review feedback

Author: VeckoTheGecko

docs/examples/tutorial_peninsula_AvsCgrid.ipynb

@@ -11,7 +11,7 @@
    "cell_type": "markdown",
    "metadata": {},
    "source": [
-    "The notebook below shows how sensitive trajectories are to the combination of grid and velocity interpolation schemes. We will use the Peninsula example (also discussed in the [Quickstart to Parcels tutorial](https://docs.oceanparcels.org/en/latest/examples/parcels_tutorial.html#Sampling-a-Field-with-Particles)), but carefully compare how trajectories on the [A-grid and C-grid](https://docs.oceanparcels.org/en/latest/examples/documentation_indexing.html) version of this flow differ. To enhance the differences, we deliberately use a very course-resolution grid."
+    "The notebook below shows how sensitive trajectories are to the combination of grid and velocity interpolation schemes. We will use the Peninsula example (also discussed in the [Quickstart to Parcels tutorial](https://docs.oceanparcels.org/en/latest/examples/parcels_tutorial.html#Sampling-a-Field-with-Particles)), and carefully compare how trajectories on the [A-grid and C-grid](https://docs.oceanparcels.org/en/latest/examples/documentation_indexing.html) version of this flow differ. To enhance the differences, we deliberately use a very coarse-resolution grid."
    ]
   },
   {
@@ -36,7 +36,7 @@
    "cell_type": "markdown",
    "metadata": {},
    "source": [
-    "We start with defining the `FieldSet` for the Peninsula flow and the grid. Note that on the A-grid we can directly calculate the velocities on the grid pints from the streamfunction `P`. On the C-grid, we need to differentiate the streamfunction `P` to get the velocities on the staggered `U` and `V` grid points."
+    "We start with defining the `FieldSet` for the Peninsula flow and the grid. Note that on the A-grid we can directly calculate the velocities on the grid points from the streamfunction `P`. On the C-grid, we need to differentiate the streamfunction `P` to get the velocities on the staggered `U` and `V` grid points."
    ]
   },
   {
@@ -230,7 +230,7 @@
    "cell_type": "markdown",
    "metadata": {},
    "source": [
-    "Then, we finally plot the trajectories for all six experiments. We see that the trajectories are very sensitive to the combination of grid and velocity interpolation scheme. Note for example that using `cgrid_velocity` interpolation on an A-grid (fifth panel) leads to particles getting grounded on the land, which is not physical."
+    "Finally, we plot the trajectories for all six experiments. We see that the trajectories are very sensitive to the combination of grid and velocity interpolation scheme. Note for example that using `cgrid_velocity` interpolation on an A-grid (fifth panel) leads to particles getting grounded on the land, which is not physical."
    ]
   },
   {
@@ -291,7 +291,7 @@
    "cell_type": "markdown",
    "metadata": {},
    "source": [
-    "Because we know that Particles have to follow lines of constant streamfunction, we can also plot the streamlines of the flow field. When we overlay the \"Agrid & linear interpolation\" and \"Cgrid & cgrid interpolation\" trajectories onto these streamlines, we see that they are subtly different."
+    "Because we know that particles must follow lines of constant streamfunction, we can also plot the streamlines of the flow field. When we overlay the \"Agrid & linear interpolation\" and \"Cgrid & cgrid interpolation\" trajectories onto these streamlines, we see that they are subtly different."
    ]
   },
   {
@@ -410,7 +410,7 @@
  ],
  "metadata": {
   "kernelspec": {
-   "display_name": "parcels",
+   "display_name": "parcels-dev",
    "language": "python",
    "name": "python3"
   },
@@ -424,7 +424,7 @@
    "name": "python",
    "nbconvert_exporter": "python",
    "pygments_lexer": "ipython3",
-   "version": "3.12.3"
+   "version": "3.10.15"
   }
  },
  "nbformat": 4,