
Cumulus mediocris
© Wetterkurs.ch
The name "mediocris" (Latin: moderate, medium-sized) describes a cumulus cloud of moderate vertical extent that appears clearly taller than it is wide, placing it between the flat Cumulus humilis and the towering Cumulus congestus. The top already shows slight turrets and rounded swellings, but does not yet have the cauliflower-like, sharply defined contours characteristic of Cumulus congestus. The cloud typically forms during the course of the day through increasing convective heating and represents a transitional stage in cumulus development. Cumulus mediocris occurs preferentially in the afternoon hours and can, given sufficient moisture and instability, continue to develop into Cumulus congestus or even Cumulonimbus. The base is usually flat and sharply defined, while the top appears bright and luminously white.
Highlighted: all genera with which mediocris occurs.
Cumulus mediocris indicates increasing atmospheric instability and growing convection. Its appearance suggests that thermals are becoming more vigorous and that the atmosphere contains sufficient moisture for further vertical cloud development. With continued heating and adequate instability, Cumulus mediocris can develop into Cumulus congestus and ultimately into Cumulonimbus, which may result in local showers or thunderstorms. If development stalls at this stage, dry weather with intermittent cloud cover can generally be expected. Cumulus mediocris alone does not typically produce precipitation, but is considered an early indicator of possible convective precipitation later in the day.