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Jason E. Nachamkin

explicitly resolving finescale phenomena. Even small phase errors can result in major losses in correlation between the forecast and the observations ( Murphy 1988 ). In response, a diverse number of verification methods have been developed to address this problem (e.g., Baldwin et al. 2002 ; Casati et al. 2004 ; Ebert and McBride 2000 ; Davis et al. 2006 ; Marzban and Sangathe 2006 ; Roberts and Lean 2008 ). Many of the verification methods mentioned above are evaluated in this special issue of

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