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  • 1
    Keywords: Forschungsbericht
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (17 Seiten, 510,92 KB) , Diagramme
    Language: German
    Note: 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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  • 2
    Publication Date: 2024-01-15
    Description: 〈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〉
    Description: 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〉
    Description: 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〉
    Description: H2020 European Research Council http://dx.doi.org/10.13039/100010663
    Description: University of Iowa http://dx.doi.org/10.13039/100008893
    Description: National Aeronautics and Space Administration http://dx.doi.org/10.13039/100000104
    Description: Southwest Research Institute http://dx.doi.org/10.13039/100011766
    Description: http://www.netpurgatory.com/zeusmp.html
    Description: https://doi.org/10.17189/1519711
    Description: https://doi.org/10.5281/zenodo.7096938
    Description: https://doi.org/10.5281/zenodo.7105334
    Keywords: ddc:523 ; Ganymede ; Juno spacecraft ; MHD model ; magnetosphere ; magnetohydrodynamics ; simulation
    Language: English
    Type: doc-type:article
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  • 3
    Publication Date: 2023-11-14
    Description: 〈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〉
    Description: 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〉
    Description: HORIZON EUROPE European Research Council
    Description: International Space Science Institute (ISSI) in Bern, through ISSI International Team project 515
    Description: https://doi.org/10.5281/zenodo.8214702
    Keywords: ddc:523 ; Io Plasma Torus ; inversion ; Io Footprint ; Alfven wings ; magnetic field model
    Language: English
    Type: doc-type:article
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  • 4
    Publication Date: 2023-11-14
    Description: 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.
    Description: 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.
    Description: 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.
    Description: European Research Council, ERC
    Description: NASA
    Description: http://archive.stsci.edu/hst/
    Keywords: ddc:523 ; Ganymede ; auroral ovals ; Hubble Space Telescope ; Juno spacecraft
    Language: English
    Type: doc-type:article
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