Paving the Way for Future Space Missions in the Context of High Tidal Dissipation in the Saturnian System

Space Science Reviews Springer Nature 222:1 (2026) 20

Authors:

Valéry Lainey, Aurélien Crida, Matija Cuk, Jeffrey N Cuzzi, Dominic Dirkx, Gianrico Filacchione, James Fuller, Carly JA Howett, Kelly Miller, Francis Nimmo, Nicolas Rambaux, Marco Zannoni

Abstract:

The recent discovery of strong tidal dissipation in Saturn’s interior has radically changed our view of the Saturnian system. While some questions are naturally answered by the new paradigm, others are emerging and require further measurement. This article presents the next key questions to be addressed by future space missions and analysis. Suggestions for space measurements to discriminate between different scenarios concerning the formation, evolution and internal state of the Saturnian system are given.

Targeting Intermittently Sunlit Areas With Thermal Stability for Buried Water Ice in the South Polar Region of the Moon

Journal of Geophysical Research Planets American Geophysical Union (AGU) 131:2 (2026)

Authors:

E Sefton‐Nash, C Orgel, T Warren, SJ Boazman, O King, DA Paige, N Bowles, DJ Heather

Abstract:

Abstract Intermittently sunlit areas near the lunar south pole are estimated to harbor thermal conditions permitting long‐term stability of water ice and other volatiles. They are targets for future science and exploration missions due to the combination of sunlight availability for solar power generation, and the possibility for extraction of volatiles for scientific analysis and ISRU. We construct a geodatabase of spatially co‐registered remote sensing and thermal model results, and perform a probabilistic analysis to determine the likelihood of successfully landing and operating on such locations for a quadrangular study area that bounds the 80°S parallel. In addition to water ice thermal stability, we consider factors relevant for the operation of solar‐powered landed spacecraft: visibility to the Earth, visibility to the sun, and local slope. For two scenarios representing sets of most‐ and least‐constrained landing site requirements, we find that circular landing ellipse diameters of ∼0.9 and 2.6 km, respectively, would allow to target available compliant terrains with 100% success. We quantify the reduction in success probability with increasing landing ellipse size. Further, we explore the distributions of geometric properties of compliant areas, and identify three sites of interest that support large areas of compliant terrain: near De Gerlache crater, near Shackleton crater, and Mons Mouton (informally named as Leibnitz‐β massif). This study is provided to support planning for future lunar missions. Plain Language Summary Researchers have identified areas near the lunar poles that receive occasional sunlight and could keep water ice and other resources stable over a long period of time. These spots are valuable for future lunar missions since they could provide solar power and possibly resources such as water for scientific study and on‐site use. To assess potential landing sites in the south polar region, we created a database combining remote sensing and thermal data set, then used it to calculate the likelihood of successful landing on accessible terrains with stable water ice conditions from the 80°S to the South Pole. The study looked at factors critical for solar‐powered landers: the terrain's visibility to Earth (for communication), sunlight access, and the slope of the ground. We analyzed two scenarios with different landing precisions. We found that landing areas with diameters of about 0.9 and 2.6 km could ensure a 100% success rate under the most‐ and least‐constrained scenarios, respectively. Larger landing areas decreased the success probability. We also mapped the physical characteristics of ideal areas and highlighted three promising locations near De Gerlache crater, Shackleton crater, and Mons Mouton. Key Points We identify intermittently sunlit areas that permit long‐term stability of sub‐surface water ice, and accessible by landed missions “Compliant terrains” in two scenarios range from 13,071 km² (least constrained) to 290 km² (most constrained) in the south polar region For areas ≥80°S, we recommend sub‐km landing precision for missions with success criteria involving exploration of lunar polar water ice

Mars Science and Exploration After Mars Express

Space Science Reviews 222:1 (2026)

Authors:

D Titov, P Martin, C Wilson, O Witasse, A Cardesín-Moinelo, H Svedhem, C Parfitt, D Paardekooper, JL Vago, E Sefton-Nash, G Kminek, A Chicarro

Abstract:

Mars Express (MEX) is one of the most productive planetary missions of the European Space Agency (ESA). This low cost (∼150 M€) mission has been instrumental in shaping the planetary community in Europe and has contributed to paving the way for many subsequent ESA endeavours. During more than two decades, Mars Express has collected a wealth of data in all disciplines of Martian science. This paper concludes the Topical Collection “Mars Express: Pioneering Two Decades of European Science and Exploration of Mars” prepared under the auspices of the International Space Science Institute. It briefly describes various aspects of the mission (leaving details to dedicated articles), summarizes the major science achievements, discusses the lessons learned from 20 years of Mars Express operations, and bridges with future Mars science and exploration.

Identifying the presence of Martian material on Phobos's surface: a visible to mid-infrared spectral investigation of Mars and Phobos regolith simulant mixtures

Monthly Notices of the Royal Astronomical Society (submitted, in review)

Authors:

Branagan-Harris E, Avdellidou C, Spathis V, Rider-Stokes BG, Belhadfa EC, Figueira EK, Delbo M, Bates HC, Shirley KA, King AJ, Bowles NE, Russell SS

Abstract:

Spectral–mineralogical correlations in meteorite and simulant analogues: implications for the composition and origin of Phobos

Europlanet Science Congress 2026, EPSC2026-650 (conference abstract)

Authors:

Branagan-Harris E, Bates H, Shirley K, King A, Bowles N, Russell S

Abstract: