Controls on the Development and Circulation of Terminal versus Transient Congestus Clouds and Implications for Midlevel Aerosol Transport

Abstract Cumulus congestus is the middle mode of tropical convection, with cloud tops around or exceeding the 0ºC level (~5km AGL). While some congestus are terminal, meaning capped by the 0°C stable layer, others are transient and may develop into deep convection. Although this distinction impacts convective transport of water vapor and aerosols into the mid-troposphere and the congestus-to-deep convection transition, there is still much to be understood about the processes causing congestus to overshoot the 0°C level and continue growing. We simulate a field of tropical congestus using high-resolution idealized model simulations, identify and track the updrafts, and composite congestus properties. Terminal and transient congestus updrafts are characterized by a similar overturning circulation between the updraft and subsiding shell. However, transient congestus have stronger updrafts, and the downward branch of their corresponding circulations are constrained by the 0°C level. The balance between buoyancy and perturbation pressure gradient accelerations predominantly determines the shape of the vertical velocity profile, though vertical advection through bulk and sub-plume fluctuations are also shown to be important near and above the 0°C level. Our findings support previous results suggesting buoyancy as a control on congestus height. We find that congestus developing in more humid midlevel environments are more likely to be transient. Finally, we explore how congestus updrafts influence their near moisture and aerosol environments: terminal congestus return more aerosol to the atmosphere through evaporation along their edges, while transient congestus create stronger midlevel detrainment layers of aerosol and water vapor due to the trapping of the regenerated aerosol above the 0°C level.