
Cirrus floccus
© Wetterkurs.ch
The name "floccus" (Latin: flake, tuft) describes the characteristic appearance of this cirrus species, which occurs in the form of small, rounded tufts or flakes. Cirrus floccus consists of small, cumuliform cloud puffs with a slightly frayed base, often accompanied by fall streaks (virga). These clouds form at high altitudes, where local instabilities in thin air layers lead to convective updrafts. The individual tufts often appear irregularly distributed across the sky and can dissolve rapidly or transition into other cirrus forms. Cirrus floccus is a rather rare sight and is sometimes confused with cirrocumulus, but is larger and less regularly arranged.
Highlighted: all genera with which floccus occurs.
Cirrus floccus indicates local instability in the upper troposphere, suggesting moisture advection and turbulence at high altitudes. When this cloud form appears more frequently, it can be an early sign of an approaching warm front or an approaching low-pressure system. In combination with increasing cloud thickening — for example, transitioning to cirrostratus — the probability of precipitation in the following 12 to 24 hours increases. When occurring in isolation and without any tendency toward thickening, the cloud is of lesser meteorological significance, merely indicating moisture at altitude. For aviation, cirrus floccus is an indicator of possible light to moderate turbulence in the upper troposphere.