12 citations as recorded by crossref.

1. Degradation and local growth of “Xing'an-Baikal” permafrost responding to climate warming and the consequences Z. Zhang et al. 10.1016/j.earscirev.2024.104865
2. A conceptual hydrological model of semiarid Andean headwater systems in Chile G. Navarro et al. 10.1177/03091333221147649
3. Current understanding, knowledge gaps, and challenges of mountain permafrost research in the Chilean and Argentinean Andes H. Fernández-Navarro et al. 10.1016/j.jsames.2024.105165
4. Spectral induced polarization imaging to monitor seasonal and annual dynamics of frozen ground at a mountain permafrost site in the Italian Alps T. Maierhofer et al. 10.5194/tc-18-3383-2024
5. Internal structure and water routing of an ice-debris landform assemblage using multiple geophysical methods in the semiarid Andes G. Navarro et al. 10.3389/feart.2023.1102620
6. Assessment of rock glaciers and their water storage in Guokalariju, Tibetan Plateau M. Li et al. 10.5194/tc-18-1-2024
7. Rock glaciers of the semi-arid northwestern Himalayas: distribution, characteristics, and hydrological significance P. Pandey et al. 10.1016/j.catena.2024.107845
8. Using a non-invasive multiple-method approach to characterize rock glaciers in the periglacial critical zone: An example from the San Juan Mountains, Colorado R. Aguilar & J. Giardino 10.1016/j.geomorph.2023.108585
9. Electrical Resistivity Tomography Investigation of Permafrost Conditions in a Thermokarst Site in Fairbanks, Alaska A. Basiru et al. 10.3934/geosci.2024001
10. Abrupt thaw and its effects on permafrost carbon emissions in the Tibetan Plateau: A remote sensing and modeling perspective Y. Yi et al. 10.1016/j.earscirev.2024.105020
11. Expanding cryospheric landform inventories – quantitative approaches for underestimated periglacial block- and talus slopes in the Dry Andes of Argentina T. Köhler et al. 10.3389/feart.2025.1534410
12. Towards accurate quantification of ice content in permafrost of the Central Andes – Part 1: Geophysics-based estimates from three different regions C. Hilbich et al. 10.5194/tc-16-1845-2022