International Symposium on Stratified Flows
Parent: Integrative Oceanography Division
eScholarship stats: Breakdown by Item for September through December, 2024
| Item | Title | Total requests | Download | View-only | %Dnld |
|---|---|---|---|---|---|
| 3n65j5v1 | Direct measurements of flux Richardson number in the nearshore coastal ocean | 82 | 5 | 77 | 6.1% |
| 5rz9z6s9 | Internal-gravity wave propagation in a range-dependent waveguide with forcing at the bottom | 77 | 1 | 76 | 1.3% |
| 5w4458tg | SOMAR-LES for multiscale modeling of internal tide generation | 76 | 2 | 74 | 2.6% |
| 5mg5v9w0 | Energy cascade in internal wave attractors | 75 | 3 | 72 | 4.0% |
| 4886t0xn | Tidal bores, turbulence and mixing above deep-ocean slopes | 74 | 3 | 71 | 4.1% |
| 4jn2c6kj | A multiscale point of view on the dynamics of stably stratified turbulence associated with geostrophic modes: simulations and mode | 72 | 2 | 70 | 2.8% |
| 71v784fw | Taylor-Caulfield instabilities in a layered stratified shear flow | 49 | 8 | 41 | 16.3% |
| 2nr7s5hh | Understanding critical layers in stratified shear flow instabilities: A wave interaction perspective | 46 | 6 | 40 | 13.0% |
| 0c03329n | Dynamics of a buoyant plume in linearly stratified environment using simultaneous PIV-PLIF | 36 | 5 | 31 | 13.9% |
| 8f480358 | Double-diffusive lock-exchange gravity currents | 34 | 7 | 27 | 20.6% |
| 3w83s9x7 | Anatomy of a turbulent patch in a large shallow lake | 33 | 4 | 29 | 12.1% |
| 3kt4t3dr | Internal tide energy transfer by nonlinear refraction | 32 | 2 | 30 | 6.3% |
| 58v7472p | Observations of high-frequency internal waves and strong turbulent dissipation rates generated by a constriction between two coral atolls | 32 | 8 | 24 | 25.0% |
| 6qk2s04m | Comparison of averaging methods for interface conductivities in one- dimensional unsaturated flow in layered soils | 31 | 2 | 29 | 6.5% |
| 8f88x7nt | First report of the Milestone experiment: strongly stratified turbulence and mixing efficiency in the Coriolis platform | 30 | 12 | 18 | 40.0% |
| 0p85t53g | Mixing efficiency in stratified turbulence | 29 | 12 | 17 | 41.4% |
| 1qg7b8nr | Particle transport due to trapped cores | 29 | 7 | 22 | 24.1% |
| 1kn2w490 | Gyre generation after a typhoon-induced upwelling in a stratified lake | 28 | 5 | 23 | 17.9% |
| 6cd149f0 | Shear instabilities in a tilting tube | 28 | 9 | 19 | 32.1% |
| 12p56378 | Measurement of vertical oxygen flux in lakes from microstructure casts | 26 | 9 | 17 | 34.6% |
| 2j80m210 | On the control of buoyancy-driven devices in stratified, uncertain flowfields | 26 | 3 | 23 | 11.5% |
| 7kv5s11k | Measurements of fluid transport by controllable vertical migrations of plankton | 26 | 5 | 21 | 19.2% |
| 94x6h9jw | Thermohaline layering in dynamically and diffusively stable shear flows | 26 | 9 | 17 | 34.6% |
| 0b65z4rs | A numerical study of axisymmetric flow regimes in a rotating annulus with local convective forcing | 25 | 4 | 21 | 16.0% |
| 3dh6501k | Thermobaric stratification and circulation in very deep freshwater lakes | 25 | 7 | 18 | 28.0% |
| 45b160s9 | Mixing efficiency in a lock exchange experiment | 25 | 3 | 22 | 12.0% |
| 5q03j5h4 | Damping of 3D internal wave attractors by lateral walls | 25 | 3 | 22 | 12.0% |
| 6hn6f21c | VIIIth ISSF Scientific Program | 25 | 6 | 19 | 24.0% |
| 9d1687wh | Instability associated baroclinic critical layers in rotating stratified shear flow | 25 | 6 | 19 | 24.0% |
| 2s45v3bp | Atmospheric boundary layer dynamics in an Alpine valley during persistent temperature inversions | 24 | 1 | 23 | 4.2% |
| 4c96109b | Propagation of near-inertial waves beneath atmospheric storm tracks on the non-traditional β-plane | 24 | 2 | 22 | 8.3% |
| 4n1357zj | On the mixing efficiency in stably stratified turbulence | 24 | 5 | 19 | 20.8% |
| 5qj444gn | Fingering convection in double-diffusive, sediment-laden flows | 24 | 0 | 24 | 0.0% |
| 0br30315 | Vorticity-based modeling of gravity currents penetrating into ambients with arbitrary shear and density stratification | 23 | 4 | 19 | 17.4% |
| 1q3025d2 | Reynolds number effects in stratified turbulent wakes | 23 | 3 | 20 | 13.0% |
| 2c767266 | Layer formation in stratified Taylor-Couette flow | 23 | 2 | 21 | 8.7% |
| 38v8s83r | Mixing in stratified-shear flows forced by internal waves | 23 | 6 | 17 | 26.1% |
| 73n231mg | Reduced modeling of strongly stratified turbulence | 23 | 3 | 20 | 13.0% |
| 0mc131zf | Interactions between surface gravity wave groups and deep stratification in the ocean | 22 | 5 | 17 | 22.7% |
| 0nc6195d | High Stokes number wave focusing by a circular ridge: Internal, inertial and inertia–gravity waves | 22 | 2 | 20 | 9.1% |
| 274251c0 | Laboratory modelling of momentum transport by internal gravity waves and eddies in the Antarctic circumpolar current | 22 | 4 | 18 | 18.2% |
| 2bh698j9 | Three-dimensional visualization of the interaction between a vortex ring and a stratified interface: the evolution of the density field | 22 | 3 | 19 | 13.6% |
| 2xm7j16t | Modeling internal solitary wave development at the head of a submarine canyon | 22 | 3 | 19 | 13.6% |
| 49x5g0ww | The effect of vortex pairing and Prandtl number on mixing in moderate Reynolds number stratified flows | 22 | 6 | 16 | 27.3% |
| 4h17v4cj | Spatial and temporal characteristics of double-diffusive layering in relic seawater | 22 | 5 | 17 | 22.7% |
| 54x5b0b3 | Orientation of vortical structures in turbulent stratified shear flow | 22 | 2 | 20 | 9.1% |
| 5kp3x801 | Influence of forced near-inertial motion on the kinetic energy of a nearly-geostrophic flow | 22 | 6 | 16 | 27.3% |
| 1sh4g636 | Phase-resolved simulations of sediment erosion due to unsteady pressure drag | 21 | 5 | 16 | 23.8% |
| 4z52f26k | Ageostrophic instability and mixing in a dense overflow | 21 | 1 | 20 | 4.8% |
| 6s96g6m8 | Entrainment in stratified environments — an interface-based approach | 21 | 6 | 15 | 28.6% |
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