International Symposium on Stratified Flows
Parent: Integrative Oceanography Division
eScholarship stats: Breakdown by Item for January through April, 2025
| Item | Title | Total requests | Download | View-only | %Dnld |
|---|---|---|---|---|---|
| 3n65j5v1 | Direct measurements of flux Richardson number in the nearshore coastal ocean | 103 | 9 | 94 | 8.7% |
| 5w4458tg | SOMAR-LES for multiscale modeling of internal tide generation | 83 | 7 | 76 | 8.4% |
| 4jn2c6kj | A multiscale point of view on the dynamics of stably stratified turbulence associated with geostrophic modes: simulations and mode | 71 | 6 | 65 | 8.5% |
| 5rz9z6s9 | Internal-gravity wave propagation in a range-dependent waveguide with forcing at the bottom | 70 | 5 | 65 | 7.1% |
| 4886t0xn | Tidal bores, turbulence and mixing above deep-ocean slopes | 65 | 5 | 60 | 7.7% |
| 5mg5v9w0 | Energy cascade in internal wave attractors | 65 | 1 | 64 | 1.5% |
| 2nr7s5hh | Understanding critical layers in stratified shear flow instabilities: A wave interaction perspective | 61 | 8 | 53 | 13.1% |
| 63p0g457 | Temperature front formation in stably stratified turbulence | 43 | 10 | 33 | 23.3% |
| 0x35m2ff | Turbulent dissipation rates, mixing, and heat fluxes in the Canadian Arctic from glider-based microstructure measurements | 42 | 6 | 36 | 14.3% |
| 274251c0 | Laboratory modelling of momentum transport by internal gravity waves and eddies in the Antarctic circumpolar current | 42 | 9 | 33 | 21.4% |
| 1c139176 | An experimental investigation of evanescent wave propagation through a turning depth | 41 | 4 | 37 | 9.8% |
| 0p85t53g | Mixing efficiency in stratified turbulence | 38 | 9 | 29 | 23.7% |
| 3rx2n92v | On the synergy between numerics and subgrid scale modeling in LES of stratified flows: Grid convergence of a stratocumulus-topped boundary layer | 38 | 6 | 32 | 15.8% |
| 3kt4t3dr | Internal tide energy transfer by nonlinear refraction | 37 | 6 | 31 | 16.2% |
| 3pr7d5zh | Oblique nonlinear interaction of internal solitary-like waves in the Andaman Sea | 37 | 9 | 28 | 24.3% |
| 6hn6f21c | VIIIth ISSF Scientific Program | 36 | 16 | 20 | 44.4% |
| 6v54465p | The dynamics of submesoscale eddies in the coastal ocean | 36 | 10 | 26 | 27.8% |
| 71v784fw | Taylor-Caulfield instabilities in a layered stratified shear flow | 35 | 5 | 30 | 14.3% |
| 73n231mg | Reduced modeling of strongly stratified turbulence | 35 | 8 | 27 | 22.9% |
| 7q52k0tf | Turbulence, mixing and Prandtl number effects in stratified plane Couette flows | 35 | 8 | 27 | 22.9% |
| 0c03329n | Dynamics of a buoyant plume in linearly stratified environment using simultaneous PIV-PLIF | 34 | 10 | 24 | 29.4% |
| 0nc6195d | High Stokes number wave focusing by a circular ridge: Internal, inertial and inertia–gravity waves | 33 | 10 | 23 | 30.3% |
| 2b59h10g | Radiation of internal waves by symmetrically unstable fronts | 33 | 6 | 27 | 18.2% |
| 3vm6v7sw | Near-inertial wave transmission in the Arctic Ocean | 33 | 8 | 25 | 24.2% |
| 4c96109b | Propagation of near-inertial waves beneath atmospheric storm tracks on the non-traditional β-plane | 33 | 7 | 26 | 21.2% |
| 236375jk | Fortnightly modulation of deep mixing inside a Mid-Ocean Ridge fracture zone in the Brazil Basin | 32 | 11 | 21 | 34.4% |
| 2bz8g03k | Prandtl number effects on mixing in Kelvin-Helmholtz billows | 32 | 7 | 25 | 21.9% |
| 2j80m210 | On the control of buoyancy-driven devices in stratified, uncertain flowfields | 32 | 8 | 24 | 25.0% |
| 5jg095wd | A new theory for downslope windstorms and trapped mountain waves | 32 | 6 | 26 | 18.8% |
| 5sm840h1 | The momentum balance of steady flow past an island | 32 | 9 | 23 | 28.1% |
| 7jt759sh | Turbulent mixing in strongly stratified shear flows | 32 | 8 | 24 | 25.0% |
| 7ts2h3mz | The sensitivity of stratified flow stability to base flow modifications | 32 | 11 | 21 | 34.4% |
| 9d1687wh | Instability associated baroclinic critical layers in rotating stratified shear flow | 32 | 9 | 23 | 28.1% |
| 0v44q35k | Vertical transport of particles, drops, and microorganisms in density-stratified fluids | 31 | 9 | 22 | 29.0% |
| 2tp6j11k | The three-dimensional propagation of tsunami-generated acoustic-gravity waves in the atmosphere | 31 | 8 | 23 | 25.8% |
| 49x5g0ww | The effect of vortex pairing and Prandtl number on mixing in moderate Reynolds number stratified flows | 31 | 9 | 22 | 29.0% |
| 0b65z4rs | A numerical study of axisymmetric flow regimes in a rotating annulus with local convective forcing | 30 | 6 | 24 | 20.0% |
| 1cx5s9x1 | Stability and mixing of shear layers forced by standing internal waves | 30 | 6 | 24 | 20.0% |
| 1qg7b8nr | Particle transport due to trapped cores | 30 | 8 | 22 | 26.7% |
| 3sn9j23m | Experimental study on periodically forced interfacial gravity waves in a rotating cylindrical basin | 30 | 12 | 18 | 40.0% |
| 61d722q6 | Acceleration-driven variable- density turbulent flow | 30 | 6 | 24 | 20.0% |
| 6qk2s04m | Comparison of averaging methods for interface conductivities in one- dimensional unsaturated flow in layered soils | 30 | 6 | 24 | 20.0% |
| 751607m9 | Turbulent mixing in a marginally-unstable stratified shear layer | 30 | 7 | 23 | 23.3% |
| 0br30315 | Vorticity-based modeling of gravity currents penetrating into ambients with arbitrary shear and density stratification | 29 | 8 | 21 | 27.6% |
| 38v8s83r | Mixing in stratified-shear flows forced by internal waves | 29 | 8 | 21 | 27.6% |
| 4797m24w | The dissolution of polar ice into a stratified ocean | 29 | 11 | 18 | 37.9% |
| 6463389s | Double-diffusive sedimentation | 28 | 10 | 18 | 35.7% |
| 76m2q1k9 | Modeling the oxygen depletion within stratified bottom boundary layers of lakes | 28 | 8 | 20 | 28.6% |
| 7hj5z639 | The significance of engulfment in the process of turbulent entrainment by plumes | 28 | 11 | 17 | 39.3% |
| 9z34g1s0 | On a slippery slope | 28 | 6 | 22 | 21.4% |
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