We now understand the nature of the giant
storms on Saturn. Through the analysis of images sent from the Cassini space
probe belonging to the North American and European space agencies (NASA and ESA
respectively), as well as the computer models of the storms and the examination
of the clouds therein, the Planetary Sciences Group of the University of the
Basque Country has managed to explain the behaviour of these storms for the
very first time. The article explaining the discovery, the lead author being Enrique
García Melendo, researcher at the Fundació Observatori Esteve Duran – Institut
de Ciències de l’Espai, of Catalonia, was published in Nature GeoSciences .Approximately once
every Saturnian year - equivalent to 30 Earth years - an enormous storm is
produced on the ringed planet and which affects the aspect of its atmosphere on
a global scale. These gigantic storms are known as Great White Spots, due to
the appearance they have on the atmosphere of the planet. The first observation
of one of these was made in 1876; the Great White Spot of 2010 was the sixth
one to be observed. On this occasion the Cassini space vehicle was able to
obtain very high resolution images of this great meteorological structure. The
storm initiated as a small brilliant white cloud in the middle latitudes of the
northern hemisphere of the planet, and grew rapidly and remained active for
more than seven months. Over this time an amalgam of white clouds was generated
which expanded to form a cloudy and turbulent ring with a surface area of
thousands of millions of square kilometres. Two year age the Planetary Sciences
Group presented a first study of the storm and which was published on the front
cover of Nature on the 7th of July, 2011. Now, with this new research, the
hidden secrets of the phenomenon have been revealed, studying in detail the
“head” and the “focus” of the Great White Spot.The team of astronomers analysed
the images taken from the Cassini probe in order to measure the winds in the
“head” of the storm, the focus where the activity originated. In this region
the storm interacts with the circulating atmosphere, forming very intense
sustained winds, typically of 500 kilometres an hour. “We did not expect to
find such violent circulation in the region of the development of the storm,
which is a symptom of the particularly violent interaction between the storm
and the planet’s atmosphere”, commented Enrique García. They were also able to
determine that these storm clouds are at 40 km above the planet’s own clouds.The
research revealed the mechanism that produces this phenomenology. The team of
scientists designed mathematical models capable of reproducing the storm on a
computer, providing a physical explanation for the behaviour of this giant
storm and for its lengthy duration. The calculations show that the focus of the
storm is deeply embedded, some 300 km above the visible clouds. The storm
transports enormous quantities of moist gas in water vapour to the highest
levels of the planet, forming visible clouds and liberating enormous quantities
of energy. This injection of energy interacts violently with the dominant wind
of Saturn to produce wind storms of 500 km/h. The research also showed that,
despite the enormous activity of the storm, this was not able to substantially
modify the prevailing winds which blow permanently in the same direction as the
Earth’s parallels, but they did interact violently with them. An important part
of the computer’s calculations were made thanks to the Centre de Serveis
Científics i Acadèmics de Catalunya (CESCA), and the computer services at the
Institut de Ciències de l’Espai (ICE), also based in the Catalan capital of Barcelona.Apart
from the curiosity of knowing the physical processes underlying the formation
of these giant storms on Saturn, the study of these phenomena enable us to
enhance our knowledge of the models employed in research into meteorology and
the behaviour of the Earth’s atmosphere, in a very different environment and
impossible to simulate in a laboratory. “The storms on Saturn are, in a way, a
test bank of the physical mechanisms underlying the generation of similar
meteorological phenomena on Earth”, commented Agustín Sánchez Lavega, Director
of the Planetary Sciences Group at the UPV/EHU.
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