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The surface shell describes nonuniform conductivities of oceans and continents.
Right: 1-D conductivity profile beneath the surface shell.
The surface shell is scaled to a thickness of 10 km.
In contrast, a current will flow from the core into the surface shell by applying a positive surface potential.
The iterative structure is due to the applied correction for the ocean effect (arising from a laterally heterogeneous surface shell).
With the term "3-D model", we denote this 1-D model plus a laterally heterogeneous surface shell.
For forward modelling, each layer (including the thin surface shell) is discretized in 72 × 36 cells of 5° × 5°.
(b) In the core, middle, and surface shells versus thickness of core taken to be equal to the surface shell.
Note that by the term "3-D model", we denote the 1-D model plus a laterally heterogeneous surface shell.
The surface shell, because of thermal activation, showed an increase in the oxygen contribution, shown in Figure 5c.
Second, each layer of surface, shell and core has single phase, random multi-phases, or ordered multi-phases.
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