activity
20172026
most citedConsequences of glacial cycles for magmatism and carbon transport at mid-ocean ridges

25 citations · 53 across the 5 of their papers we have counts for

collaborators

5 papers

physics.geo-ph2026

Resonant lunar tides of Earth's core and basal magma ocean

Murray B. C. Kiernan, Hamish C. F. C. Hay, David W. Rees Jones +2

Earth's magnetic field is generated by fluid motion in the liquid-metal core and has been active for billions of year. However, prior to the onset of inner-core growth, the sources…

physics.ao-ph2024★ 2 cited

Thermodynamic growth of sea ice: assessing the role of salinity using a quasi-static modelling framework

David W. Rees Jones

Sea ice is a mushy layer, a porous material whose properties depend on the relative proportions of solid and liquid. The growth of sea ice is governed by heat transfer through the…

physics.geo-ph2020★ 8 cited

Magmatic channelisation by reactive and shear-driven instabilities at mid-ocean ridges: a combined analysis

David W. Rees Jones, Hanwen Zhang, Richard F. Katz

It is generally accepted that melt extraction from the mantle at mid-ocean ridges (MORs) is concentrated in narrow regions of elevated melt fraction called channels. Two feedback m…

physics.geo-ph2019★ 25 cited

Consequences of glacial cycles for magmatism and carbon transport at mid-ocean ridges

Nestor G. Cerpa, David W. Rees Jones, Richard F. Katz

Magmatism and volcanism transfer carbon from the solid Earth into the climate system. This transfer may be modulated by the glacial/interglacial cycling of water between oceans and…

physics.flu-dyn2017★ 18 cited

Reaction-infiltration instability in a compacting porous medium

David W. Rees Jones, Richard F. Katz

Certain geological features have been interpreted as evidence of channelized magma flow in the mantle, which is a compacting porous medium. Aharonov et al. (1995) developed a simpl…