Last time we derived a simple PDE describing the process of non-diffusive advection in a constantly flowing stream of water. That PDE looked like this: , where was the constant speed of the water. The solution of this PDE is a function of the form .
This PDE follows a more general form that looks like this: , where and are constants. If you’ve studied multivariable calculus, you might recognize this kind of equation. It is, in fact, a directional derivative.
We can rewrite , where . We can read this equation as “the gradient (or derivative) of in the direction of is zero”. Which means that in the direction , the solution attains the same constant value. It may be easier to see by graphing it:
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