Zobrazeno 1 - 10
of 14
pro vyhledávání: '"Steven Weisscher"'
Publikováno v:
Earth Surface Dynamics, 10(2), 367. Copernicus Publications
Rivers and estuaries are flanked by floodplains built by mud and vegetation. Floodplains affect channel dynamics and the overall system's pattern through apparent cohesion in the channel banks and through filling of accommodation space and hydraulic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ba78ffdbca91867874759e892387991c
https://dspace.library.uu.nl/handle/1874/420524
https://dspace.library.uu.nl/handle/1874/420524
Dikes are the conventional means of flood defence along rivers and estuaries. However, dikes gradually lead to the superelevation of waterbodies, and the common method of enforcing dikes is unsustainable as this is expensive, contends with limited sp
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6e6d1936f7ad0a6e2743184260306923
https://doi.org/10.5194/egusphere-egu22-11058
https://doi.org/10.5194/egusphere-egu22-11058
Estuaries are often dredged for navigational access to ports and harbours. Dredging alters the natural dynamics and morphology of estuaries, tending to create deep channels and high intertidal bars and shoals. Estuaries will face many challenges in t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7b8c19e8252e61a7a85f8b1d6a5fc178
https://doi.org/10.5194/egusphere-egu22-702
https://doi.org/10.5194/egusphere-egu22-702
Some estuaries gained their planform shape and size by sedimentation of mud flats and establishment of ‘coastal floodplains’ with saltmarsh or mangrove, while others are laterally confined by valley walls. For rivers, the channel dimensions and b
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b76008d156a884bad911fe576cdd3f07
https://doi.org/10.5194/egusphere-egu22-840
https://doi.org/10.5194/egusphere-egu22-840
Normal faulting acts as a forcing on the morphodynamics of alluvial rivers by changing the topographic gradient of the river valley and channel around the fault zone. Normal faulting affects river morphodynamics either instantaneously by surface rupt
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f2bd492c0690ca0a97e5393b864181b4
https://doi.org/10.5194/egusphere-egu21-1108
https://doi.org/10.5194/egusphere-egu21-1108
Autor:
Yasuyuki Shimizu, Steven Weisscher, Maarten G. Kleinhans, Marcio Boechat-Albernaz, Wout M. van Dijk, Jasper R. F. W. Leuven
Physical scale experiments enhance our understanding of fluvial, tidal and coastal processes. However, it has proven challenging to acquire accurate and continuous data on water depth and flow velocity due to limitations of the measuring equipment an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c6a152c0e552f1ae10d42b96f6a5333a
https://www.earth-surf-dynam-discuss.net/esurf-2020-14/
https://www.earth-surf-dynam-discuss.net/esurf-2020-14/
Publikováno v:
Journal of Geophysical Research. Earth Surface; Oct2022, Vol. 127 Issue 10, p1-20, 20p
Publikováno v:
Geophysical Research Abstracts. 2016, Vol. 18, p1-16028. 16028p.
Autor:
Leuven, J. R. F. W., Kleinhans, M. G.
Publikováno v:
Journal of Geophysical Research. Earth Surface; Jul2019, Vol. 124 Issue 7, p1762-1781, 20p