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: Academy of Finland
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2019
• Subjects: Barents Sea; Svalbard; North Atlantic
• Online Access: http://dx.doi.org/10.1002/qj.3707; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fqj.3707; https://onlinelibrary.wiley.com/doi/pdf/10.1002/qj.3707; https://onlinelibrary.wiley.com/doi/full-xml/10.1002/qj.3707; https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.3707

Abstract 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–Väisälä 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.