Mother Of Pearl Clouds: Explaining The Appearance Of Nacreous Clouds
As one publication stated, "once seen are never forgotten." It refers to a rare, unique, and breathtaking meteorological phenomenon called Nacreous Clouds that occasionally occurs in the skies above the Arctic.
This phenomenon is also known as mother of pearl clouds, a sporadic cloud formation that appears in regions within and bordering the Arctic Circle. These clouds are more commonly known as nacreous clouds.
What makes nacreous clouds so unique is not only their rare occurrence but also the wide array of colors they display that has a uniquely surreal look to them. It is from their unique color pattern that the name "mother of pearl clouds" originated.
(The reason for the "mother of pearl" association and resulting name will be explained in more detail later in this article.)
For the remainder of this article, the name "nacreous clouds" will be used to describe this phenomenon. Wherever necessary, though, the term "mother of pearl clouds" will be brought into the discussion to explain the association or draw a correlation.
In this article, we will focus on what nacreous clouds are, how they form, and what their characteristics are.
Nacreous Clouds Definition
From the introduction alone, it has become crystal clear that a nacreous cloud occurrence is a very unique and awe-inspiring phenomenon. It begs the question as to what they are and how they form.
Before looking at their origin and formation, one first needs to establish a clear and concise definition of what nacreous clouds are:
What are Nacreous Clouds?
Nacreous clouds are polar stratospheric clouds that occur high in the stratosphere moments after sunset in regions close to or in the Arctic Circle. This rare meteorological phenomenon, mostly limited to polar regions, is identified by its unique display of iridescent colors and patterns.
Nacreous clouds are high-level clouds that occur in the stratosphere over polar regions at heights of 15 000 – 25 000 meters (49 000 – 82 000 ft). They are officially known as polar stratospheric clouds.
This phenomenon can be best observed within the first two hours after sunset when rays of light illuminate the clouds from below the horizon. The resulting iridescent colors produced are a product of ice crystals scattering and refracting the light as it reaches the cloud.
Iridescence is an optical occurrence that causes objects to display vivid rainbow-like colors. In the case of nacreous clouds, the colors can vary from luminous and vivid to the familiar pastel colors that are so unique and contributes to the surreal effect of this phenomenon.
Why Are They Called Mother Of Pearl Clouds?
The word "nacreous" in nacreous clouds is derived from the word "nacre." Nacre is the substance responsible for the iridescent rainbow and pastel colors known as "mother of pearl" found in certain mollusk shells.
In jewelry, a pearl starts forming in a mollusk shell as nacre starts building up around a small particle like a grain of sand. As the pearl grows, the inside of the shell also gets covered with nacre.
The unique iridescent colors of the inner shell covered with this substance closely resemble nacreous clouds. Hence the subsequent naming of the meteorological phenomenon as "mother of pearl clouds."
This section gave a clear explanation of what nacreous clouds are, their characteristics, and why they display their unique "mother of pearl" colors. The focus should now shift to how these cloud phenomena form, which we will address in the next section.
How Nacreous Clouds Form
As previously stated in the definition, nacreous clouds form at high altitudes, approximately 15 000 – 25 000 meters (49 000 – 82 000 ft) above the surface in the lower stratosphere. It is these high altitudes that allow them to remain illuminated for some period after sunset.
The clouds also need to be illuminated from below for iridescence to occur, which means mother of pearl clouds can only be observed after sunset when the sun is between 1 - 6 degrees below the horizon.
Nacreous clouds also form under very low temperatures. The clouds can only form once the air temperature drops below -78° Celsius. It is also part reason why the phenomenon is mostly observed in Arctic regions, which experience these low temperatures.
The air over the polar regions is normally very dry, making cloud formation a very rare occurrence. When clouds do form at high altitudes above the surface, the ice crystals in nacreous clouds are much smaller than those that form in normal cloud formations.
It is these smaller ice crystals that allow the sunlight to be scattered and refracted in such a way to produce the vibrant iridescent colors that are so unique to this occurrence.
During the day, nacreous clouds may resemble pale Cirrus clouds that may be almost unnoticeable. Once the sun dips below the horizon, however, the clouds start to display bright luminous colors.
As the sun continues to sinks further below the horizon, the bright luminous clouds slowly change into a mixture of pink, green, and mostly pastel-colored formations, which contributes to the the surreal effect that is so unique to nacreous clouds.
Unlike most other fast-moving cloud formations that occur much lower in the atmosphere, the aptly named mother of pearl clouds also seems to remain stationary in the sky as a result of their great height.
Nacreous (or mother of pearl) clouds are rare occurrences that appear almost exclusively over the Arctic regions and are seen by very few people in selected areas as a result.
Yet, their appearance and surreal color displays are so unique and captivating that they are better known than their rarity suggests, especially in meteorological circles.
This article examined and explained what nacreous clouds are, their characteristics, and how they are formed. It also described why they are called mother of pearl clouds and described the shared connection between the two phenomena.
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