The structure of the plasma in Jupiter’s vast magnetosphereis complicated and not fully understood. One way to study the plasma is to look at auroral emissions from the moonIo as it moves through different regions of the plasma torus that surrounds Jupiter. In this paper, the correlation between aurorabrightness on Io and the plasma density at the position of the moon is investigated. If a correlation exists, auroral emissonson Io could be used as a diagnostic for the current state ofJupiter’s plasma environment. For this purpose, a model of the Io plasma torus is developed, combining ideas from different existing models. The model is compared with observations of aurorae on Io made by the Hubble Space Telescope. Io’s position at the time of the observations is obtained with SPICE, a software developed by NASA. A moderate correlation is found when using the whole data set of observations. However, a strong correlation is found for observations on the dusk side of Jupiter. Strong correlations are also found when studying individual years and epochs. / Strukturen på plasman i Jupiters vidsträckta magnetosfär är komplicerad och inte fullständigt känd. Ett sätt att studera plasman är att undersöka ljuset från polarsken på månen Io då den passerar genom olika regioner av det torusformade plasmamolnet som omsluter Jupiter. I denna artikel undersöks korrelationen mellan polarskenets ljusstyrka och plasmans densitiet kring månens position. Om ett sådant samband finns skulle ljusstyrkan hos månens polarsken kunna användas som diagnostik för plasmans aktuella tillstånd. För detta ändamål utvecklas en modell av plasmatorusen genom att kombinera ide´er från flera tidigare modeller. Modellen jämförs sedan med observationer av polarskenet på Io genomförda med rymdteleskopet Hubble. Månens position vid de olika tidpunkterna bestäms med hjälp av SPICE, en mjukvara utvecklad av NASA. En måttligt stark korrelation uppnås när hela datamängden används. När däremot endast data från Jupiters gryningssida används uppnås en korrelation. Det hittas även starka samband när enskilda år studeras. / Kandidatexjobb i elektroteknik 2022, KTH, Stockholm

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Several studies have been conducted with the aimof finding water plumes at Jupiter’s moon Europa. The possibleevidence of plumes is important for two future space missions,the JUpiter ICy moons Explorer (JUICE) and the Europa clippermission. Multiple observations of Europa in transit of Jupiterhave been obtained with the Hubble Space Telescope (HST).In an analysis by Sparks et al. 2016 three plume candidateswere found. Later on, in the report Sparks et al. 2017 anadditional candidate was found at a similar location as a previouscandidate, potentially making the evidence of plume existencestronger. In 2020 Giono et al. reproduced the results from Sparkset al. 2016 and found uncertainties in the method that hadbeen used when finding these plume candidates. First Giono etal. claim that the position of Europa in the observation wasinadequately determined. Also, positive outliers had not beenconsidered when analyzing the z-statistic. In this study, thealgorithm developed by Giono et al. has been used to reproducethe results from Sparks et al. 2017 where additional evidence forplume activity was presented. The algorithm was then applied tothe previous observation, where plume activity had been foundin the same location. Lastly, the two observations were mergedinto one image and the algorithm was applied once again. Theresults of the z-statistic from the observations gave large negativeoutliers which can be considered as plumes. However, positive andnegative outliers had similar significance for the two independentobservations which somewhat diminishes the evidence. Also,misalignment between model and observation generates distortedstatistics. The statistical uncertainties and fluctuations can easilybe mistaken as evidence of plume existence. / Flera studier har utförts med syftet attupptäcka vattenplymer på Jupiters måne Europa. Det eventuellabeviset för att plymer existerar är viktigt för två framtidarymduppdrag, JUpiter ICy moons Explorer (JUICE) och Europaclipper mission. Flera observationer av när Europa passerarframför Jupiter har erhållits av Hubbleteleskopet (HST). I enanalys av Sparks et al. 2016 har tre kandidater för plymerhittats. I rapporten av Sparks et al. 2017 hittades ytterligare enkandidat på ungefär samma ställe, vilket potentiellt kunde stärkabeviset för att det var plymer. År 2020 reproducerade Giono et alresultaten från Sparks et al. 2016 och hittade brister i metodennär dessa plymkandidater hittades. Först pöangterar de att Europas position i observationen var felaktig. Dessutom togs detinte hänsyn till positiva avvikelser när z-statistiken betraktades.I den här rapporten har algoritmen som skapades av Gionoet al. använts för att reproducera resultaten från Sparks et al.2017 där ytterligare bevis för plymer presenterades. Algoritmenapplicerades sedan på den föregående observationen där bevis förplymer hade hittats i samma område. Därefter slogs dessa bilderihop och analyserades som en bild. Resultatet av z-statistikenfrån observationerna gav stora negativa avvikelser vilket kanses som en plym av vattenånga. Dock eftersom positiva ochnegativa avvikelser hade liknande signifikans för de två enskildaobservationerna försvagas beviset för att plymer skulle existera.Dessutom genererar lokala fel mellan modell och observation enförvrängd statistik där statistiska osäkerheter och fluktuationerenkelt kan misstas som bevis för att vattenplymer existerar / Kandidatexjobb i elektroteknik 2021, KTH, Stockholm

We study the variability of intensity of Io’s aurora asa function of Jupiter’s rotation measured in system III longitude.The far-ultraviolet intensity of Io’s aurora was measured by theHubble Space Telescope (HST) using the FUV-MAMA photondetector of the STIS. The data was processed using Matlab tofilter background and reflection, and account for the detector’soptical systems. Target regions of the detector were isolated forthe measurement of the OI(1356 ̊A) and SI(1479 ̊A) emissionsrespectively. By sampling photon detections within each emissionregion, we compute intensity reconstructions that we map tosystem III longitude. Curves were then fitted to the reconstruc-tions using a sinus fit. The results show two intensity peaks atsystem III longitudes (140±5)◦and (284±2)◦for both OIandSI. The difference in amplitude between the peaks are (38±6)%and (28±6)% for OIand SIrespectively. The asymmetriespeak intensities is possibly caused by the probability of excitingsulphur being higher than the probability of exciting sulphur.For a full explanation measurement of the oxygen to sulphurproportion in Ios atmosphere would be needed. We compare theresults to peaks of Io’s footprint on Jupiter measured by JUNOand other HST data sets. We find it likely that we confirm furthervariance in peak angle than reported in other research. This isespecially clear in the first intensity peak as it has a significantlylarger angle. Variability in Jupiter’s magnetic field and densityof the Jovian plasma torus is likely to explain peak angle andintensity variability, but further research is necessary to explainthe mechanisms in detail. / Vi studerar hur intensiteten av Ios aurora varierar i relation till Jupiters rotation mätt i system III longitud. Ios aurora mättes inom UVC området av Hubble Space Telescope (HST) med FUV-MAMA fotondetektorn. Matlab användes för att filtrera bort oönskade signaler som reflektion och bakgrund samt ta hänsyn till sensorns optiska system. Observationsområderna på sensorn konstruerades för mätningen av syre OI (1356Å ) och svavel SI (1479Å ) emissionerna. Genom att sampla fo- tondetektioner inom varje observationsområde så rekonstruerar vi en intensitetskurva som vi mappar till system III longitud. En kurva var sedan anpassad till rekonstruktionen med hjälp av en sinusanpassning. Resultaten visar två intensitetstoppar vid system III longituderna (140 ± 5)◦ och (284 ± 2)◦ för både OI och SI . Kvoten mellan topparna var (38 ± 6)% för OI och (28 ± 6)% för SI . Skillnaden i topparna kan förklaras av att sannolikheten att excitera svavel är större än att excitera syre. För fullständig beskrivning av skillnaden i topparna skulle mätningar av syre till svavel proportionen i Ios atmosfär behövas. Vi jämför våra reslutat med mätningar av Ios avtryck på Jupiter från JUNO och andra HST mätningar. Vi finner det sannolikt att vi bekräftar ytterligare varians i topparnas vinkel, främst för den första toppen vars vinkel är signifikant större. Variationer i Jupiters magnetfält och plasmadensitet av Jupiters plasmatorid kan sannolikt förklara positionen av topparna och intensitetsvariationerna. Vidare forskning behövs för att utförligt förklara dessa mekanismer. / Kandidatexjobb i elektroteknik 2020, KTH, Stockholm

La détection et la caractérisation d'exoplanètes apparaissent clairement comme des thèmes centraux de l'observation astronomique pour les années à venir. Les projets spatiaux ou au sol sont nombreux (HARPS, CoRoT, Kepler, JWST, SPHERE...), mais les études théoriques visant à l'analyse et à la compréhension des données recueillies et à venir sont nécessaires. Durant cette thèse j'ai étudié divers processus physiques affectant la structure interne et l'évolution des planètes géantes, aussi bien au sein, qu'à l'extérieur de notre système solaire. J'ai notamment modélisé en détail: -L'impact de l'irradiation intense émise par l'étoile sur l'atmosphère d'une planète à faible distance orbitale, et l'effet induit sur l'évolution interne de cette planète. -Le couplage par dissipation de marée de l'évolution orbitale et thermique d'une planète interagissant avec sa proche étoile parente. -L'effet de la déformation due aux marées sur les paramètres observables d'une planète en transit grâce au suivi photométrique de son passage devant l'étoile. -L'incidence sur la structure et l'évolution d'une diminution de l'efficacité du transport de chaleur par convection due à un gradient d'éléments lourd dans l'enveloppe gazeuse d'une planète géante, conduisant au phénomène de convection double-diffusive. A travers l'étude des ces divers processus, j'ai développé différents modèles analytiques et codes numériques qui sont à la fois flexibles et robustes, et qui permettent maintenant d'étudier certaines propriétés des nouveaux objets substellaires détectés à mesure qu'ils sont découverts. / The detection and characterization of extrasolar planets clearly appears as one of the main goals of observational astronomy for the coming years. Space and ground project are numerous, but theoretical studies aimed at analyzing and understanding available and future data are needed. During this thesis, I study various physical processes affecting the internal structure and evolution of both solar, and extrasolar giant planets. In particular I investigate : -the impact of the intense stellar irradiation received by a close in planet on its subsequent internal evolution. This allows me to quantify the radius anomaly of bloated Hot Jupiters and to constrain their internal composition. -the tidal and centrifugal distortion of a fluid planet. By using both analytical and numerical models, I show how non-sphericity of the planet affects transit measurements, yielding an underestimation of its radius. -how the presence of double-diffusive convection caused by a heavy elements gradient in the gaseous envelope of a planet can decrease the efficiency of its internal heat transport, and affect its structure and evolution. -the coupling between the orbital and the thermal evolution of a planet arising from the strong star-planet tidal interaction. Subsequently, I find that tidal heating alone is not a viable explanation for the observed radius anomaly of transiting planets. Through these different studies, I developed various analytical models and numerical codes that are both flexible and robust, and which now allow one to study the properties of new extrasolar planets and brown dwarfs as they are discovered.

Europa is one of the most interesting satellites in the solar system in the search ofextra-terrestrial life, as it harbours an interior water ocean under its icy surface. Watervapour in Europa’s atmosphere has been previously observed, suggesting water plumeeruptions from the surface. These plumes could potentially originate from the subsurfaceocean, and as such contain ocean constituents that can be examined in orbit. Twoobservations of Europa’s far-ultraviolet shadow on Jupiter were made by the HubbleSpace Telescope in 2018 and 2019. It was observed in Lyman-α (1 216 Å), a spectral lineof hydrogen. This study investigates the imaged Lyman-α shadow in search of potentialplumes at the shadow limb. Examining the shadow instead of the moon itself is a newmethod of remotely studying the Europan atmosphere. Forward modelling is applied tocreate artificial images that are compared to the observations. Any anomalies aroundthe shadow limb are then analysed and evaluated for their statistical significance. Twonoteworthy outliers are found at the limb (one on each occasion) corresponding to H2Oline of sight column densities of 3.07×1017 cm−2 and 4.72×1016 cm−2, for the 2018 and2019 observation, respectively. They are not significant however, as they lie within threestandard deviations from the expected value (< 3σ). An upper limit on what columndensity is detectable in the data is computed, yielding 6.71×1016 cm−2 (using only 2019data due to a weak signal on the 2018 occasion). A constraint on the maximum possibleH2O column density at Europa is thus provided. The new method is shown to be usefulfor the intended purpose and could potentially be applied on other icy moons. / Europa är ett av solsystemets mest intressanta objekt i jakten på utomjordiskt liv, dådet finns ett hav av vatten under månens isiga yta. Vattenånga har tidigare observeratsi Europas atmosfär, vilket kan tyda på vattenplymer som skjuts ut från ytan i kraftigautbrott. Dessa plymer kan möjligtvis ha sitt ursprung i månens inre hav, de kandärför möjliggöra en analys av havsvattnets beståndsdelar i omloppsbana. Europasultravioletta skugga på Jupiter observerades vid två tillfällen 2018 och 2019, av HubbleSpace Telescope. Observationerna gjordes i Lyman-α (1 216 Å), en spektrallinje hos väte.Denna studie undersöker den avbildade skuggan i Lyman-α för att söka efter potentiellavattenplymer vid skuggans rand. Att undersöka skuggan istället för själva månen är en nymetod för att studera Europas atmosfär genom fjärranalys. Metoden forward modellinganvänds för att skapa artificiella bilder, som jämförs med observationerna. Eventuellaavvikelser som hittas runt skuggans rand analyseras sedan och deras statistiska signifikansutvärderas. Två anmärkningsvärda avvikelser kan hittas vid randen (en vid varjeobservationstillfälle), som motsvarar H2O-kolumndensiteter på 3.07 × 1017 cm−2 och4.72 × 1016 cm−2, för 2018-observationen respektive 2019-observationen. Densiteternaär dock inte signifikanta, då de ligger inom tre standardavvikelser från deras förväntadevärden (< 3σ). Istället beräknas en övre gräns för vilken kolumndensitet som kandetekteras i datan, vilket ger 6.71 × 1016 cm−2 (där endast 2019-data används på grundav en svag signal hos 2018-observationen). Den högsta möjliga H2O-kolumndensitetenkan således begränsas. Den nya metoden visar sig vara användbar för det tänkta syftetoch kan eventuellt appliceras på andra ismånar.

Why do some religious movements succeed and spread, while others, seemingly equally popular and successful at a certain time, ultimately fail? It is from this starting point that this thesis approaches religious success or failure in the Roman Empire: exploring a new analytical method for understanding religious change: network theory. The thesis forms two parts. Part I sets out the theoretical frameworks. The focus of network theory is on the processes by which innovation spreads: how interconnectedness facilitates change. Although some innovations might be ‘superior’, viewing success or failure as the result of interplay between inherent qualities of a religious movement and the structure of the social environment in which it is embedded means it is possible to reduce value judgements about superiority or inferiority. The discussion then turns to religious change. The key point is that sociologists of religion can explain something of the processes of religious conversion (or ‘recruitment’) and the success or failure of a religious movement through an analysis of social interactions. Finally, I explain how I shall use networks both as a heuristic approach and a practical modelling technique to apply to the epigraphic data, and detail some of the previous application of networks to archaeological test cases. Part II applies these methods to the epigraphic data of three religions. In Chapter Four, I examine the cult Jupiter Dolichenus, arguing that the previous explanations for the success of the cult are untenable, showing from the epigraphy that the cult spread through a strong-tie network of Roman military officials. In Chapter Five, I look at the development of Jewish identity in the Diaspora, showing that, during the second century AD, Diaspora Jews began to actively display their Jewish identity in their epitaphs. I argue that this re-Judaization represents the ‘activation’ of an ethno-cultural network, as a response to the destruction of the Temple in Jerusalem and the crushing of the Bar Kokhba rebellion; the visible remains of the rabbinic reforms. In Chapter Six, I discuss the cult of the ‘Highest God’, Theos Hypsistos, taking Mitchell’s argument further to suggest that the huge increase in the dedications during the second-third centuries is not simply a reflection of the epigraphic habit, but rather, that the cult of Hypsistos was swelled by the Gentile god-fearers, as a result of the changes happening within Judaism itself at this time.

This study examines the practice of restoring public buildings in ancient Rome and attendant attitudes towards them in order to develop an understanding of the Roman concept of built heritage. Drawing on a combination of archaeological and textual evidence and focusing primarily on six decades from the Great Fire of AD 64 to the AD 120s, a period of dramatic urban transformation and architectural innovation, it explores the ways in which individual structures and the cityscape as a whole was rebuilt. With specific reference to the temple of Jupiter Capitolinus, it is shown how buildings developed through successive reconstructions and that the prevailing approach was to modernise the aesthetic and materiality of structures, rather than to restore them to their original appearance. Furthermore, by recognising the importance of religion as a potential agent in the restoration process, a new interpretation of the exceptional treatment of the casa Romuli is proposed. With the intention of uncovering attitudes to built heritage in society more widely, the study goes beyond analysing the physical treatment of buildings to consider also how changes to the urban fabric were received by those who experienced them firsthand. Through examining descriptions of destruction and restoration in literature of the period, particularly in the works of Seneca the Younger, Pliny the Elder, Martial and Tacitus, an insight is gained into the ways that Rome’s inhabitants responded to the redevelopment of their historic built environment. This thesis argues for a Roman concept of built heritage that is dramatically different from many modern ideas on the subject. The findings question the extent to which the historical value and identity of a structure resided in its physicality, and demonstrates that the Roman concern for historic buildings did not equate to preservation of historic architecture.

Europe est un corps silicaté enveloppé d'une couche d'H2O de 80 à 140 km d'épaisseur formant en surface une croûte de glace I. La dissipation de chaleur générée par l'effet des marées du système jovien maintiendrait un océan liquide sous la croûte de glace et permettrait une dynamique interne. L'analyse morphologique menée sur diverses structures « géologiques » imagées par Galileo apporte des informations sur la structure, l'état thermique et les vitesses de déformation de la croûte. La profondeur des transitions rhéologiques est très variable selon la localité et le type de structure, et donc selon le processus géologique impliqué. La lente relaxation de 2 bassins d'impact permet d'estimer des flux de chaleur inférieurs à 30 mW.m-2 impliquant une croûte conductive de 9 à 32 km d'épaisseur reposant sur un océan froid. Néanmoins, d'autres structures montrent des indices d'écoulements à la faveur d'une pente régionale et de déformations verticales à grande échelle (~100 km) peu fréquentes à la surface d'Europe. En outre, nous avons mis en évidence une disparition importante de croûte autour d'une bande décro-extensive dont l'ouverture serait liée à la rotation non synchrone d'Europe. Ces résultats pourront servir à contraindre les modèles physiques développés par ailleurs.