Age-old debate on Saturn’s rings reignited

Age-old debate on Saturn’s rings reignited

A team of researchers has reignited the debate about the age of Saturn’s rings with a study that dates the rings as most likely to have formed early in the Solar System. 

In a paper published today in Nature Astronomy and presented at the EPSC-DPS Joint Meeting 2019 in Geneva, the authors suggest that processes that preferentially eject dusty and organic material out of Saturn’s rings could make the rings look much younger than they actually are.

Cassini’s dive through the rings during the mission’s Grand Finale in 2017 provided data that was interpreted as evidence that Saturn’s rings formed just a few tens of millions of years ago, around the time that dinosaurs walked the Earth. Gravity measurements taken during the dive gave a more accurate estimate of the mass of the rings, which are made up of more than 95% water ice and less than 5% rocks, organic materials and metals. The mass estimate was then used to work out how long the pristine ice of the rings would need to be exposed to dust and micrometeorites to reach the level of other ‘pollutants’ that we see today. 

For many, this resolved the mystery of the age of the rings. However, Aurelien Crida, lead author of the new study, believes that the debate is not yet settled.

“We can’t directly measure the age of Saturn’s rings like the rings on a tree-stump, so we have to deduce their age from other properties like mass and chemical composition. Recent studies have made assumptions that the dust flow is constant, the mass of the rings is constant, and that the rings retain all the pollution material that they receive. However, there is still a lot of uncertainty about all these points and, when taken with other results from the Cassini mission, we believe that there is a strong case that the rings are much, much older,” said Dr Crida, of the Observatoire de la Côte d’Azur, CNRS.

Crida and colleagues argue that the mass measured during the Cassini mission finale is in extraordinarily good agreement with models of the dynamical evolution of massive rings dating back to the primordial Solar System. 

The rings are made of particles and blocks ranging in size from metres down to micrometres. Viscous interactions between the blocks cause the rings to spread out and carry material away like a conveyor-belt. This leads to mass loss from the innermost edge, where particles fall into the planet, and from the outer edge, where material crosses the outer boundary into a region where moonlets and satellites start to form. 

More massive rings spread more rapidly and lose mass faster. The models show that whatever the initial mass of the rings, there is a tendency for the rings to converge on a mass measured by Cassini after around 4 billion years, matching the timescale of the formation of the Solar System.

“From our present understanding of the viscosity of the rings, the mass measured during the Cassini Grand Finale would be the natural product of several billion years of evolution, which is appealing. Admittedly, nothing forbids the rings from having been formed very recently with this precise mass and having barely evolved since. However, that would be quite a coincidence,” said Dr Crida.

Co-author Hsiang-Wen Hsu was part of a team that announced results in October 2018 from Cassini’s Cosmic Dust Analyzer, which showed 600 kilogrammes of silicate grains fall on Saturn from the rings every second. Other studies using data from the Cassini Ion and Neutral Mass Spectrometer have shown the presence of organic molecules in Saturn’s upper atmosphere that are thought to derive from the rings. 

Dr Hsu, of the Laboratory for Space and Atmospheric Physics at Boulder, Colorado, said: “These results suggest that the rings are ‘cleaning’ themselves of pollutants. The nature of this potential ring-cleaning process is still mysterious. However, our study shows that the exposure age is not necessarily linked to the formation age, thus the rings may appear artificially young.” 

Images

The Saturn’s rings.
Credit: NASA/JPL-Caltech/Space Science Institute
www.europlanet-society.org/wp-content/uploads/2019/09/pia14943-full.jpg
An image of Saturn taken by Cassini.
Credit: NASA/JPL-Caltech/Space Science Institute
www.europlanet-society.org/wp-content/uploads/2019/09/pia12567-1600.jpg

Further information

Are Saturn’s rings actually young? Aurélien Crida, Sébastien Charnoz, Hsiang-Wen Hsu, and Luke Dones, EPSC-DPS 2019. 

meetingorganizer.copernicus.org/EPSC-DPS2019/EPSC-DPS2019-783-1.pdf

Are Saturn’s rings actually young? Crida, Charnoz, Hsu, Dones, Nature Astronomy, 876, 2019.

www.nature.com/articles/s41550-019-0876-y

Science Contacts

Aurélien Crida
Observatoire de la Côte d’Azur 
Nice, France
Email: crida@oca.eu

Media contact

Marc Fulconis
Observatoire de la Côte d’Azur
Nice, France
marc.fulconis@oca.eu

Anita Heward
EPSC Press Officer
+44 7756 034243
epsc-dps-press@europlanet-society.org

Livia Giacomini
EPSC Press Officer
epsc-dps-press@europlanet-society.org

Adriana Postiglione
EPSC Press Officer
epsc-dps-press@europlanet-society.org 

Notes for Editors

EPSC-DPS Joint Meeting 2019

The 2019 Joint Meeting (www.epsc-dps2019.eu) of the European Planetary Science Congress (EPSC) of the Europlanet Society and the Division for Planetary Sciences (DPS) of the American Astronomical Society (AAS) will take place at the Centre International de Conférences de Genève (CICG), Geneva, Switzerland, from Sunday 15 to Friday 20 September 2019. More than 1950 abstracts have been submitted and over 1500 planetary scientists from Europe, the US and around the world are expected to attend the meeting, making it one of the largest gatherings of planetary scientists held in Europe to date.

The EPSC-DPS Joint Meeting 2019 will be the third time that EPSC and the DPS Annual Meeting have been held together.

Follow: @europlanetmedia #EPSCDPS2019

Europlanet

The Europlanet Society, launched in September 2018, is an organization for individual and corporate members to promote the advancement of planetary science and related fields in Europe. The Society provides Europe’s planetary science community with a platform to exchange ideas and personnel, share research tools, data and facilities, define key science goals for the future, and engage stakeholders, policy makers and European citizens with planetary science. The Europlanet Society is the parent organisation of the European Planetary Science Congress (EPSC).

Europlanet Society website: www.europlanet-society.org

EPSC-DPSC 2019 Joint Meeting 2019 website: www.epsc-dps2019.eu

DPS

The Division for Planetary Sciences (DPS), founded in 1968, is the largest special-interest Division of the American Astronomical Society (AAS). Members of the DPS study the bodies of our own solar system, from planets and moons to comets and asteroids, and all other solar-system objects and processes. With the discovery that planets exist around other stars, the DPS has expanded its scope to include the study of extrasolar planetary systems as well.

The AAS, established in 1899, is the major organization of professional astronomers in North America. The membership (approx. 7,500) also includes physicists, mathematicians, geologists, engineers, and others whose research interests lie within the broad spectrum of subjects now comprising contemporary astronomy. The mission of the AAS is to enhance and share humanity’s scientific understanding of the universe, which it achieves through publishing, meeting organization, education and outreach, and training and professional development.

3D models of Mars to aid Rosalind Franklin rover in her quest for ancient life

3D models of Mars to aid Rosalind Franklin rover in her quest for ancient life

Scientists at TU Dortmund University have generated high-accuracy 3D models of terrain within the landing ellipse of the ESA/Roscosmos ExoMars rover, Rosalind Franklin. The Digital Terrain Models (DTMs) have a resolution of about 25 cm per pixel and will help scientists to understand the geography and geological characteristics of the region and to plan the path of the rover around the site.

To increase the accuracy of the models, the team has developed an innovative technique that integrates atmospheric data into the digitally-generated scenes. The models will be presented by Kay Wohlfarth at the EPSC-DPS Joint Meeting 2019 in Geneva on Monday 16 September.

The DTMs are based on high-resolution imagery of Mars from the HiRISE instrument on NASA’s Mars Reconnaissance Orbiter. HiRISE imagery has been widely applied to the classic stereo method of combining two images taken from slightly different angles to create a 3D picture of the landscape. However, conventional stereo techniques have limitations when applied to the featureless, homogeneous regions that characterise many dusty and sandy planetary surfaces, including the rover’s landing site. 

Oxia Planum, the landing site chosen by ESA’s ExoMars Landing Site Selection Working Group for Rosalind Franklin, is comparatively flat to minimise the risk of a hard landing and to ensure accessibility for the rover to carry out its mission. The region contains clay minerals and structures from ancient river beds that may bear hints of past traces of life.

To enhance the DTM, the team from TU Dortmund University has applied a technique called ‘Shape from Shading’ in which the intensity of reflected light in the image is translated into information on surface slopes. This slope data is integrated into the stereo imagery, giving an improved estimate of the 3D surface and achieving the best resolution possible in the reconstructed landscape. 

Kay Wohlfarth explained: “With the technique, even small-scale details such as dune ripples inside craters and rough bedrock can be reproduced.”

Marcel Hess, first author of the study, said: “We have taken special care over the interaction between light and the martian surface. Areas that are tilted towards the Sun appear brighter and areas that are facing away appear darker. Our approach uses a joint reflectance and atmospheric model that incorporates reflection by the surface as well as atmospheric effects that diffuse and scatter light.” 

The Rosalind Franklin ExoMars rover will carry a suite of scientific instruments to analyse rocks and the surface environment at Oxia Planum. To look beneath the surface, it carries a drill that will retrieve samples and deliver them to an onboard laboratory designed to detect biosignatures, as well as instruments to probe the subsurface water content. The mission will launch in the summer of 2020 on a Russian Proton-M launcher and arrive at Mars in March 2021.

ESA ExoMars pages: www.esa.int/exomars

Images

Rendered view of a small region revealing small details. Credit: Credit: TU Dortmund/NASAJPL-Caltech
www.europlanet-society.org/wp-content/uploads/2019/09/ROI1.png
Rendered view of a small region revealing small details.
Credit: TU Dortmund/NASAJPL-Caltech
https://www.europlanet-society.org/wp-content/uploads/2019/09/ROI2.png

Video

A video of the Digital Elevation Model of the landing site can be found at: https://youtu.be/L0HgyyqbsPg

Scientific Contact

Marcel Hess
Image Analysis Group 
TU Dortmund University
Germany
marcel.hess@tu-dortmund.de

Kay Wohlfarth
Image Analysis Group
TU Dortmund University
Germany
kay.wohlfarth@tu-dortmund.de

Christian Wöhler
Image Analysis Group 
TU Dortmund
Germany
christian.woehler@tu-dortmund.de

Ottaviano Ruesch 
European Space Agency 
Noordwijk 
The Netherlands 
ottaviano.ruesch@esa.int 

Media Contact

Anita Heward
EPSC Press Officer
+44 7756 034243
anita.heward@europlanet-eu.org
epsc-dps-press@europlanet-society.org

Livia Giacomini 
EPSC Press Officer
epsc-dps-press@europlanet-society.org 

Adriana Postiglione 
EPSC Press Officer
epsc-dps-press@europlanet-society.org

Shantanu Naidu
DPS Press Officer
dpspress@aas.org 

During the meeting, the EPSC-DPS Press Office can be contacted on +41 22 791 9617.

Further Information

Europlanet 

The Europlanet Society, launched in September 2018, is an organization for individual and corporate members to promote the advancement of planetary science and related fields in Europe. The Society provides Europe’s planetary science community with a platform to exchange ideas and personnel, share research tools, data and facilities, define key science goals for the future, and engage stakeholders, policy makers and European citizens with planetary science. The Europlanet Society is the parent organisation of the European Planetary Science Congress (EPSC).

Europlanet Society website: www.europlanet-society.org

EPSC-DPSC 2019 Joint Meeting 2019 website: www.epsc-dps2019.eu

DPS

The Division for Planetary Sciences (DPS), founded in 1968, is the largest special-interest Division of the American Astronomical Society (AAS). Members of the DPS study the bodies of our own solar system, from planets and moons to comets and asteroids, and all other solar-system objects and processes. With the discovery that planets exist around other stars, the DPS has expanded its scope to include the study of extrasolar planetary systems as well.

The AAS, established in 1899, is the major organization of professional astronomers in North America. The membership (approx. 7,500) also includes physicists, mathematicians, geologists, engineers, and others whose research interests lie within the broad spectrum of subjects now comprising contemporary astronomy. The mission of the AAS is to enhance and share humanity’s scientific understanding of the universe, which it achieves through publishing, meeting organization, education and outreach, and training and professional development.