Entrainment in dry and moist thermals
G. R. Vybhav and S. Ravichandran
Phys. Rev. Fluids 7, 050501 (2022) - Published 17 May, 2022
Entrainment is the process by which ambient fluid is incorporated into the flow and remains poorly understood. In cumulus clouds, entrainment governs the altitude attained by the cloud and the resulting droplet size distribution, which together determine the radiative contribution to the global energy balance. The release of latent heat by the condensation of water vapor drives the flow in cumulus clouds, which often resemble a series of isolated parcels of buoyancy, or thermals. Here, using direct numerical simulation (DNS), we study the effects of condensation heating on the entrainment in a moist thermal in contrast with a dry thermal that has no buoyancy sources.







































