Trends in cyclones in the high-latitude North Atlantic during 1979-2016

• Published in: Quarterly Journal of the Royal Meteorological Society
• Main Authors: Wickström, S., Jonassen, M. O., Vihma, T., Uotila, P.
• Other Authors: INAR Physics, Staff Services
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2021
• Subjects: Arctic; Barents Sea; Eady growth rate; extratropical cyclones; Scandinavian pattern; sea ice decline; storm tracks; Svalbard; ATMOSPHERIC MOISTURE TRANSPORT; SEA-ICE; ARCTIC CYCLONE; CLIMATE-CHANGE; VARIABILITY; CIRCULATION; ISFJORDEN; MANIFEST; 1172 Environmental sciences; 1171 Geosciences; Climate change; Isfjord*; Isfjorden; North Atlantic; Sea ice
• Online Access: http://hdl.handle.net/10138/325689

We report an increase in winter (DJF) cyclone densities in the areas around Svalbard and in northwestern Barents Sea and a decrease in cyclone densities in southeastern Barents Sea during 1979-2016. Despite high interannual variability, the trends are significant at the 90% confidence level. The changes appear as a result of a shift into a more meridional winter storm track in the high-latitude North Atlantic, associated with a positive trend in the Scandinavian Pattern. A significant decrease in the Brunt-Vaisala frequency east of Svalbard and a significant increase in the Eady Growth Rate north of Svalbard indicate increased baroclinicity, favouring enhanced cyclone activity in these regions. For the first time, we apply composite analysis to explicitly address regional consequences of these wintertime changes in the high-latitude North Atlantic. We find a tendency toward a warmer and more moist atmospheric state in the Barents Sea and over Svalbard with increased cyclone activity around Svalbard. Peer reviewed