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dc.contributor.authorBertolin, Chiara
dc.contributor.authorDominguez-Castro, Fernando
dc.date.accessioned2021-10-21T07:49:37Z
dc.date.available2021-10-21T07:49:37Z
dc.date.created2020-01-06T15:18:19Z
dc.date.issued2020
dc.identifier.citationThe Holocene. 2020, 30 (5), 682-690.en_US
dc.identifier.issn0959-6836
dc.identifier.urihttps://hdl.handle.net/11250/2824346
dc.description.abstractNoctilucent clouds (NLCs) are an uncommon phenomenon that provides information about the conditions and dynamics of the mesosphere. The first observation of NLCs was recorded in 1884/1885, following Krakatoa’s eruption in 1883. The literature speculates that this observation was trigged by the injection of millions of tons of H2O by the Krakatoa into the stratosphere. We have discovered that 43 years before Krakatoa, Antonio Colla observed an NLC in Parma. He was a meticulous astronomer and meteorologist with special interest in astronomical and atmospheric phenomena occurring during twilight. On 18 June 1840, from 21:00 to 22:15 (Local Mean Sideral Time), Antonio Colla observed a ‘phosphoric cloud’. Analysis of the Colla’s description, the local sky and the condition of the observation proves that he was recording an NLC. This finding forces to develop a new hypothesis to explain the early NLC observations and encourages the rescue of NLC observations from documentary sources.en_US
dc.language.isoengen_US
dc.publisherSAGEen_US
dc.titleThe earliest datable noctilucent cloud observation (Parma, Italy, AD 1840)en_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.rights.holderThe published version of the article will not be available due to copyright restrictions by SAGEen_US
dc.source.pagenumber682-690en_US
dc.source.volume30en_US
dc.source.journalThe Holoceneen_US
dc.source.issue5en_US
dc.identifier.doi10.1177/0959683619895584
dc.identifier.cristin1767083
cristin.ispublishedtrue
cristin.fulltextpostprint
cristin.qualitycode1


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