Wu, Y.; Dietrich, W.; Tao, X.: Parameter Regimes of Hemispherical Dynamo Waves in a Spherical Shell From 3D MHD Simulations. Journal of Geophysical Research (Planets) 129, p. e2023JE007976 (2024)
Wulff, P.; Dietrich, W.; Christensen, U. R.; Wicht, J.: Zonal winds in the gas planets driven by convection above a stably stratified layer. Monthly Notices of the Royal Astronomical Society 517 (4), pp. 5584 - 5593 (2022)
Dietrich, W.; Kumar, S.; Poser, A. J.; French, M.; Nettelmann, N.; Redmer, R.; Wicht, J.: Magnetic induction processes in hot Jupiters, application to KELT-9b. Monthly Notices of the Royal Astronomical Society 517, pp. 3113 - 3125 (2022)
Dietrich, W.; Wulff, P.; Wicht, J.; Christensen, U. R.: Linking zonal winds and gravity – II. Explaining the equatorially antisymmetric gravity moments of Jupiter. Monthly Notices of the Royal Astronomical Society 505 (3), pp. 3177 - 3191 (2021)
Kumar, S.; Poser, A. J.; Schoettler, M.; Kleinschmidt, U.; Dietrich, W.; Wicht, J.; French, M.; Redmer, R.: Ionization and transport in partially ionized multicomponent plasmas: Application to atmospheres of hot Jupiters. Physical Review E 103 (6), 063203 (2021)
Christensen, U. R.; Wicht, J.; Dietrich, W.: Mechanisms for Limiting the Depth of Zonal Winds in the Gas Giant Planets. The Astrophysical Journal 890 (1), 61 (2020)
Wicht, J.; Dietrich, W.; Wulff, P.; Christensen, U. R.: Linking zonal winds and gravity: the relative importance of dynamic self-gravity. Monthly Notices of the Royal Astronomical Society 492 (3), pp. 3364 - 3374 (2020)
Hori, K.; Wicht, J.; Dietrich, W.: Ancient dynamos of terrestrial planets more sensitive to core-mantle boundary heat flows. Planetary and Space Science 98, pp. 30 - 40 (2014)
Dietrich, W.; Wicht, J.: A hemispherical dynamo model: Implications for the Martian crustal magnetization. Phys. Earth Planet. Inter. 217, pp. 10 - 21 (2013)
The Planetary Plasma Environments group (PPE) has a strong heritage in the exploration of planetary magnetospheres and space plasma interactions throughout the solar system. It has contributed instruments to several past missions that flew-by or orbited Jupiter (Galileo, Cassini, Ulysses). The PPE participates in the JUICE mission by contributing hardware and scientific expertise to the Particle Environment Package (PEP).
The dwarf planet is a bizarre, cryovolcanic world. However, the organic deposits discovered on its surface so far are unlikely to originate from its interior.
The Uranian magnetic field is more expansive than previously thought, according to newly analyzed data from Voyager 2, making it easier to search for moons with oceans.
The Planetary Plasma Environments group (PPE) has a strong heritage in the exploration of planetary magnetospheres and space plasma interactions throughout the solar system. It has contributed instruments to several past missions that flew-by or orbited Jupiter (Galileo, Cassini, Ulysses). The PPE participates in the JUICE mission by contributing hardware and scientific expertise to the Particle Environment Package (PEP).
The dwarf planet is a bizarre, cryovolcanic world. However, the organic deposits discovered on its surface so far are unlikely to originate from its interior.
The Uranian magnetic field is more expansive than previously thought, according to newly analyzed data from Voyager 2, making it easier to search for moons with oceans.
The Planetary Plasma Environments group (PPE) has a strong heritage in the exploration of planetary magnetospheres and space plasma interactions throughout the solar system. It has contributed instruments to several past missions that flew-by or orbited Jupiter (Galileo, Cassini, Ulysses). The PPE participates in the JUICE mission by contributing hardware and scientific expertise to the Particle Environment Package (PEP).