Interpreting Curl in Vector Fields: ∇×v

In summary, the vector field has a non-zero Curl due to the faster flow of water in the middle and slower flow near the banks of a river. While in scalar fields, the gradient points towards the direction of maximum increase, the direction of gradient in a vector field can be determined by the inner product of the Curl with a normal to the plane. The cross product is not involved, but it has a similar form in Cartesian coordinates and can be seen as a measure of the line integral around a small planar loop. Similarly, divergence can be seen as a measure of net flow out of a closed surface surrounding a small volume.
  • #1
Titan97
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In a river, water flows faster in the middle and slower near the banks of the river and hence, if I placed a twig, it would rotate and hence, the vector field has non-zero Curl.
Curl{v}=∇×v
But I am finding it difficult to interpret the above expression geometrically. In scalar fields, the gradient points along the direction of maximum increase. But what's the direction of gradient in a vector field? And why does the cross product give the Curl?
 
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  • #2
It is not a cross product, it simply happens to have a similar form in Cartesian coordinates.

You can think of (the inner product of) the curl (with a normal to the plane) as being a measure of the line integral around a small planar loop. The direction of the curl is the direction which will maximise this line integral.

This is analogous to how you may see divergence as a measure of the net flow out of the closed surface surrounding a small volume.
 
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