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 dwarf planet is a bizarre, cryovolcanic world. However, the organic deposits discovered on its surface so far are unlikely to originate from its interior.
Data from NASA's Dawn mission, analyzed for the first time, suggest that brine rose from the depths and organic compounds were deposited in Urvara crater.