Search Publications

Bilobate comet morphology and internal structure controlled by shear deformation
DOI: 10.1038/s41561-019-0307-9 Bibcode: 2019NatGe..12..157M

Jorda, L.; Lamy, P. L.; Lara, L. M. +45 more

Bilobate comets—small icy bodies with two distinct lobes—are a common configuration among comets, but the factors shaping these bodies are largely unknown. Cometary nuclei, the solid centres of comets, erode by ice sublimation when they are sufficiently close to the Sun, but the importance of a comet's internal structure on its erosion is unclear.…

2019 Nature Geoscience
Rosetta 25
Widespread distribution of OH/H2O on the lunar surface inferred from spectral data
DOI: 10.1038/s41561-018-0065-0 Bibcode: 2018NatGe..11..173B

Edwards, Christopher S.; Bandfield, Joshua L.; Poston, Michael J. +1 more

Remote-sensing data from lunar orbiters have revealed spectral features consistent with the presence of OH or H2O on the lunar surface. Analyses of data from the Moon Mineralogy Mapper spectrometer onboard the Chandrayaan-1 spacecraft have suggested that OH/H2O is recycled on diurnal timescales and persists only at high latit…

2018 Nature Geoscience
Chandrayaan-1 74
Author Correction: Atmospheric mountain wave generation on Venus and its influence on the solid planet's rotation rate
DOI: 10.1038/s41561-018-0257-7 Bibcode: 2018NatGe..11..965N

Lebonnois, S.; Navarro, T.; Schubert, G.

In the version of this Article originally published, a statement regarding past measurements of the length of day and rotation rate of Venus was potentially misleading. The original statement has now been replaced in the online versions of this Article, to acknowledge that neither Magellan nor Venus Express measured an instantaneous rotation rate.

2018 Nature Geoscience
VenusExpress 0
Remote detection of widespread indigenous water in lunar pyroclastic deposits
DOI: 10.1038/ngeo2993 Bibcode: 2017NatGe..10..561M

Milliken, Ralph E.; Li, Shuai

Laboratory analyses of lunar samples provide a direct means to identify indigenous volatiles and have been used to argue for the presence of Earth-like water content in the lunar interior. Some volatile elements, however, have been interpreted as evidence for a bulk lunar mantle that is dry. Here we demonstrate that, for a number of lunar pyroclas…

2017 Nature Geoscience
Chandrayaan-1 84
Snow precipitation on Mars driven by cloud-induced night-time convection
DOI: 10.1038/ngeo3008 Bibcode: 2017NatGe..10..652S

Montmessin, Franck; Hinson, David P.; Forget, François +4 more

Although it contains less water vapour than Earth's atmosphere, the Martian atmosphere hosts clouds. These clouds, composed of water-ice particles, influence the global transport of water vapour and the seasonal variations of ice deposits. However, the influence of water-ice clouds on local weather is unclear: it is thought that Martian clouds are…

2017 Nature Geoscience
MEx 29
Timing of water plume eruptions on Enceladus explained by interior viscosity structure
DOI: 10.1038/ngeo2475 Bibcode: 2015NatGe...8..601B

Nimmo, Francis; Porco, Carolyn; Čadek, Ondřej +3 more

At the south pole of Saturn's icy moon Enceladus, eruptions of water vapour and ice emanate from warm tectonic ridges. Observations in the infrared and visible spectra have shown an orbital modulation of the plume brightness, which suggests that the eruption activity is influenced by tidal forces. However, the observed activity seems to be delayed…

2015 Nature Geoscience
Cassini 45
Groundwater activity on Mars and implications for a deep biosphere
DOI: 10.1038/ngeo1706 Bibcode: 2013NatGe...6..133M

Michalski, Joseph R.; Niles, Paul B.; Cuadros, Javier +3 more

By the time eukaryotic life or photosynthesis evolved on Earth, the martian surface had become extremely inhospitable, but the subsurface of Mars could potentially have contained a vast microbial biosphere. Crustal fluids may have welled up from the subsurface to alter and cement surface sediments, potentially preserving clues to subsurface habita…

2013 Nature Geoscience
MEx 174
Variations of sulphur dioxide at the cloud top of Venus's dynamic atmosphere
DOI: 10.1038/ngeo1650 Bibcode: 2013NatGe...6...25M

Montmessin, Franck; Bertaux, Jean-Loup; Marcq, Emmanuel +1 more

Sulphur dioxide is a million times more abundant in the atmosphere of Venus than that of Earth, possibly as a result of volcanism on Venus within the past billion years. A tenfold decrease in sulphur dioxide column density above Venus's clouds measured by the Pioneer Venus spacecraft during the 1970s and 1980s has been interpreted as decline follo…

2013 Nature Geoscience
VenusExpress 137
Transport-driven formation of a polar ozone layer on Mars
DOI: 10.1038/ngeo1957 Bibcode: 2013NatGe...6..930M

Montmessin, Franck; Lefèvre, Franck

Since the seasonal and spatial distribution of ozone on Mars was detected by the ultraviolet spectrometer onboard the spacecraft Mariner 7, our understanding has evolved considerably thanks to parallel efforts in observations and modelling. At low-to-mid latitudes, martian ozone is distributed vertically in two main layers, a near-surface layer an…

2013 Nature Geoscience
MEx 39
A chaotic long-lived vortex at the southern pole of Venus
DOI: 10.1038/ngeo1764 Bibcode: 2013NatGe...6..254G

Hueso, R.; Sánchez-Lavega, A.; Drossart, P. +3 more

Polar vortices are common in the atmospheres of rapidly rotating planets. On Earth and Mars, vortices are generated by surface temperature gradients and their strength is modulated by the seasonal insolation cycle. Slowly rotating Venus lacks pronounced seasonal forcing, but vortices are known to occur at both poles, in an atmosphere that rotates …

2013 Nature Geoscience
VenusExpress 33