Department of Earth, Planetary, and Space Sciences

Parent: UCLA

eScholarship stats: Breakdown by Item for April through July, 2024

ItemTitleTotal requestsDownloadView-only%Dnld
403071pzThickness of the crust of Mercury from geoid‐to‐topography ratios111179415.3%
5jx2s2smHeat transfer by rapidly rotating Rayleigh–Bénard convection103277626.2%
62k0726hMechanics of inner core super‐rotation95158015.8%
6qz5k7jnAxisymmetric simulations of libration-driven fluid dynamics in a spherical shell geometry91147715.4%
5bm6n165On the theory of core-mantle coupling88246427.3%
9jt5d84bConvection-driven kinematic dynamos at low Rossby and magnetic Prandtl numbers: Single mode solutions876816.9%
6g8384vkEvaporation induced <sup>18</sup>O and <sup>13</sup>C enrichment in lake systems: A global perspective on hydrologic balance effects85721384.7%
7361k8c5Anomalous rotation of the inner core and the toroidal magnetic field84107411.9%
8xq8z0g8Superfast precipitation of energetic electrons in the radiation belts of the Earth84107411.9%
83j959mcΔ 13 CH 3 D and Δ 12 CH 2 D 2 signatures of methane aerobically oxidized by Methylosinus trichosporium with implications for deciphering the provenance of methane gases83127114.5%
94r5r998OSS (Outer Solar System): a fundamental and planetary physics mission to Neptune, Triton and the Kuiper Belt8397410.8%
97s3x12hRotating convective turbulence in Earth and planetary cores79621778.5%
8fx1f8czPredominance of ECH wave contribution to diffuse aurora in Earth's outer magnetosphere7786910.4%
3m22m0rxPolar and mid-latitude vortices and zonal flows on Jupiter and Saturn76106613.2%
31r7q1j8Tornado-like vortices in the quasi-cyclostrophic regime of Coriolis-centrifugal convection756698.0%
8hz43445High Arctic wetting reduces permafrost carbon feedbacks to climate warming7596612.0%
7sr6v0fwRegimes of Coriolis-Centrifugal Convection745696.8%
7w78r8q4Strong zonal winds from thermal convection in a rotating spherical shell747679.5%
7xq1k8rqLibration‐driven flows in ellipsoidal shells7486610.8%
0t18v5vfAccelerating functional materials discovery Insights from geological sciences, data-driven approaches, and computational advances72512170.8%
3m11w73fBoundary layer control of rotating convection systems71165522.5%
5ch2w82qInfluence of methane seepage on isotopic signatures in living deep-sea benthic foraminifera, 79° N706648.6%
6r8132hmA comparison of oceanic and continental mantle lithosphere69353450.7%
73m7x0zqNitrogen fixation in sediments along a depth transect through the Peruvian oxygen minimum zone6776010.4%
37d352q9Unravelling the large-scale circulation modes in turbulent Rayleigh-Bénard convection (a) Contribution to the Focus Issue Turbulent Thermal Convection edited by Mahendra Verma and Jörg Schumacher.6475710.9%
7ff179d1Dual carbonate clumped isotope (Δ47-Δ48) measurements constrain different sources of kinetic isotope effects and quasi-equilibrium signatures in cave carbonates64154923.4%
1v0549nfRotating thermal convection in liquid gallium: multi-modal flow, absent steady columns636579.5%
2td732sdBenthic Dinitrogen Fixation Traversing the Oxygen Minimum Zone Off Mauritania (NW Africa)63115217.5%
1qp6d98wMicrobial Community Response to Simulated Petroleum Seepage in Caspian Sea Sediments626569.7%
1mj2r8jnExperimental pub crawl from Rayleigh–Bénard to magnetostrophic convection6195214.8%
3dj088bdPlease, add to the discussion for completeness610610.0%
6gg8t63nMethanogenic Hydrocarbon Degradation: Evidence from Field and Laboratory Studies61105116.4%
2m86n9zwLocal heating of radiation belt electrons to ultra-relativistic energies6075311.7%
47j2c0qjThermal evidence for Taylor columns in turbulent rotating Rayleigh-Bénard convection5975211.9%
0f86k0q7The influence of temperature and seawater carbonate saturation state on <sup>13</sup>C–<sup>18</sup>O bond ordering in bivalve mollusks5765110.5%
40f8c0s7Chorus intensity modulation driven by time‐varying field‐aligned low‐energy plasma5765110.5%
02w1x7ncThermal evidence for Taylor columns in turbulent rotating Rayleigh-Benard convection5665010.7%
9r11s5p6Brines at high pressure and temperature: Thermodynamic, petrologic and geochemical effects54262848.1%
27p899qfExperiments on Rayleigh–Bénard convection, magnetoconvection and rotating magnetoconvection in liquid gallium53183534.0%
14x4s6kpSulfur's impact on core evolution and magnetic field generation on Ganymede523495.8%
4rh4t5cjRegional stratification at the top of Earth's core due to core–mantle boundary heat flux variations52193336.5%
1b7778b5Ideas and perspectives: A strategic assessment of methane and nitrous oxide measurements in the marine environment514477.8%
5b65v425Temperature limits to deep subseafloor life in the Nankai Trough subduction zone49193038.8%
6m11w35mMeasuring Higher-Mode SurfaceWave Dispersion Using a Transdismensional Bayesian Approach490490.0%
18j8b3nzFirst observations of core-transiting seismic phases on Mars4874114.6%
5z9208xzCorrigendum to “Zircon solubility and zirconium complexation in H2O+Na2O+SiO2±Al2O3 fluids at high pressure and temperature” [Earth Planet. Sci. Lett. 349–350 (2012) 15–25]48341470.8%
26p4c1cdConvective heat transfer and the pattern of thermal emission on the gas giants471462.1%
0g80w59xDiopside, enstatite and forsterite solubilities in H2O and H2O-NaCl solutions at lower crustal and upper mantle conditions46163034.8%
8rr3m49zInsufficient Evidence of Purported Lunar Effect on Pollination in Ephedra4554011.1%
11b387snDehydration melting and the relationship between granites and granulites44311370.5%

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.