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EI2GYB > ASTRO 30.08.21 10:27l 84 Lines 4349 Bytes #999 (0) @ WW
BID : 13888_EI2GYB
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Subj: Martian global dust storm ended winter early in the south
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Sent: 210830/0925Z 13888@EI2GYB.DGL.IRL.EURO BPQ6.0.22
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Martian global dust storm ended winter early in the south
A dust storm that engulfed Mars in 2018 destroyed a vortex of cold air
around the planet's south pole and brought an early spring to the hemisphere.
By contrast, the storm caused only minor distortions to the polar vortex
in the northern hemisphere and no dramatic seasonal changes.
A dust storm that engulfed Mars in 2018 destroyed a vortex of cold air
around the planet's south pole and brought an early spring to the hemisphere.
By contrast, the storm caused only minor distortions to the polar vortex
in the northern hemisphere and no dramatic seasonal changes.
Dr Paul Streeter of The Open University's Faculty of Science, Technology,
Engineering and Mathematics will present the work today (23 July) at
the virtual National Astronomy Meeting (NAM 2021).
Over two weeks at the beginning of June 2018, localised dust storms combined
and spread to form an impenetrable blanket of dust that hid almost the
entire planet's surface.
The global dust storm, which coincided with Mars's equinox and lasted
until mid-September, proved fatal to NASA's solar-powered Opportunity rover.
Streeter and colleagues from The Open University, NASA and the Russian
Academy of Sciences examined the effects of the event on the martian
atmosphere by combining data from a Mars Global Climate Model with
observations from the European Space Agency/Roscosmos ExoMars Trace Gas
Orbiter and NASA's Mars Reconnaissance Orbiter missions.
Dr Streeter said: "This was a perfect opportunity to investigate how global
dust storms impact the atmosphere at the martian poles, which are surrounded
by powerful jets of wind in winter.
Since the last global storm in 2007, several new missions and instruments
have arrived in Mars orbit, so the 2018 event was the most-observed to date."
Previous research has shown that high levels of dust in the atmosphere
can have significant effects on polar temperatures and winds.
The vortices at the winter poles also affect temperatures and the
transport of air, dust, water and chemicals, so their disruption could
mean substantial changes in the martian atmosphere.
The team found that the 2018 storm had profoundly different effects in
each hemisphere.
At the south pole, where the vortex was almost destroyed, temperatures
rose and wind speeds fell dramatically.
While the vortex may have already been starting to decay due to the
onset of spring, the dust storm appears to have had a decisive effect in
ending winter early.
The northern polar vortex, by contrast, remained stable and the onset of
autumn followed its usual pattern. However, the normally elliptical
northern vortex was changed by the storm to become more symmetrical.
The researchers link this to the high dust content in the atmosphere
suppressing atmospheric waves caused by the extreme topography in the
northern hemisphere, which has volcanoes over twice as tall as Mount
Everest and craters as deep as terrestrial mountains.
Dr Streeter added: "Global dust storms at equinox may enhance transport
into the southern pole due to the diminished vortex, while the more
robust northern vortex continues to act as an effective barrier.
If this pattern for global dust storms holds over the course of the thousands
of years that Mars maintains this particular axial tilt, it has
implications for how dust is deposited at the north and south poles
and our understanding of the planet's climate history."
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