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
Publications
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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.