CLOUDS

HIGH LEVEL CLOUDS High-level clouds form above 20,000 feet (6,000 meters) and since the temperatures are so cold at such high elevations, these clouds are primarily composed of ice crystals. High-level clouds are typically thin and white in appearance, but can appear in a magnificent array of colors when the sun is low on the horizon.

The most common form of high-level clouds are thin and often wispy cirrus clouds. Typically found at heights greater than 20,000 feet (6,000 meters), cirrus clouds are composed of ice crystals that originate from the freezing of supercooled water droplets. Cirrus generally occur in fair weather and point in the direction of air movement at their elevation.

Cirrostratus are sheet-like, high-level clouds composed of ice crystals. Though cirrostratus can cover the entire sky and be up to several thousand feet thick, they are relatively transparent, as the sun or the moon can easily be seen through them. These high-level clouds typically form when a broad layer of air is lifted by large-scale convergence.

Sometimes the only indication of their presence is given by an observed halo around the sun or moon. Halos result from the refraction of light by the cloud's ice crystals. Cirrostratus clouds, however, tend to thicken as a warm front approaches, signifying an increased production of ice crystals. As a result, the halo gradually disappears and the sun (or moon) becomes less visible.

When the sun is low on the horizon (sunset), cirrostratus clouds can appear very colorful as longer wavelengths of sunlight (red, yellow, and orange) are reflected off of the clouds.

MIDDLE LEVEL CLOUDS The bases of mid-level clouds typically appear between 6,500 to 20,000 feet (2,000 to 6,000 meters). Because of their lower altitudes, they are composed primarily of water droplets, however, they can also be composed of ice crystals when temperatures are cold enough.

Altocumulus clouds are composed primarily of water droplets and are located between 6,500 and 20,000 feet (2,000 to 6,000 meters) above the ground.

Altocumulus may appear as parallel bands (top photograph) or rounded masses (bottom photograph). Typically a portion of an altocumulus cloud is shaded, a characteristic which makes them distinguishable from the high-level cirrocumulus. Altocumulus clouds usually form by convection in an unstable layer aloft, which may result from the gradual lifting of air in advance of a cold front. The presence of altocumulus clouds on a warm and humid summer morning is commonly followed by thunderstorms later in the day.

LOW LEVEL CLOUDS Low clouds are of mostly composed of water droplets since their bases generally lie below 6,500 feet (2,000 meters). However, when temperatures are cold enough, these clouds may also contain ice particles and snow.

Nimbostratus are dark, low-level clouds accompanied by light to moderately falling precipitation. Low clouds are primarily composed of water droplets since their bases generally lie below 6,500 feet (2,000 meters). However, when temperatures are cold enough, these clouds may also contain ice particles and snow.

Stratocumulus clouds generally appear as a low, lumpy layer of clouds that is sometimes accompanied by light precipitation. Stratocumulus vary in color from dark gray to light gray and may appear as rounded masses, with breaks of clear sky in between.

VERTICALLY-DEVELOPED CLOUDS Probably the most familiar of the classified clouds is the cumulus cloud. Generated most commonly through either thermal convection or frontal lifting, these clouds can grow to heights taller than 39,000 feet (12,000 meters), releasing incredible amounts of energy through the condensation of water vapor within the cloud itself.

Fair weather cumulus have the appearance of floating cotton and have a lifetime of 5-40 minutes. Known for their flat bases and distinct outlines, fair weather cumulus show only slight vertical growth, with the cloud tops designating the limit of the rising air. If the conditions are unstable, harmless fair weather cumulus can later develop into towering cumulonimbus clouds associated with powerful thunderstorms.

Fair weather cumulus are fueled by buoyant bubbles of air, or thermals, that rise upward from the earth's surface. As they rise, the water vapor within cools and condenses forming cloud droplets. Young fair weather cumulus have sharply defined edges and bases while the edges of older clouds appear more ragged, an artifact of cloud erosion. Evaporation along the cloud edges cools the surrounding air, making it heavier and producing sinking motion (or subsidence) outside the cloud.

The downward motion inhibits further convection and the growth of additional thermals from below, which is why fair weather cumulus typically have expanses of clear sky between them. Without a continued supply of rising air, the cloud begins to erode and eventually disappears.

Cumulonimbus clouds

Cumulonimbus clouds (Cb) are much larger and more vertically developed than fair weather cumulus. They can exist as individual towers or form a line of towers called a squall line. Fueled by vigorous convective updrafts (sometimes in excess 50 knots), the tops of cumulonimbus clouds can easily reach 39,000 feet (12,000 meters) or higher.

Supercells are large thunderstorms with deep rotating updrafts and can have a lifetime of several hours. Supercells can produce frequent lightning, large hail, damaging winds, and tornadoes.

Atmospheric Stability and Cloud Formation

An air parcel (thermal) will rise if it is warmer than the air surrounding it.

When It rises it expands and cools When It rises it expands and cools. When it gets high enough, to where the dew point temperature is reached, condensation will occur and a cumulus cloud will form. When It rises it expands and cools. When it gets high enough, to where the dew point temperature is reached, condensation will occur and a cumulus cloud will form.

A sinking air parcel will compress and warm

CONDITIONS FOR CLOUD FORMATION

OROGRAPHIC UPLIFT – lifting of an air mass over a mountain OROGRAPHIC UPLIFT – lifting of an air mass over a mountain. When the air mass is lifted high enough to where the temperature is cool enough, clouds will form.

Convergence (coming together) of two air masses Convergence (coming together) of two air masses. This happens over central Florida and…

At the Equator, where the Trade Winds converge

Cloud formation occurs at cold and warm fronts as less dense warm air rises over denser cold air