The 10 clouds names are Cirrus Clouds, Cirrocumulus Clouds, Cirrostratus Clouds, Altocumulus Clouds, Altostratus Clouds, Nimbostratus Clouds, Cumulus Clouds, Cumulonimbus Clouds, Stratocumulus clouds and Stratus Clouds.
The type of clouds that are the most beautiful are Cirrus clouds which have a delicate appearance and intricate patterns that make them a favorite among photographers.
Cirrus clouds are thin, wispy and high level clouds which appear like delicate strands or filaments.
Cirrus clouds are also often known as the most beautiful clouds due to their exceptional appearance.
The rarest cloud is Nacreous cloud which are very high clouds and known for the colored light they reflect after sunset and before sunrise.
The color of nacreous clouds are usually pastel, but can also be very vivid or mingled together and sometimes similar to mother of pearl.
When the nacreous clouds appear near the sun the effect can be difficult to spot as it is drowned in the sun's glare.
Clouds are divided into four families for identification purposes which are high clouds, middle clouds, low clouds and clouds with extensive vertical development.
The first 3 families of clouds are further classified according to the way the clouds are formed.
The 4 types of clouds are cumulus clouds, stratus clouds, cirrus clouds and nimbus clouds .
The most common type of cloud is Stratocumulus Stratiformis clouds which are essentially flat based layers of cloud that often have a few cracks between.
The fluffy cauliflower shaped cumulus cloud is one of the most common and distinctive types of clouds and all cumulus clouds develop as a result of convection.
The 3 most common cloud types are Cirrus Clouds, Stratus Clouds and Cumulus Clouds.
The type of cloud that is most likely to precede a tornado is a wall cloud.
Wall clouds are the best identifier of a tornado being possible.
The wall cloud which precedes a tornado is a compact, lowering of the cloud where an updraft and inflow of a storm is located.
There is also a lot of movement here and when they are rotating wall clouds the funnel clouds and the tornadoes can descend from them as well.
A wall cloud is a large, localized, persistent, and often abrupt lowering of cloud that develops beneath the surrounding base of a cumulonimbus cloud and from which tornadoes sometimes form.
A wall cloud is an isolated cloud lowering attached to the rain-free base of the thunderstorm.
The wall cloud is usually to the rear of the visible precipitation area.
A wall cloud that may produce a tornado can exist for 10–20 minutes before a tornado appears, but not always.
A shelf cloud will usually be associated with a solid line of storms.
The wind will come first with rain following behind it.
It may appear to rotate on a horizontal axis.
Wall clouds will rotate on a vertical axis, sometimes strongly.
Translated from latin meaning wall, the 'murus' cloud feature is found only in the cumulonimbus cloud type.
No other cloud type besides a cumulonimbus cloud can be paired with a murus cloud feature.
Murus, more popularly known as wall clouds, are cloud lowerings forming below the updraft base of a cumulonimbus cloud.
Researchers have shown that wall clouds probably develop when some rain-cooled air is pulled upward, along with the more buoyant air, as the strengthening updraft attempts to replace ever-growing volumes of rising air.