Rose, G.: Die H- und E-Wellenfeldexperimente des Heating-Raketenprogramms. Max-Planck-Institut für Sonnensystemforschung, Katlenburg-Lindau, Germany (1980)
Rose, G.: A survey of experimental E-region data obtained between 1967 and 1975. Max-Planck-Institut für Sonnensystemforschung, Katlenburg-Lindau, Germany (1976)
Schlegel, K.; Rose, G.; Widdel, H. U.: Interplanetary magnetic field polarity changes and D-region radio wave absorption. Max-Planck-Institut für Sonnensystemforschung, Katlenburg-Lindau, Germany (1976)
Widdel, H. U.; Rose, G.; Borchers, R.: Experimental results on the variation of ion condctivity and mobility in the mesosphere. Max-Planck-Institut für Sonnensystemforschung, Katlenburg-Lindau, Germany (1976)
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.