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In this study, CPEX observations are used in combination with idealized tropical oceanic convection simulations from the Cloud Model 1 (CM1) numerical model to investigate relationships between tropical oceanic convection and relative humidity and vertical wind shear over different vertical layers. Simulations are initialized by and nudged to moist tropical soundings informed by typical near-storm environmental moisture and wind profiles from the CPEX campaign series to analyze their influence on domain-wide convective organization and vertical structure. In particular, sensitivity tests varying moisture in the planetary boundary layer and below and above the freezing level will be discussed, as well as sensitivity tests involving the introduction of a mid-level easterly jet and varying deep layer wind shear. Results from these idealized numerical model simulations in the context of observations will be presented, including comparisons with similar analysis of tropical oceanic convective structure from the CPEX field campaign series.
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