Cosmos

CLOUD ATLAS

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The words may sound confusing, but giving a name to your cloud is as easy as knowing its level and its shape. Missing from this classifier are the multi-levelled nimbo- clouds: endless grey nimbostrat­us (behind) and the majestic thundersto­rm cloud cumulonimb­us (right).

Nate’s Fab Five

Choosing a favourite cloud is as hard as picking a favourite child, but here are a few stand outs:

MAMMA

Often called mammatus clouds, these are ominous, pendulous lobes that can be found hanging underneath a cumulonimb­us in the right circumstan­ces. They often indicate a severe storm cell.

FLUCTUS

An accessory cloud that gets physicists excited. Curled wave formations called Kelvin-helmholtz waves are caused when an airmass interacts with another above it that’s moving at a different speed or in a different direction. Nothing significan­t weather-wise, but a rare delight to spot.

PILEUS

When a rising airmass is creating a cloud, it can force a layer of air above it to rise, creating a small stratus above the upwelling cumulus, like a cloud with a whimsical hat.

HOMOGENITU­S

Clouds created by human activity, like cumulus forming above a smokestack or cirrus left behind a jet in a contrail (ice particles formed in the wake of the jet by a pressure disturbanc­e).

FLAMMAGENI­TUS

Clouds formed by the heat rising from a fire. The one you’ll hear about most is commonly called pyrocumulo­nimbus, but its official designatio­n is cumulonimb­us flammageni­tus. These clouds are incredibly difficult to forecast and can cause widespread havoc with sudden changes of wind direction and lightning.

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