Martian low‐altitude magnetic topology deduced from MAVEN/SWEA observations

The Mars Atmosphere and Volatile Evolution mission has obtained comprehensive particle and magnetic field measurements. The Solar Wind Electron Analyzer provides electron energy‐pitch angle distributions along the spacecraft trajectory that can be used to infer magnetic topology. This study presents pitch angle‐resolved electron energy shape parameters that can distinguish photoelectrons from solar wind electrons, which we use to deduce the Martian magnetic topology and connectivity to the dayside ionosphere. Magnetic topology in the Mars environment is mapped in three dimensions for the first time. At low altitudes (<400 km) in sunlight, the northern hemisphere is found to be dominated by closed field lines (both ends intersecting the collisional atmosphere), with more day‐night connections through cross‐terminator closed field lines than in the south. Although draped field lines with ~100 km amplitude vertical fluctuations that intersect the electron exobase (~160–220 km) in two locations could appear to be closed at the spacecraft, a more likely explanation is provided by crustal magnetic fields, which naturally have the required geometry. Around 30% of the time, we observe open field lines from 200 to 400 km, which implies three distinct topological layers over the northern hemisphere: closed field lines below 200 km, open field lines with foot points at lower latitudes that pass over the northern hemisphere from 200 to 400 km, and draped interplanetary magnetic field above 400 km. This study also identifies open field lines with one end attached to the dayside ionosphere and the other end connected with the solar wind, providing a path for ion outflow.Key PointsPitch angle‐resolved electron energy shape parameters are used to deduce magnetic topologyClosed magnetic field lines dominate low altitudes (<400 km) of the northern hemisphere on the daysideThe 3‐D view of the Martian magnetic topology is presented for the first timePeer Reviewedhttps://deepblue.lib.umich.edu/bitstream/2027.42/136484/1/jgra53291.pdfhttps://deepblue.lib.umich.edu/bitstream/2027.42/136484/2/jgra53291_am.pd

The nightside ionosphere of Mars unveiled by suprathermal electron depletions

L'ionosphère du côté nuit de Mars reste encore à ce jour une zone mystérieuse et peu connue de l'environnement Martien. Les déplétions d'électrons suprathermiques sont des structures spécifiques à cette région, observées jusqu'à présent par trois satellites : Mars Global Surveyor (MGS), Mars EXpress (MEX) et Mars Atmosphere and Volatile EvolutioN (MAVEN). Leur étude permet aussi bien l'observation de la structure et de la dynamique de l'ionosphère du côté nuit que celle de l'atmosphère neutre, de la topologie magnétique martienne, ainsi que l'étude de l'échappement atmosphérique de Mars. Des structures aussi différentes que les cornets magnétiques, les couches de courants ou encore le terminateur ultra-violet peuvent être examinées à travers les déplétions d'électrons suprathermiques, de par les mécanismes à l'origine de leur présence du côté nuit de Mars. Le but principal de ma thèse a été de tirer parties des trois jeux de données offerts par les satellites MGS, MEX et MAVEN pour mieux comprendre les mécanismes à l'origine des déplétions d'électrons suprathermiques observées du côté nuit ainsi que leur impact sur la structure et la dynamique de l'ionosphère du côté nuit. Dans cette optique, trois critères simples adaptés à chaque mission ont été développés pour identifier les déplétions d'électrons suprathermiques dans une base de données allant de 1999 à 2017. Une étude statistique a révélé la présence d'une région de transition autour de 170 km d'altitude séparant la région collisionnelle dans laquelle les déplétions d'électrons suprathermiques sont directement dues à l'absorption des électrons par le CO_2 atmosphérique, et la région non-collisionnelle dans laquelle elles sont principalement dues aux boucles fermées de champs magnétique d'origine crustale. La compréhension de ces mécanismes m'a permis d'estimer la localisation du terminateur ultra-violet. Celui-ci est situé en moyenne ~120 km au-dessus du terminateur optique. Cette altitude varie entre le côté soir et le côté matin, et une variation saisonnière est prédite par les modèles atmosphériques.The nightside ionosphere of Mars still remains an unfamiliar and mysterious place. Nightside suprathermal electron depletions are specific features of this region which have been observed at Mars by three spacecraft to date: Mars Global Surveyor (MGS), Mars EXpress (MEX) and the Mars Atmosphere and Volatile EvolutioN (MAVEN) mission. Their study enables the observation of the nightside ionosphere structure and dynamics as well as the underlying neutral atmosphere, the specific Martian magnetic topology, and possible conduits for atmospheric escape. Structures as different as magnetic cusps, current sheets or the UV terminator can be investigated through suprathermal electron depletions, due to the processes leading to their observation on the nightside of Mars. The main goal of my PhD has been to use the complementarity of the three missions MGS, MEX, and MAVEN to understand the different mechanisms at the origin of suprathermal electron depletions and their implication on the structure and the dynamics of the nightside ionosphere. In this context, three simple criteria adapted to each mission have been implemented to identify suprathermal electron depletions from 1999 to 2017. A statistical study reveals a transition region near 170 km altitude separating the collisional region where suprathermal electron depletions are directly due to electron absorption by atmospheric CO_2 and the collisionless region where they are mainly due to electron exclusion by closed crustal magnetic field loops. Understanding of these phenomena enables me to estimate the location of the UV terminator. It appears to be located ~120 km above the optical terminator, though this location is different between the dawn and dusk terminator and is expected to vary throughout the different Martian seasons

L’ionosphère du côté nuit de Mars dévoilée par les déplétions d’électrons suprathermiques

The nightside ionosphere of Mars still remains an unfamiliar and mysterious place. Nightside suprathermal electron depletions are specific features of this region which have been observed at Mars by three spacecraft to date: Mars Global Surveyor (MGS), Mars EXpress (MEX) and the Mars Atmosphere and Volatile EvolutioN (MAVEN) mission. Their study enables the observation of the nightside ionosphere structure and dynamics as well as the underlying neutral atmosphere, the specific Martian magnetic topology, and possible conduits for atmospheric escape. Structures as different as magnetic cusps, current sheets or the UV terminator can be investigated through suprathermal electron depletions, due to the processes leading to their observation on the nightside of Mars.The main goal of my PhD has been to use the complementarity of the three missions MGS, MEX, and MAVEN to understand the different mechanisms at the origin of suprathermal electron depletions and their implication on the structure and the dynamics of the nightside ionosphere. In this context, three simple criteria adapted to each mission have been implemented to identify suprathermal electron depletions from 1999 to 2017. A statistical study reveals a transition region near 170 km altitude separating the collisional region where suprathermal electron depletions are directly due to electron absorption by atmospheric CO_2 and the collisionless region where they are mainly due to electron exclusion by closed crustal magnetic field loops. Understanding of these phenomena enables me to estimate the location of the UV terminator. It appears to be located ~120 km above the optical terminator, though this location is different between the dawn and dusk terminator and is expected to vary throughout the different Martian seasons.L’ionosphère du côté nuit de Mars reste encore à ce jour une zone mystérieuse et peu connue de l’environnement Martien. Les déplétions d’électrons suprathermiques sont des structures spécifiques à cette région, observées jusqu’à présent par trois satellites : Mars Global Surveyor (MGS), Mars EXpress (MEX) et Mars Atmosphere and Volatile EvolutioN (MAVEN). Leur étude permet aussi bien l’observation de la structure et de la dynamique de l’ionosphère du côté nuit que celle de l’atmosphère neutre, de la topologie magnétique martienne, ainsi que l’étude de l’échappement atmosphérique de Mars. Des structures aussi différentes que les cornets magnétiques, les couches de courants ou encore le terminateur ultra-violet peuvent être examinées à travers les déplétions d’électrons suprathermiques, de par les mécanismes à l’origine de leur présence du côté nuit de Mars.Le but principal de ma thèse a été de tirer parties des trois jeux de données offerts par les satellites MGS, MEX et MAVEN pour mieux comprendre les mécanismes à l’origine des déplétions d’électrons suprathermiques observées du côté nuit ainsi que leur impact sur la structure et la dynamique de l’ionosphère du côté nuit. Dans cette optique, trois critères simples adaptés à chaque mission ont été développés pour identifier les déplétions d’électrons suprathermiques dans une base de données allant de 1999 à 2017. Une étude statistique a révélé la présence d’une région de transition autour de 170 km d’altitude séparant la région collisionnelle dans laquelle les déplétions d’électrons suprathermiques sont directement dues à l’absorption des électrons par le CO_2 atmosphérique, et la région non-collisionnelle dans laquelle elles sont principalement dues aux boucles fermées de champs magnétique d’origine crustale. La compréhension de ces mécanismes m’a permis d’estimer la localisation du terminateur ultra-violet. Celui-ci est situé en moyenne ~120 km au-dessus du terminateur optique. Cette altitude varie entre le côté soir et le côté matin, et une variation saisonnière est prédite par les modèles atmosphériques

Dawn/dusk asymmetry of the Martian UltraViolet terminator observed through suprathermal electron depletions

International audienceSuprathermal electron depletions are structures of the nightside ionosphere of Mars resulting from an equilibrium between electron loss and creation processes. Photoionization of oxygen and carbon dioxide by UV and EUV photons is the main ionization process of the Martian atmosphere. The observation of suprathermal electron depletions is strongly unexpected in the portion of the Martian environment where photoionization can occur. This region is delimited by the UltraViolet (UV) terminator, behind which no UV ionizing photons are detected.In this study suprathermal electron depletions are used to determine the position of the UV terminator thanks to MAVEN observations. The MAVEN spacecraft is now in its fourth year of data recording and has already covered more than one Martian year, a large range of latitude, local time and solar zenith angle in the nightside down to 110 km altitude. This coverage enables us to determine the approximate position of the UV terminator over one Martian year. We then investigate the variation of its position on the dawn and dusk sides and depending on seasons. Our results are compared with models of the Martian atmosphere and in‐situ data of the atmospheric composition which all highlight an asymmetry between the dusk and the dawn sides at equinox. However, models show an inversion in the position of the dusk and the dawn UV terminator at perihelion and aphelion, which cannot yet be confirmed or disproved by the data

MAVEN and MEX multi‐instrument study of the dayside of the Martian induced magnetospheric structure revealed by pressure analyses

International audienceA combination of statistical studies and 18 case studies have been used to investigate the structure of the induced Martian magnetosphere. The different plasma and magnetic pressure forces on the dayside of the induced magnetosphere of Mars have been studied using 3.5 years of Mars Atmosphere and Volatile Evolution (MAVEN) and Mars Express (MEX) observations. We present estimates of typical values for the dominant pressure terms, i.e., the thermal pressures of the ionosphere and the magnetosheath, the magnetic pressure of the magnetic pile‐up region, and the solar wind dynamic pressure. For 18 typical orbits the altitudes and relative distances of the pressure balance boundaries, the photoelectron boundary (PEB), the ion composition boundary (ICB), and the induced magnetosphere boundary (IMB) are estimated. The Magnetic Pile‐up Boundary (MPB) is discussed but not further studied since earlier characterisations of the MPB do not agree with our results.This study focuses on the transition region between the ionosphere and the magnetosheath on the dayside of Mars. We show that earlier definitions of the PEB, ICB, and IMB do not characterise the transition region well, mainly because each boundary is based on measurements from only one or two instruments. In order to characterise the transition region correctly changes in magnetic field strength and fluctuations, dominant ion species, electron and ion densities and energy distributions, need to be considered. This article confirms a complex interaction between Mars and the solar wind and can explain why previous studies have had difficulties to describe the force balance

Ionizing Electrons on the Martian Nightside: Structure and Variability

International audienceThe precipitation of suprathermal electrons is the dominant external source of energy deposition and ionization in the Martian nightside upper atmosphere and ionosphere. We investigate the spatial patterns and variability of ionizing electrons from 115 to 600 km altitude on the Martian nightside, using CO2 electron impact ionization frequency (EIIF) as our metric, examining more than 3 years of data collected in situ by the Mars Atmosphere and Volatile EvolutioN spacecraft. We characterize the behavior of EIIF with respect to altitude, solar zenith angle, solar wind pressure, and the geometry and strength of crustal magnetic fields. EIIF has a complex and correlated dependence on these factors, but we find that it generally increases with altitude and solar wind pressure, decreases with crustal magnetic field strength and does not depend detectably on solar zenith angle past 115°. The dependence is governed by (a) energy degradation and backscatter by collisions with atmospheric neutrals below 220 km and (b) magnetic field topology that permits or retards electron access to certain regions. This field topology is dynamic and varies with solar wind conditions, allowing greater electron access at higher altitudes where crustal fields are weaker and also for higher solar wind pressures, which result in stronger draped magnetic fields that push closed crustal magnetic field loops to lower altitudes. This multidimensional electron flux behavior can in the future be parameterized in an empirical model for use as input to global simulations of the nightside upper atmosphere, which currently do not account for this important source of energy

Plasma acceleration in the Martian magnetotail

International audienceSince November 2014, the Mars Atmosphere and Volatile EvolutioN (MAVEN) spacecraft has been collecting data from Mars’s upper atmosphere and induced magnetosphere (Jakosky et al., 2015). Evidences of escaping planetary ions have been reported from earlier missions as Mars-Express (Barabash et al., 2007) and more recently from MAVEN (e.g. Dong et al., 2015, Brain et al., 2015). Our goal is to determine the acceleration mechanism responsible for the energization of planetary ions in the Martian plasma sheet. MAVEN has a full plasma package with a magnetometer and plasma particles instruments, which allow to address the question of plasma particle acceleration.According to Dubinin et al. (2011), the j x B force due to magnetic shear stresses of the draped field lines is expected to play a major role in such energization process. On MAVEN data, we have first identified and characterized current sheet crossings taking place in Mars’ magnetotail and then tested the Walén relation to infer the significance of the j x B force in the particle’s energization. To characterize the plasma sheet crossing we have worked with MAVEN magnetometer (MAG, Connerney et al., SSR, 2015) and mass spectrometer (STATIC, McFadden et al., SSR, 2015) data, focusing on a particular event. We have performed a minimum variance analysis, on the magnetic field observations which allows to characterize the current sheet. We present results of the Walén test and our conclusions on planetary plasma acceleration in the plasma sheet region

The LatHyS database for planetary plasma environment investigations: Overview and a case study of data/model comparisons

International audienceWe present the Latmos Hybrid Simulation (LatHyS) database, which is dedicated to the investigations of planetary plasma environment. Simulation results of several planetary objects (Mars, Mercury, Ganymede) are available in an online catalogue. The full description of the simulations and their results is compliant with a data model developped in the framework of the FP7 IMPEx project. The catalogue is interfaced with VO-visualization tools such AMDA, 3DView, TOPCAT, CLweb or the IMPEx portal. Web services ensure the possibilities of accessing and extracting simulated quantities/data. We illustrate the interoperability between the simulation database and VO-tools using a detailed science case that focuses on a three-dimensional representation of the solar wind interaction with the Martian upper atmosphere, combining MAVEN and Mars Express observations and simulation results

MAVEN observations of the response of Mars to an interplanetary coronal mass ejection

International audienceCoupling between the lower and upper atmosphere, combined with loss of gas from the upper atmosphere to space, likely contributed to the thin, cold, dry atmosphere of modern Mars. To help understand ongoing ion loss to space, the Mars Atmosphere and Volatile Evolution (MAVEN) spacecraft made comprehensive measurements of the Mars upper atmosphere, ionosphere, and interactions with the Sun and solar wind during an interplanetary coronal mass ejection impact in March 2015. Responses include changes in the bow shock and magnetosheath, formation of widespread diffuse aurora, and enhancement of pick-up ions. Observations and models both show an enhancement in escape rate of ions to space during the event. Ion loss during solar events early in Mars history may have been a major contributor to the long-term evolution of the Mars atmosphere

Loss of the Martian atmosphere to space: Present-day loss rates determined from MAVEN observations and integrated loss through time

International audienceObservations of the Mars upper atmosphere made from the Mars Atmosphere and Volatile Evolution (MAVEN) spacecraft have been used to determine the loss rates of gas from the upper atmosphere to space for a complete Mars year (16 Nov 2014 – 3 Oct 2016). Loss rates for H and O are sufficient to remove ∼2-3 kg/s to space. By itself, this loss would be significant over the history of the planet. In addition, loss rates would have been greater early in history due to the enhanced solar EUV and more-active Sun. Integrated loss, based on current processes whose escape rates in the past are adjusted according to expected solar evolution, would have been as much as 0.8 bar CO2 or 23 m global equivalent layer of H2O; these losses are likely to be lower limits due to the nature of the extrapolation of loss rates to the earliest times. Combined with the lack of surface or subsurface reservoirs for CO2 that could hold remnants of an early, thick atmosphere, these results suggest that loss of gas to space has been the dominant process responsible for changing the climate of Mars from an early, warmer environment to the cold, dry one that we see today