International Symposium on Stratified Flows
Parent: Integrative Oceanography Division
eScholarship stats: Breakdown by Item for December, 2024 through March, 2025
| Item | Title | Total requests | Download | View-only | %Dnld |
|---|---|---|---|---|---|
| 3n65j5v1 | Direct measurements of flux Richardson number in the nearshore coastal ocean | 118 | 9 | 109 | 7.6% |
| 5w4458tg | SOMAR-LES for multiscale modeling of internal tide generation | 94 | 7 | 87 | 7.4% |
| 4jn2c6kj | A multiscale point of view on the dynamics of stably stratified turbulence associated with geostrophic modes: simulations and mode | 82 | 6 | 76 | 7.3% |
| 4886t0xn | Tidal bores, turbulence and mixing above deep-ocean slopes | 81 | 7 | 74 | 8.6% |
| 5mg5v9w0 | Energy cascade in internal wave attractors | 80 | 2 | 78 | 2.5% |
| 5rz9z6s9 | Internal-gravity wave propagation in a range-dependent waveguide with forcing at the bottom | 77 | 4 | 73 | 5.2% |
| 2nr7s5hh | Understanding critical layers in stratified shear flow instabilities: A wave interaction perspective | 66 | 9 | 57 | 13.6% |
| 0c03329n | Dynamics of a buoyant plume in linearly stratified environment using simultaneous PIV-PLIF | 45 | 10 | 35 | 22.2% |
| 71v784fw | Taylor-Caulfield instabilities in a layered stratified shear flow | 45 | 8 | 37 | 17.8% |
| 274251c0 | Laboratory modelling of momentum transport by internal gravity waves and eddies in the Antarctic circumpolar current | 41 | 9 | 32 | 22.0% |
| 3pr7d5zh | Oblique nonlinear interaction of internal solitary-like waves in the Andaman Sea | 41 | 10 | 31 | 24.4% |
| 4c96109b | Propagation of near-inertial waves beneath atmospheric storm tracks on the non-traditional β-plane | 40 | 7 | 33 | 17.5% |
| 8f480358 | Double-diffusive lock-exchange gravity currents | 40 | 9 | 31 | 22.5% |
| 0p85t53g | Mixing efficiency in stratified turbulence | 39 | 10 | 29 | 25.6% |
| 2j80m210 | On the control of buoyancy-driven devices in stratified, uncertain flowfields | 39 | 9 | 30 | 23.1% |
| 3kt4t3dr | Internal tide energy transfer by nonlinear refraction | 39 | 7 | 32 | 17.9% |
| 3rx2n92v | On the synergy between numerics and subgrid scale modeling in LES of stratified flows: Grid convergence of a stratocumulus-topped boundary layer | 39 | 5 | 34 | 12.8% |
| 58v7472p | Observations of high-frequency internal waves and strong turbulent dissipation rates generated by a constriction between two coral atolls | 39 | 7 | 32 | 17.9% |
| 3w83s9x7 | Anatomy of a turbulent patch in a large shallow lake | 38 | 7 | 31 | 18.4% |
| 2b59h10g | Radiation of internal waves by symmetrically unstable fronts | 37 | 6 | 31 | 16.2% |
| 2s45v3bp | Atmospheric boundary layer dynamics in an Alpine valley during persistent temperature inversions | 37 | 5 | 32 | 13.5% |
| 6hn6f21c | VIIIth ISSF Scientific Program | 37 | 12 | 25 | 32.4% |
| 63p0g457 | Temperature front formation in stably stratified turbulence | 36 | 7 | 29 | 19.4% |
| 7q52k0tf | Turbulence, mixing and Prandtl number effects in stratified plane Couette flows | 36 | 8 | 28 | 22.2% |
| 0nc6195d | High Stokes number wave focusing by a circular ridge: Internal, inertial and inertia–gravity waves | 35 | 9 | 26 | 25.7% |
| 3dh6501k | Thermobaric stratification and circulation in very deep freshwater lakes | 35 | 8 | 27 | 22.9% |
| 45b160s9 | Mixing efficiency in a lock exchange experiment | 35 | 11 | 24 | 31.4% |
| 9d1687wh | Instability associated baroclinic critical layers in rotating stratified shear flow | 35 | 10 | 25 | 28.6% |
| 12p56378 | Measurement of vertical oxygen flux in lakes from microstructure casts | 34 | 10 | 24 | 29.4% |
| 1qg7b8nr | Particle transport due to trapped cores | 34 | 9 | 25 | 26.5% |
| 38v8s83r | Mixing in stratified-shear flows forced by internal waves | 34 | 12 | 22 | 35.3% |
| 0b65z4rs | A numerical study of axisymmetric flow regimes in a rotating annulus with local convective forcing | 33 | 9 | 24 | 27.3% |
| 0x35m2ff | Turbulent dissipation rates, mixing, and heat fluxes in the Canadian Arctic from glider-based microstructure measurements | 33 | 5 | 28 | 15.2% |
| 1kn2w490 | Gyre generation after a typhoon-induced upwelling in a stratified lake | 33 | 7 | 26 | 21.2% |
| 5sm840h1 | The momentum balance of steady flow past an island | 33 | 9 | 24 | 27.3% |
| 8pv683c1 | The generation of internal waves by explosive volcanic eruptions | 33 | 8 | 25 | 24.2% |
| 2bz8g03k | Prandtl number effects on mixing in Kelvin-Helmholtz billows | 32 | 8 | 24 | 25.0% |
| 2tp6j11k | The three-dimensional propagation of tsunami-generated acoustic-gravity waves in the atmosphere | 32 | 10 | 22 | 31.3% |
| 49x5g0ww | The effect of vortex pairing and Prandtl number on mixing in moderate Reynolds number stratified flows | 32 | 10 | 22 | 31.3% |
| 6qk2s04m | Comparison of averaging methods for interface conductivities in one- dimensional unsaturated flow in layered soils | 32 | 6 | 26 | 18.8% |
| 6s96g6m8 | Entrainment in stratified environments — an interface-based approach | 32 | 10 | 22 | 31.3% |
| 6v54465p | The dynamics of submesoscale eddies in the coastal ocean | 32 | 5 | 27 | 15.6% |
| 76m2q1k9 | Modeling the oxygen depletion within stratified bottom boundary layers of lakes | 32 | 9 | 23 | 28.1% |
| 0br30315 | Vorticity-based modeling of gravity currents penetrating into ambients with arbitrary shear and density stratification | 31 | 8 | 23 | 25.8% |
| 0v44q35k | Vertical transport of particles, drops, and microorganisms in density-stratified fluids | 31 | 8 | 23 | 25.8% |
| 61d722q6 | Acceleration-driven variable- density turbulent flow | 31 | 10 | 21 | 32.3% |
| 7ts2h3mz | The sensitivity of stratified flow stability to base flow modifications | 31 | 8 | 23 | 25.8% |
| 1cx5s9x1 | Stability and mixing of shear layers forced by standing internal waves | 30 | 6 | 24 | 20.0% |
| 2kc7r67n | High variability in cross-shore thermally driven exchange | 30 | 8 | 22 | 26.7% |
| 2xm7j16t | Modeling internal solitary wave development at the head of a submarine canyon | 30 | 6 | 24 | 20.0% |
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