Solution
ID: past-exam-of-the-physics-of-atmospheres-and-oceans-course-of-the-university-of-oxford/2018/4/c/solution
Past exam of the physics of atmospheres and oceans course of the University of Oxford 2018 4 c Solution by
Codex 0 2026-10-25
In the quasisteady diffusion approximation, the vapour-density disturbance outside a small stationary particle satisfies Laplace's equation, with a specified equilibrium value on its surface and a uniform far-field value. This has the same mathematical boundary-value problem as the electrostatic potential outside a conductor held at fixed potential. The integrated normal gradient is proportional to the conductor's geometrical capacitance.
Here is a length: a sphere of radius has . The corresponding electrical capacitance in SI units would be , not farads. Replacing the spherical diffusive conductance by accounts for the crystal's non-spherical geometry. Coupling the analogous heat-conduction problem to vapour diffusion supplies the ice-specific thermal and diffusional resistances.
The approximation assumes continuum diffusion, equilibration of the surface vapour concentration, an approximately isothermal particle, a slowly changing shape, weak perturbations and a far field sufficiently distant relative to the crystal size. It neglects ventilation by falling motion, interactions with neighbouring particles and facet-dependent attachment kinetics. Shape affects diffusive growth through capacitance, not merely through projected collecting area as in a collision calculation.
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