Articles | Volume 4, issue 1
https://doi.org/10.5194/wcd-4-61-2023
© 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/wcd-4-61-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
The role of Rossby waves in polar weather and climate
Tim Woollings
CORRESPONDING AUTHOR
Atmospheric, Oceanic and Planetary Physics, Oxford University, Oxford, UK
Camille Li
Geophysical Institute, University of Bergen, Bergen, Norway
Bjerknes Centre for Climate Research, University of Bergen, Bergen, Norway
Marie Drouard
Atmospheric, Oceanic and Planetary Physics, Oxford University, Oxford, UK
Instituto de Geociencias (IGEO), CSIC-UCM, Madrid, Spain
Etienne Dunn-Sigouin
NORCE Norwegian Research Centre AS, Bergen, Norway
Bjerknes Centre for Climate Research, University of Bergen, Bergen, Norway
Karim A. Elmestekawy
Atmospheric, Oceanic and Planetary Physics, Oxford University, Oxford, UK
Momme Hell
Department of Earth, Environmental, and Planetary Sciences, Brown University, Providence, RI, USA
Brian Hoskins
Grantham Institute, Imperial College London, London, UK
Department of Meteorology, University of Reading, Reading, UK
Cheikh Mbengue
Atmospheric, Oceanic and Planetary Physics, Oxford University, Oxford, UK
Climate Modeling Alliance, California Institute of Technology, Pasadena, CA, USA
Matthew Patterson
Atmospheric, Oceanic and Planetary Physics, Oxford University, Oxford, UK
Thomas Spengler
Geophysical Institute, University of Bergen, Bergen, Norway
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13 citations as recorded by crossref.
- The possible links between the Barents–Kara sea‐ice area, Ural blocking, and the North Atlantic Oscillation R. Ahmadi & O. Alizadeh 10.1002/qj.4560
- The maintenance of coherent vortex topology by Lagrangian chaos in drift-Rossby wave turbulence N. Cao & D. Qi 10.1063/5.0207687
- The Summer North Atlantic Oscillation, Arctic sea ice, and Arctic jet Rossby wave forcing C. Folland et al. 10.1126/sciadv.adk6693
- Physical mechanisms for the dominant summertime high-latitude atmospheric teleconnection pattern and the related Northern Eurasian climates J. Kim & K. Seo 10.1088/1748-9326/acfa13
- Movement of decaying quasi-2-day wave in the austral summer-time mesosphere C. Salinas & D. Wu 10.1038/s41598-024-68559-5
- Influence of Sudden Stratospheric Warmings on the Migrating Diurnal Tide in the Equatorial Middle Atmosphere Observed by Aura/Microwave Limb Sounder K. Hocke 10.3390/atmos14121743
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- Circulation responses to surface heating and implications for polar amplification P. Siew et al. 10.5194/wcd-5-985-2024
- Evaluating Causal Arctic‐Midlatitude Teleconnections in CMIP6 E. Galytska et al. 10.1029/2022JD037978
- Splitting of the Wave Disturbance Spectrum in the Isothermal Atmosphere Due to Its Rotation O. Cheremnykh et al. 10.3103/S0884591323060028
- Splitting of the wave disturbance spectrum in the isothermal atmosphere due to its rotation O. Cheremnykh et al. 10.15407/kfnt2023.06.003
- Reconciling conflicting evidence for the cause of the observed early 21st century Eurasian cooling S. Outten et al. 10.5194/wcd-4-95-2023
- Radiological Evaluation of Non-infectious Mastitis Outside the Idiopathic Granulomatous R. Yılmaz & R. Günöz Cömert 10.4274/trs.2023.2319124
9 citations as recorded by crossref.
- The possible links between the Barents–Kara sea‐ice area, Ural blocking, and the North Atlantic Oscillation R. Ahmadi & O. Alizadeh 10.1002/qj.4560
- The maintenance of coherent vortex topology by Lagrangian chaos in drift-Rossby wave turbulence N. Cao & D. Qi 10.1063/5.0207687
- The Summer North Atlantic Oscillation, Arctic sea ice, and Arctic jet Rossby wave forcing C. Folland et al. 10.1126/sciadv.adk6693
- Physical mechanisms for the dominant summertime high-latitude atmospheric teleconnection pattern and the related Northern Eurasian climates J. Kim & K. Seo 10.1088/1748-9326/acfa13
- Movement of decaying quasi-2-day wave in the austral summer-time mesosphere C. Salinas & D. Wu 10.1038/s41598-024-68559-5
- Influence of Sudden Stratospheric Warmings on the Migrating Diurnal Tide in the Equatorial Middle Atmosphere Observed by Aura/Microwave Limb Sounder K. Hocke 10.3390/atmos14121743
- Persistent warm and cold spells in the Northern Hemisphere extratropics: regionalisation, synoptic-scale dynamics and temperature budget A. Tuel & O. Martius 10.5194/wcd-5-263-2024
- Circulation responses to surface heating and implications for polar amplification P. Siew et al. 10.5194/wcd-5-985-2024
- Evaluating Causal Arctic‐Midlatitude Teleconnections in CMIP6 E. Galytska et al. 10.1029/2022JD037978
4 citations as recorded by crossref.
- Splitting of the Wave Disturbance Spectrum in the Isothermal Atmosphere Due to Its Rotation O. Cheremnykh et al. 10.3103/S0884591323060028
- Splitting of the wave disturbance spectrum in the isothermal atmosphere due to its rotation O. Cheremnykh et al. 10.15407/kfnt2023.06.003
- Reconciling conflicting evidence for the cause of the observed early 21st century Eurasian cooling S. Outten et al. 10.5194/wcd-4-95-2023
- Radiological Evaluation of Non-infectious Mastitis Outside the Idiopathic Granulomatous R. Yılmaz & R. Günöz Cömert 10.4274/trs.2023.2319124
Latest update: 20 Nov 2024
Executive editor
The paper by Tim Woollings et al. provides first a theoretical summary of the role of Rossby wave dynamics for polar variability, regarding the large-scale polar flow conceptually as a superposition of geostrophic turbulence and Rossby wave propagation, emphasising the key role of isolated vortices at high latitudes. In a second part, the paper addresses how comparatively weak Rossby waves can be triggered from high latitudes in the presence of a relative vorticity gradient as a direct response to sea ice loss, which often manifests as a heat low. The paper provides a well written and much needed foundation for an active area of research.
The paper by Tim Woollings et al. provides first a theoretical summary of the role of Rossby...
Short summary
This paper investigates large-scale atmospheric variability in polar regions, specifically the balance between large-scale turbulence and Rossby wave activity. The polar regions are relatively more dominated by turbulence than lower latitudes, but Rossby waves are found to play a role and can even be triggered from high latitudes under certain conditions. Features such as cyclone lifetimes, high-latitude blocks, and annular modes are discussed from this perspective.
This paper investigates large-scale atmospheric variability in polar regions, specifically the...