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Robert Wood

al. 1999 ), or for point observations, out to time scales of several hours or more ( Wood and Taylor 2001 ; Comstock et al. 2005 ). This scaling regime in the beta and gamma mesoscales is frequently associated with mesoscale cellular convection and is imprinted on the cloud liquid water or cloud optical thickness field ( Cahalan and Snider 1989 ; Cahalan et al. 1994 ; Davis et al. 1996 , 1999 ; Wood and Taylor 2001 ; Wood et al. 2002b ; Wood and Hartmann 2006 ). Thus, there is rarely a

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Craig S. Schwartz and Ryan A. Sobash

, doi: 10.1175/WAF-D-12-00022.1 . 10.1175/WAF-D-12-00022.1 Tegen , I. , P. Hollrig , M. Chin , I. Fung , D. Jacob , and J. Penner , 1997 : Contribution of different aerosol species to the global aerosol extinction optical thickness: Estimates from model results . J. Geophys. Res. , 102 , 23 895 – 23 915 , doi: 10.1029/97JD01864 . 10.1029/97JD01864 Theis , S. E. , A. Hense , and U. Damrath , 2005 : Probabilistic precipitation forecasts from a deterministic model: A

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