15 citations as recorded by crossref.

1. Modulation of Polar Low Activity by the Madden‐Julian Oscillation Z. Wang et al. 10.1029/2023GL103719
2. The Value of Sentinel-1 Ocean Wind Fields Component for the Study of Polar Lows E. Khachatrian & P. Asemann 10.3390/rs16203755
3. 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
4. Extreme Wind Speeds in the Atlantic Sector of the Arctic: Statistics and Circulation Models A. Kislov et al. 10.1134/S0001433824700531
5. Subseasonal Predictions of Polar Low Activity Using a Hybrid Statistical‐Dynamical Approach K. Boyd et al. 10.1029/2022GL102145
6. Spatiotemporal Patterns of Polar Low Activity Over the Southern Ocean H. Farjami & A. Kazemi 10.1029/2023JD039832
7. Warm Core and Deep Convection in Medicanes: A Passive Microwave-Based Investigation G. Panegrossi et al. 10.3390/rs15112838
8. A Meso-scale Low System with a Multi-scale Structure, Developed over the East Sea on 20 January 2017: Sensitivity Experiments Y. Kim & J. Lee 10.9798/KOSHAM.2022.22.2.1
9. Arctic cyclones have become more intense and longer-lived over the past seven decades X. Zhang et al. 10.1038/s43247-023-01003-0
10. Polar low research: recent developments and promising courses of research M. Moreno-Ibáñez 10.3389/feart.2024.1368179
11. Arctic and Sub‐Arctic Mechanisms Explaining Observed Increasing Northward Flow Through the Bering Strait and Why Models May Be Getting It Wrong C. Peralta‐Ferriz & R. Woodgate 10.1029/2023GL104697
12. Influence of mesoscale sea surface temperature anomaly on polar lows T. Lin et al. 10.1088/1748-9326/ad9ec6
13. 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
14. Marine Operations in the Norwegian Sea and the Ice-Free Part of the Barents Sea with Emphasis on Polar Low Pressures O. Gudmestad 10.3390/w16223313
15. A global climatology of polar lows investigated for local differences and wind-shear environments P. Stoll 10.5194/wcd-3-483-2022