Interactions of weakly or nonmagnetized bodies with solar system plasmas: Mars and the moons of Saturn
Von der Fakultät für Elektrotechnik, Informationstechnik, Physik der Technischen Universität CaroloWilhelmina zu Braunschweig zur Erlangung des Grades eines Doktors der Naturwissenschaften (Dr.rer.nat.) genehmigte Dissertation
von Elias Roussos aus Athen, Griechenland
Bibliografische Information Der Deutschen Bibliothek Die Deutsche Bibliothek verzeichnet diese Publikation in der Deutschen Nationalbibliografie; detaillierte bibliografische Daten sind im Internet über http://dnb.ddb.deabrufbar.
1. Referentin oder Referent: Prof. Dr. Uwe Motschmann 2. Referentin oder Referent: Prof. Dr. Joachim Saur eingereicht am: 28 November 2007 mündliche Prüfung (Disputation) am: 6 February 2008
ISBN 9783936586794
Copernicus Publications 2008 http://publications.copernicus.org Roussosc Elias
Images of Rhea from Cassini . . . . . . . . . . . . . . . . . . . . . . . . Overview of the simulation results for the “ideal case” run . . . . . . . . Illustration of Equations 6.7 . . . . . . . . . . . . . . . . . . . . . . . . Comparison of Equation 6.7 solutions with the simulated data . . . . . . The asymmetric shape of Rhea’s density wake parallel and perpendicular to the magnetic field lines . . . . . . . . . . . . . . . . . . . . . . . . . . Magnetic field perturbations in a the yzplane, just behind Rhea . . . . . . Magnetic field perturbations in a the xzplane downstream of Rhea . . . . Perturbations ofvyandvzin an yzcut just behind Rhea . . . . . . . . . . Perturbations ofvxandvzin an yzcut just behind Rhea . . . . . . . . . . Comparison of Equation 6.10 solution with the simulated data . . . . . . Velocity and electric field in the plasma rest frame in the wake of Rhea . . Comparison of simulation results with Cassini magnetometer data . . . . Density and velocity of escaping heavy ions from Rhea . . . . . . . . . . Synthetic spectrogram for the Rhea flyby trajectory . . . . . . . . . . . . Phasespace plot ofVzalong a trajectory parallel to the xaxis . . . . . . .
135 141 143 144
146 148 149 150 151 151 153 154 156 157 158
Reference values for charged particle motion scales at Saturn . . . . . . . 168
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List of Tables
2.1
4.1 4.2 4.3
5.1
5.2
6.1
6.2
List of LEMMS electron channels and their energy ranges . . . . . . . . 38
List of Saturn’s large icy moons . . . . . . . . . . . . . . . . . . . . . . Tethys microsignatures in the first seven orbits of Cassini . . . . . . . . . Analysis of Mimas microsignatures . . . . . . . . . . . . . . . . . . . .
70 85 94
List of several physical and orbital parameters for Telesto, Helene and Methone . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 112 Summary of the observed microsignatures from small moons . . . . . . . 119
Values and ranges of the various parameters describing Rhea’s space en vironment . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 137 List of parameters used for the two simulation runs. . . . . . . . . . . . . 139
9
Summary
The interaction of weakly or nonmagnetized planets and moons with the solar wind as well as with a magnetospheric plasma have been studied at Mars and the moons of Saturn using plasma data from the ASPERA3 instrument onboard Mars Express and energetic charged particle measurements at the moons of Saturn from the MIMI/LEMMS instru ment aboard Cassini, respectively. The analysis of data recorded for Saturn’s moons was complemented by hybrid plasma simulations. A series of results have been obtained from the study of each individual system: (a) Using plasma data from the ASPERA3 instrument onboard Mars Express, plasma fluid parameters (moments) have been extracted using two standard methods: by inte gration of the particle flux over the instruments energy range and by fitting the phase space density profiles to maxwellian distributions. The estimated moment values from two ASPERA3 sensors were evaluated by comparing them with the expected values for the solar wind and the various interaction regions within the martian magnetospheric cav ity. This comparison helped to identify the best calculation method and the limitations of each sensor. Following these steps, plasma moment maps that describe the interaction of Mars with the solar wind have been constructed for the first time and an estimation of the planet’s atmospheric erosion rates has been performed. (b) Using data on nonionospheric electrons from the ELS sensor of ASPERA3 on board Mars Express, the influence of two different factors that can control the global configuration of the Martian magnetosphere has been investigated. These two factors are the direction that the solar wind convective electric field,ES W, is pointing and the loca tion and intensity of the crustal magnetic field sources of the planet. Information on the pointing of the solar wind convective electric field was extracted by the magnetometer observations of Mars Global Surveyor (MGS), which was operating in parallel with Mars Express in orbit around Mars. Crustal magnetic field data were retrieved from standard ized maps that were originally constructed from MGS observations. The nonionospheric electron data were organized in different coordinate systems based on theES Wpointing and on the crustal field intensity. Interesting asymmetries were found for magnetosheath electrons, during extreme cases (high flux events). More specifically, it was found that high fluxes of magnetosheath electrons, measured at the terminator of the planet can in trude towards the wake under certain, combined geometries involving the planet’s crustal field locations and the pointing of theES Winfluence of the crustal fields on the in. The trusion of magnetosheath electrons at low altitudes on the planet’s dayside, has also been evaluated. (c) Within 9Rsfrom the center of Saturn (1Rs=60268 km) seven moons with a diam eter greater than 100 km are orbiting the planet in almost circular and equatorial orbits. These moons interact continuously with the trapped plasma of radiation belts. Many of