Step 1: Recall the physical origin of the Grashof number.
The Grashof number, Gr, is a dimensionless group that arises in free (natural) convection heat transfer problems, where fluid motion is driven purely by density differences caused by temperature gradients, without any externally imposed velocity. It plays the same role in natural convection that the Reynolds number plays in forced convection.
Step 2: Write the defining expression and identify each force.
For a characteristic length L, the Grashof number is defined as Gr = g beta Delta T L^3 / nu^2, where g is gravitational acceleration, beta is the volumetric thermal expansion coefficient, Delta T is the temperature difference driving the flow, and nu is the kinematic viscosity. This can be interpreted physically as Gr ~ (buoyancy force)/(viscous force).
Step 3: Contrast with the other options.
Option (A), buoyancy to inertia force, is closer to an intermediate ratio used only inside the derivation. Option (C), viscous to capillary force, is closer to the Capillary number. Option (D), viscous to inertia force, is essentially the inverse-style comparison used inside the Reynolds number.
Step 4: Conclude.
By its standard physical definition used throughout heat transfer texts, the Grashof number represents the ratio of buoyancy force to viscous force acting on the fluid.
\[ \boxed{Gr = \dfrac{\text{buoyancy force}}{\text{viscous force}} \ \text{(option B)}} \]