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  2. Noctilucent cloud - Wikipedia

    en.wikipedia.org/wiki/Noctilucent_cloud

    Noctilucent clouds may be confused with cirrus clouds, but appear sharper under magnification. [50] Those caused by rocket exhausts tend to show colours other than silver or blue, [51] because of iridescence caused by the uniform size of the water droplets produced. [55] Noctilucent clouds may be seen at latitudes of 50° to 65°. [56]

  3. List of cloud types - Wikipedia

    en.wikipedia.org/wiki/List_of_cloud_types

    Mesospheric noctilucent clouds over Estonia. Noctilucent clouds are thin clouds that come in a variety of forms based from about 80 to 85 kilometres (262,000–279,000 ft) and occasionally seen in deep twilight after sunset and before sunrise. [6] [7] Type 1 Veils, very tenuous stratiform; resembles cirrostratus or poorly defined cirrus. Type 2

  4. Wikipedia : Featured pictures/Natural phenomena/Weather

    en.wikipedia.org/wiki/Wikipedia:Featured...

    Cirrus clouds, by Fir0002 Damage from the 1900 Galveston hurricane , by Griffith & Griffith (edited by Durova ) Dust storm at Dust Bowl , by Arthur Rothstein (edited by Mvuijlst )

  5. Mesosphere - Wikipedia

    en.wikipedia.org/wiki/Mesosphere

    Noctilucent clouds are located in the mesosphere. The upper mesosphere is also the region of the ionosphere known as the D layer , which is only present during the day when some ionization occurs with nitric oxide being ionized by Lyman series -alpha hydrogen radiation.

  6. Cloud - Wikipedia

    en.wikipedia.org/wiki/Cloud

    Noctilucent cloud over Estonia. Noctilucent clouds are the highest in the atmosphere and are found near the top of the mesosphere at about 80 to 85 km (50 to 53 mi) or roughly ten times the altitude of tropospheric high clouds. [131] They are given this Latin derived name because of their illumination well after sunset and before sunrise.

  7. Aeronomy of Ice in the Mesosphere - Wikipedia

    en.wikipedia.org/wiki/Aeronomy_of_Ice_in_the...

    Noctilucent clouds as seen by AIM. The scientific purpose of the Aeronomy of Ice in the Mesosphere (AIM) mission is focused on the study of polar mesospheric clouds (PMCs) that form about 80 km (50 mi) above the surface of Earth in summer and mostly in the polar regions of Earth. The overall goal is to resolve why PMCs form and why they vary.

  8. Category:Cloud types - Wikipedia

    en.wikipedia.org/wiki/Category:Cloud_types

    This page was last edited on 14 September 2019, at 17:47 (UTC).; Text is available under the Creative Commons Attribution-ShareAlike 4.0 License; additional terms may apply.

  9. Black Brant (rocket) - Wikipedia

    en.wikipedia.org/wiki/Black_Brant_(rocket)

    On September 19, 2009, a Black Brant XII that was launched to study clouds caused numerous calls from the northeastern U.S. reporting "strange lights in the sky". NASA reported that the light came from an artificial noctilucent cloud formed by the exhaust particles of the rocket's fourth stage at an altitude of about 278 km (173 mi).