Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Cati Cremer"'
Gully erosion is a damaging process not yet sufficiently understood and parameterized. Gully head topographic thresholds are empirical models used to predict the gully head formation. Such model have been used to investigate gully processes mostly in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4d2dd52ba74142b1f0f9438a53633dcb
https://doi.org/10.5194/egusphere-egu23-11902
https://doi.org/10.5194/egusphere-egu23-11902
ispartof: EARTH SURFACE PROCESSES AND LANDFORMS vol:47 issue:15 pages:3558-3587 status: published
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d01510c185dae7630646355a98f1860b
https://lirias.kuleuven.be/handle/20.500.12942/706744
https://lirias.kuleuven.be/handle/20.500.12942/706744
Publikováno v:
Earth Surface Processes and Landforms. 43:2547-2561
Publikováno v:
8TH INTERNATIONAL SYMPOSIUM ON GULLY EROSION ISGE 2019, TOWNSVILLE (AUSTRALIA), 21/07/2019
info:cnr-pdr/source/autori:Dino Torri (1), Jean Poesen (2), Mauro Rossi (1), Sofie de De Geeter (2), Cati Cremer (2)/congresso_nome:8TH INTERNATIONAL SYMPOSIUM ON GULLY EROSION ISGE 2019/congresso_luogo:TOWNSVILLE (AUSTRALIA)/congresso_data:21%2F07%2F2019/anno:2019/pagina_da:/pagina_a:/intervallo_pagine
info:cnr-pdr/source/autori:Dino Torri (1), Jean Poesen (2), Mauro Rossi (1), Sofie de De Geeter (2), Cati Cremer (2)/congresso_nome:8TH INTERNATIONAL SYMPOSIUM ON GULLY EROSION ISGE 2019/congresso_luogo:TOWNSVILLE (AUSTRALIA)/congresso_data:21%2F07%2F2019/anno:2019/pagina_da:/pagina_a:/intervallo_pagine
The prediction of the location of gully heads in various environments is an important step towards predicting slope and catchment dynamics and to properly estimate soil erosion rates. So far, data collection and modelling of topographic thresholds fo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::fe3b4ea9d154e231b9f49710c1e9a42a
http://www.cnr.it/prodotto/i/429739
http://www.cnr.it/prodotto/i/429739
Autor:
Rorke B. Bryan, Jean Poesen, Dino Torri, Lorenzo Borselli, Marta S. Yañez, M. Pilar Salvador Sanchis, Cati Cremer
Publikováno v:
Earth surface processes and landforms
34 (2009): 2023–2030. doi:10.1002/esp.1887
info:cnr-pdr/source/autori:Salvador Sanchis M.P.; Torri D.; Borselli L.; Bryan R.; Poesen J.; Yañez M. S.; Cremer C./titolo:Estimating parameters of the channel width-flow discharge relation using rill and gully channel junction data/doi:10.1002%2Fesp.1887/rivista:Earth surface processes and landforms (Print)/anno:2009/pagina_da:2023/pagina_a:2030/intervallo_pagine:2023–2030/volume:34
34 (2009): 2023–2030. doi:10.1002/esp.1887
info:cnr-pdr/source/autori:Salvador Sanchis M.P.; Torri D.; Borselli L.; Bryan R.; Poesen J.; Yañez M. S.; Cremer C./titolo:Estimating parameters of the channel width-flow discharge relation using rill and gully channel junction data/doi:10.1002%2Fesp.1887/rivista:Earth surface processes and landforms (Print)/anno:2009/pagina_da:2023/pagina_a:2030/intervallo_pagine:2023–2030/volume:34
Eroding channels can usually be characterized by a power relationship between channel width (W) and channel discharge (Q). This paper examines the WQ relation using a recently developed channel junction approach to extend the validity of the WQ relat