I want to know that the difference is between the following equations:
$$ \frac{\delta h_d}{\delta t} = -\nabla.(\vec{v_s} h_d) = -u_s(\frac{\delta h_d}{\delta x}) -v_s(\frac{\delta h_d}{\delta y}) - h_d(\frac{\delta u_s}{\delta x}) - h_d(\frac{\delta v_s}{\delta y})$$
$$ \frac{\delta h_d}{\delta t} = -\vec{v_s}.\nabla(h_d) = -u_s(\frac{\delta h_d}{\delta x}) -v_s(\frac{\delta h_d}{\delta y})$$
Here, $\vec{v_s}$ is the 2D velocity vector with components $u_s$ and $v_s$, and $h_d$ the thickness of a rock layer that is being advected. How does the addition of the last 2 terms in the first equation change the physical meaning of the equation? Does it make a ddifference if the velocity field is constant or non-constant in time?