Abstract

Designated a new cloud feature in 2017, asperitas clouds are wave-like formations on the underside of layer clouds. We propose a mechanism for asperitas cloud formation: an instability driven by the settling and evaporation of water droplets. For suitable droplet size and liquid water content, a layer of dense air forms, which in moderate ambient shear gives rise to cloud structures of the asperitas type.

Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call