Precipitation and Clouds, Formation of





Clouds are condensed droplets or ice crystals from atmospheric water vapor. Clouds form by the rising and cooling of air caused by convection, topography, convergence, and frontal lifting. Convection occurs when the Sun's radiation heats the ground surface, and warm air rises, cooling as it goes. Air also is cooled if an air mass is forced to move upward as a result of higher topography (e.g., a mountain range) in a process known as orographic lifting. Interestingly, when the air mass descends on the other side of the mountain, it warms and the clouds may disappear as the droplets transfer back to vapor. *

The counterclockwise motion of a low-pressure center draws air inward, and the convergence forces the air upward. Air also is lifted and cooled along either a cold front or a warm front. A cold front is the leading edge of an air mass that is colder than the air it is replacing. The front forms a wedge that pushes under the warmer air ahead, lifting it. A warm front is the leading edge of an air mass warmer than the air it is replacing. As the air mass pushes forward, the warm air slides up over the wedge of cold air ahead of it, as shown in the following figure.

Precipitation and Clouds, Formation of

Classification of Clouds

Clouds are classified based on their shape and the height of the cloud's base above the ground. The most common shapes are cirriform, appearing feathery or fibrous; stratoform, appearing layered; and cumuloform, appearing as if piled up. Two additional words used to describe clouds are "nimbus," meaning rain, and "alto," meaning middle. Basic cloud types are based on height above the land surface and on the cloud's vertical development, as summarized below.

  • High clouds (cloud base above 7 kilometers or 23,000 feet). Usually consisting of ice crystals, these include cirrus, cirrostratus, and cirrocumulus.
  • Middle clouds (2 to 7 kilometers or 6,500 to 23,000 feet). Consisting of liquid droplets, these include altocumulus and altostratus.
  • Low clouds (below 2 kilometers or 6,500 feet). Consisting of liquid droplets, these include stratus, stratocumulus, and nimbostratus.
  • Clouds of vertical development (cloud base generally is in the low cloud range, but the tops may reach great heights). These include cumulus clouds and the towering cumulonimbus. *

Fog represents a special case of cloud-like formation. Although not truly a cloud, fog is essentially stratoform clouds on the ground.

Cumulus Clouds.

Cumulus clouds are among the most interesting in terms of their shapes, which stir peoples' imagination and allow them to see a variety of "objects" or "scenes" in the sky. All cumulus clouds have two characteristics in common. They tend to be bulbous or popcorn-like on top, and have relatively flat bottoms. Why do they all share these features?

Cumulus clouds are classified as clouds of vertical extent. They form as air moves vertically, cooling until the water vapor in the air condenses. This vertical movement is the key to understanding the flat-bottomed character of these clouds. In a given area, for a given air mass, it is common to find that the cooling rate of ascending air is relatively constant. In other words, rising air will cool to a certain temperature at the same height above the ground throughout the area. Air moving vertically in that area will reach the condensation temperature at the same height above the ground and cloud formation will begin at that height. Consequently, the base of the cloud will be at the same height throughout and the cloud's base will appear flat.

As the air continues to rise and water vapor continues to condense, the cloud will extend vertically. The column of rising air actually consists of a number of currents with slightly different directions and may move as pulses. These currents move upward as they condense and give rise to the apparently independent bulbous lobes of the cloud.

Precipitation Types

Precipitation elements begin to form in the part of the cloud where ice crystals and cloud droplets coexist. Most precipitation starts out as snow, except for rain that comes out of very low clouds. Precipitation will remain snow unless it falls through a layer of warmer air, in which case it will melt and remain rain unless it falls through a colder layer of air, where it may freeze and become sleet or ice pellets (as shown in the following figure). When the air at the ground level is below freezing, the raindrops can freeze when they hit the ground or other cold surfaces: it is then called freezing rain.

Precipitation and Clouds, Formation of

Hail is formed when a particle, like dust, attracts a drop of moisture to itself. The particle gets blown upward by strong updrafts in the cloud, and freezes as it goes through a colder layer of air. It is heavier and begins to fall, attracts more moisture and then gets forced upward again and again adding more frozen layers.

The varying intensities of rainfall have specific names. Liquid precipitation that is of a longer duration and larger drop size is called rain; when it falls in shorter spurts it is called a shower. Rain typically falls from lowlevel stratoform clouds with greater vertical extent. When the drops are very small, rain is called drizzle. A raindrop is about 1,000 times larger than drizzle.

Thunderstorms.

Thunderstorms go through stages of development from the beginning cumulus stage, when the cloud starts to grow vertically; to the mature stage, when heights may reach from 12 to 18 kilometers (8 to 11 miles); to the dissipating stage (see figure below).

In the cumulus stage, there is an updraft of warm air throughout the cloud, as shown in part (a) of the figure. As the warm updraft increases, the

This schematic illustrates the three general stages of thunderstorm development. An elevation of 40,000 feet is equivalent to 12 kilometers or 8 miles.
This schematic illustrates the three general stages of thunderstorm development. An elevation of 40,000 feet is equivalent to 12 kilometers or 8 miles.
cloud builds well above the freezing level (the point at which the temperature of the rising air has cooled to water's freezing point). The precipitation particles grow larger and become heavier. The rising air soon cannot hold them up, and they begin to fall. The particles drag some of the air along with them, creating a downdraft, as shown in part (b) of the figure.

As the updraft pulls more dry air into the cloud, some of the raindrops evaporate, and the air cools, making it colder and heavier than the surrounding air. This usually strengthens the downdraft. The falling precipitation causes more downdrafts to form throughout the cloud, beginning the dissipating stage, as shown in part (c) of the figure. During the dissipating stage, precipitation occurs from the entire cloud base.

Some thunderstorms can develop into lines of severe thunderstorms, producing high winds, hail, frequent lightning, heavy rain, flash floods, and even tornadoes.

SEE ALSO C LIMATE M ODERATOR , W ATER AS A ; H YDROLOGIC C YCLE ; P RECIPITATION , G LOBAL D ISTRIBUTION OF ; W EATHER AND THE O CEAN .

Timothy A. Chuey

and Dennis O. Nelson

Bibliography

Ahrens, C. Donald. Meteorology Today. St. Paul, MN: West Publishing, 1985.

Internet Resource

"Clouds and Precipitation." WW2010 Weather World Project, Department of Atmospheric Sciences, University of Illinois at Urbana-Champaign. <http://ww2010.atmos.uiuc.edu/(Gh)/guides/mtr/cld/home.rxml� 3e; .

* See "Climate Moderator, Water as a" for a diagram of orographic lifting and the rain shadow effect.

* See "Precipitation, Global Distribution of" for a photograph of a cloud of vertical development.

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