Update link to remote datasets

009_paper_GR2020/pygmt_jn_fig_4/GR_2020_Fig_4.ipynb

@@ -32,7 +32,7 @@
  {
  "data": {
  "text/plain": [
- "<pygmt.src.config.config at 0x1a3587f0f50>"
+ "<pygmt.src.config.config at 0x1a70d16cb90>"
  ]
  },
  "execution_count": 1,
@@ -79,8 +79,8 @@
  "cell_type": "markdown",
  "metadata": {},
  "source": [
- "Next we define the map content and plot an elevation grid as background using the `grdimage` function.\n",
- "* Here we can directly access the elevation grid via PyGMT by defining the desired resolution (`'@earth_relief_01m'`, corresponds to ETOPO1 data). Afterwards the required grid of the area is automatically extracted based on the defined region limits (`region = [3.5, 36.5, 54, 71.5]`). The first time you access an elevation grid file it will be downloaded from the GMT server and stored under your GMT user directory. Then the grid file is read from there. For further details see http:https://gmt.soest.hawaii.edu/doc/latest/datasets.html.\n",
+ "Next we define the map content and plot an elevation grid as background using the `grdimage` method.\n",
+ "* Here we can directly access the elevation grid via PyGMT by defining the desired resolution (`'@earth_relief_01m'`, corresponds to ETOPO1 data). Afterwards the required grid of the area is automatically extracted based on the defined region limits (`region = [3.5, 36.5, 54, 71.5]`). The first time you access an elevation grid file it will be downloaded from the GMT server and stored under your GMT user directory. Then the grid file is read from there. For further details see https:https://www.generic-mapping-tools.org/remote-datasets/.\n",
  "* We use an Albers conic equal-area projection via `projection = 'l20/60/16/80/1:10000000'`.\n",
  "* The background is colored by using the colormap `gray.cpt` and shading is set to `True`."
  ]