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

located across the northern South China Sea and Philippines archipelago during the intermediate phases, similar to the location of the convectively enhanced regime during the later phases of the MJO. This similar, phase-shifted relationship between the enhanced and suppressed phases of the MJO suggests that convective depth may be tied to geographical variability within the Maritime Continent, which does not seem to be the case for cell longevity, expanse, or number. 6. Convection evolution and the

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James H. Ruppert Jr. and Fuqing Zhang

further evidence in support of this view. Yet, unique from other regions, the specific geography of the MC may favor a unique phase speed and/or amplify a specific mode; namely, this can occur owing to diurnal phase locking across multiple islands and diurnal cycles, as will be described. Given the difficulty of adequately observing such high-frequency modes, to explore this phenomenon herein we exploit an observationally validated cloud-permitting model simulation that explicitly represents both

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