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surface of discontinuity

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surface of discontinuity [¦sər·fəs əv ‚dis‚känt·ən′ü·əd·ē]
(fluid mechanics)
A surface within a fluid across which there is a discontinuity in fluid velocity; often generated in the wake of a body moving relative to the fluid.
(meteorology)
An interface, applied to the atmosphere; for example, an atmospheric front is represented ideally by a surface of discontinuity of velocity, density, temperature, and pressure gradient.


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A common approach to this problem is to consider the boundary as a moving surface of discontinuity in the deformation gradient, regardless of how the fine structure looks like close to the interface [3;4].
 
 
 
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