Examining the predictability of the Stratospheric Sudden Warming of January 2013 using multiple NWP systems

• Published in: Monthly Weather Review
• Main Authors: Tripathi, Om P., Baldwin, Mark, Charlton-Perez, Andrew, Charron, Martin, Cheung, Jacob C. H., Eckermann, Stephen D., Gerber, Edwin, Jackson, David R., Kuroda, Yuhji, Lang, Andrea, Mclay, Justin, Mizuta, Ryo, Reynolds, Carolyn, Roff, Greg, Sigmond, Michael, Son, Seok-Woo, Stockdale, Tim
• Format: Article in Journal/Newspaper
• Language: English
• Published: American Meteorological Society 2016
• Subjects: North Atlantic
• Online Access: https://centaur.reading.ac.uk/56573/; https://centaur.reading.ac.uk/56573/1/mwr-d-15-0010%252E1.pdf; https://doi.org/10.1175/MWR-D-15-0010.1

The first multi-model study to estimate the predictability of a boreal Sudden Stratospheric Warming (SSW) is performed using five NWP systems. During the 2012-2013 boreal winter, anomalous upward propagating planetary wave activity was observed towards the end of December, which followed by a rapid deceleration of the westerly circulation around 2 January 2013, and on 7 January 2013 the zonal mean zonal wind at 60°N and 10 hPa reversed to easterly. This stratospheric dynamical activity was followed by an equatorward shift of the tropospheric jet stream and by a high pressure anomaly over the North Atlantic, which resulted in severe cold conditions in the UK and Northern Europe. In most of the five models, the SSW event was predicted 10 days in advance. However, only some ensemble members in most of the models predicted weakening of westerly wind when the models were initialized 15 days in advance of the SSW. Further dynamical analysis of the SSW shows that this event was characterized by the anomalous planetary wave-1 amplification followed by the anomalous wave-2 amplification in the stratosphere, which resulted in a split vortex occurring between 6 January 2013 and 8 January 2013. The models have some success in reproducing wave-1 activity when initialized 15 days in advance, they but generally failed to produce the wave-2 activity during the final days of the event. Detailed analysis shows that models have reasonably good skill in forecasting tropospheric blocking features that stimulate wave-2 amplification in the troposphere, but they have limited skill in reproducing wave-2 amplification in the stratosphere.