Abstract
At night, the low-level water vapor and mass convergence that precedes convective rainfall is typically elevated about 1.5 km above the surface. We use 15 summers (2009–2023) of meteorological data from the Rapid Refresh/Rapid Update Cycle analysis, and rainfall data from the IMERG dataset, to show that elevated rain events over the Great Plains can be most clearly distinguished from surface-based events during their developmental stage, 0–3 hours prior to peak rainfall. The upward shift in low-level water vapor and mass convergence that is characteristic of elevated convection during the development phase usually occurs after local midnight, and is accompanied by an increase in low-level stability, convective inhibition (CIN), and in the height of maximum Convective Available Potential Energy (CAPE). While the Nocturnal Low-Level Jet (NLLJ) plays a major role in promoting nocturnal convection by modifying the low-level stability and providing favorable wind and moisture conditions, the region of elevated nocturnal convection extends over much of the interior of North America, far beyond the immediate influence of the NLLJ. Upward shifts in water vapor convergence and CAPE also appear in rain weighted composites against the mean low-level lapse rate. Water vapor convergence in the layer 1.5–3 km above the surface is more efficient at promoting nocturnal convection when it is positively correlated with CAPE at a similar altitude. Finally, we show that elevated nocturnal rain events exhibit stronger low-level warm anomalies, and weaker cold anomalies, than surface-based nocturnal rain events.
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