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Benjamin A. Toms, Susan C. van den Heever, Emily M. Riley Dellaripa, Stephen M. Saleeby, and Eric D. Maloney

considered the MJO to have consistent characteristics throughout the entire year ( Hendon and Salby 1994 ; Wheeler and Hendon 2004 ). However, it has been shown that the consideration of the seasonality of the MJO is important both for developing real-time proxies for its location and magnitude and for process-based studies ( Kikuchi et al. 2012 ; Kiladis et al. 2014 ; Jiang et al. 2018 ). Within this study, we focus on cross-scale interactions within the boreal summer MJO, which has been labeled with

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Emily M. Riley Dellaripa, Eric D. Maloney, Benjamin A. Toms, Stephen M. Saleeby, and Susan C. van den Heever

explicitly been discussed in the literature, Figs. 4 and 10 of Neena et al. (2017) and Fig. 3 of Sobel et al. (2010) imply such interactions are possible and serve as motivation for this work to explicitly understand the impact topography has on the diurnal cycle of precipitation during BSISO suppressed versus active conditions. Along with the effects of topography over the MC on MJO evolution, previous work has suggested that the diurnal cycle (DC) of precipitation (DCP) over the MC has important

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