In the review of current textbooks1, it is pointed out that g should be described as the strength of the gravitational field rather than as an acceleration. The distinction may benefit from a little elaboration.
A book of mass m rests on a table. What is its weight w? A typical textbook answer is that w = mg where g is “the acceleration due to gravity.”
Given that the book is in equilibrium2 it has no acceleration due to gravity, nor has anything else in the figure, so the statement is self-contradictory. A worse case arises where a body is falling but is not in free fall. Its weight is still described as the “mass times the acceleration due to gravity,” but its acceleration is less than this—potentially very confusing.
Even if g is called the acceleration of a body in free fall, it is not at all obvious to a beginner that the product of a mass m kilogram and g m/s2 gives w Newton. It is more logical and much more transparent if g is introduced as the gravitational field at the surface of Earth in Newton/kilogram. This may or may not be related to GM/R2 according to the level of the course. If the concept of a field is not required, g can be called the strength or intensity of gravity. The gravitational field (or the strength of gravity) at a point can be defined as the force in Newtons experienced by each kilogram of mass placed there. It is not hard to see that m kg x g N/kg gives w N. Because this is analogous to how we deal with forces on electric charges in an electric field it also makes pedagogical sense.
Applying Newton’s second law to a body at Earth’s surface shows that, when w = mg is the net force, the acceleration of the body, in m/s2 is numerically equal to the strength of the field in Newton/kilogram. This is free fall. In all other cases, the net force is different from w and the acceleration is different from the acceleration in free fall. In other words, the acceleration in free fall is both a consequence of the strength of the gravitational field and a special case.
Away from Earth’s surface, there really is no satisfactory way to arrive at the acceleration of a body in free fall except through the strength of the gravitational field there. For example, at the surface of the Moon, g=1.6 N/kg, so the acceleration of a body in free fall is 1.6 m/s2.
There are probably two reasons why it has become conventional to define g as an acceleration rather than as a field strength. One is that most introductory textbooks cover kinematics before dynamics and use examples of bodies taken to be falling freely, often including projectiles. Having introduced a value for the acceleration in free fall and attributed it to gravity, it then becomes “the acceleration due to gravity” in all that follows. The other is that it is possible to obtain a quite reasonable value for this acceleration experimentally. To be logically and pedagogically sound, we should quote g in Newton/kilogram, refer to “the acceleration in free fall,” and mothball the expression “acceleration due to gravity.”
References
1. Editorial comment, “Quibbles, misunderstandings and egregious mistakes,” Phys. Teach. 37, 297 (1999).
2. If the table is on a rotating Earth it is not in equilibrium.