11 citations as recorded by crossref.

1. Efficient geomorphological mapping based on geographic information systems and remote sensing data: an example from Jena, Germany I. Zangana et al. https://doi.org/10.1080/17445647.2023.2172468
2. Combining Satellite and UAV Imagery to Delineate Forest Cover and Basal Area after Mixed-Severity Fires F. Rossi et al. https://doi.org/10.3390/su10072227
3. A general methodological framework for hazard assessment in remote mountain areas combining geomorphological mapping with UAV survey E. Garova et al. https://doi.org/10.1007/s11629-024-9096-8
4. The Muschelkalk aquifer of the Molasse basin in SW-Germany: implications on the origin and development of highly saline lithium-rich brines in calcareous hydrothermal reservoirs I. Stober et al. https://doi.org/10.1186/s40517-023-00270-6
5. Last Glacial Maximum glacier fluctuations on the northern Alpine foreland: Geomorphological and chronological reconstructions from the Rhine and Reuss glacier systems S. Kamleitner et al. https://doi.org/10.1016/j.geomorph.2022.108548
6. The extent of the Rhine Glacier in eastern Upper Swabia (southern Germany) at the height of the Last Glacial Maximum: new morphological constraints from high-resolution digital terrain models M. Jong et al. https://doi.org/10.1127/zdgg/2025/0456
7. High-resolution mapping of ice-marginal landforms in the Barnim region, northeast Germany J. Hardt et al. https://doi.org/10.1016/j.geomorph.2015.07.045
8. Numerical reconstructions of the flow and basal conditions of the Rhine glacier, European Central Alps, at the Last Glacial Maximum D. Cohen et al. https://doi.org/10.5194/tc-12-2515-2018
9. Reconstructing basal ice flow patterns of the Last Glacial Maximum Rhine glacier (northern Alpine foreland) based on streamlined subglacial landforms S. Kamleitner et al. https://doi.org/10.1002/esp.5733
10. High-resolution DTM-based stratigraphic correlation of fluvial terraces along River Würm T. Bueche & K. Loesch https://doi.org/10.1007/BF03544503
11. Subglacial hydrology from high-resolution ice-flow simulations of the Rhine Glacier during the Last Glacial Maximum: a proxy for glacial erosion D. Cohen et al. https://doi.org/10.5194/egqsj-72-189-2023