Zobrazeno 1 - 5
of 5
pro vyhledávání: '"D. S. van Maren"'
Autor:
D. S. van Maren, C. Maushake, J.-W. Mol, D. van Keulen, J. Jürges, J. Vroom, H. Schuttelaars, T. Gerkema, K. Schulz, T. H. Badewien, M. Gerriets, A. Engels, A. Wurpts, D. Oberrecht, A. J. Manning, T. Bailey, L. Ross, V. Mohrholz, D. M. L. Horemans, M. Becker, D. Post, C. Schmidt, P. J. T. Dankers
Publikováno v:
Earth System Science Data, Vol 15, Pp 53-73 (2023)
An extensive field campaign, the Ems-Dollard Measurements (EDoM), was executed in the Ems Estuary, bordering the Netherlands and Germany, aimed at better understanding the mechanisms that drive the exchange of water and sediments between a relatively
Externí odkaz:
https://doaj.org/article/2ac047afaa584696bcfd4b8bbb7b4fc4
Autor:
D. S. van Maren, A. Colina Alonso, A. Engels, W. Vandenbruwaene, P. L. M. de Vet, J. Vroom, Z. B. Wang
Publikováno v:
Frontiers in Earth Science, Vol 11 (2023)
Many estuaries and tidal basins are strongly influenced by various human interventions (land reclamations, infrastructure development, channel deepening, dredging and disposal of sediments). Such interventions lead to a range of hydrodynamic and morp
Externí odkaz:
https://doaj.org/article/daf8be4993f342bfa97fc842b9014b46
Publikováno v:
Advances in Geosciences, Vol 39, Pp 15-19 (2014)
River floods are usually featured by a downstream flattening discharge peak whereas a downstream increasing discharge peak is observed at a rate exceeding the tributary discharge during highly silt-laden floods (hyperconcentrated floods) in China's Y
Externí odkaz:
https://doaj.org/article/d5c16f033be74884a942afc198bd9579
Publikováno v:
Journal Of Geophysical Research-Oceans, 127(6)
The mechanisms controlling the formation of an estuarine turbidity maximum (ETM) in estuaries have been extensively investigated, but one aspect that has received much less scientific attention is the role of high suspended sediment concentrations in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::aae746f2d59209d45e283c8a53a6d42b
https://doi.org/10.1029/2021jc018029
https://doi.org/10.1029/2021jc018029
Autor:
A. Colina Alonso, D. S. van Maren, P. M. J. Herman, R. J. A. van Weerdenburg, Y. Huismans, S. J. Holthuijsen, L. L. Govers, A. I. Bijleveld, Z. B. Wang
Publikováno v:
Geophysical research letters, 49(22):e2022GL101141. AMER GEOPHYSICAL UNION
Geophysical Research Letters, 49(22)
Geophysical Research Letters, 49(22)
The sediment composition of the seabed governs its mobility, hence determining sediment transport and morphological evolution of estuaries and tidal basins. Bed sediments often consist of mixtures of sand and mud, with spatial gradients in the sand/m
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::fc356255a069f76b63ac34afe740c15a
https://www.vliz.be/imisdocs/publications/76/385376.pdf
https://www.vliz.be/imisdocs/publications/76/385376.pdf
