Afterglow: Difference between revisions
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[[File:Abenddämmerung mit Purpurlicht und Schattenstrahlen.jpg|thumb|Afterglow with its bright segment and purple light above, interrupted by [[crepuscular rays]]]] | [[File:Abenddämmerung mit Purpurlicht und Schattenstrahlen.jpg|thumb|Afterglow with its bright segment and purple light above, interrupted by [[crepuscular rays]]]] | ||
In [[meteorology]], an '''afterglow''' is an [[optical phenomenon]], generally referring to a broad arch of whitish or pinkish [[sunlight]] in the [[twilight]] [[sky]] after [[sunset]], consisting of ''purple light'' and ''bright segment''. It consists of several [[Optical phenomena#Atmospheric optical phenomena|atmospheric optical phenomena]].<ref name="ametsoc">{{cite web |title=afterglow |website=AMS Glossary |publisher=[[American Meteorological Society]] |date=2015-10-05 |url=https://glossary.ametsoc.org/wiki/Afterglow |archive-url=https://web.archive.org/web/20151005210202/https://glossary.ametsoc.org/wiki/Afterglow |archive-date=2015-10-05 |url-status=dead |access-date=2022-08-14}}</ref><ref name="Glossary">{{cite web |publisher=The Formula |title=Full text of 'Weather Glossary' |website=Internet Archive |date=2022-01-14 |url=https://archive.org/stream/in.ernet.dli.2015.217458/2015.217458.Weather-Glossary_djvu.txt |access-date=2022-08-14}}</ref> The purple light mainly occurs when the Sun is 2–6° below the [[horizon]], during [[civil twilight]] (from sunset to [[civil dusk]]), while the bright segment lasts until the end of the [[nautical twilight]].<ref name="ametsoc-purple">{{cite web |title=purple light |website=AMS Glossary |publisher=[[American Meteorological Society]] |url=https://glossary.ametsoc.org/wiki/Purple_light |access-date=2022-08-14}}</ref><ref name="ametsoc-bright">{{cite web |title=bright segment |website=AMS Glossary |publisher=[[American Meteorological Society]] |url=https://glossary.ametsoc.org/wiki/Bright_segment |access-date=2022-08-14}}</ref> Similarly, a '''foreglow''' is a broad arch of whitish or pinkish sunlight in the twilight sky before [[sunrise]], consisting of ''purple light'' and ''bright segment''. | |||
Afterglow is often seen in [[volcanic eruption]]s,<ref name="Corfidi">{{cite web |title=The Colors of Twilight and Sunset |first= Stephen F.|last=Corfidi |publisher=[[NOAA]]/[[National Weather Service|NWS]] [[Storm Prediction Center]] |url=https://spc.noaa.gov/publications/corfidi/sunset |access-date=2022-08-14}}</ref> in which the purple light might also be called ''volcanic purple light''.<ref name="Purple">{{cite journal | last1=Lee | first1=Raymond L. | last2=Hernández-Andrés | first2=Javier | title=Measuring and modeling twilight's purple light | journal=Applied Optics | publisher=The Optical Society | volume=42 | issue=3 | date=2003-01-20 | pages=445–457 | issn=0003-6935 | doi=10.1364/ao.42.000445 | pmid=12570266 | bibcode=2003ApOpt..42..445L }}</ref> In volcanic occurrences specifically, the [[light scattering|light is scattered]] by fine [[particulates]], like [[dust]], suspended in the [[Earth's atmosphere|atmosphere]].<ref name="Purple" /> Afterglow may refer to the golden-red glowing light from the sunset and sunrise reflected in the sky in [[alpenglow]] (similar to the [[Belt of Venus]])<ref name="Powell 2018 pp. 105–130">{{cite book | last=Powell | first=Jonathan | title=The Patrick Moore Practical Astronomy Series | chapter=Atmospheric Factors and Features | publisher=Springer International Publishing | publication-place=Cham | year=2018 | isbn=978-3319977003 | issn=1431-9756 | doi=10.1007/978-3-319-97701-0_8 | pages=105–130}}</ref> and in particularly for its last stage, when the purple light is reflected.<ref name="Glossary" /><ref name="ametsoc" /> | |||
During [[Golden hour (photography)|golden hour]] (before sunset or after sunrise), sunlight reaches Earth intensely in its low-[[Energy of light|energy]] and low-frequency red [[Electromagnetic spectrum#Visible radiation (light)|component]]. During a period of civil twilight (after sunset or before sunrise), the red sunlight remains visible by [[scattering]] through particles in the air. [[Backscatter]]ing, possibly after being [[reflection (optics)|reflected]] off [[cloud]]s or high [[Snow field|snowfields]] in [[mountain]] regions, furthermore creates a reddish to pinkish light. On top of that, the high-energy and high-frequency components of light towards blue are [[scattering of electromagnetic radiation|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.<ref name="Corfidi" /> This period of blue dominating is referred to as the [[blue hour]] and is, like the golden hour, widely treasured by photographers and painters. | |||
== History == | |||
After the [[1883 eruption of Krakatoa|1883 eruption]] of the [[volcano]] [[Krakatoa]], a remarkable series of red [[sunset]]s 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. | After the [[1883 eruption of Krakatoa|1883 eruption]] of the [[volcano]] [[Krakatoa]], a remarkable series of red [[sunset]]s 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. | ||
== Gallery == | |||
<gallery class="center"> | <gallery class="center"> | ||
File:Dämmerung mit Purpurlicht und Schattenstrahlen, 10.10.2011 bei Limburg VIII.jpg|Purple light with crepuscular shadow | File:Dämmerung mit Purpurlicht und Schattenstrahlen, 10.10.2011 bei Limburg VIII.jpg|Purple light with crepuscular shadow | ||
Latest revision as of 15:13, 20 August 2025
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In meteorology, an afterglow is an optical phenomenon, generally referring to a broad arch of whitish or pinkish sunlight in the twilight sky after sunset, consisting of purple light and bright segment. It consists of several atmospheric optical phenomena.[1][2] The purple light mainly occurs when the Sun is 2–6° below the horizon, during civil twilight (from sunset to civil dusk), while the bright segment lasts until the end of the nautical twilight.[3][4] Similarly, a foreglow is a broad arch of whitish or pinkish sunlight in the twilight sky before sunrise, consisting of purple light and bright segment.
Afterglow is often seen in volcanic eruptions,[5] in which the purple light might also be called volcanic purple light.[6] In volcanic occurrences specifically, the light is scattered by fine particulates, like dust, suspended in the atmosphere.[6] Afterglow may refer to the golden-red glowing light from the sunset and sunrise reflected in the sky in alpenglow (similar to the Belt of Venus)[7] and in particularly for its last stage, when the purple light is reflected.[2][1]
During golden hour (before sunset or after sunrise), sunlight reaches Earth intensely in its low-energy and low-frequency red component. During a period of civil twilight (after sunset or before sunrise), 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. On top of that, 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.
History
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.
Gallery
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Purple light with crepuscular shadow
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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
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An afterglow on skyscrapers in New Taipei, Taiwan
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An afterglow on a Kraków housing estate
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Additional to foreglow here refracted sunlight reaches the South Pole just before actual sunrise. At Earth's poles the Sun appears at the horizon only and all day around equinox, marking the change between the half year long polar night and polar day.
See also
References
External links
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