Jan Erik Weber

• Weber, Jan Erik H.; Whitchelo, Yiyi; Pirolt, Jon Alexander; Christensen, Kai Håkon; Rabault, Jean & Jensen, Atle (2023). Observations of transient wave-induced mean drift profiles caused by virtual wave stresses in a two-layer system. Journal of Fluid Mechanics. ISSN 0022-1120. 975( A12). doi: 10.1017/jfm.2023.864. Fulltekst i vitenarkiv
• Christensen, Kai Håkon & Weber, Jan Erik H. (2023). Application of a Robin boundary condition to surface waves. Frontiers in Marine Science. ISSN 2296-7745. 10. doi: 10.3389/fmars.2023.1129643. Fulltekst i vitenarkiv
• Weber, Jan Erik H. & Isachsen, Pål Erik (2023). Energy transfer from sub-inertial Kelvin waves to continental shelf waves at a transverse bottom escarpment. Continental Shelf Research. ISSN 0278-4343. 258. doi: 10.1016/j.csr.2023.104985. Fulltekst i vitenarkiv
• Weber, Jan Erik H. (2022). On the coupling between surface waves and the motion in a flexible porous surface layer. Ocean Modelling. ISSN 1463-5003. 174. doi: 10.1016/j.ocemod.2022.102013. Fulltekst i vitenarkiv
• Weber, Jan Erik H. (2022). A note on the temporal and spatial attenuation of ocean waves. Ocean Modelling. ISSN 1463-5003. 175. doi: 10.1016/j.ocemod.2022.102027. Fulltekst i vitenarkiv
• Weber, Jan Erik H. & Børve, Eli (2022). On group velocity and spatial damping of diurnal continental shelf waves . Continental Shelf Research. ISSN 0278-4343. 232. doi: 10.1016/j.csr.2021.104630. Fulltekst i vitenarkiv Vis sammendrag

  Diurnal continental shelf waves (CSWs) are studied theoretically for an idealized shelf topography. Wave attenuation is caused by the exchange of fluid on the sloping shelf with an inner region through a permeable coastline. As an example, we consider the region outside Lofoten-Vesterålen in north Norway. Here CSWs with diurnal tidal frequencies are possible in a small wave number range centered around zero group velocity. A previous investigation with a Robin condition (a weighted combination of Dirichlet and Neumann conditions) at the permeable boundary has shown that the spatial damping coefficient becomes infinitely large when the group velocity of the CSWs approaches zero. Here we demonstrate that this is not a result of the mathematical formulation, but reflects a physical reality. We show this by modelling the highly convoluted inner archipelagic region as a series of densely packed vertical Hele Shaw cells. By comparing the two ways of describing a permeable coastal boundary (Robin/Hele Shaw), we may express the Robin parameter in terms of the physical parameters (permeability, eddy viscosity) that characterize the flow on the inner porous shelf. The radiation stresses that drive the Lagrangian mean currents are the same in the two cases. This means that the spatial mean current distribution over the sloping shelf becomes unaltered when we compare the Robin case and the porous inner shelf case.

• Weber, Jan Erik H. & Ghaffari, Peygham (2021). Wave-induced Lagrangian drift in a porous seabed . Environmental Fluid Mechanics. ISSN 1567-7419. doi: 10.1007/s10652-021-09823-4. Fulltekst i vitenarkiv
• Weber, Jan Erik H. (2021). On the Stokes drift in traveling surface pulses. Ocean Modelling. ISSN 1463-5003. 166. doi: 10.1016/j.ocemod.2021.101847. Fulltekst i vitenarkiv
• Weber, Jan Erik H. & Broström, Göran (2021). Convection in conditionally unstable seawater. AIP Advances. ISSN 2158-3226. 11(7). doi: 10.1063/5.0053629. Fulltekst i vitenarkiv
• Weber, Jan Erik H. & Børve, Eli (2021). Diurnal continental shelf waves with a permeable coastal boundary: Application to the shelf northwest of Norway. European journal of mechanics. B, Fluids. ISSN 0997-7546. 89, s. 64–71. doi: 10.1016/j.euromechflu.2021.05.003. Fulltekst i vitenarkiv
• Weber, Jan Erik H. & Christensen, Kai Håkon (2021). On the analogy between rigid plate motion and mean momentum transfer in surface gravity waves . AIP Advances. ISSN 2158-3226. 11(4). doi: 10.1063/5.0043751. Fulltekst i vitenarkiv
• Weber, Jan Erik H. (2021). Lagrangian drift in a permeable bottom layer induced by internal gravity waves. Tellus A: Dynamic Meteorology and Oceanography. ISSN 0280-6495. 73(1), s. 1–9. doi: 10.1080/16000870.2021.1877461. Fulltekst i vitenarkiv
• Weber, Jan Erik H. & Christensen, Kai Håkon (2021). On the singular behavior of the Stokes drift in layered miscible fluids. Wave motion. ISSN 0165-2125. 102, s. 1–8. doi: 10.1016/j.wavemoti.2021.102712. Fulltekst i vitenarkiv
• Ghaffari, Peygham; Weber, Jan Erik Hobæk; Nøst, Ole Anders & Drivdal, Magnus Bjørn (2020). Stokes Drift in Topographic Waves over an Enclosed Basin Shelf. Journal of Physical Oceanography. ISSN 0022-3670. doi: 10.1175/JPO-D-19-0126.1.
• Weber, Jan Erik Hobæk; Nøst, Ole Anders & Drivdal, Magnus Bjørn (2020). Stokes Drift in Topographic Waves over an Enclosed Basin Shelf. Journal of Physical Oceanography. ISSN 0022-3670. doi: 10.1175/jpo-d-19-0126.1.
• Weber, Jan Erik Hobæk; Nøst, Ole Anders & Drivdal, Magnus Bjørn (2020). Stokes Drift in Topographic Waves over an Enclosed Basin Shelf. Journal of Physical Oceanography. ISSN 0022-3670. doi: 10.1175/jpo-d-19-0126.1.
• Ghaffari, Peygham; Weber, Jan Erik H.; Nøst, Ole Anders & Drivdal, Magnus (2020). Stokes drift in topographic waves over an enclosed basin shelf. Journal of Physical Oceanography. ISSN 0022-3670. 50(5), s. 1197–1211. doi: 10.1175/JPO-D-19-0126.1. Fulltekst i vitenarkiv
• Weber, Jan Erik H. (2019). A Lagrangian study of internal Gerstner- and Stokes-type gravity waves. Wave motion. ISSN 0165-2125. 88, s. 257–264. doi: 10.1016/j.wavemoti.2019.06.002. Fulltekst i vitenarkiv
• Weber, Jan Erik H. & Christensen, Kai Håkon (2019). Virtual wave stress and transient mean drift in spatially damped long interfacial waves. European journal of mechanics. B, Fluids. ISSN 0997-7546. 77, s. 162–170. doi: 10.1016/j.euromechflu.2019.04.004. Fulltekst i vitenarkiv
• Weber, Jan Erik H. (2019). Lagrangian studies of wave-induced flows in a viscous ocean. Deep-Sea Research Part II: Topical Studies in Oceanography. ISSN 0967-0645. 160, s. 68–81. doi: 10.1016/j.dsr2.2018.10.011. Fulltekst i vitenarkiv
• Ghaffari, Peygham; Isachsen, Pål Erik; Nøst, Ole Anders & Weber, Jan Erik H. (2018). The influence of topography on the stability of the Norwegian Atlantic Current off Northern Norway. Journal of Physical Oceanography. ISSN 0022-3670. 48(11), s. 2761–2777. doi: 10.1175/JPO-D-17-0235.1. Fulltekst i vitenarkiv
• Weber, Jan Erik H. (2018). An interfacial Gerstner-type trapped wave. Wave motion. ISSN 0165-2125. 77, s. 186–194. doi: 10.1016/j.wavemoti.2017.12.002. Fulltekst i vitenarkiv
• Weber, Jan Erik H. (2017). Equatorial Stokes drift and Rossby rip currents. Journal of Geophysical Research (JGR): Oceans. ISSN 2169-9275. 122(6), s. 4819–4828. doi: 10.1002/2016JC012653. Fulltekst i vitenarkiv Vis sammendrag

  The Stokes drift in long baroclinic equatorial Rossby waves is investigated theoretically by using eigenfunction expansions in the vertical. These waves are non-dispersive and propagate westward along the equator. Particular attention is paid to the first baroclinic, first meridional Rossby wave mode which has been observed in the equatorial Pacific. It is demonstrated that the Stokes drift depends very much on the depth-variation of the Brunt-Väisälä frequency. Even more importantly, it is found that, for arbitrary stable stratification, the total zonal Stokes volume transport induced by the Rossby wave mode (1,1) is identically zero. The eastward drift due reflected wave energy in the form of internal equatorial Kelvin waves is also addressed. Due to the very long period of the incident Rossby wave mode (1,1), the reflected equatorial Kelvin wave must at least be a 2. mode component in the vertical. The corresponding Stokes drift only induces a minor change near the surface of the total westward drift velocity at the equator. The implication for the existence of compensating Rossby rip currents along the equator is discussed.

• Weber, Jan Erik H. (2017). Vertically varying Eulerian mean currents induced by internal coastal Kelvin waves. Journal of Geophysical Research (JGR): Oceans. ISSN 2169-9275. 122(2), s. 1222–1231. doi: 10.1002/2016JC012377. Fulltekst i vitenarkiv Vis sammendrag

  The lost momentum in spatially damped internal Kelvin waves reappears as Eulerian mean currents through the action of the nonlinear wave-wave interaction terms. A novel expression is derived for the steady balance between the frictional force on the coastally trapped horizontal Eulerian mean flow, and the forcing from the wave field in terms of the mean wave Reynolds stresses and the horizontal divergence of the Stokes drift. The forcing can be expressed in terms of orthogonal eigenfunctions for internal waves, yielding the vertical variation of the Eulerian mean flow. For arbitrary values of the Brunt-Väisälä frequency , it is shown that the wave forcing on the Eulerian mean is always negative, yielding a Poiseuille type flow. Therefore, unlike the Stokes drift velocity in internal Kelvin waves which exhibits a backward drift for the first mode in the region of maximum , the wave-induced horizontal Eulerian mean current is always in the direction of the waves. The results are illustrated by an example from Van Mijenfjorden in Svalbard, which is an arctic sill fjord where internal waves are generated by the action of the barotropic semi-diurnal tide.

• Drivdal, Magnus Bjørn; Weber, Jan Erik H. & Debernard, Jens B. (2016). Dispersion relation for continental shelf waves when the shallow shelf part has an arbitrary width: Application to the shelf west of Norway. Journal of Physical Oceanography. ISSN 0022-3670. 46(2), s. 537–549. doi: 10.1175/JPO-D-15-0023.1.
• Weber, Jan Erik H.; Drivdal, Magnus Bjørn; Christensen, Kai Håkon & Brostrøm, Gøran (2015). Some aspects of the Coriolis-Stokes forcing in the oceanic momentum and energy budgets. Journal of Geophysical Research (JGR): Oceans. ISSN 2169-9275. 120(8), s. 5589–5596. doi: 10.1002/2015JC010717.
• Weber, Jan Erik H. (2015). Eulerian volume transport induced by spatially damped internal equatorial Kelvin waves. Journal of Physical Oceanography. ISSN 0022-3670. 45(7), s. 1794–1803. doi: 10.1175/JPO-D-14-0102.1.
• Broström, Göran; Christensen, Kai Håkon; Drivdal, Magnus & Weber, Jan Erik H. (2014). Note on Coriolis-Stokes force and energy. Ocean Dynamics. ISSN 1616-7341. 64(7), s. 1039–1045. doi: 10.1007/s10236-014-0723-8.
• Weber, Jan Erik H. & Ghaffari, Peygham (2014). Mass transport in internal coastal Kelvin waves. European journal of mechanics. B, Fluids. ISSN 0997-7546. 47, s. 151–157. doi: 10.1016/j.euromechflu.2014.02.006.
• Ghaffari, Peygham & Weber, Jan Erik H. (2014). Mass transport in the Stokes edge wave for constant arbitrary bottom slope in a rotating ocean. Journal of Physical Oceanography. ISSN 0022-3670. 44(4), s. 1161–1174. doi: 10.1175/JPO-D-13-0171.1.
• Weber, Jan Erik H.; Christensen, Kai Håkon & Broström, Göran (2014). Stokes drift in internal equatorial Kelvin waves; continuous stratification versus two-layer models. Journal of Physical Oceanography. ISSN 0022-3670. 44(2), s. 591–599. doi: 10.1175/JPO-D-13-0135.1.
• Weber, Jan Erik H. & Drivdal, Magnus Bjørn (2012). Radiation stress and mean drift in continental shelf waves. Continental Shelf Research. ISSN 0278-4343. 35, s. 108–116. doi: 10.1016/j.csr.2012.01.001.
• Weber, Jan Erik H. (2012). A note on trapped Gerstner waves. Journal of Geophysical Research (JGR): Oceans. ISSN 2169-9275. 117. doi: 10.1029/2011JC007776.
• Weber, Jan Erik H. & Støylen, Eivind (2011). Mean drift velocity in the Stokes interfacial edge wave. Journal of Geophysical Research (JGR): Oceans. ISSN 2169-9275. 116(C04002). doi: 10.1029/2010JC006619.
• Weber, Jan Erik H. (2011). Do we observe Gerstner waves in wave tank experiments? Wave motion. ISSN 0165-2125. 48(4), s. 301–309. doi: 10.1016/j.wavemoti.2010.11.005.
• Støylen, Eivind & Weber, Jan Erik H. (2010). Mass transport induced by internal Kelvin waves beneath shore-fast ice. Journal of Geophysical Research (JGR): Oceans. ISSN 2169-9275. 115(C03022). doi: 10.1029/2009JC005298. Vis sammendrag

  A one-layer reduced-gravity model is used to investigate the wave-induced mass flux in internal Kelvin waves along a straight coast beneath shore-fast ice. The waves are generated by barotropic tidal pumping at narrow sounds, and the ice lid introduces a no-slip condition for the horizontal wave motion. The mean Lagrangian fluxes to second order in wave steepness are obtained by integrating the equations of momentum and mass between the material interface and the surface. The mean flow is forced by the conventional radiation stress for internal wave motion, the mean pressure gradient due to the sloping surface, and the frictional drag at the boundaries. The equations that govern the mean fluxes are expressed in terms of mean Eulerian variables, while the wave forcing terms are given by the horizontal divergence of the Stokes flux. Analytical results show that the effect of friction induces a mean Eulerian flux along the coast that is comparable to the Stokes flux. In addition, the horizontal divergence of the total mean flux along the coast induces a small mass flux in the cross-shore direction. This flux changes the mean thickness of the upper layer outside the trapping region and may facilitate geostrophically balanced boundary currents in enclosed basins. This is indeed demonstrated by numerical solutions of the flux equations for confined areas larger than the trapping region. Application of the theory to Arctic waters is discussed, with emphasis on the transport of biological material and pollutants in nearshore regions.

• Wåhlin, Anna Kristine; Johansson, A. M.; Aas, Eyvind; Brostrøm, G.; Weber, Jan Erik H. & Grue, John (2010). Horizontal convection in water heated by infrared radiation and cooled by evaporation: scaling analysis and experimental results. Tellus A: Dynamic Meteorology and Oceanography. ISSN 0280-6495. 62A(2), s. 154–169. doi: 10.1111/j.1600-0870.2009.00427.x.
• Weber, Jan Erik H.; Christensen, Kai Håkon & Denamiel, Clea (2009). Wave-induced setup of the mean surface over a sloping beach. Continental Shelf Research. ISSN 0278-4343. 29(11-12), s. 1448–1453. doi: 10.1016/j.csr.2009.03.010.
• Weber, Jan Erik H. & Ghaffari, Peygham (2009). Mass transport in the Stokes edge wave. Journal of Marine Research. ISSN 0022-2402. 67(2), s. 213–224. doi: 10.1357/002224009789051182.
• Brostrøm, Gøran; Christensen, Kai Håkon & Weber, Jan Erik H. (2008). A quasi-Eulerian, quasi-Lagrangian view of surface-wave- induced flow in the ocean. Journal of Physical Oceanography. ISSN 0022-3670. 38, s. 1122–1130.
• Weber, Jan Erik H. (2008). A note on mixing due to surface wave breaking. Journal of Geophysical Research (JGR): Oceans. ISSN 2169-9275. 113(C11009). doi: 10.1029/2008JC004758.
• Weber, Jan Erik H.; Brostrom, G & Christensen, Kai Håkon (2008). Radiation stress and depth-dependent drift in surface waves with dissipation. International Journal of Offshore and Polar Engineering. ISSN 1053-5381. 18(1), s. 8–13.
• Weber, Jan Erik & Løyning, Terje B. (2006). Thermobaric effect on slantwise convection in cold seawater. Tellus A: Dynamic Meteorology and Oceanography. ISSN 0280-6495. 58(3), s. 385–391.
• Weber, Jan Erik; Brostrøm, Gøran & Saetra, Øyvind (2006). Eulerian versus Lagrangian approaches to the wave-induced transport in the upper ocean. Journal of Physical Oceanography. ISSN 0022-3670. 36(11), s. 2106–2118.
• Christensen, Kai Håkon & Weber, Jan Erik (2005). Drift of an inextensible sheet caused by surface waves. Environmental Fluid Mechanics. ISSN 1567-7419. 5, s. 495–505. doi: 10.1007/s10652-005-1052-8.
• Christensen, Kai Håkon & Weber, Jan Erik (2005). Wave-induced drift of large floating sheets. Geophysical and Astrophysical Fluid Dynamics. ISSN 0309-1929. 99(6), s. 433–443. doi: 10.1080/03091920500357119. Vis sammendrag

  In this article we study the wave-induced drift of large, flexible shallow floating objects, referred to as sheets. When surface waves propagate through a sheet, they provide a mean stress on the sheet, resulting in a mean drift. In response, the sheet generates an Ekman current. The drift velocity of the sheet is determined by (i) the wave-induced stress, (ii) the viscous stress due to the Ekman current, and (iii) the Coriolis force. The sheet velocity and the current beneath the sheet are determined for constant and depth-varying eddy viscosities.

• Weber, Jan Erik (2005). Mean drift velocity in viscous flow over a corrugated bottom. Physics of Fluids. ISSN 1070-6631. 17, s. 113102-1–113102-8.
• Høydalsvik, Frode & Weber, Jan Erik (2003). Mass transport velocity in free barotropic Poincare waves. Journal of Physical Oceanography. ISSN 0022-3670. 33, s. 2000–2012.

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• Weber, Jan Erik H. (2019). Internal Gerstner- and Stokes-type gravity waves.
• Weber, Jan Erik H. (2018). Virtual wave stress and transient particle drift in spatially damped long interfacial waves.
• Weber, Jan Erik H. (2018). Cold ice in warm seawater - freezing or melting?
• Weber, Jan Erik H. (2018). Lagrangian approach to wave-induced flow in a viscous rotating ocean. Vis sammendrag

  The presence of viscosity has a profound effect on the wave-induced drift. In a pioneering paper (Longuet-Higgins, 1953) it was demonstrated that the inclusion of a small viscosity not only modified the motion in thin boundary layers near the surface and at the bottom, but also produced significant changes from Stokes (1847) irrotational solution in the interior. We here present results for wave-induced drift in a fluid layer of finite depth by applying a direct Lagrangian description of fluid motion. The Lagrangian form is (usually) more mathematically demanding than the traditional Eulerian approach. However, it yields directly the mean particle drift velocity in periodic motion. The solution to the wave-drift problem in a Lagrangian description depends crucially on the viscosity ν being non-zero, however small. It exemplifies the singular nature of this problem, in which the limit of solutions as ν→0 is different from solutions obtained with ν=0.

• Weber, Jan Erik H. & Ghaffari, Peygham (2016). Mean currents induced by spatially damped internal Kelvin waves: Application to Van Mijenfjorden in Svalbard.
• Weber, Jan Erik H. (2016). Mechanical plate analogy to nonlinear wave-induced mass transport.
• Weber, Jan Erik H. & Christensen, Kai Håkon (2016). Mean particle drift in long gravity waves at the interface between immiscible viscous fluids.
• Weber, Jan Erik H. (2015). Baroclinic wave-induced mass transport in an Arctic sill fjord.
• Weber, Jan Erik H. (2015). Mean drift in baroclinic Rossby waves.
• Weber, Jan Erik H. (2014). Mechanical analogy to nonlinear wave-induced mass transport.
• Weber, Jan Erik H. (2014). Buoyancy effects in fluids – An educational journey.
• Weber, Jan Erik H. (2014). Stokes drift in internal waves.
• Weber, Jan Erik H.; Christensen, Kai Håkon & Broström, Göran (2013). Stokes drift in internal equatorial Kelvin waves.
• Weber, Jan Erik H. (2013). Mixing induced by breaking waves.
• Weber, Jan Erik H. (2012). Offshore vindmølleparker og havmiljø.
• Weber, Jan Erik H. (2012). Trapped Gerstner waves over a steeply sloping shelf.
• Weber, Jan Erik H. (2012). The Stokes edge wave in a Gerstner formulation.
• Drivdal, Magnus & Weber, Jan Erik H. (2012). Mean Lagrangian drift in contintnetal shelf waves.
• Weber, Jan Erik H. (2011). Minnetale over professor dr. philos. Hans Ragnar Kristian Økland. Årbok / Det norske videnskaps-akademi. ISSN 0332-6209.
• Weber, Jan Erik H. (2011). Bølger i havet.
• Weber, Jan Erik H. & Støylen, Eivind (2010). Mass transport in the Stokes interfacial edge wave.
• Weber, Jan Erik H. & Støylen, Eivind (2010). Nonlinear drift in the Stokes interfacial edge wave.
• Weber, Jan Erik H. & Ghaffari, Peygham (2010). Mass transport in the Stokes edge wave.
• Støylen, Eivind & Weber, Jan Erik H. (2009). Mass transport induced by internal Kelvin waves beneath shorefast ice. Geophysical Research Abstracts. ISSN 1029-7006. 11.
• Weber, Jan Erik H. & Brostrøm, Gøran (2009). Density-driven convection between horizontal planes in a conditionally unstable fluid.
• Weber, Jan Erik H. (2009). Do we observe Gerstner waves in wave tank experiments?
• Weber, Jan Erik H. & Støylen, Eivind (2009). Mass transport induced by internal Kelvin waves beneath shore fast ice.
• Weber, Jan Erik H. (2008). Mixing due to surface-wave breaking. Geophysical Research Abstracts. ISSN 1029-7006. 10.
• Weber, Jan Erik H. & Gjevik, Bjørn (2008). Havnivået langs Norskekysten. Forskning.no. ISSN 1891-635X.
• Støylen, Eivind & Weber, Jan Erik H. (2008). Mean mass transport induced by internal Kelvin waves, with application to the circulation in the Van Mijen fjord in Svalbard.
• Wåhlin, Anna Kristine; Ericsson, A.M.; Aas, Eyvind; Brostrøm, G.; Weber, Jan Erik H. & Grue, John (2008). Horizontal convection in water heated by infrared radiation and cooled by evaporation.
• Brostrøm, Gøran; Christensen, Kai Håkon & Weber, Jan Erik H. (2008). How to include surfaces waves in an ocean model.
• Weber, Jan Erik H. (2008). Mixing due to breaking surface waves.
• Weber, Jan Erik H. (2008). Fakta om havnivået i norske farvann.
• Weber, Jan Erik H. (2008). Mixing at the top of the mixed layer - the effect of surface-wave breaking.
• Christensen, Kai Håkon; Brostrøm, Gøran & Weber, Jan Erik H. (2007). A new model for the drift in progressive surface gravity waves.
• Weber, Jan Erik; Brostrøm, Gøran & Saetra, Øyvind (2006). A wave-driven surge model for the deep ocean. Geophysical Research Abstracts. ISSN 1029-7006. 8.
• Weber, Jan Erik; Christensen, Kai Håkon & Brostrøm, Gøran (2006). Radiation stress and the drift in gravity waves with Rayleigh friction.
• Christensen, Kai Håkon; Brostrøm, Gøran & Weber, Jan Erik (2006). A new model for the mean drift in surface gravity waves.
• Weber, Jan Erik; Brostrøm, Gøran & Christensen, Kai Håkon (2006). Radiation stress and the drift in gravity waves with weak friction.
• Weber, Jan Erik (2006). How shallow-water waves induce an anti-cyclonic mean drift around banks and islands in an inviscid rotating ocean.
• Weber, Jan Erik (2006). Turbulent plumes driven by horizontal buoyancy fluxes.
• Weber, Jan Erik (2005). Wave-induced transport in the upper ocean.
• Weber, Jan Erik & Løyning, Terje B. (2005). Thermobaric effect on slantwise convection in cold seawater.
• Weber, Jan Erik (2005). Freezing of seawater at a cold wall.
• Christensen, Kai Håkon & Weber, Jan Erik (2005). Drift of an inextensible sheet caused by surface waves.
• Weber, Jan Erik (2005). Eulerian vs Lagrangian analyses of the wave-induced transport in the upper ocean.
• Wåhlin, Anna Kristine; Ericsson, A. M.; Aas, Eyvind & Weber, Jan Erik (2005). Horizontal convection in water heated by infra-red radiation and cooled by evaporation.
• Weber, Jan Erik (2004). Destruktive havbølger eller tsunamier. I Reisegg, Øyvind (Red.), Store Norske Årbok 2004. Gyldendalske bokhandel, Nordisk forlag A/S. ISSN 8257314692.
• Weber, Jan Erik (2004). A Lagrangian approach to wave-induced oceanic mass transport.
• Weber, Jan Erik (2004). Wave-mean flow interaction in a very viscous fluid.
• Weber, Jan Erik (2003). Sea-Ice Interactions, Encyclopedia of Life Support Systems (EOLSS). UNESCO.

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