International Symposium on Stratified Flows
Parent: Integrative Oceanography Division
eScholarship stats: Breakdown by Item for March through June, 2024
| Item | Title | Total requests | Download | View-only | %Dnld |
|---|---|---|---|---|---|
| 5mg5v9w0 | Energy cascade in internal wave attractors | 82 | 1 | 81 | 1.2% |
| 2nr7s5hh | Understanding critical layers in stratified shear flow instabilities: A wave interaction perspective | 81 | 3 | 78 | 3.7% |
| 3n65j5v1 | Direct measurements of flux Richardson number in the nearshore coastal ocean | 81 | 3 | 78 | 3.7% |
| 5w4458tg | SOMAR-LES for multiscale modeling of internal tide generation | 76 | 0 | 76 | 0.0% |
| 71v784fw | Taylor-Caulfield instabilities in a layered stratified shear flow | 68 | 0 | 68 | 0.0% |
| 4886t0xn | Tidal bores, turbulence and mixing above deep-ocean slopes | 66 | 1 | 65 | 1.5% |
| 6qk2s04m | Comparison of averaging methods for interface conductivities in one- dimensional unsaturated flow in layered soils | 64 | 1 | 63 | 1.6% |
| 4jn2c6kj | A multiscale point of view on the dynamics of stably stratified turbulence associated with geostrophic modes: simulations and mode | 63 | 0 | 63 | 0.0% |
| 5rz9z6s9 | Internal-gravity wave propagation in a range-dependent waveguide with forcing at the bottom | 63 | 0 | 63 | 0.0% |
| 6ft077b5 | An affordable, open-source, microscale conductivity and temperature probe for density measurements in stratified flows | 58 | 1 | 57 | 1.7% |
| 38v8s83r | Mixing in stratified-shear flows forced by internal waves | 57 | 5 | 52 | 8.8% |
| 3kt4t3dr | Internal tide energy transfer by nonlinear refraction | 53 | 3 | 50 | 5.7% |
| 6hn6f21c | VIIIth ISSF Scientific Program | 44 | 14 | 30 | 31.8% |
| 8f88x7nt | First report of the Milestone experiment: strongly stratified turbulence and mixing efficiency in the Coriolis platform | 42 | 6 | 36 | 14.3% |
| 45b160s9 | Mixing efficiency in a lock exchange experiment | 39 | 5 | 34 | 12.8% |
| 2xm7j16t | Modeling internal solitary wave development at the head of a submarine canyon | 38 | 1 | 37 | 2.6% |
| 0c03329n | Dynamics of a buoyant plume in linearly stratified environment using simultaneous PIV-PLIF | 37 | 1 | 36 | 2.7% |
| 0nc6195d | High Stokes number wave focusing by a circular ridge: Internal, inertial and inertia–gravity waves | 36 | 3 | 33 | 8.3% |
| 5sm840h1 | The momentum balance of steady flow past an island | 36 | 6 | 30 | 16.7% |
| 1c139176 | An experimental investigation of evanescent wave propagation through a turning depth | 35 | 0 | 35 | 0.0% |
| 2b59h10g | Radiation of internal waves by symmetrically unstable fronts | 35 | 1 | 34 | 2.9% |
| 55g4h6q5 | Three-dimensional instability of internal gravity wave beams | 35 | 2 | 33 | 5.7% |
| 5qj444gn | Fingering convection in double-diffusive, sediment-laden flows | 35 | 4 | 31 | 11.4% |
| 60v9h6wx | Three-dimensional, time-resolved velocity and density measurements of the stratified shear flow in an inclined duct | 35 | 1 | 34 | 2.9% |
| 6cd149f0 | Shear instabilities in a tilting tube | 35 | 0 | 35 | 0.0% |
| 7xf635tk | A study of a model for the generation of internal waves by a moving body and its turbulent wake | 35 | 7 | 28 | 20.0% |
| 8pv683c1 | The generation of internal waves by explosive volcanic eruptions | 35 | 1 | 34 | 2.9% |
| 07m314vk | A filtering approach for analyzing turbulent stratified shear flows | 34 | 0 | 34 | 0.0% |
| 0b65z4rs | A numerical study of axisymmetric flow regimes in a rotating annulus with local convective forcing | 34 | 4 | 30 | 11.8% |
| 0p85t53g | Mixing efficiency in stratified turbulence | 34 | 7 | 27 | 20.6% |
| 12p56378 | Measurement of vertical oxygen flux in lakes from microstructure casts | 34 | 10 | 24 | 29.4% |
| 1960f9fd | The influence of a shoaling internal gravity wave on a dense gravity current | 34 | 2 | 32 | 5.9% |
| 1q3025d2 | Reynolds number effects in stratified turbulent wakes | 34 | 2 | 32 | 5.9% |
| 5jg095wd | A new theory for downslope windstorms and trapped mountain waves | 34 | 1 | 33 | 2.9% |
| 7jt759sh | Turbulent mixing in strongly stratified shear flows | 34 | 3 | 31 | 8.8% |
| 8f480358 | Double-diffusive lock-exchange gravity currents | 34 | 4 | 30 | 11.8% |
| 1kn2w490 | Gyre generation after a typhoon-induced upwelling in a stratified lake | 33 | 0 | 33 | 0.0% |
| 58v7472p | Observations of high-frequency internal waves and strong turbulent dissipation rates generated by a constriction between two coral atolls | 33 | 3 | 30 | 9.1% |
| 5kp3x801 | Influence of forced near-inertial motion on the kinetic energy of a nearly-geostrophic flow | 33 | 0 | 33 | 0.0% |
| 6jm3r22m | High-resolution observations of internal wave induced turbulence in the deep ocean | 33 | 2 | 31 | 6.1% |
| 7474v5sh | Stability of stratified downslope flows with an overlying isolating layer | 33 | 1 | 32 | 3.0% |
| 7kv5s11k | Measurements of fluid transport by controllable vertical migrations of plankton | 33 | 3 | 30 | 9.1% |
| 8d61h3sj | Stability and nonlinear dynamics of a settling fresh water particle laden fluid below a salt water layer | 33 | 1 | 32 | 3.0% |
| 0g7803d9 | High-resolution simulations of down-slope turbidity currents into a stratified saline ambient | 32 | 1 | 31 | 3.1% |
| 0v44q35k | Vertical transport of particles, drops, and microorganisms in density-stratified fluids | 32 | 1 | 31 | 3.1% |
| 0x35m2ff | Turbulent dissipation rates, mixing, and heat fluxes in the Canadian Arctic from glider-based microstructure measurements | 32 | 1 | 31 | 3.1% |
| 1cx5s9x1 | Stability and mixing of shear layers forced by standing internal waves | 32 | 2 | 30 | 6.3% |
| 3vm6v7sw | Near-inertial wave transmission in the Arctic Ocean | 32 | 1 | 31 | 3.1% |
| 556311q5 | Decaying stratified grid turbulence measurements | 32 | 3 | 29 | 9.4% |
| 5h66n59t | Boussinesq dynamics of an idealized tropopause | 32 | 0 | 32 | 0.0% |
Disclaimer: due to the evolving nature of the web traffic we receive and the methods we use to collate it, the data presented here should be considered approximate and subject to revision.