Zobrazeno 1 - 10
of 13
pro vyhledávání: '"Giulio Calvani"'
Autor:
Paolo Perona, Giulio Calvani
The engineering design of hydraulic infrastructures in either urban or rural environments requires flow hydrograph scenarios to be tested in numerical models. Whilst peak flow discharge is calculated according to a return period analysis of historica
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f091881b392a2fd46d2f14e0d851b15d
https://doi.org/10.5194/egusphere-egu23-14306
https://doi.org/10.5194/egusphere-egu23-14306
Publikováno v:
Water Resources Research. 58
Aquatic vegetation in fluvial systems is often characterized by spatial patterning of the plant patches. To investigate the conditions for the formation of vegetation patches, we explore the stability of a uniform flow over a non-erodible bed with a
Publikováno v:
River Research and Applications. 37:615-626
River bars often form at river confluences due to variation in flow discharges or in sediment transport capacity; once these bars are grown, they constitute favourable habitats for vegetation development. In this work, we analysed the effect of veget
Publikováno v:
Journal of Geophysical Research: Earth Surface. 124:1018-1034
Sediment deposition and bank accretion are promoted by the establishment and growth of pioneer plant species, a direct consequence of plant survival during flood events. Similarly, the uprooting of riparian vegetation on river bars during floods can
Publikováno v:
River Flow 2020 ISBN: 9781003110958
River Flow 2020
River Flow 2020
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ce3d7f0ce10cdafd0e18890a8912692a
https://doi.org/10.1201/b22619-209
https://doi.org/10.1201/b22619-209
Publikováno v:
Calvani, G, Perona, P, Schick, C & Solari, L 2019, ' Biomorphological scaling laws from convectively accelerated streams ', Earth Surface Processes and Landforms . https://doi.org/doi.org/10.1002/esp.4735
Worldwide convectively accelerated streams flowing into downstream-narrowing7 river sections show that riverbed vegetation growing on alluvial sediment bars gradually8 disappears forming a front beyond which vegetation is absent. We revise a recent
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2630590b730eb5d3c5bda2134ffc75dd
https://www.pure.ed.ac.uk/ws/files/106645982/Paper_ESPL.pdf
https://www.pure.ed.ac.uk/ws/files/106645982/Paper_ESPL.pdf
Publikováno v:
38th IAHR World Congress - "Water: Connecting the World".
Publikováno v:
Calvani, G, Perona, P, Zen, S, Bau', V & Solari, L 2019, ' Return period of vegetation uprooting by flow ', Journal of Hydrology, vol. 578, 124103 . https://doi.org/10.1016/j.jhydrol.2019.124103
Fluvial environments are dynamic systems whose evolution and management are strongly affected by the resilience of riparian vegetation to uprooting by flow. Similarly to other natural phenomena, the interactions between flow, sediment and vegetation
Publikováno v:
E3S Web of Conferences, Vol 40, p 02034 (2018)
The planform morphology of a river reach is the result of the combined actions of sediment motion (erosion, transport and deposition), hydrological regime, development and growth of vegetation. However, the interactions among these processes are stil