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2004/10/04 | 蓝色喷流[Blue Jet]
类别(¤〖天文〗)
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发表于 11:00
A sporadic optical high-altitude conical emission which occurs between the tops of some thunder clouds and the ionosphere. They were first reported by Wescott
et al
. (1995), although they had previously been reported by airline pilots. They are conical emissions at heights of about 40-50 km which persist for about 300 ms. The mechanism for generating blue jets is not understood.
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