BEGIN:VCALENDAR VERSION:2.0 PRODID:-//132.216.98.100//NONSGML kigkonsult.se iCalcreator 2.20.4// BEGIN:VEVENT UID:20250806T031636EDT-2720POSpoD@132.216.98.100 DTSTAMP:20250806T071636Z DESCRIPTION:The Shallow-to-Deep Convective Transition Over an Idealized Mes oscale Convergence Zone\n\nAbstract\n\nThe initiation of deep convection w ithin a conditionally unstable atmosphere requires air parcels to reach th eir level of free convection\, above which latent-heat release generates p ositive buoyancy. However\, air parcels that satisfy this condition often fail to undergo deep ascent due to mitigating factors such as entrainment and adverse perturbation vertical pressure gradients. Recent studies sugge st that the transition from shallow-to-deep convection may additionally re quire the formation of evaporative cold pools\, a sufficient cloud-layer l apse rate\, gradual moistening of the mid-troposphere through shallow-cumu lus detrainment\, and/or the fortuitous development of new cumuli through the remnants of their predecessors. In this study\, we use cloud-resolving simulations of cumulus convection over an idealized surface-based converg ence zone to study the mechanisms and sensitivities of deep-convection ini tiation forced by mesoscale ascent. The surface convergence forms in respo nse to a localized diurnal heating anomaly over an otherwise homogenous an d unheated surface\, producing an organized boundary-layer updraft with a maximal amplitude of around 3 m/s over the center of the heat source. It g ives rise to a line of cumuli that gradually deepens and\, in some cases\, transitions into deep convection. Detailed analysis of the simulations re veals several notable aspects of cumulus evolution. For example\, with a t hermal tracking algorithm developed for the purpose\, it can be shown that \, in a marginally unstable atmosphere\, the average horizontal area of th e thermal just above the lower condensation level (LCL) is an important fa ctor in determining the height reached by the thermal.\n DTSTART:20151202T193000Z DTEND:20151202T200000Z LOCATION:Room 934\, Burnside Hall\, CA\, QC\, Montreal\, H3A 0B9\, 805 rue Sherbrooke Ouest SUMMARY:Student Seminar: Raphael Rousseau-Rizzi URL:/meteo/channels/event/student-seminar-raphael-rous seau-rizzi-255062 END:VEVENT END:VCALENDAR