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pro vyhledávání: '"Jones, David W. Rees"'
Autor:
Jones, David W. Rees
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 ice together with appropriate boundary conditions at the interfaces wi
Externí odkaz:
http://arxiv.org/abs/2409.17696
Publikováno v:
Geophysical Journal International, Volume 226, Issue 1, July 2021, Pages 582-609
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 mechanisms have been proposed to explain why these channels grow by lin
Externí odkaz:
http://arxiv.org/abs/2008.13674
Autor:
Jones, David W. Rees, Rudge, John F.
Publikováno v:
Earth and Planetary Science Letters, 2020, Volume 542, 116324
Partial melting of asthenospheric mantle generates magma that supplies volcanic systems. The timescale of melt extraction from the mantle has been hotly debated. Microstructural measurements of permeability typically suggest relatively slow melt extr
Externí odkaz:
http://arxiv.org/abs/1910.08318
Publikováno v:
Earth Planet. Sci. Lett., 528, 115845 (2019)
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 continental ice sheets, which alters the surface loading of the solid
Externí odkaz:
http://arxiv.org/abs/1904.03154
Autor:
Jones, David W. Rees, Katz, Richard F.
Publikováno v:
Journal of Fluid Mechanics, 852, pp. 5-36 (2018)
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 simple model of reactive porous flow and numerically analysed its instabili
Externí odkaz:
http://arxiv.org/abs/1711.07779
Publikováno v:
Earth and Planetary Science Letters, Volume 481, 2018, Pages 73-79
Magmatism in subduction zones builds continental crust and causes most of Earth's subaerial volcanism. The production rate and composition of magmas are controlled by the thermal structure of subduction zones. A range of geochemical and heat flow evi
Externí odkaz:
http://arxiv.org/abs/1701.02550
Autor:
Jones, David W. Rees, Wells, Andrew J.
Publikováno v:
Phys. Rev. E 92 (2015) 022406
The physics of ice crystal growth from the liquid phase, especially in the presence of salt, has received much less attention than the growth of snow crystals from the vapour phase. The growth of so-called frazil ice by solidification of a supercoole
Externí odkaz:
http://arxiv.org/abs/1504.02721
Autor:
Worster, M. Grae, Jones, David W. Rees
Publikováno v:
Philosophical Transactions: Mathematical, Physical and Engineering Sciences, 2015 Jul . 373(2045), 1-13.
Externí odkaz:
http://www.jstor.org/stable/24505071
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