The Nature of Noctilucent Clouds
The Nature of Noctilucent Clouds
复制标题
夜光云的本质
DOI：
10.1007/978-3-642-48626-5_10
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发表时间：
1989
影响因子：
5.2
通讯作者：
W. Schröder
中科院分区：
文献类型：
--
作者：
M. Gadsden;W. Schröder
在对强对流云进行系统观测以来的世纪里，许多观测数据被记录下来并进行了详细的讨论。从这一时期一开始，就形成了各种假设，并在一定程度上进行了实际检验。很自然地，由于喀拉喀托火山爆发后，人们对黄昏天空现象的认识越来越多，因此最早的建议是，冰碛云是在大气层最上层出现的简单的火山尘层（经过一两年的延迟）。这些假设后来被更复杂的解释所取代，解释了云出现在大气中非常干燥和压力非常低的一部分中的原因。Chvostikov 1966 b; Hesstvedt 1961，1962，1964，1969 b; Iwaskawa 1982; Turco et al. 1982; Vestine and Deirmendijan 1961; Webb 1965; Witt 1969）。
In the century that has elapsed since systematic observations of noctilucent clouds began, many observational data have been recorded and discussed at length. From the very start of the period, hypotheses have been formed and, to the extent practical, tested. Quite naturally, because noctilucent clouds came to notice with the increased awareness of twilight sky phenomena following the Krakatoa eruption, the earliest suggestions were that noctilucent clouds were simple layers of volcanic dust appearing (after a delay of a year or two) in the uppermost parts of the atmosphere. These hypotheses later gave place to more complex explanations, to account for the clouds appearing at all in a part of the atmosphere that is very dry and at a very low pressure (cf. Chvostikov 1966b; Hesstvedt 1961, 1962, 1964, 1969b; Iwaskawa 1982; Turco et al. 1982; Vestine and Deirmendijan 1961; Webb 1965; Witt 1969).