Articles | Volume 2, issue 1
https://doi.org/10.5194/wcd-2-19-2021
© Author(s) 2021. 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-2-19-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
15 Jan 2021
Research article |
| 15 Jan 2021
| 15 Jan 2021
Polar lows – moist-baroclinic cyclones developing in four different vertical wind shear environments
Patrick Johannes Stoll
CORRESPONDING AUTHOR
Department of Physics and Technology, Arctic University of Norway, Tromsø, Norway
Thomas Spengler
Geophysical Institute, University of Bergen, and Bjerknes Centre for Climate Research, Bergen, Norway
Annick Terpstra
Geophysical Institute, University of Bergen, and Bjerknes Centre for Climate Research, Bergen, Norway
Rune Grand Graversen
Department of Physics and Technology, Arctic University of Norway, Tromsø, Norway
Norwegian Meteorological Institute, Tromsø, Norway
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Cited
17 citations as recorded by crossref.
- The global atmospheric energy transport analysed by a wavelength-based scale separation P. Stoll et al. 10.5194/wcd-4-1-2023
- Developing a methodology for user‐oriented verification of polar low forecasts M. Hallerstig et al. 10.1002/qj.4819
- A global climatology of polar lows investigated for local differences and wind-shear environments P. Stoll 10.5194/wcd-3-483-2022
- Impact of sea spray‐mediated heat fluxes on polar low development T. Lin et al. 10.1002/qj.4746
- The Response of Northern Hemisphere Polar Lows to Climate Change in a 25 km High‐Resolution Global Climate Model H. Bresson et al. 10.1029/2021JD035610
- Interactive 3-D visual analysis of ERA5 data: improving diagnostic indices for marine cold air outbreaks and polar lows M. Meyer et al. 10.5194/wcd-2-867-2021
- Arctic Maritime Cyclone Distribution and Trends in the ERA5 Reanalysis Z. Chen & A. Lynch 10.1175/JAMC-D-21-0016.1
- Analysis of the Development Mechanisms of a Polar Low over the Norwegian Sea Simulated with the Canadian Regional Climate Model M. Moreno-Ibáñez et al. 10.3390/atmos14060998
- Sensitivity of Air‐Sea Heat Exchange in Cold‐Air Outbreaks to Model Resolution and Sea‐Ice Distribution C. Spensberger & T. Spengler 10.1029/2020JD033610
- Application of low-altitude wind shear recognition algorithm and laser wind radar in aviation meteorological services T. Xu et al. 10.1515/phys-2023-0154
- Modulation of Polar Low Activity by the Madden‐Julian Oscillation Z. Wang et al. 10.1029/2023GL103719
- Modulation of North Atlantic Polar Low Activity and Associated Flow Patterns by Sudden Stratospheric Warmings C. Chang et al. 10.1175/JCLI-D-21-0905.1
- The importance of diabatic processes for the dynamics of synoptic-scale extratropical weather systems – a review H. Wernli & S. Gray 10.5194/wcd-5-1299-2024
- Assessment of simulations of a polar low with the Canadian Regional Climate Model M. Moreno-Ibáñez et al. 10.1371/journal.pone.0292250
- Polar low research: recent developments and promising courses of research M. Moreno-Ibáñez 10.3389/feart.2024.1368179
- Recognition of Polar Lows in Sentinel-1 SAR Images With Deep Learning J. Grahn & F. Bianchi 10.1109/TGRS.2022.3204886
- Influence of mesoscale sea surface temperature anomaly on polar lows T. Lin et al. 10.1088/1748-9326/ad9ec6
17 citations as recorded by crossref.
- The global atmospheric energy transport analysed by a wavelength-based scale separation P. Stoll et al. 10.5194/wcd-4-1-2023
- Developing a methodology for user‐oriented verification of polar low forecasts M. Hallerstig et al. 10.1002/qj.4819
- A global climatology of polar lows investigated for local differences and wind-shear environments P. Stoll 10.5194/wcd-3-483-2022
- Impact of sea spray‐mediated heat fluxes on polar low development T. Lin et al. 10.1002/qj.4746
- The Response of Northern Hemisphere Polar Lows to Climate Change in a 25 km High‐Resolution Global Climate Model H. Bresson et al. 10.1029/2021JD035610
- Interactive 3-D visual analysis of ERA5 data: improving diagnostic indices for marine cold air outbreaks and polar lows M. Meyer et al. 10.5194/wcd-2-867-2021
- Arctic Maritime Cyclone Distribution and Trends in the ERA5 Reanalysis Z. Chen & A. Lynch 10.1175/JAMC-D-21-0016.1
- Analysis of the Development Mechanisms of a Polar Low over the Norwegian Sea Simulated with the Canadian Regional Climate Model M. Moreno-Ibáñez et al. 10.3390/atmos14060998
- Sensitivity of Air‐Sea Heat Exchange in Cold‐Air Outbreaks to Model Resolution and Sea‐Ice Distribution C. Spensberger & T. Spengler 10.1029/2020JD033610
- Application of low-altitude wind shear recognition algorithm and laser wind radar in aviation meteorological services T. Xu et al. 10.1515/phys-2023-0154
- Modulation of Polar Low Activity by the Madden‐Julian Oscillation Z. Wang et al. 10.1029/2023GL103719
- Modulation of North Atlantic Polar Low Activity and Associated Flow Patterns by Sudden Stratospheric Warmings C. Chang et al. 10.1175/JCLI-D-21-0905.1
- The importance of diabatic processes for the dynamics of synoptic-scale extratropical weather systems – a review H. Wernli & S. Gray 10.5194/wcd-5-1299-2024
- Assessment of simulations of a polar low with the Canadian Regional Climate Model M. Moreno-Ibáñez et al. 10.1371/journal.pone.0292250
- Polar low research: recent developments and promising courses of research M. Moreno-Ibáñez 10.3389/feart.2024.1368179
- Recognition of Polar Lows in Sentinel-1 SAR Images With Deep Learning J. Grahn & F. Bianchi 10.1109/TGRS.2022.3204886
- Influence of mesoscale sea surface temperature anomaly on polar lows T. Lin et al. 10.1088/1748-9326/ad9ec6
Latest update: 04 Mar 2025
Short summary
Polar lows are intense meso-scale cyclones occurring at high latitudes. The research community has not agreed on a conceptual model to describe polar-low development. Here, we apply self-organising maps to identify the typical ambient sub-synoptic environments of polar lows and find that they can be described as moist-baroclinic cyclones that develop in four different environments characterised by the vertical wind shear.
Polar lows are intense meso-scale cyclones occurring at high latitudes. The research community...
