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NASA spots “Strange Ice Cloud” over Saturn’s moon titan


NASA spots “strange Ice cloud” over Saturn’s largest moon, Titan. Saturn’s moon Titan has been known as the most Earthlike world found to date.

Founded strange Ice clouds appearance battle everything known about the moon’s environment.


The strange appearance of the ice cloud has inspire NASA scientists to inform that a various process than already guess  may be identical to one view over Earth’s poles . It could be take the form of the clouds.

Founded in Titan’s stratosphere, the cloud is made of a modulate of nitrogen and carbon known as dicyanoacetylene  as C4N2, an organizer in the chemical cocktail that colours the specious moon’s cloudy, it’s like  brownish orange atmosphere.


Decades ago, the infrared appliance on NASA’s navigator one spacecraft spotted strange  ice cloud same as this one on Moon’s Titan.

What has involved scientists ever since is that they find out less than one per cent of the dicyanoacetylene gas required for the cloud to concentrate, as NASA said.

Using Cassini’s compounded infrared spectrometer,  researchers found a large, CIRS , large-altitude cloud made of the same dense chemical.


Just as navigator found, when it comes to the steam form of this chemical, CIRS reported that Titan’s stratosphere is as tedious as a desert, as NASA said.

“The appearance of this strange ice cloud goes against everything we know about the way clouds form on Moon’s Titan,” said Carrie Anderson, a CIRS co-investigator at NASA’s Goddard Space Flight Center and lead author of the study.

The typical process for take the form of clouds involves moisture. On Earth, we are aware with the cycle of steam and moisture of water.


A different condensation process takes place in the Titan’s stratosphere , the field above the troposphere  at the moon’s south and north winter poles.

In this case, layers of clouds castrate as the universal broadcast pattern forces warm gases downward at the pole. The gases then thicken  as they drown through cooler and cooler layers of the polar stratosphere.

Some way, a cloud forms when the air pressure and temperature are beneficial  for the steam to concentrate into ice. The steam and the ice access a balance point  moderation  that is laid down  by the air pressure temperature.

Because of this communize, scientists can calculate the amount of steam where ice is present.


“For clouds that concentrate, this moderation is compulsory, like the law of depth,” said Robert Samuelson, scientist at Goddard.

However, the numbers do not tally for the cloud made from dicyanoacetylene. The scientists rated that they would required at least 100 times more steam to form an ice cloud where the cloud top was watched by Cassini’s CIRS.

Instead of the cloud forming by summarization, they think the C4N2 ice forms because of respond taking place on other kinds of ice particles.


Researchers call this “solid-state chemistry,” because the reactions aggregate the ice, or solid, form of the chemical.

The speculation will need to be confirmed through further Cassini observations, so until then, Titan’s cloud remains a mystery.

To solve the issue, NASA scientists deeply obliterate into how polar stratospheric clouds, also called as nacreous clouds, form on Earth. When chlorofluorocarbon gases are formed and enter into the stratosphere, they will not unite with water steam. Instead, they magnate to small ice crystals.



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