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Young-Joon Kim, William Campbell, and Benjamin Ruston

al. 1987 ). A successful simulation/forecast of the SSW is a useful indication of an atmospheric model’s capability to capture the forcing, propagation, and breaking of planetary waves and is, thus, an indication of the adequate representation of the stratosphere–troposphere coupling in the model. Part I of our study ( Kim and Flatau 2010 , hereafter referred to as KF ) presented our effort to improve the hindcasting of the 2009 late January Arctic SSW ( Manney et al. 2009 ) utilizing a stand

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