activity
20172020
most citedIron Snow in the Martian Core?

44 citations · 139 across the 4 of their papers we have counts for

collaborators

6 papers

physics.geo-ph202015 cited

A regime diagram for the slurry F-layer at the base of Earth's outer core

Jenny Wong, Christopher J. Davies, Christopher A. Jones

Seismic observations of a slowdown in P wave velocity at the base of Earth's outer core suggest the presence of a stably-stratified region known as the F-layer. This raises an impo…

physics.comp-ph2020

Performance of parallel-in-time integration for Rayleigh Bénard Convection

Andrew Clarke, Chris Davies, Daniel Ruprecht +2

Rayleigh-Bénard convection (RBC) is a fundamental problem of fluid dynamics, with many applications to geophysical, astrophysical, and industrial flows. Understanding RBC at parame…

physics.flu-dyn2018

Penetration of boundary-driven flows into a rotating spherical thermally-stratified fluid

Grace A. Cox, Christopher J. Davies, Philip W. Livermore +1

Motivated by the dynamics within terrestrial bodies, we consider a rotating, strongly thermally stratified fluid within a spherical shell subject to a prescribed laterally inhomoge…

physics.geo-ph201744 cited

Iron Snow in the Martian Core?

Christopher Davies, and Anne Pommier

The decline of Mars' global magnetic field some 3.8-4.1 billion years ago is thought to reflect the demise of the dynamo that operated in its liquid core. The dynamo was probably p…

physics.geo-ph201744 cited

Geomagnetic spikes on the core-mantle boundary

Christopher Davies, Catherine Constable

Extreme variations of Earth's magnetic field occurred in the Levant region around 1000 BC, when the field intensity rapidly rose and fell by a factor of 2. No coherent link current…

physics.geo-ph201736 cited

Heat Flow and Boundary Heterogeneity in Rotating Convection

Jon E. Mound, Christopher J. Davies

Convection in the metallic cores of terrestrial planets is likely to be subjected to lateral variations in heat flux through the outer boundary imposed by creeping flow in the over…