minor cosmetic fixes to recently updated tutorials

Author: andrewdelman

ECCO-ACCESS/Cloud_access_to_ECCO_datasets/Tutorial_AWS_Cloud_getting_started.ipynb

@@ -1618,8 +1618,7 @@
        "</svg>\n",
        "        </td>\n",
        "    </tr>\n",
-       "</table></div></li></ul></div></li><li class='xr-section-item'><input id='section-4534c482-4856-4a5b-9904-7c17d494a600' class='xr-section-summary-in' type='checkbox'  checked><label for='section-4534c482-4856-4a5b-9904-7c17d494a600' class='xr-section-summary' >Data variables: <span>(2)</span></label><div class='xr-section-inline-details'></div><div class='xr-section-details'><ul class='xr-var-list'><li class='xr-var-item'><div class='xr-var-name'><span>THETA</span></div><div class='xr-var-dims'>(time, k, tile, j, i)</div><div class='xr-var-dtype'>float32</div><div class='xr-var-preview xr-preview'>dask.array&lt;chunksize=(1, 10, 13, 90, 90), meta=np.ndarray&gt;</div><input id='attrs-c7db93d0-a65f-4b24-94ab-5c7ef12c907f' class='xr-var-attrs-in' type='checkbox' ><label for='attrs-c7db93d0-a65f-4b24-94ab-5c7ef12c907f' title='Show/Hide attributes'><svg class='icon xr-icon-file-text2'><use xlink:href='#icon-file-text2'></use></svg></label><input id='data-fe191852-2135-4ae3-81bc-b68085a9b730' class='xr-var-data-in' type='checkbox'><label for='data-fe191852-2135-4ae3-81bc-b68085a9b730' title='Show/Hide data repr'><svg class='icon xr-icon-database'><use xlink:href='#icon-database'></use></svg></label><div class='xr-var-attrs'><dl class='xr-attrs'><dt><span>long_name :</span></dt><dd>Potential temperature </dd><dt><span>units :</span></dt><dd>degree_C</dd><dt><span>coverage_content_type :</span></dt><dd>modelResult</dd><dt><span>standard_name :</span></dt><dd>sea_water_potential_temperature</dd><dt><span>comment :</span></dt><dd>Sea water potential temperature is the temperature a parcel of sea water would have if moved adiabatically to sea level pressure. Note: the equation of state is a modified UNESCO formula by Jackett and McDougall (1995), which uses the model variable potential temperature as input assuming a horizontally and temporally constant pressure of $p_0=-g \r",
-       "ho_{0} z$.</dd><dt><span>valid_min :</span></dt><dd>-2.2909388542175293</dd><dt><span>valid_max :</span></dt><dd>36.032955169677734</dd></dl></div><div class='xr-var-data'><table>\n",
+       "</table></div></li></ul></div></li><li class='xr-section-item'><input id='section-4534c482-4856-4a5b-9904-7c17d494a600' class='xr-section-summary-in' type='checkbox'  checked><label for='section-4534c482-4856-4a5b-9904-7c17d494a600' class='xr-section-summary' >Data variables: <span>(2)</span></label><div class='xr-section-inline-details'></div><div class='xr-section-details'><ul class='xr-var-list'><li class='xr-var-item'><div class='xr-var-name'><span>THETA</span></div><div class='xr-var-dims'>(time, k, tile, j, i)</div><div class='xr-var-dtype'>float32</div><div class='xr-var-preview xr-preview'>dask.array&lt;chunksize=(1, 10, 13, 90, 90), meta=np.ndarray&gt;</div><input id='attrs-c7db93d0-a65f-4b24-94ab-5c7ef12c907f' class='xr-var-attrs-in' type='checkbox' ><label for='attrs-c7db93d0-a65f-4b24-94ab-5c7ef12c907f' title='Show/Hide attributes'><svg class='icon xr-icon-file-text2'><use xlink:href='#icon-file-text2'></use></svg></label><input id='data-fe191852-2135-4ae3-81bc-b68085a9b730' class='xr-var-data-in' type='checkbox'><label for='data-fe191852-2135-4ae3-81bc-b68085a9b730' title='Show/Hide data repr'><svg class='icon xr-icon-database'><use xlink:href='#icon-database'></use></svg></label><div class='xr-var-attrs'><dl class='xr-attrs'><dt><span>long_name :</span></dt><dd>Potential temperature </dd><dt><span>units :</span></dt><dd>degree_C</dd><dt><span>coverage_content_type :</span></dt><dd>modelResult</dd><dt><span>standard_name :</span></dt><dd>sea_water_potential_temperature</dd><dt><span>comment :</span></dt><dd>Sea water potential temperature is the temperature a parcel of sea water would have if moved adiabatically to sea level pressure. Note: the equation of state is a modified UNESCO formula by Jackett and McDougall (1995), which uses the model variable potential temperature as input assuming a horizontally and temporally constant pressure of $p_0=-g \\rho_{0} z$.</dd><dt><span>valid_min :</span></dt><dd>-2.2909388542175293</dd><dt><span>valid_max :</span></dt><dd>36.032955169677734</dd></dl></div><div class='xr-var-data'><table>\n",
        "    <tr>\n",
        "        <td>\n",
        "            <table style=\"border-collapse: collapse;\">\n",

Tutorials_as_Jupyter_Notebooks/ECCO_v4_Coordinates_and_Dimensions_of_ECCOv4_NetCDF_files.ipynb

@@ -65,7 +65,7 @@
     "## ================\n",
     "\n",
     "\n",
-    "# indicate whether the notebook is being run on an AWS Cloud instance (True if running on a cloud instance, False otherwise)\n",
+    "# indicate whether you are working in a cloud instance (True if yes, False otherwise)\n",
     "incloud_access = False\n",
     "\n",
     "\n",

Tutorials_as_Jupyter_Notebooks/ECCO_v4_Gradient_calc_on_native_grid.ipynb

@@ -70,7 +70,7 @@
     "import warnings\n",
     "\n",
     "\n",
-    "# set incloud_access = True if accessing ECCO datasets from an EC2 instance in the cloud, otherwise False\n",
+    "# indicate whether you are working in a cloud instance (True if yes, False otherwise)\n",
     "incloud_access = False\n",
     "\n",
     "\n",

Tutorials_as_Jupyter_Notebooks/ECCO_v4_data_structure_basics.ipynb

@@ -135,7 +135,7 @@
     }
    ],
    "source": [
-    "# indicate whether you are working in the cloud\n",
+    "# indicate whether you are working in a cloud instance (True if yes, False otherwise)\n",
     "incloud_access = False\n",
     "\n",
     "\n",