Home News Science & Astronomy The Mars Color Imager (MARCI) camera onboard NASA’s Mars Reconnaissance Orbiter (MRO) shows the typical state of Mars, seen here in May 2018, and what the planet looked like during a planet-encircling dust storm in July 2018. (Image: © NASA/JPL-Caltech/MSSS) Massive dust towers on Mars that formed during global storms…
The Mars Color Imager (MARCI) camera onboard NASA’s Mars Reconnaissance Orbiter (MRO) shows the typical state of Mars, seen here in May 2018, and what the planet looked like during a planet-encircling dust storm in July 2018.
(Image: © NASA/JPL-Caltech/MSSS)
Massive dust towers on Mars that formed during global storms may be “space elevators” that contributed to the loss of the planet’s ancient water, according to NASA’s description of new research.
Dust towers can loom dozens of miles above Mars’ surface and are part of larger dust storms that sweep up the planet’s iconic reddish dirt, blanketing the world. One giant storm last year brought NASA’s Opportunity mission to an end and masked Mars’ features in a dull coating of dust, as seen in an incredible moving image from NASA’s Mars Reconnaissance Orbiter. The scientists behind the new research said they wanted to better understand how storms like these work.
During a global storm, dust towers “are renewed continuously for weeks,” the lead author for both papers, Nicholas Heavens of Hampton University in Hampton, Virginia, said in a recent NASA statement about the dust towers. The space agency said that in some cases, it observed multiple towers for as long as 3.5 weeks. These structures stretch upward, much like thunderstorm clouds do on Earth, and the researchers said the dust towers may have played a part in the evaporation of Mars’ ancient water into space.
The sight of an Earthly thunderstorm cloud is unmistakable: The tall formation is ominous, and people exercise caution after spotting one, as the cloud could bring dramatic atmospheric activity like a lightning strike. Thunderstorm clouds grow tall because of the sun; as the heat from the star warms the moisture in Earth’s atmosphere, water particles ascend higher into the sky.
That heat also powers dust towers on Mars. The dust clouds, described in NASA’s statement as “space elevators,” lift particles of water and dirt that have hitched a ride on the rising dust streamers that create the cloud. The updraft carries water vapor and one of its gaseous building blocks, hydrogen, up to the planet’s upper atmosphere; here, in Mars’ ancient past, these particles may have then evaporated and disappeared from the Red Planet in large quantities.
To understand how Earthly thunderstorm clouds affect our daily lives, meteorologists study the larger phenomenon, known as deep convection, that produces them. Mars has a deep convection system as well, and the scientists behind the new research studied that system for answers about Martian dust storms.
The first of the two recent papers published by Heavens’ team laid out a framework for how to study this Martian convection system. Researchers called the Red Planet’s atmospheric conveyor belt “dusty deep convection.”
In their more recent paper, the researchers studied the last two dust events that engulfed Mars, which occurred in 2007 and 2018, and how water molecules were moving around the planet at the time.
There are still some mysteries about dust towers and the role they play in massive dust storms. One idea is that the dust towers form randomly from lifted dust; another is that they come together as hurricane-like storms that then envelop the planet in dust.
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