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Bart Root

Publications

  • Benchmark forward gravity schemes: the gravity field of a realistic lithosphere model WINTERC-G
  • The interior-atmosphere coupling of rocky worlds
  • The use of Non-Linear Geometry (NLGEOM) and gravity loading in flat and spherical Finite Element models of Abaqus for Glacial Isostatic Adjustment (GIA)
  • Benchmark forward gravity schemes: the gravity field of a realistic lithosphere model WINTERC-G
  • Combining the deep Earth and lithospheric gravity field to study the density structure of the upper mantle
  • Supplementary material to "Benchmark forward gravity schemes: the gravity field of a realistic lithosphere model WINTERC-G"
  • A re-analysis of the lithospheric flexure on Mars
  • Is the lithospheric flexure strong enough to hold up the Tharsis Rise? A re-analysis of flexure on Mars
  • Asteroid Gravity-Field Estimation
  • MaQuIs - Mars Quantum Gravity Mission
  • The changing gravity field due to a superplume under the Tharsis Region
  • Rocky worlds: What do a planet's orbital parameters tell us about its mantle state?
  • Inversion of the lateral density variations of the lithosphere using the full gravity gradient tensor
  • Simulating horizontal crustal motions of glacial isostatic adjustment using compressible Cartesian models
  • The global gravity field of Mars reveals an active interior
  • Sensitivity analysis on gravity change data in order to observe mantle convection
  • Present-day surface heat flux variations on the Moon from global geodynamic and crustal thickness models
  • Exploration of high mass subsurface structures in the northern hemisphere with joint flexure and mantle convection modelling of the Martian gravity field
  • Glacial isostatic adjustment on Mars
  • Satellite gravity-rate observations to uncover Martian plume-lithosphere dynamics
  • The present-day surface heat flux of the Moon from global geodynamic and crustal thickness models.
  • GRACE and GRACE-FO constraints on 3D GIA models
  • GRACE constraints on Earth rheology of the Barents Sea and Fennoscandia
  • GRACE constraints on Earth rheology of the Barents Sea and Fennoscandia
  • Glacial isostatic adjustment reveals Mars’s interior viscosity structure
  • Constraining the distribution of radiogenics on the Moon from global geodynamic models
  • Geodynamic modelling the thermochemical structure of the Earth's mantle using integrated geophysical and petrological inversion of surface wave and satellite gravity data
  • 3D Lithospheric-scale thermal model of central and southern California
  • Benchmarking dynamic topography across geodynamical codes
  • Exploring the origin of lunar magnetic anomalies through the Parker Inversion method
  • Application of Satellite Gravimetry and AI to Map the Density Distributions of Mars’s Upper Layers

Bart Root's public data