Europlanet Science Congress 2020
Virtual meeting
21 September – 9 October 2020
Europlanet Science Congress 2020
Virtual meeting
21 September – 9 October 2020

Oral presentations and abstracts

TP16

Martian research in Europe has grown exceptionally over the past decades, first thanks to the longstanding achievements of the Mars Express community and more recently thanks to the great contributions of the ExoMars 2016 Trace Gas Orbiter mission, leading Europe to a prime role within the international martian community. This valuable experience has paved the way for the new exciting discoveries expected in the next years from the ExoMars Rover and Surface Platform and in the future by the Mars Sample Return programme.

The aim of this session is to recognize the experience gained with European Mars missions and promote new synergies to enhance the collaboration within the European science community, in close coordination with other international agencies (NASA, Roscomos, JAXA, CSA, etc.)

This session welcomes contributions from any field of Martian scientific research, including also operational, technical and interdisciplinary aspects involving the different Mars missions, especially those covering multi-mission and international collaborations over a wide range of topics: Mars subsurface, surface geology and mineralogy, atmosphere, magnetosphere, martian moons and any potential exo-biological implication in the context of the new exploration missions.

Public information:
Session summary is now available online with the showcase presentation given by the Project Scientists of all ESA's Mars missions. This includes the latest science highlights from Mars Express and Trace Gas Orbiter, the status of the ExoMars 2022 Rover and Surface Platform and the preparations for the Mars Sample Return programme. Please visit the presentations and do not hesitate to comment and discuss with all authors, especially Early Career Researchers.

Convener: Alejandro Cardesin-Moinelo | Co-conveners: Dmitrij Titov, Elliot Sefton-Nash, Håkan Svedhem, Jorge Vago, Patrick Martin, Gerhard Kminek

Session assets

Session summary

Chairperson: Alejandro Cardesin-Moinelo
Mars Express
Chairperson: Alejandro Cardesin-Moinelo
EPSC2020-720
| MI
Dmitrij Titov, Jean-Pierre Bibring, Alejandro Cardesin, Tom Duxbury, Francois Forget, Marco Giuranna, Francisco González-Galindo, Mats Holmström, Ralf Jaumann, Anni Määttänen, Patrick Martin, Franck Montmessin, Roberto Orosei, Martin Pätzold, and Jeffrey Plaut and the Mex Sgs Team

After 16 years in orbit Mars Express remains one of ESA’s most scientifically productive Solar System missions which publication record now approaches 1300 papers. Characterization of the geological processes on a local-to-regional scale by HRSC, OMEGA and partner experiments on NASA spacecraft has allowed constraining land-forming processes in space and time. Recent studies suggest geological evidence of a planet-wide groundwater system on Mars and surface clay formation during short-term warmer and wetter conditions on a largely cold ancient Mars. HRSC team released the Digital Elevation Model (DEM) of the MC-11 quadrangle and the Southern polar cap at 50 m/px resolution. Mars Express provided essential contribution to the selection of the Mars-2020 landing sites and supporting characterization of potential landing sites for Chinese Tianwen-1 mission.

One-and-one-half decade of monitoring of atmospheric parameters such as temperature, dust loading, water vapor and ozone abundance, water ice and CO2 clouds distribution, collected by SPICAM, PFS, OMEGA, HRSC and VMC together with subsequent modeling have provided key contributions to our understanding of the Martian climate. In 2019 PFS confirmed observations of a methane abundance “spike” in the Gale crater observed in situ by the Curiosity Rover. Recent similar quasi-simultaneous observations were in disagreement, thus indicating that the methane “enigma” continues. This poses a significant challenge to both observers and modelers. The radio-science experiment MaRS revealed fine structure of the boundary layer which depth varies from 2 km in topographic lows to ~10 km over highlands.

Observations of the ion escape during a complete solar cycle revealed that ion escape can be responsible for removal of about 10 mbar of the atmosphere over Mars’ history. This implies existence of other, more effective, escape channels. The structure of the ionosphere derived from MARSIS and MaRS sounding was found to be significantly affected by the solar activity, dust loading in the lower atmosphere, and crustal magnetic field. The observations suggest that the sunlit ionosphere over the regions with strong crustal fields is denser and extends to higher altitudes as compared to the regions with no crustal anomalies. Ionospheric models aim at creating user-friendly data base of plasma parameters that would be of great service to the planetary community. Focused exploration of the Martian moons continues.

The mission is notionally extended till the end of 2022. A science case for the mission extension till the end of 2025 has been submitted. The talk will give the Mars Express status, review the recent science highlights, and outline future plans including synergistic science with TGO.

How to cite: Titov, D., Bibring, J.-P., Cardesin, A., Duxbury, T., Forget, F., Giuranna, M., González-Galindo, F., Holmström, M., Jaumann, R., Määttänen, A., Martin, P., Montmessin, F., Orosei, R., Pätzold, M., and Plaut, J. and the Mex Sgs Team: Mars Express science highlights and future plans, Europlanet Science Congress 2020, online, 21 Sep–9 Oct 2020, EPSC2020-720, https://doi.org/10.5194/epsc2020-720, 2020.

Chairperson: Alejandro Cardesin-Moinelo
EPSC2020-632ECP
| MI
Julia Marín-Yaseli de la Parra, Alejandro Cardesín-Moinelo, Donald Merritt, Michel Breitfellner, Manuel Castillo Fraile, Emmanuel Grotheer, Marc Costa í Sitjà, Carlos Muñiz Solaz, Eleni Ravanis, Patrick Martin, and Dimitri Titov

INTRODUCTION

MEX remains one of ESA’s most scientifically productive missions and has fully accomplished its initial mission objectives. It was the first European mission to Mars and the first ESA mission to orbit another planet. Its global surveys of the surface, the atmosphere and the plasma environment of the Red Planet were possible to achieve thanks to the elliptical orbit of MEX. The mission provides a unique platform for Mars climate evolution research to help understand the complex atmospheric processes present on Mars. This scenario is ideal for fulfilling diverse science goals from the instruments on board with new scientific and operational challenges in the coming years.

NEW CHALLENGES FOR MISSION EXTENSIONS 2021-2022 and 2023-2025

In addition to the regular global surface, climate and plasma monitoring, the future mission extensions will have various new challenging science campaigns. The scientific goals for the extensions 2021-2022 and 2023-2025 are described in detail by (Titov et al EPSC2020).

Figure 1. Main scientific and operational seasons for Mars Express between 2021 and 2025

These are some of the new challenging objectives that are planned for the mission extensions :

  • Hi-resolution observations of atmosphere & ionosphere

  • First active plasma sounding at another planet (MARSIS/ASPERA)

  • MEX/TGO inter-spacecraft occultation radio science

  • Ionosphere and plasma at Solar Maximum

  • Global topography (completion of colour & stereo imagery)

  • Active & transient surface effects

  • Phobos observatios with full instrument suite

  • Joint observations with TGO and Rosalind Franklin (RSP)

With the successive confirmations of the Mars Express (MEX) mission extension, doors are opened to gather new science. New technological challenges appear in the Science Ground Segment (SGS) of the European Space Agency, which is characterized by its variability, flexibility and diversity.

IMPLEMENTATION OF NEW SCIENCE OBSERVATIONS

In this manuscript we present here various new observation campaigns that are defined to fulfil the scientific objectives of the new mission extensions and summarize the inventive modifications our team has made in order to continue with the flexibility in terms of planning the mission extensions.

Mars Express has a highly elliptical polar orbit that crosses the equatorial orbit of Phobos every 5~7 months (Figure 2 and Witasse et al.2014). During these seasons, several flyby campaigns are organized and all instruments are pointed to the moon with different observation requirements (illumination, distance, rotation rates, etc).

Figure 2. Illustration of Mars Express crossing Phobos orbit. Image taken by HRSC in November

2019, orbit 20076, at a distance of ~2400 km (ESA/DLR/FU Berlin).

A good example of new science campaigns are the new Local Time Scans, where the spacecraft is rotated (Figure 3) to cover a wide range of local times and longitudes in the same latitude region.

Figure 3. Mars Express Local Time Scans. Left: spacecraft is rotated along the scan direction,

perpendicular to the satellite motion. Right: three local time scans over Hellas planitia; red circles

show PFS field of view; colours represent illumination angle (cyan is dark around local morning,

yellow is brighter close to local noon). (Credit ESA/DLR/FU Berlin/MAPPS/J.Marín-Yaseli)

This Local Time Scanning campaign was created in 2019 based on a new request by the Planetary Fourier Spectrometer (PFS) to increase the local time coverage of the measurements to improve the climatic record, which was limited by the spacecraft trajectory. Based on this requirement, a new pointing type was defined to improve the local time coverage over certain regions of the planet. This new observation type is now used by all spectrometers (PFS, SPICAM, OMEGA) allowing for the identification of inter-diurnal variations in certain regions of interest, as shown for Hellas Planitia above.

New tests will be executed throughout summer 2020 to assess the performance of radio measurements at the exit of the earth occultations (Figure4). Although the operational concepts of ingress+egress occultations were formulated at the beginning of the mission, it was not until mid-2020 that the first campaigns were revised for execution. The egress occultations will bring the opportunity to observe wider latitude/longitude areas still uncovered by previous campaigns.

Figure 4. Radio Science ingress+egress occultations as seen from the Earth (left) and plotted against

latitude and true anomaly (right).

The first tests to carry out radio science communications between the two spacecraft are expected to start by the end of 2020 (Figure 5 and Cardesín-Moinelo, et al. Icarus 2020). The technical and scientific requirements for these new observations impose new challenges in the operations of the two missions. In particular, the preparation of the observations requires a long-term geometrical analysis of the pointing requirements and visibility opportunities between the two spacecraft, as well as detailed coordination between the scientific and technical teams for the configuration and execution of the measurements to ensure the correct data interpretation.