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  2. Cloud height - Wikipedia

    en.wikipedia.org/wiki/Cloud_height

    The cloud height, more commonly known as cloud thickness or depth, is the distance between the cloud base and the cloud top. [1] It is traditionally expressed either in metres or as a pressure difference in hectopascal (hPa, equivalent to millibar ).

  3. Cloud base - Wikipedia

    en.wikipedia.org/wiki/Cloud_base

    The height of the cloud base can be measured using a ceilometer. This device reflects a beam of light off the cloud base and then calculates its distance using either triangulation or travel time. Alternatively, the cloud base can be estimated from surface measurements of air temperature and humidity by calculating the lifted condensation level.

  4. Cloud top - Wikipedia

    en.wikipedia.org/wiki/Cloud_top

    The cloud top is where the snow, rain and sleet come from. Cloud top height can be estimated from the ground by triangulation.However, this is often inconvenient as this is practically feasible only for isolated clouds in full view of (and some horizontal distance away from) the observers.

  5. Ceilometer - Wikipedia

    en.wikipedia.org/wiki/Ceilometer

    A ceilometer is a device that uses a laser or other light source to determine the height of a cloud ceiling or cloud base. [1] Ceilometers can also be used to measure the aerosol concentration within the atmosphere. [2] A ceilometer that uses laser light is a type of atmospheric lidar (light detection and ranging) instrument. [3] [4]

  6. Lifting condensation level - Wikipedia

    en.wikipedia.org/wiki/Lifting_condensation_level

    The LCL is a good approximation of the height of the cloud base which will be observed on days when air is lifted mechanically from the surface to the cloud base (e.g. due to convergence of airmasses).

  7. Cloud physics - Wikipedia

    en.wikipedia.org/wiki/Cloud_physics

    the cloud height, measured above sea level, ranging from 0 to 20 km; the cloud IR emissivity, with values between 0 and 1, with a global average around 0.7; the effective cloud amount, the cloud amount weighted by the cloud IR emissivity, with a global average of 0.5; the cloud (visible) optical depth varies within a range of 4 and 10.

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  9. Ceiling balloon - Wikipedia

    en.wikipedia.org/wiki/Ceiling_balloon

    If the balloon is visible for a considerable distance into the cloud layer the observer should make note of it as it is of importance to aircraft. The ceiling balloon is a reliable, safe and simple way to get an indication of the height of clouds. However, it does suffer from some disadvantages that the observer must be aware of.