Multi-instrument analysis of Rosetta data – Establishing a new paradigm for cometary activity

Informazioni relative al progetto

MiARD

ID dell’accordo di sovvenzione: 686709

DOI

10.3030/686709

Progetto chiuso

Data della firma CE 26 Novembre 2015

Data di avvio 1 Marzo 2016

Data di completamento 31 Agosto 2018

Finanziato da

• INDUSTRIAL LEADERSHIP - Leadership in enabling and industrial technologies – Space

Costo totale

€ 1 659 064,50

Contributo UE

€ 984 437,50

Coordinato da

UNIVERSITAET BERN
Switzerland

Periodic Reporting for period 2 - MiARD (Multi-instrument analysis of Rosetta data – Establishing a new paradigm for cometary activity)

Periodo di rendicontazione: 2017-06-01 al 2018-08-31

Sintesi del contesto e degli obiettivi generali del progetto

The MiARD project has used data from the Rosetta space mission to better understand the origin and evolution of comets, and their role in the solar system (including the possibility that they may have indirectly influenced the emergence of life, by delivering volatile species such as water to the Earth).
The broad objectives of the MiARD project were to use an interdisciplinary multi-instrument approach to the analysis of data from the Rosetta mission, in order to make progress towards answering some fundamental questions about comets and the formation and evolution of the solar system. In doing this, the project has also derived information that is expected to be useful in risk mitigation for cometary and cometary-related impacts with Earth and man-made objects.
The fundamental questions are:
• How did our solar system and other planetary systems form?
• How did life develop on Earth?
• How unique are these processes?
We did not, however, expect to obtain definitive answers to these questions within the MiARD project! The project has though proceeded in a structured way to obtain information required to address these questions. We began by deriving an accurate and detailed shape model of the comet, a pre-requisite for subsequent studies of the strength of cometary materials, and for numerical modelling of the activity (outgassing of the comet). The nature of the cometary surface, its strength, and the extent of material loss are key to understanding the evolution of the comet 67P/Churyumov-Gerasimenko (and by extension, other comets), and to what extent the current state of the comet can tell us about its past. In the second half of the project, we focused on comparing what is known about 67P/Churyumov-Gerasimenko with information from other comets, and on considering the scientific case for a cometary nucleus sample return mission. We were also able to quantify the non-gravitational forces that perturb the orbit of 67P and thr comets, and the trajectories of material (dust) ejected from comets - highly relevant to the risks to Earth and spacecraft.

Lavoro eseguito dall’inizio del progetto fino alla fine del periodo coperto dalla relazione e principali risultati finora ottenuti

The MiARD project work has led to the most accurate, complete and highest resolution shape models available for comet 67P/Churyumov-Gerasimenko. The generation of these improved shape models of the comet is of central importance to the project as the global shape models are used as inputs for further work within the project e.g. the temperature and activity modelling (WP2 and WP4), and the processing of spectral datasets used for line-of-sight compositional and temperature measurements. The global shape model and local Digital Terrain Models (DTMs) have been used to make deductions about the strength and erosion rate of the cometary materials.
Analysis of data from the PHILAE lander, together with constraints derived from the shape model and laboratory analogues, has allowed the project to place numerical bounds on the material strength of different areas of the comet (in general very weak, just tens of Newtons per square metre, but with stronger icy layers). This information will be of use in interpreting the topography of the comet, in models of formation of the comet, and for any future cometary missions involving a lander, sampling of the comet or attempts to perturb a comet's trajectory. Quantitative stress maps for the comet have been derived (taking into account both self-gravity and thermal effects) and show that the highest stresses are in the neck of the comet, and may correlate with highly active regions.
'Activity' modelling of the outgassing from the comet has been successful so that the agreement between numerical models and observed data is now rather good. The extent of the agreement for different model assumptions has been tested statistically, so that some physical models can be ruled out. This work has also shown that there is unlikely to be a unique solution, and that it is not possible for example to distinguish between completely homogenous degassing, and degassing from small-scale more active sites that are distributed more or less uniformly.
Compositional maps of the major ice species have been made, and compared to models that seek to explain the chemical heterogeniety of the comet's surface. A thorough analysis of non-gravitational forces on the comet (as a result of outgassing) has been made: these affect both the comets positin/velocity and its spin.

Ten papers from the project have been published, two are in review and more are in preparation. See http://www.miard.eu/homepage/publications/

Progressi oltre lo stato dell’arte e potenziale impatto previsto (incluso l’impatto socioeconomico e le implicazioni sociali più ampie del progetto fino ad ora)

The MiARD project has developed the most accurate and complete shape model of comet 67P, and used this shape model to support better physical and numerical models of the activity (out-gassing) of the comet, including the sub-surface flow of gases through the porous cometary surface. Data from Rosetta (images and the derived shape model) have been combined with PHILAE lander observations and laboratory measurements on analogue cometary materials and processes to constrain the tensile and compressive strengths of cometary materials. Better constraints on the composition of the comet have been obtained by combining mass spectral data (from instruments on Rosetta and PHILAE) with spectroscopic data (Rosetta). Models that describe the temperature of the surface and the thermal behaviour of the comet have been developed and tested with constraints from several datasets. The (sometimes unexpected) effect of the cometary activity on surface features has been studied, proving the the surface is a dynamic environment on all timescales. A metric to relate surface topography to the dynamical 'age' of the comet has been suggested, and evidence that some boulders on the surface may be from other icy bodies has been gathered. The modelling of non-gravitational forces has constrained the value of the 'eta' momentum transfer parameter to lie between 0.6 and 0.7. All of these results are applicable to a greater or lesser extent to the study of other comets.

We do not expect the prpject to have a large or immediate socio-economic impact, but the human fascination with the origins of life and the Earth is widespread, and this project contributes to progress in this field.

A high resolution digital terrain model of the Agilkia region on comet 67P/Churyumov-Gerisimenko