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James H. Ruppert Jr. and Fuqing Zhang

distinction in phase speed remains unclear; however, density current theory may at least shed light on the propagation rate of individual rainfall systems. This is explored next. Cross sections depicting the low-level atmospheric structure, both in the zonal and in the diagonal (cross-Sumatra) contexts, are provided in Figs. 11 and 12 . In the boundary layer over and west of Borneo, low-level isentropes (of constant θ υ ) reveal a localized surface-based cold anomaly extending from the landmass across

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