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The relationship between linearised 3D and 2DH models for tidally dominated shallow waters. <i>Ocean Modelling 188</i>: 102330. <a href=\"https://dx.doi.org/10.1016/j.ocemod.2024.102330\" target=\"_blank\">https://dx.doi.org/10.1016/j.ocemod.2024.102330</a>","AutID":237040,"MonDate":null,"AnaDate":2024,"PeerRev":1,"outputType":"1_A1","OpenAcc":0},{"BRefID":361414,"RR":"<b>Deng, X.; De Mulder, T.; Schuttelaars, H.</b> (2023). Initial formation of channel-shoal patterns in double-inlet systems. <i>Ocean Dynamics 73(1)</i>: 1-21. <a href=\"https://dx.doi.org/10.1007/s10236-022-01528-6\" target=\"_blank\">https://dx.doi.org/10.1007/s10236-022-01528-6</a>","AutID":403122,"MonDate":null,"AnaDate":2023,"PeerRev":1,"outputType":"1_A1","OpenAcc":0},{"BRefID":337288,"RR":"<b>Boelens, T.; Qi, T.; Schuttelaars, H.; De Mulder, T.</b> (2021). Morphodynamic equilibria in short tidal basins using a 2DH exploratory model. <i>JGR: Earth Surface 126(3)</i>: e2020JF005555. <a href=\"https://hdl.handle.net/10.1029/2020JF005555\" target=\"_blank\">https://hdl.handle.net/10.1029/2020JF005555</a>","AutID":403122,"MonDate":null,"AnaDate":2021,"PeerRev":1,"outputType":"1_A1","OpenAcc":0},{"BRefID":352993,"RR":"<b>Deng, X.; Meerman, C.; Boelens, T.; De Mulder, T.; Salles, P.; Schuttelaars, H.M.</b> (2021). Morphodynamic equilibria in double-inlet systems: existence and stability. <i>JGR: Earth Surface 126(12)</i>: e2021JF006266. <a href=\"https://dx.doi.org/10.1029/2021JF006266\" target=\"_blank\">https://dx.doi.org/10.1029/2021JF006266</a>","AutID":237040,"MonDate":null,"AnaDate":2021,"PeerRev":1,"outputType":"1_A1","OpenAcc":1},{"BRefID":336202,"RR":"<b>Horemans, D.M.L.; Dijkstra, Y.M.; Schuttelaars, H.M.; Sabbe, K.; Vyverman, W.; Meire, P.; Cox, T.J.S.</b> (2021). Seasonal variations in flocculation and erosion affecting the large‐scale suspended sediment distribution in the Scheldt estuary: the importance of biotic effects. <i>JGR: Oceans 126(4)</i>: e2020JC016805. <a href=\"https://dx.doi.org/10.1029/2020jc016805\" target=\"_blank\">https://dx.doi.org/10.1029/2020jc016805</a>","AutID":237040,"MonDate":null,"AnaDate":2021,"PeerRev":1,"outputType":"1_A1","OpenAcc":1},{"BRefID":353622,"RR":"<b>Jalón-Rojas, I.; Dijkstra, Y.M.; Schuttelaars, H.M.; Brouwer, R.L.; Schmidt, S.; Sottolichio, A.</b> (2021). Multidecadal evolution of the turbidity maximum zone in a macrotidal river under climate and anthropogenic pressures. <i>JGR: Oceans 126(5)</i>: e2020JC016273. <a href=\"https://dx.doi.org/10.1029/2020JC016273\" target=\"_blank\">https://dx.doi.org/10.1029/2020JC016273</a>","AutID":237040,"MonDate":null,"AnaDate":2021,"PeerRev":1,"outputType":"1_A1","OpenAcc":0},{"BRefID":321778,"RR":"<b>Boelens, T.; Schuttelaars, H.; Plancke, Y.; De Mulder, T.</b> (2020). Historical and future development of the tidally averaged transport of sandy sediments in the Scheldt estuary: a 2D exploratory model. <i>Ocean Dynamics 70(4)</i>: 481-504. <a href=\"https://dx.doi.org/10.1007/s10236-019-01339-2\" target=\"_blank\">https://dx.doi.org/10.1007/s10236-019-01339-2</a>","AutID":403122,"MonDate":null,"AnaDate":2020,"PeerRev":1,"outputType":"1_A1","OpenAcc":0},{"BRefID":331381,"RR":"<b>Hepkema, T.M.; de Swart, H.E.; Nnafie, A.; Schramkowski, G.P.; Schuttelaars, H.M.</b> (2020). Oblique sand ridges in confined tidal channels due to Coriolis and frictional torques. <i>Ocean Dynamics 70(12)</i>: 1505-1513. <a href=\"https://dx.doi.org/10.1007/s10236-020-01413-0\" target=\"_blank\">https://dx.doi.org/10.1007/s10236-020-01413-0</a>","AutID":237040,"MonDate":null,"AnaDate":2020,"PeerRev":1,"outputType":"1_A1","OpenAcc":1},{"BRefID":333524,"RR":"<b>Horemans, D.M.L.; Dijkstra, Y.M.; Schuttelaars, H.M.; Meire, P.; Cox, T.J.S.</b> (2020). Unraveling the essential effects of flocculation on large-scale sediment transport patterns in a tide-dominated estuary. <i>J. Phys. Oceanogr. 50(7)</i>: 1957-1981. <a href=\"https://dx.doi.org/10.1175/jpo-d-19-0232.1\" target=\"_blank\">https://dx.doi.org/10.1175/jpo-d-19-0232.1</a>","AutID":237040,"MonDate":null,"AnaDate":2020,"PeerRev":1,"outputType":"1_A1","OpenAcc":0},{"BRefID":329555,"RR":"<b>Schulz, K.; Burchard, H.; Mohrholz, V.; Holtermann, P.; Schuttelaars, H.M.; Becker, M.; Maushake, C.; Gerkema, T.</b> (2020). Intratidal and spatial variability over a slope in the Ems estuary: Robust along-channel SPM transport versus episodic events. <i>Est., Coast. and Shelf Sci. 243</i>: 106902. <a href=\"https://dx.doi.org/10.1016/j.ecss.2020.106902\" target=\"_blank\">https://dx.doi.org/10.1016/j.ecss.2020.106902</a>","AutID":237040,"MonDate":null,"AnaDate":2020,"PeerRev":1,"outputType":"1_A1","OpenAcc":1},{"BRefID":307840,"RR":"<b>Dijkstra, Y.M.; Schuttelaars, H.M.; Schramkowski, G.; Brouwer, R.L.</b> (2019). Modeling the transition to high sediment concentrations as a response to channel deepening in the Ems river estuary. <i>JGR: Oceans 124(3)</i>: 1578-1594. <a href=\"https://dx.doi.org/10.1029/2018jc014367\" target=\"_blank\">https://dx.doi.org/10.1029/2018jc014367</a>","AutID":292755,"MonDate":null,"AnaDate":2019,"PeerRev":1,"outputType":"1_A1","OpenAcc":1},{"BRefID":312514,"RR":"<b>Dijkstra, Y.M.; Schuttelaars, H.M.; Schramkowski, G.P.</b> (2019). Can the Scheldt river estuary become hyperturbid? <i>Ocean Dynamics 69(7)</i>: 809-827. <a href=\"https://dx.doi.org/10.1007/s10236-019-01277-z\" target=\"_blank\">https://dx.doi.org/10.1007/s10236-019-01277-z</a>","AutID":237040,"MonDate":null,"AnaDate":2019,"PeerRev":1,"outputType":"1_A1","OpenAcc":1},{"BRefID":323203,"RR":"<b>Dijkstra, Y.M.; Schuttelaars, H.M.; Schramkowski, G.P.</b> (2019). A regime shift from low to high sediment concentrations in a tide-dominated estuary. <i>Geophys. Res. Lett. 46(8)</i>: 4338-4345. <a href=\"https://dx.doi.org/10.1029/2019GL082302\" target=\"_blank\">https://dx.doi.org/10.1029/2019GL082302</a>","AutID":237040,"MonDate":null,"AnaDate":2019,"PeerRev":1,"outputType":"1_A1","OpenAcc":1},{"BRefID":289649,"RR":"<b>Dijkstra, Y.M.; Brouwer, R.L.; Schuttelaars, H.M.; Schramkowski, G.P.</b> (2017). The iFlow modelling framework v2.4: a modular idealized process-based model for flow and transport in estuaries. <i>Geosci. Model Dev. 10(7)</i>: 2691-2713. <a href=\"https://dx.doi.org/10.5194/gmd-10-2691-2017\" target=\"_blank\">https://dx.doi.org/10.5194/gmd-10-2691-2017</a>","AutID":292755,"MonDate":null,"AnaDate":2017,"PeerRev":1,"outputType":"1_A1","OpenAcc":1},{"BRefID":261309,"RR":"<b>Wei, X.; Schramkowski, G.P.; Schuttelaars, H.M.</b> (2016). Salt dynamics in well-mixed estuaries: importance of advection by tides. <i>J. Phys. Oceanogr. 46(5)</i>: 1457-1475. <a href=\"https://dx.doi.org/10.1175/JPO-D-15-0045.1\" target=\"_blank\">https://dx.doi.org/10.1175/JPO-D-15-0045.1</a>","AutID":237040,"MonDate":null,"AnaDate":2016,"PeerRev":1,"outputType":"1_A1","OpenAcc":0},{"BRefID":332296,"RR":"<b>De Jonge, V.N.; Schuttelaars, H.M.; van Beusekom, J.E.E.; Talke, S.A.; de Swart, H.E.</b> (2014). The influence of channel deepening on estuarine turbidity levels and dynamics, as exemplified by the Ems. <i>Est., Coast. and Shelf Sci. 139</i>: 46-59. <a href=\"https://dx.doi.org/10.1016/j.ecss.2013.12.030\" target=\"_blank\">https://dx.doi.org/10.1016/j.ecss.2013.12.030</a>","AutID":237040,"MonDate":null,"AnaDate":2014,"PeerRev":1,"outputType":"1_A1","OpenAcc":0},{"BRefID":206765,"RR":"<b>Huijts, K.M.H.; de Swart, H.E.; Schramkowski, G.P.; Schuttelaars, H.M.</b> (2011). Transverse structure of tidal and residual flow and sediment concentration in estuaries: sensitivity to tidal forcing and water depth. <i>Ocean Dynamics 61(8)</i>: 1067-1091. <a href=\"http://dx.doi.org/10.1007/s10236-011-0414-7\" target=\"_blank\">dx.doi.org/10.1007/s10236-011-0414-7</a>","AutID":69176,"MonDate":null,"AnaDate":2011,"PeerRev":1,"outputType":"1_A1","OpenAcc":0},{"BRefID":141840,"RR":"<b>Schramkowski, G.; de Swart, H.E.; Schuttelaars, H.M.</b> (2010). 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