1236: Q-ARCTIC
active project
Principal investigator: Victor Brovkin
Max-Planck-Institut für Meteorologie (Community project)
Project abstract
Report 1/2022 to 12/2022
Report 1/2023 to 12/2023
Report 1/2024 to 12/2024
Report 1/2025 to 12/2025
Publications
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DOI: 10.1007/s10712-025-09885-9,
Brovkin, V., Bartsch, A., Hugelius, G. et al. Permafrost and Freshwater Systems in the Arctic as Tipping Elements of the Climate System. Surv Geophys 46, 303–326 (2025).
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DOI: 10.1029/2024GL109034,
de Vrese, P., Stacke, T., Gayler, V., & Brovkin, V. (2024). Permafrost cloud feedback may amplify climate change. Geophysical Research Letters, 51, e2024GL109034.
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DOI: 10.5194/egusphere-2025-3791,
Yazbeck, T., Schlutow, M., Bolek, A., Triches, N. Y., Wahl, E., Heimann, M., and Göckede, M.: Quantifying landcover-specific fluxes over a heterogeneous landscape through coupling UAV-measured mixing ratios with a large-eddy simulation model and Eddy-covariance measurements, EGUsphere [preprint], https://doi.org/10.5194/egusphere-2025-3791, 2025
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DOI: 10.1002/ppp.2269,
Matthes, H., Damseaux, A., Westermann, S., Beer, C., Boone, A., Burke, E., Decharme, B., Genet, H., Jafarov, E., Langer, M., Parmentier, F.-J., Porada, P., Gagne-Landmann, A., Huntzinger, D., Rogers, B., Schädel, C., Stacke, T., Wells, J. and Wieder, W. (2025), Advances in Permafrost Representation: Biophysical Processes in Earth System Models and the Role of Offline Models. Permafrost and Periglac Process, 36: 302-318.
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DOI: 10.1029/2024GL109034,
de Vrese, P., Stacke, T., Gayler, V., & Brovkin, V. (2024). Permafrost cloud feedback may amplify climate change. Geophysical Research Letters, 51, e2024GL109034.
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DOI: 10.1029/2024JD040794,
Schlutow, M., Stacke, T., Doerffel, T., Smolarkiewicz, P. K., & Göckede, M. (2024). Large eddy simulations of the interaction between the atmospheric boundary layer and degrading Arctic permafrost. Journal of Geophysical Research: Atmospheres, 129, e2024JD040794.
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DOI: 10.1038/s41558-023-01715-3,
de Vrese, P., Beckebanze, L., Galera, L.d.A. et al. Sensitivity of Arctic CH4 emissions to landscape wetness diminished by atmospheric feedbacks. Nat. Clim. Chang. 13, 832–839 (2023). https://doi.org/10.1038/s41558-023-01715-3
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DOI: 10.5194/tc-17-2095-2023,
de Vrese, P., Georgievski, G., Gonzalez Rouco, J. F., Notz, D., Stacke, T., Steinert, N. J., Wilkenskjeld, S., and Brovkin, V.: Representation of soil hydrology in permafrost regions may explain large part of inter-model spread in simulated Arctic and subarctic climate, The Cryosphere, 17, 2095–2118, https://doi.org/10.5194/tc-17-2095-2023, 2023.