Articles | Volume 23, issue 17
https://doi.org/10.5194/acp-23-9963-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-23-9963-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
07 Sep 2023
Research article |
| 07 Sep 2023
| 07 Sep 2023
Constraints on simulated past Arctic amplification and lapse rate feedback from observations
Olivia Linke
Leipzig Institute for Meteorology, Leipzig University, Leipzig, Germany
Johannes Quaas
CORRESPONDING AUTHOR
Leipzig Institute for Meteorology, Leipzig University, Leipzig, Germany
Finja Baumer
Leipzig Institute for Meteorology, Leipzig University, Leipzig, Germany
Sebastian Becker
Leipzig Institute for Meteorology, Leipzig University, Leipzig, Germany
Jan Chylik
Institute of Geophysics and Meteorology, University of Cologne, Cologne, Germany
Sandro Dahlke
Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Potsdam, Germany
André Ehrlich
Leipzig Institute for Meteorology, Leipzig University, Leipzig, Germany
Dörthe Handorf
Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Potsdam, Germany
Christoph Jacobi
Leipzig Institute for Meteorology, Leipzig University, Leipzig, Germany
Heike Kalesse-Los
Leipzig Institute for Meteorology, Leipzig University, Leipzig, Germany
Luca Lelli
Institute of Environmental Physics, University of Bremen, Bremen, Germany
Remote Sensing Technology Institute, German Aerospace Centre (DLR), Weßling, Germany
Sina Mehrdad
Leipzig Institute for Meteorology, Leipzig University, Leipzig, Germany
Roel A. J. Neggers
Institute of Geophysics and Meteorology, University of Cologne, Cologne, Germany
Johannes Riebold
Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Potsdam, Germany
Pablo Saavedra Garfias
Leipzig Institute for Meteorology, Leipzig University, Leipzig, Germany
Niklas Schnierstein
Institute of Geophysics and Meteorology, University of Cologne, Cologne, Germany
Matthew D. Shupe
Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, Boulder, CO, USA
Physical Sciences Laboratory, National Oceanic and Atmospheric Administration, Boulder, CO, USA
Chris Smith
School of Earth and Environment, University of Leeds, Leeds, UK
Energy, Climate and Environment Program, International Institute for Applied Systems Analysis, Laxenburg, Austria
Gunnar Spreen
Institute of Environmental Physics, University of Bremen, Bremen, Germany
Baptiste Verneuil
Leipzig Institute for Meteorology, Leipzig University, Leipzig, Germany
Department of Mechanics and Energetics, École Polytechnique, Palaiseau, France
Kameswara S. Vinjamuri
Institute of Environmental Physics, University of Bremen, Bremen, Germany
Marco Vountas
Institute of Environmental Physics, University of Bremen, Bremen, Germany
Manfred Wendisch
Leipzig Institute for Meteorology, Leipzig University, Leipzig, Germany
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Cited
3 citations as recorded by crossref.
- Tethered Balloon-Borne Turbulence Measurements in Winter and Spring during the MOSAiC Expedition E. Akansu et al. 10.1038/s41597-023-02582-5
- Robust and perfectible constraints on human-induced Arctic amplification H. Douville 10.1038/s43247-023-00949-5
- Satellite remote sensing of regional and seasonal Arctic cooling showing a multi-decadal trend towards brighter and more liquid clouds L. Lelli et al. 10.5194/acp-23-2579-2023
1 citations as recorded by crossref.
2 citations as recorded by crossref.
Latest update: 01 Dec 2023
Short summary
Lapse rate feedback (LRF) is a major driver of the Arctic amplification (AA) of climate change. It arises because the warming is stronger at the surface than aloft. Several processes can affect the LRF in the Arctic, such as the omnipresent temperature inversion. Here, we compare multimodel climate simulations to Arctic-based observations from a large research consortium to broaden our understanding of these processes, find synergy among them, and constrain the Arctic LRF and AA.
Lapse rate feedback (LRF) is a major driver of the Arctic amplification (AA) of climate change....
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