The gradient is a differential operator on a scalar field, \phi. The gradient, grad\phi, is a "vector field" defined by the requirement that
grad\,\phi\,\cdot d
s = d\,\phi
where d\,\phi is the differential change in the scalar field, \phi, corresponding to the arbitrary space displacement, d
s, and from this,
d\,\phi = | grad \,\phi\,| |d
s| cos \theta, where is the angle between the displacement vector and the line formed between two points of interest in the scalar field.
Since cos \theta has a maximum value of 1, that is when \theta=0, it is clear that the rate of change is greatest if the differential displacement is in the direction of grad\,\phi\,, or stated another way,
"The direction of the vector grad\,\phi is the direction of maximum rate of change (spatially-speaking) of \,\phi from the point of consideration, i.e. direction in which \frac{d\phi}{ds} is greatest."
The gradient of \phi is considered 'directional derivative' in the direction of the maximum rate of change of the scalar field \phi.
Think of contours of elevation on a mountain slope. Points of the same (constant) elevation have the same gravitational potential, \phi. Displacement along (parallel) to the contours produce no change in \phi (i.e. d\phi = 0). Displacements perpendicular (normal) to the equipotential are oriented in the direction of most rapid change of altitude, and d\phi has the maximum value.
Isotherms are equipotentials with respect to heat flow.
See related discussion on the directional derivative (forthcoming).
Examples of scalar fields:
- density (mass distribution) in an object or matter (solid, liquid, gas, . . .)
- electrostatic (charge distribution)
Examples of vector fields:
- velocity at each point in a moving fluid (e.g. hurricane or tornado, river, . . .)
I am doing something similar for
div and
curl