Atmospheric phenomena are those that originate in the atmosphere, such as wind , clouds, rain, snow, auroras, thunderstorms, and others. However, in this article, I will be discussing three atmospheric phenomena that are undoubtedly a source of fascination for humans.
3 atmospheric phenomena
Next, I will talk about 3 atmospheric phenomena that are undoubtedly dreamlike; these are:
1. Polar lights
When we see the Northern Lights, we should note that if they originate in areas near the North Pole, they are called the aurora borealis . When we see them at the South Pole, they are called the aurora australis. These tend to appear specifically from September to October and from March to April, during periods of peak sunspot activity. They are best seen in Norway, Alaska, Canada, Sweden, Finland, Scotland, Russia, and other locations. The Northern Lights are a phenomenal display of light.
In another sense, this aurora is triggered by the expression of electrons carrying an energy charge similar to a spectrum ranging from 1 to 15 electronvolts, and the light is released when they collide with the atoms of the air we breathe, especially with fractions of oxygen and nitrogen, usually at altitudes between 80 and 150 km. An anomalous process of ionization, segregation, and particle motion then develops.
the northern lights
The aurora borealis is a natural phenomenon that produces astonishing clarity , where diverse colors and indescribable beauty can be observed. This occurs when solar winds disturb Earth's magnetic field . Similarly, the particles released in each solar flare become trapped in the atmosphere, causing ejections on the star's surface and initiating what we know as solar storms. Solar storms are another fascinating phenomenon worth exploring.
In this sense, the aurora borealis can appear in various forms; that is, it can be seen as points of light or as different bands with a horizontal or circular orientation. However, it is always formed by the Earth's magnetic field . The colors can be many; in other words, we can find them in orange, red, blue, yellow, and green. Often, they appear in several shades at the same time.
Origin of an aurora borealis
An aurora borealis is produced by various violent transformations that occur specifically in the magnetic field of our sun, releasing a large amount of energy into the sky. Thus, when solar storms occur , the Earth is bombarded by a significant increase in solar winds. At these times, auroras are more frequent. However, while we are rewarded with this beautiful display of natural light, we are also influenced by the media.
The 11 best places to catch a glimpse of the northern lights
Some of the areas to see the magnificent Northern Lights include: Fairbanks, Alaska, USA; Yellowknife, Canada; Abisko , Sweden; Unstad, Lofoten, Norway; Jökulsárlón, Iceland; Cairngorms National Park, Scotland; Kangerlussuaq, Greenland; Tromsø, Norway; Paatsjoki, Finnish Lapland; and Muonio, Finnish Lapland.
2. Thunderstorm
A thunderstorm is a localized storm, an atmospheric or meteorological phenomenon characterized by flashes of lightning and thunder. It is a fascinating and sometimes feared atmospheric phenomenon due to the potential danger it poses, as well as the loud noises it produces. Meteorological phenomena are often associated with extreme weather events.
Thunderstorms bring intense and torrential rains , accompanied by loud but short-lived thunder, followed by flashes of lightning. If one observes a thunderstorm closely, it resembles an anvil, as the clouds above appear flat.
On another note, thunderstorms can occur anywhere on our planet , provided there are warm, saturated conditions. They are more common during the spring and summer months, and particularly during the evenings and nights.
Creating an electrical storm
A thunderstorm requires high humidity, as well as rising air and a prominence mechanism that tends to push the air. The process involved in the creation of this atmospheric phenomenon is as follows:
1. First, one must witness hot air containing water vapor.
2. Hot air rises , but remains hotter than the air surrounding it.
3. As it rises, it transfers heat from the Earth's surface to the higher levels of the atmosphere. The water vapor freezes, clumps together, and forms a cloud.
4. It is important to note that the cloud, specifically its upper portion, tends to be colder than its lower portion. The water vapor originating in the upper area then transforms into ice fragments that continue to rise.
5. Heat increases within the cloud, and more gas forms, at the same time that very cold wind blows from the top of the cloud . Hail is another phenomenon that can be related to these types of whirlwinds.
THE FACT: Ice fragments from the inner part of the cloud are carried up and down by the air. The collision of these fragments creates lightning bolts that jump, forming areas of enormous electrical charge and subsequently erupting as flashes of light.
3. Zodiac light
Zodiacal light is an atmospheric phenomenon that occurs every spring . It's created by a cloud of dust that blankets the entire Solar System. This "fog" is composed primarily of particles from the debris of thousands of comets that pass through our system over many years. The sun's rays are then reflected by this dust, and what we see in the sky is this glow. However, it's not visible just anywhere; we have to look for it. Natural phenomena are fascinating and offer many surprises.
Ways to find the zodiacal light
The first thing you should do is stay away from bright light sources or areas with high light pollution. The reflection of zodiacal light is so fragile that it wouldn't be considered significant in these situations.
After that, crane your neck and look west after twilight. You will find a radiant band with a triangular shape extending along the plane of the ecliptic, where each of the constellations of the Zodiac is located.
Representation of the phenomenon
Zodiacal light is a glow that makes the night sky appear more serene in the west after sunset. This light is caused by a ring of dust 600 million kilometers across, extending as far as Jupiter's orbit. Only the central portion is thick enough to scatter sunlight and be visible just after twilight or before dawn. The zodiacal halo is only partially visible.
Undoubtedly, talking about the 3 atmospheric phenomena is very important since we realize the detailed way in which the essences of nature are perceived.
