极光电影内容介绍英语作文（极光影视yyds）

本文目录一览：

• 1、北极光 英文介绍

• 2、极光英文介绍

• 3、《极光》请用∥给文章分层要从哪几个方面介绍了极光？

• 4、极光：最奇妙的天象之谜

• 5、谁有极光的英文介绍？

北极光 英文介绍

不是上面的翻译。

是介绍 北极光（Aurora Borealis）的英文短文：

极光：

Auroras (North/South Polar Lights) are natural colored light displays in the sky, usually observed at night, particularly in the polar zone. They typically occur in the ionosphere. Some scientists[who?] call them "polar auroras". In northern latitudes, the effect is known as the aurora borealis, named after the Roman goddess of dawn, Aurora, and the Greek name for north wind, Boreas. It often appears as a greenish glow or sometimes a faint red, as if the sun was rising from an unusual direction. The aurora borealis is also called the northern polar lights, as it is only visible in the North sky from the Northern Hemisphere. The aurora borealis most often occurs from September to October and from March to April. The Cree call this phenomenon the Dance of the Spirits.

Its southern counterpart, the aurora australis/southern polar lights, has similar properties. Australis is the Latin word for "of the South".

Benjamin Franklin first brought attention to the "mystery of the Northern Lights." He theorized the shifting lights to a concentration of electrical charges in the polar regions intensified by the snow and other moisture.

极光英文介绍

Sometimes on Earth we can see pretty light shows in the sky called the Northern Lights or the Southern Lights. These light shows are also called the aurora. Guess what? Earth isn't the only planet with aurora! This picture shows the aurora around the North Pole of the planet Jupiter. The Hubble Space Telescope took the picture in 1998. The aurora form a ring or oval around Jupiter's pole. What makes the aurora? Charged particles zoom along Jupiter's magnetic field lines. When the particles crash into gases in Jupiter's atmosphere, they give off light. That light is the aurora!

《极光》请用∥给文章分层要从哪几个方面介绍了极光？

《极光》一书中，以诗意的笔触记录了自己到世界各地观察观光的追光之旅，并以科学严谨的态度描述了关于极光的各种知识。

对于极光，人类有一个漫长的认知过程。

有人在《圣经旧约》中找到了最早关于极光的文字记载，《创世纪》中写道：“日落天黑，不料有冒烟的炉，并点燃的灯，从那些肉块中经过。”炉和灯代表上帝，上帝被描绘成天光，但这代表着上帝的天光，完全符合北极光的特征。

极光的珍异罕见与变化无常，或者可以解释它为何会被奉为天神的原因。

更令人惊异的是，极光还在中国古代传说中被赋予了黄帝父亲的身份。

许多史书中的记载告诉我们，异常天象与伟人降生这件事总是有着密切联系。

有记录显示，公元前2000年，黄帝轩辕氏的母亲看到“大电绕枢斗星，大霓绕北斗枢星（大熊座）”之后生了黄帝。

极光：最奇妙的天象之谜

极光多姿多彩，变化万千，任何彩笔都很难绘出那在严寒的两极空气中嬉戏无常、变幻莫测的炫目之光。

极光有时出现时间极短，犹如节日的焰火在空中闪现一下就消失得无影无踪；有时却可以在苍穹之中辉映几个小时；有时像一条彩带，有时像一团火焰，有时像一张五光十色的巨大银幕，仿佛上映一场球幕电影。

极光形成之谜长期以来，人们一直认为极光可能是由以下三种原因形成的：一种看法认为，极光是红日西沉以后，透射反照出来的辉光。另一种看法认为，极光是地球外面燃起的大火，因为北极区临近地球的边缘，所以能看到这种大火。还有一种看法认为，极地冰雪丰富，它们在白天吸收阳光，贮存起来，到夜晚释放出来，便成了极光。直到20世纪60年代，科学家将地面观测结果与卫星和火箭探测到的资料结合起来研究，才逐步形成了极光的物理性描述。

如今人们认识到，极光主要是由地球磁层亚暴活动产生的高速粒子流与大气原子冲撞而产生的。太阳风与大气原子冲撞后可以产生极光，但这种极光极其微弱，肉眼一般无法看到。我们现在肉眼所能见的那些绚烂多姿的极光都是所谓的“亚暴极光”。

磁层亚暴是地球磁层中巨大能量贮存和突然释放的瞬变活动，大约每天发生3至4次，每次释放能量大约相当于一次中等地震的能量，除了在地球极区空间环境的剧烈变化，还在地球电离层激发强烈扰动，影响GPS导航信号的接收，以及卫星和地球之间的通信联络。

在哪儿可以看到极光现象极光出现于星球的高磁纬地区上空，是一种绚丽多彩的发光现象，一般呈带状、弧状、幕状或放射状。地球的极光是来自地球磁层或太阳的高能带电粒子流（太阳风）使高层大气分子或原子激发（或电离）而产生。在南极发生的叫南极光，在北极发生的叫北极光。我国在北半球，所以在我国只能看到北极光。极光不只在地球上出现，太阳系内的其他一些具有磁场的行星上也有极光。

极光的奇妙作用极光不仅是个光学现象，而且是个无线电现象，可以用雷达进行探测研究，它还会辐射出某些无线电波。通过极光谱分析，可以了解沉降粒子束来源、粒子种类、能量大小、地球磁尾的结构、地球磁场与行星磁场的相互作用，以及太阳扰乱对地球的影响方式与程度等。有人还说，极光能发出各种各样的声音。极光不仅是科学研究的重要课题，它还直接影响到无线电通信、长电缆通信以及长的管道和电力传送线等许多实用工程项目。极光还可以影响到气候，影响生物学过程。当然，极光也还有许许多多没有解开的谜。

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谁有极光的英文介绍？

An aurora (plural: auroras or aurorae) is a natural light display in the sky, particularly in the high latitude (Arctic and Antarctic) regions, caused by the collision of energetic charged particles with atoms in the high altitude atmosphere (thermosphere). The charged particles originate in the magnetosphere and solar wind and are directed by the Earth's magnetic field into the atmosphere. Aurora is classified as diffuse or discrete aurora. Most aurora occur in a band known as the auroral zone[1][2] which is typically 3° to 6° in latitudinal extent and at all local times or longitudes. The auroral zone is typically 10° to 20° from the magnetic pole defined by the axis of the Earth's magnetic dipole. During a geomagnetic storm, the auroral zone will expand to lower latitudes. The diffuse aurora is a featureless glow in the sky which may not be visible to the naked eye even on a dark night and defines the extent of the auroral zone. The discrete aurora are sharply defined features within the diffuse aurora which vary in brightness from just barely visible to the naked eye to bright enough to read a newspaper at night. Discrete aurorae are usually observed only in the night sky because they are not as bright as the sunlit sky. Aurorae occur occasionally poleward of the auroral zone as diffuse patches[3] or arcs (polar cap arcs[4]) which are generally invisible to the naked eye.