2 ਜਾਂ 3 ਮੀਲ ਦੀ ਵਿਚਕਾਰਲੀ ਉਚਾਈ 'ਤੇ ਤੂਫਾਨ ਦੇ ਬੱਦਲ,

altostratus's Usage Examples:

Variants When sheet of altostratus cloud is seen lower down and skirting a cumulonimbus cloud, it is classified as a velum cloud.

They are also often seen underneath the cirrostratus and altostratus sheets that often precede a warm front, as these higher clouds decrease.

precipitation increases in persistence and intensity, the altostratus cloud may thicken into nimbostratus.

conjoined altocumulus perlucidus is sometimes found preceding a weakening warm front, where the altostratus is starting to fragment, resulting in patches of.

thickening and lowering of these high clouds into middle-stage altostratus or altocumulus is a good sign the warm front or low has moved closer and precipitation.

Fractonimbus exist only under precipitation clouds (such as nimbostratus, altostratus or cumulonimbus), and don"t produce precipitation themselves.

preceded by higher-level clouds such as cirrostratus and altostratus.

The altostratus undulatus is a type of altostratus cloud with signature undulations within it.

They are sometimes similar to altostratus and are distinguishable from the latter because the sun or moon is always.

Areas of cirrocumulus and altocumulus within cirrostratus and altostratus more commonly seen than at a warm.

when a high grey nebulous altostratus layer thins out into a whitish layer of featureless high cloud.

Genus altostratus (As): Altostratus is a midlevel opaque or translucent nonconvective veil of grey/blue-grey.

visible through transparent cirrostratus, in contrast to altostratus which tends to be opaque or translucent.