extensive experience in applying state-of-the-art ocean and climate models, in particular the Alfred-Wegner-Institute Climate Model and the Finite Volume Ocean and Sea Ice Model FESOM2.1, with strong programming skills in Python, MATLAB, and Fortran90. My research is documented in high-impact journals, and I thrive in interdisciplinary collaborations to address pressing climate challenges. Passionate about advancing Earth system modeling, I also enjoy sharing scientific insights through teaching, outreach, and engaging with diverse audiences.
Heukamp et al. 2025 | Nature Communications
Over the past 50 years, Arctic sea ice has declined in all seasons, with particularly pronounced winter reductions in the Barents Sea. While temperature changes in the Atlantic Water inflow and atmospheric-driven melt have been identified as key drivers of this decline, the role of the return-flow of Atlantic Water in the northern Barents Sea Opening, linked to its recirculation back into the Nordic Seas, has remained largely unrecognized. Using a global ocean and sea ice model, we find that the volume transport of the Atlantic Water return-flow is strongly correlated with the sea ice area in the Barents Sea. In addition, we find that, over the past 40 years, the return-flow has steadily weakened without a corresponding change in inflow. Here, we show that reduced Atlantic Water removal by a weakened return-flow contributes to both interannual variability and the sustained loss of Barents Sea sea ice.
original publication | press release
Atlantic water recirculation in the northern Barents Sea affects winter sea ice extent (2025)
Finn Ole Heukamp, Claudia Wekerle, Torsten Kanzow, Rebecca McPherson & Till M. Baumann
Nat Commun 16, 5148 (2025).
https://doi.org/10.1038/s41467-025-59992-9
Atmospheric blocking slows ocean-driven melting of Greenland’s largest glacier tongue (2025)
Rebecca McPherson, Claudia Wekerle, Torsten Kanzow, Finn Ole Heukamp, Ole Zeising, Angelika Humbert
Science Vol 385, Issue 6715, pp. 1360-1366
https://doi.org/10.1126/science.ado5008
Cyclones Modulate the Control of the North Atlantic Oscillation on Transports into the Barents Sea (2023)
Finn Ole Heukamp, Lars Aue, Qiang Wang, Monica Ionita, Torsten Kanzow, Claudia Wekerle, Annette Rinke
Communications Earth & Environment 4 (1), 324
https://doi.org/10.1038/s43247-023-00985-1
Impact of cyclonic wind anomalies caused by massive winter sea ice retreat in the Barents Sea on Atlantic Water transport toward the Arctic: A model study (2023)
Finn Ole Heukamp, Torsten Kanzow, Qiang Wang, Claudia Wekerle, Rüdiger Gerdes
Journal of Geophysical Research: Oceans 128 (3)
https://doi.org/10.1029/2022JC019045
Tropical Instability Waves and Wind-Forced Cross-Equatorial Flow in the Central Atlantic Ocean (2022)
Finn Ole Heukamp, Peter Brandt, Marcus Dengler, Franz-Phillipp Tuchen, Michael McPhaden, James Moum
Geophysical Research Letters 49 (19)
https://doi.org/10.1029/2022GL099325
Arctic Subarctic Ocean Fluxes (2023) | La Palma, Gran Canaria | Talk
EGU 2022 | Vienna, Austria | Talk
EGU 2018 | Vienna, Austria | Talk (co-author)
Feel free to reach out to me.
Mail: Finn.Heukamp@awi.de
Finn Heukamp
Alfred-Wegener-Institut
Helmholz Center for Polar and Marine Research
Klußmannstraße 3
27570 Bremerhaven
Germany