Medvedev, A. S.; Yiğit, E.; Kuroda, T.; Hartogh, P.: Dynamical coupling between the lower Martian atmosphere and thermosphere. 40th COSPAR Scientific Assembly, Moscow, Russia (2014)
Medvedev, A.; Yiğit, E.; Kuroda, T.; Hartogh, P.: Influence of global dust storms on the mesosphere and lower thermosphere of Mars. European Planetary Science Congress 2014, Cascais, Portugal (2014)
Sethunadh, J. A.; Medvedev, A. S.; Hartogh, P.: General circulation modeling of the Jovian stratosphere. European Planetary Science Congress 2014, Cascais, Portugal (2014)
Shaposhnikov, D.; Rodin, A. V.; Medvedev, A. S.; Hartogh, P.: Hydrological cycle in the general circulation model of the Martian atmosphere. Sixth international workshop on the Mars atmosphere: Modelling and observations , Granada, Spain (2017)
Various application review phases in 2025. PhD projects in cosmochemistry, planetary science, solar and stellar physics, helioseismology, asteroseismology, ...
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).