airglow layer

简明释义

气辉层;

英英释义

The airglow layer refers to a faint emission of light by the Earth's atmosphere, primarily occurring at night due to various chemical reactions and photochemical processes in the upper atmosphere.

空气发光层是指地球大气中微弱的光发射,主要在夜间发生,源于上层大气中的各种化学反应和光化学过程。

例句

1.During the meteor shower, the airglow layer 空气辉光层 provided a beautiful backdrop for the falling stars.

在流星雨期间,空气辉光层为流星提供了美丽的背景。

2.The scientists observed the airglow layer 空气辉光层 during their nighttime study of atmospheric phenomena.

科学家们在夜间研究大气现象时观察到了空气辉光层

3.Astronomers often take images of the airglow layer 空气辉光层 to study its effects on astronomical observations.

天文学家经常拍摄空气辉光层的图像,以研究其对天文观测的影响。

4.The airglow layer 空气辉光层 emits light due to chemical reactions in the upper atmosphere.

由于高层大气中的化学反应,空气辉光层会发出光。

5.The brightness of the airglow layer 空气辉光层 can vary depending on solar activity.

根据太阳活动的不同,空气辉光层的亮度可能会有所变化。

作文

The universe is a vast and mysterious place, filled with wonders that continue to captivate the minds of scientists and enthusiasts alike. One such phenomenon is the airglow layer, which is a faint emission of light produced by various processes occurring in the Earth's atmosphere. Understanding this ethereal glow not only enhances our knowledge of atmospheric science but also deepens our appreciation for the intricate interactions between different layers of the atmosphere. The airglow layer can be observed during the night, providing a subtle illumination that is often overshadowed by the brightness of stars and other celestial bodies. It is most noticeable in regions with minimal light pollution, where the natural beauty of the night sky can be fully appreciated.The origins of the airglow layer are primarily linked to the interaction of solar radiation with atmospheric particles. When ultraviolet light from the sun strikes atoms and molecules in the upper atmosphere, it excites them, causing them to emit light as they return to their original state. This process results in a continuous, albeit faint, glow that can be seen from the ground. The airglow layer is typically found at altitudes ranging from 30 to 100 kilometers above the Earth's surface, where the atmosphere is thin yet still capable of sustaining these complex interactions.Various factors can influence the intensity and visibility of the airglow layer. Solar activity plays a significant role; during periods of heightened solar activity, such as solar flares or coronal mass ejections, the emissions can become more pronounced. Additionally, seasonal changes and geographic location also affect the visibility of the airglow layer. For instance, regions closer to the equator may experience more intense airglow due to higher levels of atmospheric ionization.The study of the airglow layer has implications beyond mere observation. Scientists utilize this phenomenon to gather valuable data about the composition and dynamics of the atmosphere. By analyzing the characteristics of the emitted light, researchers can infer information about atmospheric temperatures, densities, and chemical compositions. This research contributes to our understanding of climate change and atmospheric processes, making the airglow layer a vital component of atmospheric science.In conclusion, the airglow layer is a fascinating aspect of our atmosphere that serves as a reminder of the complexity and beauty of the natural world. Its subtle glow, born from the interactions of solar radiation and atmospheric particles, highlights the delicate balance of forces at play above us. As we continue to explore the mysteries of our universe, the airglow layer stands as a testament to the wonders that await our discovery, urging us to look up and appreciate the night sky in all its glory.

宇宙是一个广阔而神秘的地方,充满了让科学家和爱好者们不断着迷的奇观。其中一个现象就是空气辉光层,它是由地球大气中发生的各种过程产生的微弱光 emission。理解这种空灵的光辉不仅增强了我们对大气科学的认识,还加深了我们对大气不同层次之间复杂相互作用的欣赏。空气辉光层可以在夜间观察到,提供了一种微妙的照明,常常被星星和其他天体的亮度所掩盖。在光污染最小的地区,这种现象最为明显,让人们能够充分欣赏夜空的自然美。空气辉光层的起源主要与太阳辐射与大气粒子的相互作用有关。当来自太阳的紫外线照射到高层大气中的原子和分子时,它们会被激发,导致它们在回到原始状态时发出光。这一过程导致了一种持续的、虽然微弱的光辉,可以从地面看到。空气辉光层通常位于离地球表面30到100公里的高度,在这个高度上,大气稀薄,但仍然能够维持这些复杂的相互作用。各种因素可以影响空气辉光层的强度和可见性。太阳活动起着重要作用;在太阳活动增强的时期,例如太阳耀斑或日冕物质抛射,发射的光可能会更加明显。此外,季节变化和地理位置也会影响空气辉光层的可见性。例如,靠近赤道的地区可能由于更高水平的大气电离而经历更强烈的空气辉光。对空气辉光层的研究不仅仅是观察。科学家利用这一现象收集关于大气成分和动态的宝贵数据。通过分析发射光的特征,研究人员可以推断出关于大气温度、密度和化学成分的信息。这项研究有助于我们理解气候变化和大气过程,使空气辉光层成为大气科学的重要组成部分。总之,空气辉光层是我们大气中一个迷人的方面,提醒我们自然界的复杂性和美丽。它微弱的光辉,源于太阳辐射和大气粒子之间的相互作用,突显了我们头顶上力量之间的微妙平衡。随着我们继续探索宇宙的奥秘,空气辉光层作为我们发现奇迹的见证,促使我们仰望天空,欣赏夜空的所有辉煌。

相关单词

airglow

airglow详解:怎么读、什么意思、用法

layer

layer详解:怎么读、什么意思、用法