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  2. Nimbostratus cloud - Wikipedia

    en.wikipedia.org/wiki/Nimbostratus_cloud

    Nimbostratus ( rain, layered) Altitude. 500–5,500 m (2,000–18,000 ft) Appearance. Dark and featureless layer cloud full of water vapor; responsible for rain and snow. Precipitation. Yes: rain, ice pellets, or snow; sometimes virga. A nimbostratus cloud is a multilevel, amorphous, nearly uniform, and often dark-grey cloud that usually ...

  3. Stratus cloud - Wikipedia

    en.wikipedia.org/wiki/Stratus_cloud

    Stratus fractus clouds on the other hand, appear with an irregular shape, and forms with a clearly fragmented or ragged appearance. They mostly appear under the precipitation of major rain-bearing clouds; these are nimbostratus and cumulonimbus clouds, and are classified as types of pannus clouds.

  4. Fractus cloud - Wikipedia

    en.wikipedia.org/wiki/Fractus_cloud

    Fractus clouds, also called fractostratus or fractocumulus, [1] are small, ragged cloud fragments that are usually found under an ambient cloud base. They form or have broken off from a larger cloud, and are generally sheared by strong winds, giving them a jagged, shredded appearance. Fractus have irregular patterns, appearing much like torn ...

  5. Cirrus cloud - Wikipedia

    en.wikipedia.org/wiki/Cirrus_cloud

    Sky containing different types of cirrus clouds. Cirrus ( cloud classification symbol: Ci) is a genus of high cloud made of ice crystals. Cirrus clouds typically appear delicate and wispy with white strands. Cirrus are usually formed when warm, dry air rises, causing water vapor deposition onto rocky or metallic dust particles at high altitudes.

  6. List of cloud types - Wikipedia

    en.wikipedia.org/wiki/List_of_cloud_types

    Multi-level and vertical genus-types not limited to a single altitude level include nimbostratus, cumulonimbus, and some of the larger cumulus species. The list of cloud types groups all genera as high (cirro-, cirrus), middle (alto-), multi-level (nimbo-, cumulo-, cumulus), and low (strato-, stratus). These groupings are determined by the ...

  7. Stratocumulus cloud - Wikipedia

    en.wikipedia.org/wiki/Stratocumulus_cloud

    Stratocumulus clouds are the main type of cloud that can produce crepuscular rays. Thin stratocumulus clouds are also often the cause of corona effects around the Moon at night. All stratocumulus subtypes are coded C L 5 except when formed from free convective mother clouds (C L 4) or when formed separately from co-existing (C L 8).

  8. Altostratus cloud - Wikipedia

    en.wikipedia.org/wiki/Altostratus_cloud

    Altostratus is a middle-altitude cloud genus made up of water droplets, ice crystals, or a mixture of the two. Altostratus clouds are formed when large masses of warm, moist air rise, causing water vapor to condense. Altostratus clouds are usually gray or blueish featureless sheets, although some variants have wavy or banded bases.

  9. Cirrostratus cloud - Wikipedia

    en.wikipedia.org/wiki/Cirrostratus_cloud

    Cirrostratus cloud. Thin, transparent, high-altitude layer capable of producing a halo. No, but usually signal the approach of a warm front. But rain in 24 hours. Cirrostratus / ˌsɪroʊˈstrɑːtəs / is a high-altitude, very thin, generally uniform stratiform genus-type of cloud. It is made out of ice -crystals, which are pieces of frozen water.