Lühr, H.; Geisler, H.; Schlegel, K.: Current density models of the eastward electrojet derived from ground-based magnetic field and radar measurements. Journal of Atmospheric and Terrestrial Physics 56, pp. 81 - 91 (1994)
Lühr, H.; Schlegel, K.: Combined measurements of EISCAT and the EISCAT magnetometer cross to study Ω bands. Journal Geophysical Research 99 (A5), pp. 8951 - 8959 (1994)
Schlegel, K.; Haldoupis, C.: Observation of the modified two-stream plasma instability in the midlatitude E region ionosphere. Journal Geophysical Research 99 (A4), pp. 6219 - 6226 (1994)
Haldoupis, C.; Schlegel, K.: A 50-MHz radio Doppler experiment for midlatitude E region coherent backscatter studies: System description and first results. Radio Science 28, pp. 959 - 978 (1993)
Haldoupis, C.; Schlegel, K.; Nielsen, E.: Some observations of radio auroral backscatter at 140 MHz during E-region electron gas heating. Annales Geophysicae 11, pp. 283 - 295 (1993)
Kirchengast, G.; Leitinger, R.; Schlegel, K.; Hocke, K.: Modellsimulationen zur Interpretation von TIDs in hohen Breiten. Kleinheubacher Berichte 36, pp. 399 - 408 (1993)
Ma, S. Y.; Schlegel, K.: Nonlinear wave-wave interactions related to gravity wave reflection in the auroral upper F-region observed with the EISCAT radar. Journal of Atmospheric and Terrestrial Physics 55, pp. 719 - 738 (1993)
Shibata, T.; Schlegel, K.: Vertical structure of AGW associated ionospheric fluctuations in the E- and lower F-region observed with EISCAT - A case study. Journal of Atmospheric and Terrestrial Physics 55, pp. 739 - 749 (1993)
Jakowski, N.; Jungstand, A.; Schlegel, K.; Kohl, H.; Rinnert, K.: The ionospheric response to perturbation electric fields during the onset phase of geomagnetic storms. Canadian Journal of Physics 70, pp. 575 - 581 (1992)
Kirchengast, G.; Leitinger, R.; Schlegel, K.: A high-resolution model for the ionospheric F-region at mid- and high-latitude sites. Annales Geophysicae 10, pp. 577 - 596 (1992)
Kohl, H.; Nielsen, E.; Rinnert, K.; Schlegel, K.: EISCAT results during the ROSE campaign and comparison with STARE measurements. Journal of Atmospheric and Terrestrial Physics 54, pp. 733 - 739 (1992)
Ma, S.-Y.; Schlegel, K.: Ionospheric responses to atmospheric grvity waves in various plasma quantities and inversion of GW's parameters. Acta Geophysica Sinica 35, pp. 405 - 414 (1992)
Natorf, L.; Schlegel, K.; Wernik, A. W.: Gravity wave parameters derived from traveling ionospheric disturbances observations in the auroral zone. Journal of Atmospheric and Terrestrial Physics 27, pp. 829 - 840 (1992)
Pfaff, R. F.; Sahr, J.; Providakes, J. F.; Schwarz, W. E.; Farley, D. T.; Kintner, P. M.; Häggström, I.; Hedberg, A.; Opgenoorth, H.; Holmgren, G.et al.; McNamara, A.; Wallis, D.; Whalen, B.; Yau, A.; Watanabe, S.; Creutzberg, F.; Williams, P.; Nielsen, E.; Schlegel, K.; Robinson, T. R.: The E-region rocket/radar instability study (ERRRIS): scientific objectives and campaign overview. Journal of Atmospheric and Terrestrial Physics 54, pp. 779 - 808 (1992)
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.