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  • 1
    Buch
    Buch
    Köln : Inst. für Geophysik und Meteorologie der Univ. zu Köln
    Schlagwort(e): Hochschulschrift ; Jupiter ; Jupitermond ; Magnetosphäre ; Plasmawechselwirkung ; Jupiter ; Io ; Europa ; Plasmawechselwirkung ; Jupiter ; Jupitermond ; Magnetosphäre ; Plasmawechselwirkung ; Jupiter ; Io ; Europa ; Plasmawechselwirkung
    Materialart: Buch
    Seiten: IV, 151 S. , Ill., graph. Darst.
    Serie: Mitteilungen aus dem Institut für Geophysik und Meteorologie der Universität zu Köln 138
    Sprache: Englisch
    Anmerkung: Zsfassung in engl. und dt. Sprache , Zugl.: Köln, Univ., Diss., 2000
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    Schlagwort(e): Forschungsbericht
    Materialart: Online-Ressource
    Seiten: 1 Online-Ressource (17 Seiten, 510,92 KB) , Diagramme
    Sprache: Deutsch
    Anmerkung: Förderkennzeichen BMWi 50 OR 1705 , Paralleltitel dem englischen Berichtsblatt , Unterschiede zwischen dem gedruckten Dokument und der elektronischen Ressource können nicht ausgeschlossen werden , Sprache der Zusammenfassung: Deutsch, Englisch
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  • 3
    Schlagwort(e): Forschungsbericht ; Europa ; Atmosphäre ; Wasser
    Materialart: Online-Ressource
    Seiten: 1 Online-Ressource (17 Seiten, 1,15 MB) , Illustrationen, Diagramme
    Sprache: Deutsch
    Anmerkung: Förderkennzeichen BMWi 50OR1313 , Im Kopf der Titelseite: IGM Geophysics Cologne , Unterschiede zwischen dem gedruckten Dokument und der elektronischen Ressource können nicht ausgeschlossen werden , Sprache der Zusammenfassung: Deutsch, Englisch
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 4
    Schlagwort(e): Forschungsbericht ; Ganymed ; Polarlicht ; Unterirdisches Wasser ; Hubble-Weltraumteleskop
    Materialart: Online-Ressource
    Seiten: 1 Online-Ressource (19 Seiten, 1,17 MB) , Illustrationen, Diagramme
    Sprache: Deutsch
    Anmerkung: Förderkennzeichen BMBF 50 OR 1116 , Unterschiede zwischen dem gedruckten Dokument und der elektronischen Ressource können nicht ausgeschlossen werden , Zusammenfassungen in deutscher und englischer Sprache
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 5
    Schlagwort(e): Forschungsbericht ; Io ; Europa ; Atmosphäre ; Magnetosphäre ; Hubble-Weltraumteleskop
    Materialart: Online-Ressource
    Seiten: Online-Ressource (22 S., 2,76 MB) , Ill., graph. Darst.
    Sprache: Deutsch
    Anmerkung: Förderkennzeichen BMWi 50 OR 0805. - Engl. Berichtsblatt u.d.T.: Analysis of hubble space telescope observations of Jupiters moons Europa and Io , Unterschiede zwischen dem gedruckten Dokument und der elektronischen Ressource können nicht ausgeschlossen werden , Systemvoraussetzungen: Acrobat reader.
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  • 6
    Materialart: Buch
    Seiten: 26 S , graph. Darst , 30 cm
    Serie: Research notes / Institut für Geophysik und Meteorologie, Universität zu Köln No. 002
    Sprache: Englisch
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 7
    Publikationsdatum: 2022-09-22
    Beschreibung: Io's movement relative to the plasma in Jupiter's magnetosphere creates Alfvén waves propagating along the magnetic field lines which are partially reflected along their path. These waves are the root cause for auroral emission, which is subdivided into the Io Footprint (IFP), its tail and leading spot. New observations of the Juno spacecraft by Mura et al. (2018, https://doi.org/10.1126/science.aat1450) have shown puzzling substructure of the footprint and its tail. In these observations, the symmetry between the poleward and equatorward part of the footprint tail is broken and the tail spots are alternatingly displaced. We show that the location of these bright spots in the tail are consistent with Alfvén waves reflected at the boundary of the Io torus and Jupiter's ionosphere. Then, we investigate three different mechanisms to explain this phenomenon: (a) The Hall effect in Io's ionosphere, (b) travel time differences of Alfvén waves between Io's Jupiter facing and its opposing side and (c) asymmetries in Io's atmosphere. For that, we use magnetohydrodynamic simulations within an idealized geometry of the system. We use the Poynting flux near the Jovian ionosphere as a proxy for the morphology of the generated footprint and its tail. We find that the Hall effect is the most important mechanism under consideration to break the symmetry causing the “Alternating Alfvén spot street.” The travel time differences contributes to enhance this effect. We find no evidence that the inhomogeneities in Io's atmosphere contribute significantly to the location or shape of the tail spots.
    Beschreibung: Key Points: Hall effect in Io's ionosphere produces Poynting flux morphology similar to observed alternating Alfvén spot street in Io footprint tail (IFP). Alfvén wave travel time difference and asymmetries in Io's atmosphere are not sufficient to produce observed structures in IFP. IFP emission inter‐spot distance correlates with reflected Alfvén waves.
    Beschreibung: Regional Computing Center of the University of Cologne (RRZK)
    Beschreibung: European Research Council (ERC)
    Beschreibung: http://plutocode.ph.unito.it/download.html
    Schlagwort(e): ddc:523
    Sprache: Englisch
    Materialart: doc-type:article
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 8
    Publikationsdatum: 2024-01-15
    Beschreibung: 〈title xmlns:mml="http://www.w3.org/1998/Math/MathML"〉Abstract〈/title〉〈p xmlns:mml="http://www.w3.org/1998/Math/MathML" xml:lang="en"〉On 7 June 2021 the Juno spacecraft visited Ganymede and provided the first in situ observations since Galileo's last flyby in 2000. The measurements obtained along a one‐dimensional trajectory can be brought into global context with the help of three‐dimensional magnetospheric models. Here we apply the magnetohydrodynamic model of Duling et al. (2014, 〈ext-link ext-link-type="uri" xlink:href="https://doi.org/10.1002/2013ja019554"〉https://doi.org/10.1002/2013ja019554〈/ext-link〉) to conditions during the Juno flyby. In addition to the global distribution of plasma variables we provide mapping of Juno's position along magnetic field lines, Juno's distance from closed field lines and detailed information about the magnetic field's topology. We find that Juno did not enter the closed field line region and that the boundary between open and closed field lines on the surface matches the poleward edges of the observed auroral ovals. To estimate the sensitivity of the model results, we carry out a parameter study with different upstream plasma conditions and other model parameters.〈/p〉
    Beschreibung: Plain Language Summary: In June 2021 the Juno spacecraft flew close to Ganymede, the largest moon of Jupiter, and explored its magnetic and plasma environment. Ganymede's own magnetic field forms a magnetosphere, which is embedded in Jupiter's large‐scale magnetosphere, and which is unique in the solar system. The vicinity of Ganymede is separated into regions that differ in whether the magnetic field lines connect to Ganymede's surface at both or one end or not at all. These regions are deformed by the plasma flow and determine the state of the plasma and the location of Ganymede's aurora. We perform simulations of the plasma flow and interaction to reveal the three‐dimensional structure of Ganymede's magnetosphere during the flyby of Juno. The model provides the three‐dimensional state of the plasma and magnetic field, predicted locations of the aurora and the geometrical magnetic context for Juno's trajectory. These results are helpful for the interpretation of the in situ and remote sensing obtained during the flyby. We find that Juno did not cross the region with field lines that connect to Ganymede's surface at both ends. Considering possible values for unknown model parameters, we also estimate the uncertainty of the model results.〈/p〉
    Beschreibung: Key Points: 〈list list-type="bullet"〉 〈list-item〉 〈p xml:lang="en"〉Our magnetohydrodynamic model illustrates the state of Ganymede's magnetosphere during Juno's flyby and locates its trajectory outside closed field lines〈/p〉〈/list-item〉 〈list-item〉 〈p xml:lang="en"〉The location of the open‐closed‐field line‐boundary is predicted and matches the poleward edges of the aurora as observed by Juno〈/p〉〈/list-item〉 〈list-item〉 〈p xml:lang="en"〉We investigate model uncertainties caused by incomplete knowledge of upstream conditions and other parameters〈/p〉〈/list-item〉 〈/list〉 〈/p〉
    Beschreibung: H2020 European Research Council http://dx.doi.org/10.13039/100010663
    Beschreibung: University of Iowa http://dx.doi.org/10.13039/100008893
    Beschreibung: National Aeronautics and Space Administration http://dx.doi.org/10.13039/100000104
    Beschreibung: Southwest Research Institute http://dx.doi.org/10.13039/100011766
    Beschreibung: http://www.netpurgatory.com/zeusmp.html
    Beschreibung: https://doi.org/10.17189/1519711
    Beschreibung: https://doi.org/10.5281/zenodo.7096938
    Beschreibung: https://doi.org/10.5281/zenodo.7105334
    Schlagwort(e): ddc:523 ; Ganymede ; Juno spacecraft ; MHD model ; magnetosphere ; magnetohydrodynamics ; simulation
    Sprache: Englisch
    Materialart: doc-type:article
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 9
    Publikationsdatum: 2023-11-14
    Beschreibung: 〈title xmlns:mml="http://www.w3.org/1998/Math/MathML"〉Abstract〈/title〉〈p xmlns:mml="http://www.w3.org/1998/Math/MathML" xml:lang="en"〉Standard models of force balance along Jovian field lines predict the location of the Io Plasma Torus to be the centrifugal equator of Jupiter’s magnetosphere, that is, the position along the magnetic field lines farthest away from Jupiter’s rotational axis. In many models, the centrifugal equator is assumed to lay on a plane, calculated from a (shifted) dipole magnetic field, rather than on a warped surface which incorporates Jupiter’s higher magnetic field moments. In this work, we use Hubble Space Telescope observations of the Io Main Footprint to constrain density, scale height, and lateral position of the Io Plasma Torus. Therefore, we employ the leading angle of the footprints to calculate expected travel times of Alfvén waves and carry out an inversion of the observations. For the magnetic field, we use the JRM33 magnetic field model. The inversion results show peak densities between 〈italic〉ρ〈/italic〉〈sub〉0〈/sub〉 = 1,830 cm〈sup〉−3〈/sup〉 and 〈italic〉ρ〈/italic〉〈sub〉0〈/sub〉 = 2,032 cm〈sup〉−3〈/sup〉 and scale heights between 〈italic〉H〈/italic〉 = 0.92〈italic〉R〈/italic〉〈sub〉〈italic〉J〈/italic〉〈/sub〉 and 〈italic〉H〈/italic〉 = 0.97〈italic〉R〈/italic〉〈sub〉〈italic〉J〈/italic〉〈/sub〉 consistent with current literature values. Using a warped multipole centrifugal equator instead of a planar dipole increases the quality of the fit by about 25%. We additionally develop two tests to confirm that the multipole centrifugal equator from the JRM33 model fits explains the applied data set better than the dipole centrifugal equator. The quadropole moments alter Io’s relative position to the torus, which changes the plasma density around Io by up to Δ〈italic〉ρ〈/italic〉/〈italic〉ρ〈/italic〉 = 20%.〈/p〉
    Beschreibung: Key Points: 〈list list-type="bullet"〉 〈list-item〉 〈p xml:lang="en"〉Based on the Io Footprint positions, we show quantitatively that the Io Plasma Torus is centered on the centrifugal equator of Jupiter’s multipole magnetic field〈/p〉〈/list-item〉 〈list-item〉 〈p xml:lang="en"〉Position of the Io Footprint can be used to constrain a density model of the Io Plasma Torus〈/p〉〈/list-item〉 〈list-item〉 〈p xml:lang="en"〉The displacement of the Io Plasma Torus due to higher magnetic field moments can change the plasma density at Io by up to 20%〈/p〉〈/list-item〉 〈/list〉 〈/p〉
    Beschreibung: HORIZON EUROPE European Research Council
    Beschreibung: International Space Science Institute (ISSI) in Bern, through ISSI International Team project 515
    Beschreibung: https://doi.org/10.5281/zenodo.8214702
    Schlagwort(e): ddc:523 ; Io Plasma Torus ; inversion ; Io Footprint ; Alfven wings ; magnetic field model
    Sprache: Englisch
    Materialart: doc-type:article
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 10
    Publikationsdatum: 2023-11-14
    Beschreibung: We report results of Hubble Space Telescope observations from Ganymede's orbitally trailing side which were taken around the flyby of the Juno spacecraft on 7 June 2021. We find that Ganymede's northern and southern auroral ovals alternate in brightness such that the oval facing Jupiter's magnetospheric plasma sheet is brighter than the other one. This suggests that the generator that powers Ganymede's aurora is the momentum of the Jovian plasma sheet north and south of Ganymede's magnetosphere. Magnetic coupling of Ganymede to the plasma sheet above and below the moon causes asymmetric magnetic stresses and electromagnetic energy fluxes ultimately powering the auroral acceleration process. No clear statistically significant timevariability of the auroral emission on short time scales of 100s could be resolved. We show that electron energy fluxes of several tens of mW m−2 are required for its OI 1,356 Å emission making Ganymede a very poor auroral emitter.
    Beschreibung: Plain Language Summary: Jupiter's moon Ganymede is the largest moon in the solar system and the only known moon with an intrinsic magnetic field and two auroral ovals around its north and south poles. Earth also possesses two auroral ovals, which are bands of emission around its poles. This emission is also referred to as northern and southern lights. We use the Hubble Space Telescope to observe Ganymede's aurora around the time when NASA's Juno spacecraft had a close flyby at Ganymede. We find that the brightness of the northern and southern ovals alternate in intensity with a period of 10 hr. Additionally, we derive that an energy flux of several tens of milli‐Watt per square meter is necessary to power the auroral emission. This energy flux comes from energetic electrons accelerated in the vicinity of Ganymede.
    Beschreibung: Key Points: Hubble Space Telescope observations of Ganymede's orbitally trailing hemisphere on 7 June 2021 in support of Juno flyby. Brightness ratio of northern and southern auroral ovals oscillates such that the oval facing the Jovian plasma sheet is brighter. Oscillation suggests the aurora is driven by magnetic stresses coupling the moon's magnetic field to the surrounding Jovian plasma sheet.
    Beschreibung: European Research Council, ERC
    Beschreibung: NASA
    Beschreibung: http://archive.stsci.edu/hst/
    Schlagwort(e): ddc:523 ; Ganymede ; auroral ovals ; Hubble Space Telescope ; Juno spacecraft
    Sprache: Englisch
    Materialart: doc-type:article
    Standort Signatur Einschränkungen Verfügbarkeit
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