International Symposium on Stratified Flows
Parent: Integrative Oceanography Division
eScholarship stats: Breakdown by Item for June through September, 2026
| Item | Title | Total requests | Download | View-only | %Dnld |
|---|---|---|---|---|---|
| 9hd783wq | Internal wave focusing by annular forcing | 209 | 138 | 71 | 66.0% |
| 8f88x7nt | First report of the Milestone experiment: strongly stratified turbulence and mixing efficiency in the Coriolis platform | 200 | 116 | 84 | 58.0% |
| 3sn9j23m | Experimental study on periodically forced interfacial gravity waves in a rotating cylindrical basin | 170 | 92 | 78 | 54.1% |
| 49956025 | Global stability and flow transition in horizontal convection | 168 | 98 | 70 | 58.3% |
| 6hn6f21c | VIIIth ISSF Scientific Program | 161 | 52 | 109 | 32.3% |
| 2s45v3bp | Atmospheric boundary layer dynamics in an Alpine valley during persistent temperature inversions | 154 | 29 | 125 | 18.8% |
| 5w4458tg | SOMAR-LES for multiscale modeling of internal tide generation | 151 | 58 | 93 | 38.4% |
| 4c96109b | Propagation of near-inertial waves beneath atmospheric storm tracks on the non-traditional β-plane | 146 | 84 | 62 | 57.5% |
| 51591640 | Non-linear internal waves pulse cold water into the shallow inner-shelf and surfzone | 145 | 95 | 50 | 65.5% |
| 2b59h10g | Radiation of internal waves by symmetrically unstable fronts | 144 | 29 | 115 | 20.1% |
| 5m34x2wk | Observations and processes of persistent near-bottom offshore flow at the shelfbreak off South Carolina, USA | 141 | 24 | 117 | 17.0% |
| 1qg7b8nr | Particle transport due to trapped cores | 139 | 65 | 74 | 46.8% |
| 4hg9p6rw | Experimental study of flow instabilities in a rotating annulus with local convective forcing | 136 | 85 | 51 | 62.5% |
| 1kn2w490 | Gyre generation after a typhoon-induced upwelling in a stratified lake | 134 | 31 | 103 | 23.1% |
| 61d722q6 | Acceleration-driven variable- density turbulent flow | 134 | 33 | 101 | 24.6% |
| 0p85t53g | Mixing efficiency in stratified turbulence | 127 | 49 | 78 | 38.6% |
| 2sn5p3fg | Tidal effects in a realistic model of a thermally buoyant plume north of Pt. Conception | 126 | 34 | 92 | 27.0% |
| 1rg2f5jd | Dynamics of flow over a sphere at Re=3700 in moderate to highly stratified environments | 124 | 41 | 83 | 33.1% |
| 0nc6195d | High Stokes number wave focusing by a circular ridge: Internal, inertial and inertia–gravity waves | 123 | 24 | 99 | 19.5% |
| 2nr7s5hh | Understanding critical layers in stratified shear flow instabilities: A wave interaction perspective | 123 | 22 | 101 | 17.9% |
| 3kt4t3dr | Internal tide energy transfer by nonlinear refraction | 119 | 29 | 90 | 24.4% |
| 2495c4mr | The bottom-intensification of mixing causes large abyssal upwelling and downwelling | 118 | 39 | 79 | 33.1% |
| 2j80m210 | On the control of buoyancy-driven devices in stratified, uncertain flowfields | 118 | 38 | 80 | 32.2% |
| 5q03j5h4 | Damping of 3D internal wave attractors by lateral walls | 117 | 28 | 89 | 23.9% |
| 07m314vk | A filtering approach for analyzing turbulent stratified shear flows | 116 | 32 | 84 | 27.6% |
| 0v44q35k | Vertical transport of particles, drops, and microorganisms in density-stratified fluids | 116 | 37 | 79 | 31.9% |
| 0mm966fh | The Barostrat instability: the baroclinic instability in a rotating stratified fluid | 113 | 37 | 76 | 32.7% |
| 22q7x1xh | Internal solitary wave-induced bed failure in a stratified water column | 113 | 40 | 73 | 35.4% |
| 3dh6501k | Thermobaric stratification and circulation in very deep freshwater lakes | 113 | 24 | 89 | 21.2% |
| 4797m24w | The dissolution of polar ice into a stratified ocean | 113 | 23 | 90 | 20.4% |
| 3n65j5v1 | Direct measurements of flux Richardson number in the nearshore coastal ocean | 112 | 44 | 68 | 39.3% |
| 71v784fw | Taylor-Caulfield instabilities in a layered stratified shear flow | 112 | 25 | 87 | 22.3% |
| 1gc9783p | Basin mode internal tides | 111 | 29 | 82 | 26.1% |
| 2df48121 | Characteristics of salt water movement in mouth of River Iwaki | 110 | 25 | 85 | 22.7% |
| 7hj5z639 | The significance of engulfment in the process of turbulent entrainment by plumes | 110 | 30 | 80 | 27.3% |
| 0mc131zf | Interactions between surface gravity wave groups and deep stratification in the ocean | 109 | 41 | 68 | 37.6% |
| 3w83s9x7 | Anatomy of a turbulent patch in a large shallow lake | 109 | 28 | 81 | 25.7% |
| 6c87585z | Coherent structures in stably stratified plane Couette flow | 109 | 35 | 74 | 32.1% |
| 274251c0 | Laboratory modelling of momentum transport by internal gravity waves and eddies in the Antarctic circumpolar current | 108 | 35 | 73 | 32.4% |
| 1423q64h | Instability, evolution, and mixing in stratified shear flow as a function of Richardson number | 107 | 39 | 68 | 36.4% |
| 4368p87t | Convection in rotating flows with simultaneous imposition of radial and vertical temperature gradients | 107 | 28 | 79 | 26.2% |
| 62z96987 | Internal hydraulic jumps with upstream shear and topography | 107 | 26 | 81 | 24.3% |
| 84r4n96j | Toward Direct Numerical Simulations of the stratified turbulence inertial range | 107 | 26 | 81 | 24.3% |
| 1q3025d2 | Reynolds number effects in stratified turbulent wakes | 106 | 29 | 77 | 27.4% |
| 3z78027h | Variability of the internal wave continuum: study of 2500 worldwide seasonal to inter-annual time series | 106 | 28 | 78 | 26.4% |
| 80v8w16h | Temperature fronts and vortical structures in turbulent stably stratified atmospheric boundary layers | 106 | 42 | 64 | 39.6% |
| 8f480358 | Double-diffusive lock-exchange gravity currents | 105 | 40 | 65 | 38.1% |
| 4886t0xn | Tidal bores, turbulence and mixing above deep-ocean slopes | 104 | 34 | 70 | 32.7% |
| 49x5g0ww | The effect of vortex pairing and Prandtl number on mixing in moderate Reynolds number stratified flows | 104 | 26 | 78 | 25.0% |
| 5dz568wk | Large eddy simulations of turbulence under internal solitary waves of depression | 104 | 20 | 84 | 19.2% |
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