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Articles by Robert Chant
Lateral transport controls the tidally averaged gravitationally driven estuarine circulation: Tidal mixing effects
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Circulation and Retention of River Plumes Around Capes
1 Introduction River plumes often interact with coastal capes, which are pointed landforms projecting into the ocean, typically spanning from a few hundred meters to a few kilometers. However, the mechanisms leading to river plume separation and freshwater retention at capes have not been widely researched.
Parameterizing Subglacial Discharge in Modeling Buoyancy Driven Flow in Tidewater Glacier Fjords
Supporting Information Filename Description 20230412BPM-sup-0001-Supporting Information SI-S01.docx968.3 KB Supporting Information S1 References , , , , , , et al. (2023). Persistent overcut regions dominate the terminus morphology of a rapidly melting tidewater glacier. Annals of Glaciology, 1–12. https://doi.org/10.1017/aog.2023.38 (2002). Two-dimensional plumes in stratified environments. Journal of Fluid Mechanics, 471, 315–337. https://doi.org/10.1017/s0022112002002215 (2008).
Surface Convergence Zones due to Lagrangian Residual Flow in Tidally Driven Estuaries
ProCite RefWorks Reference Manager BibTeX Zotero Bühler, O., 2009: , 374 pp., https://doi.org/10.1017/CBO9781107478701. Burchard, H., R. D.Hetland, E.Schulz, and H. M.Schuttelaars, 2011: Drivers of residual estuarine circulation in tidally energetic estuaries: Straight and irrotational channels with parabolic cross section. J. Phys. Oceanogr., 41, 548–570, https://doi.org/10.1175/2010JPO4453.1. Burchard, H., R. D. Hetland, E. Schulz, and H. M.
Parameterization of mixing by secondary circulation in estuaries
Eddy viscosity parameterizations that depend on a gradient Richardson number R have been most pertinent to the open ocean. Parameterizations applicable to stratified coastal regions typically require implementation of a numerical model. Two novel parameterizations of the vertical eddy viscosity, based on R , are proposed here for coastal waters. One turbulence closure considers temporal changes in stratification and bottom stress and is coined the ‘regular fit'.
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