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The elevation of points on a hill is a scalar 'field'. It can have a different value

at every point, but each one is a scalar value.

Imagine a lumpy bumpy irregular hill, and pick a point to talk about, say,

somewhere on the side of the hill.

At that point, the directional derivative of the elevation is the rate at which

the elevation changes leaving the point in that direction.

It has different values in different directions: If you're looking up the hill, then

the d.d. is positive in that direction; if you're looking down the hill, the d.d. is

negative in that direction. If you're looking along the side of the hill, the d.d.

could be zero, because the elevation doesn't change in that particular direction.

The directional derivative is a vector. The direction is whatever direction you're

talking about, and the magnitude is the rate of change in that direction.

The gradient is the vector that's simply the greatest positive directional derivative

at that point. Its direction is the direction of the steepest rise, and its magnitude

is the rate of rise in that direction.

If your hill is, say, a perfect cone, and you're on the side, then the gradient is the

vector from you straight toward the top, with magnitude equal to the slope of the

side of the cone. Any other vector is a directional derivative, with a smaller slope,

and it isn't the gradient.

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Q: What is the physical interpretation of gradient of a scalar field and directional derivative?
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