Different Kinds Of Clouds And Their Meanings – There are many different types of clouds and they are categorized using a system based on where they are in the atmosphere. This classification system is similar to the Linnaean taxonomy used to classify living things, where each word refers to a different component. For example, nimbus or nimbus clouds refer to clouds that produce precipitation. Clouds with strata or stratus in the name usually form in layers.

In this activity, students will create a chat that identifies and illustrates different types of clouds and their altitude. This activity can be scaffolded, where pictures of clouds are provided and students are asked to label them. You can also encourage students to go outside and identify different types of clouds and upload photos of any of them.

Different Kinds Of Clouds And Their Meanings

To learn more about cloud types, see the World Meteorological Organization’s International Cloud Atlas.

Description Of The Different Types Of Clouds

Cirrus – A tall, atmospherically separated cloud characterized by thin hair-like wisps. The name comes from the Latin word cirrus, meaning “hair”.

Cirrostratus – Characterized by a smooth, transparent sheet that covers part or all of the sky. This type of cloud can cause a halo around the Sun.

Altocumulus – It is characterized by patches and sheets formed by rounded masses, layers or rolls. They can be diffused or made of fibers.

Altostratus – Greyish or bluish leaves cover all or part of the sky. Unlike Cirrostratus, this type of cloud does not cause halos to form around the Sun.

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Nimbostratus – A gray cloud layer associated with rain or snow. The cloud layer is usually thick enough to block the Sun.

Stratocumulus – Gray or white patches and layers formed by groups of rounded masses. Stratocumulus clouds are usually not fibrous.

Cumulus – separate, fluffy clouds with clearly defined edges. The bases of these clouds are flat and gray, while the tops form brilliant white ridges that can look like cauliflower.

Stratus – A low, smooth layer of gray cloud often associated with precipitation. These clouds often block the Sun.

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Cumulonimbus – These types of clouds have a large vertical height that forms huge mountains. Most of these clouds are flat and spread out at the top. They are sometimes known as a thundercloud.

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Each type of cloud has its own image, but some of them are not clear or appropriate for the term. In meteorology, clouds are visible masses made of a large amount of liquid droplets and/or frozen crystals suspended in the atmosphere. These clouds are formed from very small water droplets and/or ice crystals (2 to 200 microns in diameter) obtained by condensation of water vapor from the atmosphere around small particles (dust, aerosols,…) called condensation nuclei.

The aspect of a cloud is characterized by its shape, texture, opacity and colors. These parameters vary as a function of cloud composition and atmospheric conditions.

Student Project: The Types Of Clouds And What They Mean

The international classification uses families, genera, species and varieties. This is similar to the classifications used for plants and animals and as these classifications Latin names are used.

In total, the World Meteorological Organization currently recognizes 10 genera that are grouped into 4 families. These families correspond to 3 different height intervals of the troposphere and 1 cloud family with high vertical development in 3 different layers.

Polar regions: 3 km to 8 km (10,000 to 25,000 ft) temperate regions: 5 km to 13 km (16,500 ft to 40,000 ft) tropical regions: 6 km to 18 km (20,000 ft) to 60,000 ft )

Polar regions: ~2 km to 5 km (6,500 ft to 16,500 ft) temperate regions: ~2 km to 9 km (6,500 ft to 30,000 ft) tropical regions: ~2 km to 12 km ( 6,500 feet to 40,000 feet)

A Rare Look At An Iridescent Cloud

Polar regions: 0.5 km to 8 km (1,650 ft to 25,000 ft) temperate regions: 0.5 km to 13 km (1,650 ft to 40,000 ft) tropical regions: 0.5 km to 18 km (1 650 ft) to 60,000 ft)

These are fibrous pieces of delicate white ice crystal clouds. They can be found in large fields or in narrow white bands. Fairly opaque, sunlight can pass through it. These clouds are pink or red after sunset. These clouds do not produce precipitation.

These clouds are made of ice crystals and form a transparent whitish veil that completely or partially covers the sky. These clouds are often accompanied by a halo phenomenon. This type of cloud also does not produce precipitation, but heralds the arrival of a depression.

These clouds are rarely seen. They are shaped like a cotton flower and are very small. They consist of ice crystals or supercooled water droplets. These clouds are without precipitation, but may indicate the arrival of a front.

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These clouds are layered and present in layers where boundaries are difficult to determine. They form a broad gray, slightly mottled or fibrous layer. They let the light spread without a visible shadow on the ground. They range in thickness from 500 m to 3,000 m (1,650 ft to 10,000 ft). They consist of water droplets, but at higher altitudes they can be mixed with ice crystals. Widespread opaque altostratus can produce light continuous or intermittent precipitation (rain or snow). These clouds are relative to stable air.

These clouds are in the form of lamellae, pebbles, rings, sometimes with a partially fibrous or fuzzy appearance. They may or may not be welded. They are white and/or gray and appear as a bank, in a sheet or in a layer. These clouds usually have their own shadow, which distinguishes them from cirrocumulus clouds.

These clouds have a characteristic grayish color and a fairly uniform appearance. Sometimes they consist of separate elements with a jagged appearance. They are often accompanied by a foggy atmosphere. It is also likely to produce rain (precipitation of very small water droplets or granular snow (less than one millimeter in diameter)). This type of cloud can be the result of night cooling, inflow of moist air from a lake, sea or ocean, evaporation over the water surface or after heavy rain.

This type of cloud looks like a large, dark, rounded mass. Individually, each cloud is larger than the altocumulus cloud. They are usually present in groups, lines or waves. This type of cloud has a convective origin, but its vertical extension is immediately limited by the stability of the upper layer.

All The Different Types Of Clouds

This type of cloud is loose, normally dense and looks like a bud (cauliflower) with little vertical extension. This type of cloud is formed during convection after adiabatic expansion. They can form in many situations, but often after a disturbance has passed (a cold front moves away and the sun becomes visible again, causing the ground to warm).

This type of cloud is dense with a very high vertical extension (the largest). It is of convective origin. The tip is anvil-shaped. This cloud is the source of thunderstorms and generally develops as a cold front approaches.

This cloud is stratiform with significant vertical extension. It often consists of several layers without a defined shape and a dark gray color. It also completely hides the sun. It produces low to moderate rainfall, but over large areas.

10 genera of clouds is the best classification, but most genera are divided into species due to the peculiarity of their shapes. A species may belong to more than one cloud genus. A genus can have more than one species, and some genera have no species. Types are mutually exclusive, in other words a cloud can only be assigned to one type.

How To Identify Cloud Types

Separate clouds or fine veil consisting of almost straight or more or less irregularly curved threads and not ending in hooks or tufts.

The cirrus usually has the shape of a notch that ends in a hook or tuft in the upper part and whose upper end is not in the form of a rounded protrusion.

Clouds that in their upper part represent protrusions in the form of towers and that give them a jagged appearance. The towers are from the same base and are arranged in a row.

Each cloud is a tuft of cumuliform appearance, the base of which is more or less serrated and which is often accompanied by a virgo (a conspicuous streak or bundle of precipitation falling from a cloud that evaporates or sublimates before reaching the ground).

Most Common Types Of Clouds Found In The Sky

A cumulonimbus whose peak ridges begin to lose their cumuliform appearance, but in which we do not differ from the circular parts.

Cumulonimbus is characterized by the presence at the top of circular parts of fibrous or striped, anvil-shaped, plumes or large masses of more or less disordered hair. It is often accompanied by rain or thunder.

Finally we have the following classification for the 9 types of clouds. Varieties are a function of the arrangement of elements and the degree of transparency of the genera. Varieties

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