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Notes on historical aspects on the earliest known observations of noctilucent clouds

机译:关于夜光云的最早已知观测的历史方面的注释

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The present paper considers historical aspects of the earliest knownobservations of noctilucent clouds (NLCs). The 1884 and 1885 are discussedby considering important historical citations by the pioneers of theearliest known observations of noctilucent clouds. For the first time in NLCstudies, we consider seven major volcanic eruptions: Laki in 1783, Mount St. Helensin 1800, Tambora in 1815, Galunggung in 1822, Cosigüina in 1835,Shiveluch in 1854 and Askja in 1875. These all preceded the catastrophic1883 eruption of Krakatoa, which despite having a lesser magnitude thanTambora in 1815, had pronounced effects on the atmosphere. These eruptionsrepresent possible triggers for the appearance of NLCs. For the first time,we publish an unknown, in English-speaking literature, historical fact onthe first determinations of the altitude of noctilucent clouds made by twoRussian astronomers V. K. Tseraskii and A. A. Belopolskii on 26 June 1885, whomanaged to infer the altitude of the clouds in the range of 73–83 km, thatis, for the first time, demonstrating the possible existence of the cloudsat great altitudes in the Earth's atmosphere. Moreover, V. K. Tseraskii wasthe first observer to photograph noctilucent clouds in 1885 or 1886, whichis 1–2 yr before the German astronomer O. Jesse, who owns the firstpublished images of noctilucent clouds. The photographs made by V. K. Tseraskii,unfortunately, did not reach us.
机译:本文考虑了夜光云(NLC)的最早已知观测的历史方面。在讨论1884年和1885年时,考虑了对夜光云的最早已知观测的开创者的重要历史引文。在NLC研究中,我们首次考虑了七个主要的火山喷发:1783年的拉基,1800年的圣海伦辛火山,1815年的坦波拉,1822年的Gal伦贡,1835年的科西格纳,1854年的希维卢奇和1875年的阿斯贾。克拉卡托亚火山的震级虽然比1815年的坦波拉要小,但对大气的影响却很明显。这些爆发代表了NLC出现的可能诱因。我们第一次在英语文学中发表了一个未知的历史事实,该事实是由两位俄罗斯天文学家VK Tseraskii和AA Belopolskii于1885年首次确定夜光云的高度确定的,他们设法推断出这是73-83公里的范围,这是首次证明地球大气层高空可能存在云。此外,V。K. Tseraskii是1885年或1886年拍摄夜光云的第一位观察者,这比德国天文学家杰西(O. Jesse)早了1-2年,后者拥有夜光云的首张图像。不幸的是,V。K. Tseraskii拍摄的照片没有送达我们。

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