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Following drastic changes in geoenvironmental components by coseismic landslides in mountainous watersheds, more gradual changes can be observed in the elements, including bare-land surface conditions, sediment connectivity, and vegetation recovery o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3bc16d841514b7c5b169efb0d3e70312
https://doi.org/10.5194/egusphere-egu23-5689
https://doi.org/10.5194/egusphere-egu23-5689