Rengel, M.; Reach, W.; Hartogh, P.; Sagawa, H.: Tracing the Composition of Hydrogen Cyanide in the Stratosphere of Titan from Space, Airborne, and Ground-Based Observations. ESA SCI Science Workshop #9, Aklersloot, Netherlands (2016)
Rengel, M.; Sagawa, H.; Hartogh, P.: Venusian Mesospheric thermal structure and winds from May 2009 SMT CO spectral- line observations. 40th COSPAR Scientific Assembly, Moscow, Russia (2014)
Rezac, L.; de Val-Borro, M.; Hartogh, P.; Cavalié, T.; Jarchow, C.; Rengel, M.; Dobrijevic, M.: New Determination of the HCN Profile in the Stratosphere of Neptune from Millimeter-wave Spectroscopy. Asia Oceania Geosciences Society (AOGS) 11th Annual Meeting, Sapporo, Japan (2014)
Hartogh, P.: Chirptransformations-Spektrometer für die passive Millimeterwellenradiometrie: Messungen der 142 GHz Emissionslinie des atmosphärischen Ozons. Dissertation, Georg-August-Universität Göttingen (1989)
Hartogh, P.: Raumflugtauglicher FM-Pulskompressionsempfänger mit Oberflächenwellenfiltern für die Millimeter- und Submillimeterwellenspektroskopie. Diploma, Georg-August-Universität Göttingen (1985)
Biver, N.; Bockelée-Morvan, D.; Moreno, R.; Crovisier, J.; Hartogh, P.; de Val-Borro, M.; Kidger, M.; Kueppers, M.; Szutowicz, S.; Lis, D. C.et al.; Blake, G. A.; Gonzalez, J. J.; Seargent, D. A. J.; Mattiazzo, M.: Comet C/2011 L4 (Panstarrs). Central Bureau Electronic Telegrams 3230, 1 (2012)
Meister, C.-V.; Hartogh, P.; Villanueva, G.; Berger, U.: Hydrodynamic model of the Martian atmosphere between near-surface layers and an altitude of about 130 km. Max-Planck-Institut für Aeronomie, Katlenburg-Lindau, Germany (2002)
Gulkis, S.; Forget, F.; Janssen, M.; Riley, L.; Hartogh, P.; Clancy, T.; Allen, M.; Frerking, M.: Microwave Investigation of the Martian Atmosphere and Surface. JPL, California Institute of Technology, Pasadena, CA, USA (2000)
Gurevich, A. V.; Borison, N. D.; Montecinos-Geisse, S. E.; Hartogh, P.: Artificial ozone layer. Max-Planck-Institut für Aeronomie, Katlenburg-Lindau, Germany (1995)
Lopez, J. E.; Montecinos, S. E.; Hartogh, P.: A photochemical model of the atmosphere. Max-Planck-Institut für Aeronomie, Katlenburg-Lindau, Germany (1995)
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).