Remove last comments

docs/src/model_docs/lateral/gwf.md

@@ -153,7 +153,7 @@ MODFLOW:
     \end{cases}
   \end{align*}
 ```
-<!-- It seems rather inconsistent to use units everywhere and then suddenly use dimensions instead here. -->
+
 where ``\SIb{\subtext{Q}{riv}}{L^3 T^{-1}}`` is the exchange flux from river to aquifer, ``\SIb{C_i}{L^2 T^{-1}}`` is the river bed infiltration conductance, ``\SIb{C_e}{L^2 T^{-1}}``
 is the river bed exfiltration conductance, ``\SIb{\subtext{B}{riv}}{L}`` the bottom of the river bed,
 ``\SIb{\subtext{h}{riv}}{L}`` is the river stage and ``\SIb{\phi}{L}`` is the hydraulic head in the river cell.

docs/src/model_docs/lateral/local-inertial.md

@@ -106,7 +106,6 @@ Q_{i-1/2}^{n+1} = \frac{\left[ \theta Q_{i-1/2}^{n} +\frac{(1-\theta)}{2}(Q_{(i-
    n^2 |Q_{i-1/2}^{n}|/(h_f^{7/3} \Delta y)}
 ```
 
-<!-- n is used both as a time index and as the Manning roughness coefficient! -->
 where subscripts ``i`` and ``n`` refer to space and time indices, respectively. Subscript
 ``i-\frac{1}{2}`` is to the link between node ``i`` and ``i-1``, subscript ``i+\frac{1}{2}`` is the link
 between node ``i`` and node ``i+1``, and subscript ``i-\frac{3}{2}`` is the link between node ``i-1``