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)
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)
How does our star heat its outer atmosphere, the solar corona, to unimaginable temperatures of up to 10 million degrees Celsius? With unprecedented observational data from ESA's Solar Orbiter spacecraft and powerful computer simulations, ERC starting grant awardee Pradeep Chitta intends to bring new momentum to the search for the coronal heating mechanism.
The research group “Solar Lower Atmosphere and Magnetism” (SLAM) studies the conditions and dynamic processes in the atmospheric layer between the solar surface (photosphere) and the overlying chromosphere, an approximately 2000 km thick gas layer.
The main research fields of the department "Sun and Heliosphere" are covered by the research groups "Solar and Stellar Coronae", "Solar Lower Atmosphere and Magnetism", "Solar and Stellar Magnetohydrodynamics" and "Solar Variability and Climate".