When the threat of severe weather looms, clouds are often the first sign that skies are turning unfriendly. Look for the following types of clouds during disturbed weather; recognizing them and the severe weather they're linked to could give you a head start to finding shelter. Once you know which clouds are related to severe weather and what they look like, you'll be one step closer to becoming a Kernow Weather Team storm spotter.
Asperitas cloudss are another cloud type that resembles a roughened sea surface. They appear as if you were underwater looking upward toward the surface when the sea is particularly roughened and chaotic.
Although they look like dark and storm-like doomsday clouds, asperitas tend to develop after convective thunderstorm activity has developed. Much is still unknown about this cloud type, as it is the newest species to be added to the World Meteorological Organization's International Cloud Atlas in over 50 years
Whoever first exclaimed "The sky is falling!" must have seen mammatus clouds overhead. Mammatus appear as bubble-like pouches that hang on the underside of clouds. As odd as they look, mammatus aren't dangerous — they simply signal that a storm may be nearby.
When seen in association with thunderstorm clouds, they're typically found on the underside of anvils.
Cumulonimbus clouds are thunderstorm clouds. They develop from convection — the transport of heat and moisture upward into the atmosphere. But, whereas other clouds form when air currents rise several thousand feet and then condense where those currents stop, the convective air currents that create cumulonimbus are so powerful, their air rises tens of thousands of feet, condensing rapidly, and often while still journeying upward. The result is a cloud tower with bulging upper portions (that look something like cauliflower).
If you see a cumulonimbus, you can be sure there's a nearby threat of severe weather, including bursts of rainfall, hail, and possibly even tornadoes. Generally, the taller the cumulonimbus cloud, the more severe the storm will be.
An anvil cloud isn't a stand-alone cloud, but more of a feature that forms at the top of a cumulonimbus cloud.
The anvil top of a cumulonimbus cloud is actually caused by it hitting the top of the stratosphere — the second layer of the atmosphere. Since this layer acts as a "cap" to convection (the cooler temperatures at its top discourage thunderstorms), the tops of storm clouds have nowhere to go but outward. Strong winds high up fan this cloud moisture (so high up that it takes the form of ice particles) out over great distances, which is why anvils can extend outward for hundreds of miles from the parent storm cloud.
Wall clouds form under the rain-free base (bottom) of cumulonimbus clouds. It takes its name from the fact that it resembles a dark gray wall (sometimes rotating) that lowers down from the base of the parent storm cloud, usually just before a tornado is about to form. In other words, it is the cloud from which a tornado spins.
Wall clouds form as the thunderstorm updraft draws in air near the ground from several miles around, including from the nearby rain shaft. This rain-cooled air is very humid and the moisture within it quickly condenses below the rain-free base to create the wall cloud.
Wave, or Kelvin-Helmholtz clouds, resemble breaking ocean waves in the sky. Wave clouds are created when air is stable and winds at the top of a cloud layer are moving faster across it than those below it, causing the top clouds to be whipped around in a downward curling motion after hitting the stable layer of air above.
While wave clouds aren't related to storms, they are a visual cue for aviators that a large amount of vertical wind shear and turbulence are in the area.
Like wall clouds, shelf clouds also form underneath thunderstorm clouds. As you can imagine, this fact doesn't help observers differentiate between the two. While one is easily mistaken for the other to the untrained eye, cloud spotters know that a shelf cloud is associated with thunderstorm outflow (not inflow like wall clouds) and can be found in the storm's precipitation area (not rain-free area like walls clouds).
Another hack to telling a shelf cloud and wall cloud apart is to think of rain "sitting" on the shelf and a tornado funnel "coming down" from the wall.
Scud clouds aren't dangerous clouds in and of themselves, but because they form when warm air from outside of a thunderstorm is lifted up by its updraft, seeing scud clouds is a good indication that a cumulonimbus cloud (and hence, a thunderstorm) is nearby.
Their low height above ground, ragged appearance, and presence beneath cumulonimbus and nimbostratus clouds mean scud clouds are often mistaken for funnel clouds. But there's one way to tell the two apart -—look for rotation. Scud do move when caught in the outflow (downdraft) or inflow (updraft) regions but that motion typically isn't rotation
One of the most feared and easily recognized storm clouds is the funnel cloud. Produced when a rotating column of air condenses, funnel clouds are the visible part of tornadoes that extend downward from the parent thunderstorm cloud.
But remember, not until the funnel reaches the ground or "touches down" is it called a tornado.
Roll or arcus clouds are tube-shaped clouds that literally look like they've been rolled up into a horizontal band across the sky. They appear low in the sky and are one of the few severe weather clouds that are actually detached from the storm cloud base. (This is one trick for telling them apart from shelf clouds.) Spotting one is rare, but will tell you where a thunderstorm's gust front or another weather boundary, like cold fronts or sea breezes lay, since these clouds are formed by outflows of cold air.
Those in aviation may recognize roll clouds by another name — "Morning Glorys".
info by www.thoughtco.com