International Symposium on Stratified Flows
Parent: Integrative Oceanography Division
eScholarship stats: Breakdown by Item for May through August, 2026
| Item | Title | Total requests | Download | View-only | %Dnld |
|---|---|---|---|---|---|
| 8f88x7nt | First report of the Milestone experiment: strongly stratified turbulence and mixing efficiency in the Coriolis platform | 284 | 161 | 123 | 56.7% |
| 9hd783wq | Internal wave focusing by annular forcing | 244 | 168 | 76 | 68.9% |
| 3sn9j23m | Experimental study on periodically forced interfacial gravity waves in a rotating cylindrical basin | 216 | 118 | 98 | 54.6% |
| 5w4458tg | SOMAR-LES for multiscale modeling of internal tide generation | 210 | 91 | 119 | 43.3% |
| 4c96109b | Propagation of near-inertial waves beneath atmospheric storm tracks on the non-traditional β-plane | 201 | 129 | 72 | 64.2% |
| 49956025 | Global stability and flow transition in horizontal convection | 197 | 124 | 73 | 62.9% |
| 2s45v3bp | Atmospheric boundary layer dynamics in an Alpine valley during persistent temperature inversions | 195 | 47 | 148 | 24.1% |
| 51591640 | Non-linear internal waves pulse cold water into the shallow inner-shelf and surfzone | 191 | 123 | 68 | 64.4% |
| 4hg9p6rw | Experimental study of flow instabilities in a rotating annulus with local convective forcing | 183 | 127 | 56 | 69.4% |
| 1kn2w490 | Gyre generation after a typhoon-induced upwelling in a stratified lake | 170 | 58 | 112 | 34.1% |
| 1qg7b8nr | Particle transport due to trapped cores | 170 | 92 | 78 | 54.1% |
| 5m34x2wk | Observations and processes of persistent near-bottom offshore flow at the shelfbreak off South Carolina, USA | 169 | 41 | 128 | 24.3% |
| 1cx5s9x1 | Stability and mixing of shear layers forced by standing internal waves | 168 | 65 | 103 | 38.7% |
| 07m314vk | A filtering approach for analyzing turbulent stratified shear flows | 167 | 52 | 115 | 31.1% |
| 0mc131zf | Interactions between surface gravity wave groups and deep stratification in the ocean | 162 | 56 | 106 | 34.6% |
| 0nc6195d | High Stokes number wave focusing by a circular ridge: Internal, inertial and inertia–gravity waves | 160 | 43 | 117 | 26.9% |
| 6hn6f21c | VIIIth ISSF Scientific Program | 160 | 61 | 99 | 38.1% |
| 2495c4mr | The bottom-intensification of mixing causes large abyssal upwelling and downwelling | 159 | 65 | 94 | 40.9% |
| 0c03329n | Dynamics of a buoyant plume in linearly stratified environment using simultaneous PIV-PLIF | 156 | 56 | 100 | 35.9% |
| 61d722q6 | Acceleration-driven variable- density turbulent flow | 154 | 56 | 98 | 36.4% |
| 0p85t53g | Mixing efficiency in stratified turbulence | 151 | 64 | 87 | 42.4% |
| 0x35m2ff | Turbulent dissipation rates, mixing, and heat fluxes in the Canadian Arctic from glider-based microstructure measurements | 151 | 59 | 92 | 39.1% |
| 8f480358 | Double-diffusive lock-exchange gravity currents | 151 | 55 | 96 | 36.4% |
| 556311q5 | Decaying stratified grid turbulence measurements | 149 | 58 | 91 | 38.9% |
| 0br30315 | Vorticity-based modeling of gravity currents penetrating into ambients with arbitrary shear and density stratification | 148 | 51 | 97 | 34.5% |
| 1q3025d2 | Reynolds number effects in stratified turbulent wakes | 148 | 59 | 89 | 39.9% |
| 2b59h10g | Radiation of internal waves by symmetrically unstable fronts | 147 | 46 | 101 | 31.3% |
| 2j80m210 | On the control of buoyancy-driven devices in stratified, uncertain flowfields | 147 | 53 | 94 | 36.1% |
| 0b65z4rs | A numerical study of axisymmetric flow regimes in a rotating annulus with local convective forcing | 146 | 59 | 87 | 40.4% |
| 22q7x1xh | Internal solitary wave-induced bed failure in a stratified water column | 146 | 54 | 92 | 37.0% |
| 2sn5p3fg | Tidal effects in a realistic model of a thermally buoyant plume north of Pt. Conception | 146 | 53 | 93 | 36.3% |
| 7hj5z639 | The significance of engulfment in the process of turbulent entrainment by plumes | 145 | 56 | 89 | 38.6% |
| 2df48121 | Characteristics of salt water movement in mouth of River Iwaki | 144 | 57 | 87 | 39.6% |
| 2kc7r67n | High variability in cross-shore thermally driven exchange | 144 | 39 | 105 | 27.1% |
| 71v784fw | Taylor-Caulfield instabilities in a layered stratified shear flow | 144 | 46 | 98 | 31.9% |
| 2nr7s5hh | Understanding critical layers in stratified shear flow instabilities: A wave interaction perspective | 142 | 37 | 105 | 26.1% |
| 45b160s9 | Mixing efficiency in a lock exchange experiment | 140 | 48 | 92 | 34.3% |
| 80v8w16h | Temperature fronts and vortical structures in turbulent stably stratified atmospheric boundary layers | 140 | 57 | 83 | 40.7% |
| 0mm966fh | The Barostrat instability: the baroclinic instability in a rotating stratified fluid | 139 | 50 | 89 | 36.0% |
| 1gc9783p | Basin mode internal tides | 139 | 44 | 95 | 31.7% |
| 0v44q35k | Vertical transport of particles, drops, and microorganisms in density-stratified fluids | 138 | 51 | 87 | 37.0% |
| 1423q64h | Instability, evolution, and mixing in stratified shear flow as a function of Richardson number | 137 | 63 | 74 | 46.0% |
| 3dh6501k | Thermobaric stratification and circulation in very deep freshwater lakes | 137 | 47 | 90 | 34.3% |
| 7ts2h3mz | The sensitivity of stratified flow stability to base flow modifications | 136 | 53 | 83 | 39.0% |
| 4h17v4cj | Spatial and temporal characteristics of double-diffusive layering in relic seawater | 135 | 53 | 82 | 39.3% |
| 4n1357zj | On the mixing efficiency in stably stratified turbulence | 135 | 39 | 96 | 28.9% |
| 5sm840h1 | The momentum balance of steady flow past an island | 135 | 51 | 84 | 37.8% |
| 6c87585z | Coherent structures in stably stratified plane Couette flow | 135 | 58 | 77 | 43.0% |
| 6ps841sg | Extended fully-nonlinear and strongly-dispersive internal wave equations in a three-layer system | 135 | 59 | 76 | 43.7% |
| 7jt759sh | Turbulent mixing in strongly stratified shear flows | 135 | 37 | 98 | 27.4% |
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