Stratus silvagenitus

Source: Wikipedia, the free encyclopedia.
Stratus silvagenitus
Precipitation
None

Stratus silvagenitus is a type of

relative humidity levels, for example, after precipitation has passed, through evaporation and/or evapotranspiration.[2]

Silvagenitus cloud formed over a coastal mountain.

If the cloud is uniform, it is called a "stratus" silvagenitus cloud, if the cloud is ragged and wispy, then it is called a "stratus

adiabatic cooling like in cumulus
clouds.

References

  1. ^ "Learn About Silvagenitus Clouds: Evaporation from a Forest". Archived from the original on 2021-11-13.
  2. ^ "Silvagenitus". Archived from the original on 2021-11-10.