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postulated (e.g., Ciesielski et al. 2017 ). This feedback focuses more on the interaction of the large-scale circulation with convective variability at smaller scales, such as through shallow-to-deep convective transitions (e.g., Xu and Rutledge 2016 ) and through the diurnal cycle ( Ruppert and Johnson 2015 ). Accurate estimates of the moisture field and its variability at a range of time scales are essential for studying convection and its two-way interaction with humidity. The continuing number of
postulated (e.g., Ciesielski et al. 2017 ). This feedback focuses more on the interaction of the large-scale circulation with convective variability at smaller scales, such as through shallow-to-deep convective transitions (e.g., Xu and Rutledge 2016 ) and through the diurnal cycle ( Ruppert and Johnson 2015 ). Accurate estimates of the moisture field and its variability at a range of time scales are essential for studying convection and its two-way interaction with humidity. The continuing number of
