Zobrazeno 1 - 7
of 7
pro vyhledávání: '"B. G. Ruessink"'
Publikováno v:
Earth Surface Dynamics, Vol 2, Iss 1, Pp 309-321 (2014)
Subtidal sandbars often exhibit alongshore variable patterns, such as crescentic plan shapes and rip channels. While the initial formation of these patterns is reasonably well understood, the morphodynamic mechanisms underlying their subsequent finit
Externí odkaz:
https://doaj.org/article/4073dc9d4c2144ada8b4e0dccf4e8c7e
Publikováno v:
Nonlinear Processes in Geophysics, Vol 17, Iss 5, Pp 395-404 (2010)
An artificial neural network (ANN) was developed to predict the depth-integrated alongshore suspended sediment transport rate using 4 input variables (water depth, wave height and period, and alongshore velocity). The ANN was trained and validated us
Externí odkaz:
https://doaj.org/article/5cde932195e0403083fc6bb37c8f538f
Autor:
L. Pape, B. G. Ruessink
Publikováno v:
Nonlinear Processes in Geophysics, Vol 15, Iss 1, Pp 145-158 (2008)
Alongshore sandbars are often present in the nearshore zones of storm-dominated micro- to mesotidal coasts. Sandbar migration is the result of a large number of small-scale physical processes that are generated by the incoming waves and the interacti
Externí odkaz:
https://doaj.org/article/dc9489eef95d423c9bf7a48ddde47ef1
Publikováno v:
Nonlinear Processes in Geophysics, Vol 12, Iss 5, Pp 661-670 (2005)
Complex principal component analysis (CPCA) is a useful linear method for dimensionality reduction of data sets characterized by propagating patterns, where the CPCA modes are linear functions of the complex principal component (CPC), consisting of a
Externí odkaz:
https://doaj.org/article/8e83742edb234830adfac964df7bbf81
Nearshore sandbars are ubiquitous morphological features along many sandy, wave-dominated, coasts. They are approximately shore-parallel ridges of sand, located in water depths of less than 10 m. Depending on the wave conditions, sandbars regularly d
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::02b7eb3a3116749e99d69487a717febe
https://doi.org/10.5194/esurfd-1-1209-2013
https://doi.org/10.5194/esurfd-1-1209-2013
Autor:
B. G. Ruessink, H. Michallet, T. Abreu, F. Sancho, D. A. Van der A, J. J. Van der Werf, P. A. Silva
Publikováno v:
Journal of geophysical research-Oceans, 116, C03004/1. American Geophysical Union
Repositório Científico de Acesso Aberto de Portugal
Repositório Científico de Acesso Aberto de Portugal (RCAAP)
instacron:RCAAP
Journal of geophysical research: Oceans, 116(C3):C03004. Wiley-Blackwell
Journal of Geophysical Research. Oceans
Journal of Geophysical Research. Oceans, Wiley-Blackwell, 2011, 116, pp.C03004. ⟨10.1029/2010JC006443⟩
Repositório Científico de Acesso Aberto de Portugal
Repositório Científico de Acesso Aberto de Portugal (RCAAP)
instacron:RCAAP
Journal of geophysical research: Oceans, 116(C3):C03004. Wiley-Blackwell
Journal of Geophysical Research. Oceans
Journal of Geophysical Research. Oceans, Wiley-Blackwell, 2011, 116, pp.C03004. ⟨10.1029/2010JC006443⟩
U‐tube measurements of instantaneous velocities, concentrations, and fluxes for a well‐sorted, medium‐sized sand in oscillatory sheet flow are analyzed. The experiments involved two velocity‐asymmetric flows, the same two flows with an opposi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::fc51f925f5788dd781dce9d0c65808f0
https://dspace.library.uu.nl/handle/1874/209235
https://dspace.library.uu.nl/handle/1874/209235
Autor:
B. G. Ruessink, M. C. J. L. Jeuken
Publikováno v:
Earth Surface Processes & Landforms; Sep2002, Vol. 27 Issue 10, p1043-1056, 14p