Zobrazeno 1 - 10
of 12
pro vyhledávání: '"Michele, Amaddii"'
Publikováno v:
Geosciences, Vol 12, Iss 10, p 385 (2022)
On 27–28 July 2019, in a catchment of the Mt. Amiata area (Italy), an extreme rainfall induced a debris flow, which caused a channeled erosive process just upstream of the Abbadia San Salvatore village, the obstruction of a culvert at the entrance
Externí odkaz:
https://doaj.org/article/4fe235c6d1ae4fedb2860cc3190534b8
Publikováno v:
Geosciences; Volume 12; Issue 10; Pages: 385
On 27–28 July 2019, in a catchment of the Mt. Amiata area (Italy), an extreme rainfall induced a debris flow, which caused a channeled erosive process just upstream of the Abbadia San Salvatore village, the obstruction of a culvert at the entrance
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::bf0b65d592aaefdec63b6f5e000222b8
Autor:
Enrico D'Addario, Taraka Venkatadripathi Pattela, Lorenzo Marzini, Gianni Lombardi, Michele Amaddii, Leonardo Disperati
The Monte Amiata is a volcano located in central Italy composed by trachytic to olivine latitic lava flows and domes emplaced between 305 and 231 ka (Pleistocene). These volcanic products, affected by saprolite alteration processes of spatially varia
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c019da1b280961a7eb26b16a01844a02
https://doi.org/10.5194/icg2022-611
https://doi.org/10.5194/icg2022-611
Mountain environments are naturally exposed to debris flows, a mass movement which represents one of the major geomorphological hazard sources for urbanized alluvial fan. In the last decades, climate change has contributed to extreme precipitations i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cba91b7c4b8e31f439cc97993f98dc71
https://doi.org/10.5194/icg2022-305
https://doi.org/10.5194/icg2022-305
Autor:
Taraka Venkatadripathi Pattela, Leonardo Disperati, Lorenzo Marzini, Michele Amaddii, Gianni Lombardi, Daniele Rappuoli
Landslides are considered one of the major hazards causing economic and human losses worldwide. Slope instability processes are affecting buildings and infrastructures in the towns of the eastern slope of the Mt. Amiata volcanic complex (Tuscany, Ita
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c105f007fda2401d72adea84353738b4
https://doi.org/10.5194/egusphere-egu22-12120
https://doi.org/10.5194/egusphere-egu22-12120
Autor:
Lorenzo Marzini, Enrico D'Addario, Michele Pio Papasidero, Michele Amaddii, Leonardo Disperati, Francesco Chianucci
Shallow landslides susceptibility assessment by physically based methods relies on the parametrization of both hydraulic and geotechnical properties of soils, which in turn depend on the conditions of root structures and vegetation cover. Vegetation
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::11060c30292b4cfb26222c862f704eeb
https://doi.org/10.5194/egusphere-egu22-2641
https://doi.org/10.5194/egusphere-egu22-2641
As the climate changes are expected to generally increase the hydrogeological hazard, a better knowledge of the catchment-scale response to intense rainfalls is a relevant issue. Hence, in this work, different approaches of infiltration processes est
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::eb0c6bbebf03c257290ecead9d8a1ca1
http://hdl.handle.net/11365/1141017
http://hdl.handle.net/11365/1141017
During the June 19th of 1996 a storm involved the Tyrrhenian sector of northern Tuscany (Italy), especially hitting the Versilia and Garfagnana areas. Major consequences and damages, due to the extremely intense precipitation (about 500 mm/13 h and 1
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::511364c90b3ca7d353d1d893ff1f979b
https://doi.org/10.5194/egusphere-egu2020-15609
https://doi.org/10.5194/egusphere-egu2020-15609
Autor:
Enrico D'Addario, Nazariy Broda, Michele Pio Papasidero, Lorenzo Marzini, Marco Pignatiello, Michele Amaddii, Leonardo Disperati
Apart high elevation and arid regions, bedrock is generally covered by unconsolidated materials that result from recent or actual bedrock weathering and fracturing, consequent transport along the hillslope mainly by un-channelized flux or gravity-dom
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0ae2a5b81fcfe1cce2c54fa3237ad131
https://doi.org/10.5194/egusphere-egu2020-18101
https://doi.org/10.5194/egusphere-egu2020-18101
Autor:
Leonardo Disperati, Enrico D’Addario, Lorenzo Bottai, Riccardo Giusti, Guido Lavorini, Gianni Lombardi, Elisa Mammoliti, Francesco Manetti, Lorenzo Marzini, Michele Pio Papasidero, Michele Amaddii
Publikováno v:
Abstracts of the ICA. 3:1-1
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e19a7498ec7d412b232182dbd2ac64e1
https://doi.org/10.5194/ica-abs-3-68-2021
https://doi.org/10.5194/ica-abs-3-68-2021