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Patrick A. Reinecke and Dale R. Durran

diabatic effects associated with moist processes are modulating the strength of the windstorm. Jiang and Doyle (2009) argued that low-level moisture during IOP 6 strengthened the mountain-wave response by reducing the below-mountaintop stability and decreasing the depth of the blocked layer. To asses the role of moisture and latent heating on the error growth of the Owens Valley metric a “dry” version of the IOP 6 ensemble simulation is conducted in which diabatic and radiative effects associated

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