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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- Advances in understanding the mechanisms of Arctic amplification J. Li et al. 10.1007/s11430-024-1438-5
- Too cold, too saturated? Evaluating climate models at the gateway to the Arctic F. Pithan et al. 10.5194/acp-25-3269-2025
- Arctic climate feedback response to local sea-ice concentration and remote sea surface temperature changes in PAMIP simulations M. Jenkins et al. 10.1007/s00382-024-07465-y
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10 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
- Arctic climate response to European radiative forcing: a deep learning study on circulation pattern changes S. Mehrdad et al. 10.5194/wcd-5-1223-2024
- Advances in understanding the mechanisms of Arctic amplification J. Li et al. 10.1007/s11430-024-1438-5
- Too cold, too saturated? Evaluating climate models at the gateway to the Arctic F. Pithan et al. 10.5194/acp-25-3269-2025
- Arctic climate feedback response to local sea-ice concentration and remote sea surface temperature changes in PAMIP simulations M. Jenkins et al. 10.1007/s00382-024-07465-y
- “北极放大”现象驱动机制的研究进展 杰. 李 et al. 10.1360/SSTe-2024-0190
- Increasing fluctuations in the Arctic summer sea ice cover are expected with future global warming A. Poltronieri et al. 10.1088/2752-5295/ad519d
- Thermodynamic and cloud evolution in a cold-air outbreak during HALO-(AC)3: quasi-Lagrangian observations compared to the ERA5 and CARRA reanalyses B. Kirbus et al. 10.5194/acp-24-3883-2024
- Elevation-dependent warming: observations, models, and energetic mechanisms M. Byrne et al. 10.5194/wcd-5-763-2024
- Overview: quasi-Lagrangian observations of Arctic air mass transformations – introduction and initial results of the HALO–(𝒜 𝒞)3 aircraft campaign M. Wendisch et al. 10.5194/acp-24-8865-2024
2 citations as recorded by crossref.
Latest update: 27 May 2025
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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