An afterglow in meteorology consists of several atmospheric optical phenomena, with a general definition as a broad arch of whitish or pinkish sunlight in the twilight sky, consisting of the bright segment and the purple light.[1][2] Purple light mainly occurs when the Sun is 2–6° below the horizon, from civil to nautical twilight, while the bright segment lasts until the end of the nautical twilight.[3][4] Afterglow is often in cases of volcanic eruptions discussed,[5] while its purple light is discussed as a different particular volcanic purple light.[6] Specifically in volcanic occurrences it is light scattered by fine particulates, like dust, suspended in the atmosphere.[6] In the case of alpenglow, which is similar to the Belt of Venus,[7] afterglow is used in general for the golden-red glowing light from the sunset and sunrise reflected in the sky, and in particularly for its last stage, when the purple light is reflected.[2][1] The opposite of an afterglow is a foreglow, which occurs before sunrise.[citation needed]
Sunlight reaches Earth around civil twilight during golden hour intensely in its low-energy and low-frequency red component. During this part of civil twilight after sunset and before sundawn the red sunlight remains visible by scattering through particles in the air. Backscattering, possibly after being reflected off clouds or high snowfields in mountain regions, furthermore creates a reddish to pinkish light. The high-energy and high-frequency components of light towards blue are scattered out broadly, producing the broader blue light of nautical twilight before or after the reddish light of civil twilight, while in combination with the reddish light producing the purple light.[5] This period of blue dominating is referred to as the blue hour and is, like the golden hour, widely treasured by photographers and painters.
After the 1883 eruption of the volcano Krakatoa, a remarkable series of red sunsets appeared worldwide. An enormous amount of exceedingly fine dust were blown to a great height by the volcano's explosion, and then globally diffused by the high atmospheric winds. Edvard Munch's painting The Scream possibly depicts an afterglow during this period.
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Purple light with crepuscular shadow -
Sunset in Hong Kong after the 1991 eruption of Mount Pinatubo -
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An afterglow in Slovenian mountains, near Triglav Lakes Valley -
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An afterglow at a pier in Australia -
An afterglow on Kraków's housing estate
See also
References
- ^ a b "afterglow". AMS Glossary. American Meteorological Society. 2015-10-05. Archived from the original on 2015-10-05. Retrieved 2022-08-14.
- ^ a b "Full text of 'Weather Glossary'". Internet Archive. The Formula. 2022-01-14. Retrieved 2022-08-14.
- ^ "purple light". AMS Glossary. American Meteorological Society. Retrieved 2022-08-14.
- ^ "bright segment". AMS Glossary. American Meteorological Society. Retrieved 2022-08-14.
- ^ a b Corfidi, Stephen F. "The Colors of Twilight and Sunset". NOAA/NWS Storm Prediction Center. Retrieved 2022-08-14.
- ^ a b Lee, Raymond L.; Hernández-Andrés, Javier (2003-01-20). "Measuring and modeling twilight's purple light". Applied Optics. 42 (3). The Optical Society: 445–457. Bibcode:2003ApOpt..42..445L. doi:10.1364/ao.42.000445. ISSN 0003-6935. PMID 12570266.
- ^ Powell, Jonathan (2018). "Atmospheric Factors and Features". The Patrick Moore Practical Astronomy Series. Cham: Springer International Publishing. pp. 105–130. doi:10.1007/978-3-319-97701-0_8. ISBN 978-3319977003. ISSN 1431-9756.
External links
This page was last edited on 28 October 2023, at 00:34