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  2. Pileus (meteorology) - Wikipedia

    en.wikipedia.org/wiki/Pileus_(meteorology)

    A pileus (/ ˈ p aɪ l i ə s /; Latin for 'cap'), also called scarf cloud or cap cloud, is a small, horizontal, lenticular cloud appearing above a cumulus or cumulonimbus cloud. Pileus clouds are often short-lived, appearing for typically only a few minutes, [ 1 ] with the main cloud beneath them rising through convection to absorb them.

  3. Cumulonimbus cloud - Wikipedia

    en.wikipedia.org/wiki/Cumulonimbus_cloud

    Arcus (including roll and shelf clouds): low, horizontal cloud formation associated with the leading edge of thunderstorm outflow. [5] Pannus: accompanied by a lower layer of fractus species cloud forming in precipitation. [6] Pileus (species calvus only): small cap-like cloud over parent cumulonimbus.

  4. Cumulonimbus capillatus - Wikipedia

    en.wikipedia.org/wiki/Cumulonimbus_capillatus

    A cumulonimbus capillatus is a cumulonimbus cloud with dense cirrus clouds above it, making the cloud top appear to contain hair-like structures. The name comes from the Latin word capillatus, meaning "with hair". [1] It is an intermediate stage between cumulonimbus calvus and cumulonimbus incus.

  5. Lenticular cloud - Wikipedia

    en.wikipedia.org/wiki/Lenticular_cloud

    A lenticular cloud covers the summit crater of Mayon Volcano, Philippines.. As air travels along the surface of the Earth, obstructions are often encountered, including natural features, such as mountains or hills, and artificial structures, such as buildings and other constructions, which disrupt the flow of air into "eddies", or areas of turbulence.

  6. List of cloud types - Wikipedia

    en.wikipedia.org/wiki/List_of_cloud_types

    Clouds of the genus nimbostratus tend to bring constant precipitation and low visibility. This cloud type normally forms above 2 kilometres (6,600 ft) [10] from altostratus cloud but tends to thicken into the lower levels during the occurrence of precipitation. The top of a nimbostratus deck is usually in the middle level of the troposphere.

  7. Capping inversion - Wikipedia

    en.wikipedia.org/wiki/Capping_inversion

    Cloud formation from the lower layer is "capped" by the inversion layer. Air stagnation may result from a capping inversion from diffusing from a region, increasing the concentration of pollutants and exacerbating poor air quality. [1] If the capping inversion layer or "cap" is too strong it will prevent thunderstorms from developing.

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    www.aol.com/3-000-3-stocks-could-101000488.html

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  9. Mushroom cloud - Wikipedia

    en.wikipedia.org/wiki/Mushroom_cloud

    Mushroom cloud in an engraving from Gerhard Vieth's Physikalischer Kinderfreund, 1798. In 1798, Gerhard Vieth published a detailed and illustrated account of a cloud in the neighborhood of Gotha that was "not unlike a mushroom in shape". The cloud had been observed by legation counselor Lichtenberg a few years earlier on a warm summer afternoon.