International Symposium on Stratified Flows
Parent: Integrative Oceanography Division
eScholarship stats: Breakdown by Item for March through June, 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% |
| 3sn9j23m | Experimental study on periodically forced interfacial gravity waves in a rotating cylindrical basin | 265 | 155 | 110 | 58.5% |
| 4c96109b | Propagation of near-inertial waves beneath atmospheric storm tracks on the non-traditional β-plane | 255 | 171 | 84 | 67.1% |
| 9hd783wq | Internal wave focusing by annular forcing | 249 | 179 | 70 | 71.9% |
| 5w4458tg | SOMAR-LES for multiscale modeling of internal tide generation | 227 | 98 | 129 | 43.2% |
| 0mc131zf | Interactions between surface gravity wave groups and deep stratification in the ocean | 223 | 80 | 143 | 35.9% |
| 49956025 | Global stability and flow transition in horizontal convection | 215 | 143 | 72 | 66.5% |
| 51591640 | Non-linear internal waves pulse cold water into the shallow inner-shelf and surfzone | 212 | 127 | 85 | 59.9% |
| 4hg9p6rw | Experimental study of flow instabilities in a rotating annulus with local convective forcing | 211 | 140 | 71 | 66.4% |
| 1kn2w490 | Gyre generation after a typhoon-induced upwelling in a stratified lake | 203 | 93 | 110 | 45.8% |
| 556311q5 | Decaying stratified grid turbulence measurements | 203 | 89 | 114 | 43.8% |
| 0br30315 | Vorticity-based modeling of gravity currents penetrating into ambients with arbitrary shear and density stratification | 202 | 78 | 124 | 38.6% |
| 07m314vk | A filtering approach for analyzing turbulent stratified shear flows | 198 | 74 | 124 | 37.4% |
| 0c03329n | Dynamics of a buoyant plume in linearly stratified environment using simultaneous PIV-PLIF | 198 | 61 | 137 | 30.8% |
| 1cx5s9x1 | Stability and mixing of shear layers forced by standing internal waves | 198 | 77 | 121 | 38.9% |
| 1qg7b8nr | Particle transport due to trapped cores | 195 | 108 | 87 | 55.4% |
| 22q7x1xh | Internal solitary wave-induced bed failure in a stratified water column | 195 | 98 | 97 | 50.3% |
| 80v8w16h | Temperature fronts and vortical structures in turbulent stably stratified atmospheric boundary layers | 193 | 92 | 101 | 47.7% |
| 6cd149f0 | Shear instabilities in a tilting tube | 190 | 95 | 95 | 50.0% |
| 6hn6f21c | VIIIth ISSF Scientific Program | 189 | 87 | 102 | 46.0% |
| 2kc7r67n | High variability in cross-shore thermally driven exchange | 188 | 61 | 127 | 32.4% |
| 2b59h10g | Radiation of internal waves by symmetrically unstable fronts | 187 | 65 | 122 | 34.8% |
| 2s45v3bp | Atmospheric boundary layer dynamics in an Alpine valley during persistent temperature inversions | 186 | 65 | 121 | 34.9% |
| 2j80m210 | On the control of buoyancy-driven devices in stratified, uncertain flowfields | 185 | 66 | 119 | 35.7% |
| 71v784fw | Taylor-Caulfield instabilities in a layered stratified shear flow | 184 | 69 | 115 | 37.5% |
| 0b65z4rs | A numerical study of axisymmetric flow regimes in a rotating annulus with local convective forcing | 183 | 74 | 109 | 40.4% |
| 8f480358 | Double-diffusive lock-exchange gravity currents | 183 | 83 | 100 | 45.4% |
| 7ts2h3mz | The sensitivity of stratified flow stability to base flow modifications | 182 | 70 | 112 | 38.5% |
| 0nc6195d | High Stokes number wave focusing by a circular ridge: Internal, inertial and inertia–gravity waves | 181 | 61 | 120 | 33.7% |
| 0p85t53g | Mixing efficiency in stratified turbulence | 181 | 74 | 107 | 40.9% |
| 2495c4mr | The bottom-intensification of mixing causes large abyssal upwelling and downwelling | 180 | 80 | 100 | 44.4% |
| 3dh6501k | Thermobaric stratification and circulation in very deep freshwater lakes | 180 | 67 | 113 | 37.2% |
| 9jp1326c | Mixing efficiency in a run-down gravity current | 180 | 71 | 109 | 39.4% |
| 1q3025d2 | Reynolds number effects in stratified turbulent wakes | 178 | 73 | 105 | 41.0% |
| 3n65j5v1 | Direct measurements of flux Richardson number in the nearshore coastal ocean | 178 | 71 | 107 | 39.9% |
| 7jt759sh | Turbulent mixing in strongly stratified shear flows | 178 | 66 | 112 | 37.1% |
| 8pv683c1 | The generation of internal waves by explosive volcanic eruptions | 178 | 80 | 98 | 44.9% |
| 1gc9783p | Basin mode internal tides | 177 | 58 | 119 | 32.8% |
| 2nr7s5hh | Understanding critical layers in stratified shear flow instabilities: A wave interaction perspective | 176 | 54 | 122 | 30.7% |
| 45b160s9 | Mixing efficiency in a lock exchange experiment | 176 | 77 | 99 | 43.8% |
| 0x35m2ff | Turbulent dissipation rates, mixing, and heat fluxes in the Canadian Arctic from glider-based microstructure measurements | 174 | 72 | 102 | 41.4% |
| 3tn9s414 | Understanding inertial instability on the f-plane with complete Coriolis force | 174 | 74 | 100 | 42.5% |
| 61d722q6 | Acceleration-driven variable- density turbulent flow | 174 | 71 | 103 | 40.8% |
| 4687h9tk | Interacting SQG vortices and passive scalar transport | 173 | 68 | 105 | 39.3% |
| 7q52k0tf | Turbulence, mixing and Prandtl number effects in stratified plane Couette flows | 173 | 58 | 115 | 33.5% |
| 0mm966fh | The Barostrat instability: the baroclinic instability in a rotating stratified fluid | 172 | 67 | 105 | 39.0% |
| 0ws8326k | Quantification of highly unsteady and inhomogeneous stratified turbulence in breaking internal waves on slopes | 172 | 84 | 88 | 48.8% |
| 54x2q2f3 | Transmission of internal waves generated by a localized surface forcing | 170 | 89 | 81 | 52.4% |
| 58v7472p | Observations of high-frequency internal waves and strong turbulent dissipation rates generated by a constriction between two coral atolls | 170 | 63 | 107 | 37.1% |
| 7hj5z639 | The significance of engulfment in the process of turbulent entrainment by plumes | 170 | 82 | 88 | 48.2% |
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