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  2. 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.

  3. Stratocumulus cloud - Wikipedia

    en.wikipedia.org/wiki/Stratocumulus_cloud

    However, the cloud sheet is not completely uniform, so that separate cloud bases still can be seen. This is the main precipitating type, however any rain is usually light. If the cloud layer becomes grayer to the point when individual clouds cannot be distinguished, stratocumulus turn into stratus clouds.

  4. Cloud - Wikipedia

    en.wikipedia.org/wiki/Cloud

    Overlapping clouds (in meteorology, probably duplicatus clouds) are thought to imply eternal happiness [170] and clouds of different colors are said to indicate "multiplied blessings". [170] Informal cloud watching or cloud gazing is a popular activity involving watching the clouds and looking for shapes in them, a form of pareidolia. [171] [172]

  5. D'Nealian - Wikipedia

    en.wikipedia.org/wiki/D'Nealian

    D'Nealian cursive writing. The D'Nealian Method (sometimes misspelled Denealian) is a style of writing and teaching handwriting script based on Latin script which was developed between 1965 and 1978 by Donald N. Thurber (1927–2020) in Michigan, United States.

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  7. International Cloud Atlas - Wikipedia

    en.wikipedia.org/wiki/International_Cloud_Atlas

    The International Cloud Atlas or simply the Cloud Atlas, is a cloud atlas that was first published in 1896 [1] and has remained in print since. Its initial purposes included aiding the training of meteorologists and promoting more consistent use of vocabulary describing clouds , which were both important for early weather forecasting .

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  9. Scud (cloud) - Wikipedia

    en.wikipedia.org/wiki/Scud_(cloud)

    These clouds are often ragged or wispy in appearance. When caught in the outflow beneath a thunderstorm, scud clouds will often move faster than the storm clouds themselves. If the parent cloud that scud clouds pair with were to suddenly dissipate, the pannus cloud accessory would not be able to be told apart from a fractus cloud formation.

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