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Cloud Identification

GOES-R

Clouds that Produce Precipitation

Nimbostratus

Nimbostratus Clouds

Nimbostratus are layered clouds with low bases that produce precipitation and are usually formed by advection. They are thick, dark gray with a ragged base, and are often associated with the passage of warm fronts. The Sun is always obscured.

Usually, nimbostratus is a sign of steady moderate to heavy precipitation, as opposed to the shorter period of typically heavier precipitation released by a cumulonimbus cloud. However, local conditions may cause nimbostratus to quickly develop into a thunderstorm (cumulonimbus).

Cumulonimbus

Cumulonimbus with anvil top

When the atmosphere becomes unstable the convection intensifies and cumulus clouds can develop into rain clouds or thunderstorms. Even though the base of a cumulonimbus cloud may be as low as 3 or 4000 feet, they can grow vertically up to 50 or 60,000 feet high (as high as the tropopause) in the summer. At this height, the top of the cloud spreads out and high winds flatten the top of the cloud out into an anvil-like shape. Powerful cumulonimbus clouds with bright white overshooting tops that punch through the tropopause are especially easy to pick out on visible satellite images. These are big storms!

Cumulonimbus clouds form in moist atmospheres and are common in spring and summer. They often occur in the advance of a cold front. In summer they can form over mountains due to orographic lifting in combination with solar heating. Precipitation falls from these clouds and severe weather (lightning, hail, tornado, flash flood) is common. Cumulonimbus can be isolated storms or organized in groups. When cumulonimbus clouds form together in an organized system, the chance of severe weather increases.

Cumulonimbus with overshooting top Cumulonimbus overshooting top visible satellite image Cumulonimbus infrared satellite image
Cumulonimbus overshooting top Cumulonimbus overshooting top
Visible satellite image
Cumulonimbus IR satellite image

Identify Cumulonimbus Clouds in Satellite Images

The first satellite image is a visible image using reflected light, the second satellite image is an IR image that measures thermal energy.

hands-on activityUse your mouse or finger and slide across the image to fade between the different images.