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)
Hartogh, P.; Hartmann, G. K.; Heimesaat, G.: The use of Chirp-transform-spectrometers for real time Fouriertransform of stochastic signals. Max-Planck-Institut für Aeronomie, Katlenburg-Lindau, Germany (1989)
Puliafito, E.; Puliafito, C.; Hartmann, G. K.; Degenhardt, W.; Hartogh, P.: Bestimmung des Wasserdampf- und Ozongehaltes der Stratosphäre und Mesosphäre aus radiometrischen Messungen. Max-Planck-Institut für Aeronomie, Katlenburg-Lindau, Germany (1989)
Hartogh, P.: Low cost system used for process control and data acquisition for a millimeter-wave radiometer-spectrometer. Max-Planck-Institut für Aeronomie, Katlenburg-Lindau, Germany (1988)
Hartmann, G. K.; Hartogh, P.; Loidl, A.: Heterodyne-Spectroscopy in the Millimeter and Submillimeter Domain. Max-Planck-Institut für Aeronomie, Katlenburg-Lindau, Germany (1987)
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.