Forecasting extreme stratospheric polar vortex events

• Published in: Nature communications Vol. 11; no. 1; p. 4630
• Main Authors: Gray, L. J., Brown, M. J., Knight, J., Andrews, M., Lu, H., O’Reilly, C., Anstey, J.
• Format: Journal Article
• Language: English
• Published: London Nature Publishing Group UK 15-09-2020; Nature Publishing Group; Nature Portfolio
• Subjects: 639/766/189; 704/106/35/823; 704/106/694/1108; 704/106/694/2786; Fluid flow; Humanities and Social Sciences; multidisciplinary; Ozone; Polar vortex; Science; Science (multidisciplinary); Stratosphere; Stratospheric warming; Troposphere; Vortices; Weather forecasting; Winter
• ISSN: 2041-1723; 2041-1723
• DOI: 10.1038/s41467-020-18299-7

Extreme polar vortex events known as sudden stratospheric warmings can influence surface winter weather conditions, but their timing is difficult to predict. Here, we examine factors that influence their occurrence, with a focus on their timing and vertical extent. We consider the roles of the troposphere and equatorial stratosphere separately, using a split vortex event in January 2009 as the primary case study. This event cannot be reproduced by constraining wind and temperatures in the troposphere alone, even when the equatorial lower stratosphere is in the correct phase of the quasi biennial oscillation. When the flow in the equatorial upper stratosphere is also constrained, the timing and spatial evolution of the vortex event is captured remarkably well. This highlights an influence from this region previously unrecognised by the seasonal forecast community. We suggest that better representation of the flow in this region is likely to improve predictability of extreme polar vortex events and hence their associated impacts at the surface.
Extreme events high up in the winter stratosphere are known to influence our weather and their predictability has potential to improve seasonal weather forecasts. Here, the authors examine factors that influence their generation and highlight a previously unrecognised sensitivity to the upper equatorial stratosphere.