All cirriform clouds are classified as high and therefore constitute a single cloud genus altocumulus.
2.
Contrails formed from the exhaust of aircraft flying in the high �tage can persist and spread into formations resembling any of the high cloud genus-types.
3.
Low stratus clouds usually produce only light precipitation, but this always occurs as the feature praecipitatio due to the fact this cloud genus lies too close to the ground to allow for the formation of virga.
4.
It has basically all the weather-associated cloud genus types generated by active wind circulation, although very tall cumulonimbus thunder clouds can penetrate the tropopause from below and rise into the lower part of the stratosphere.
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