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Krzysztof Wargan and Lawrence Coy

-2 and in the model. The 2009 SSW was chosen for this case study because the increase of the TIL’s strength associated with it was exceptionally strong compared to other recent SSW events. In a later part of the paper, we place the analysis in the broader context of other boreal winters in the past decade. Older data assimilation systems failed to represent the TIL correctly ( Birner et al. 2006 ) owing to excessive vertical smoothing. However, more recent reanalyses do reproduce the near

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