Cloud height

From Wikipedia, the free encyclopedia

The cloud height (or the height of the cloud) is the distance between the cloud base and the cloud top. It is traditionally expressed either in metres or as a pressure difference in hectopascal (hPa, equivalent to millibar). Sometimes, the expression cloud height is used instead of cloud base, in which case the context has to clarify whether the intent is to designate the elevation or the size of the cloud.

1 Measurement
2 Weather and climate relevance
3 See also
4 References

[edit] Measurement

Cloud height is not measured directly, but derived from separate measurements of cloud base and cloud top altitudes.

[edit] Weather and climate relevance

Cloud height is often related to the intensity of precipitation generated by a cloud: deeper clouds tend to produce more intense rainfall. For instance, cumulonimbus clouds can develop vertically through a substantial part of the troposphere and often result in thunderstorms with lightning and heavy showers. By contrast, very thin clouds (such as cirrus clouds) do not generate any precipitation at the surface.

For a synthetic discussion of the impact of clouds on the climate system, see the IPCC Third Assessment Report, in particular chapter 7.2.