Update documentation

ecmwf-projects · Dec 9, 2024 · ffb984f · ffb984f
1 parent 44aaa57
commit ffb984f
Show file tree

Hide file tree

Showing 24 changed files with 42 additions and 60 deletions.
diff --git a/_sources/cds-tutorial.ipynb b/_sources/cds-tutorial.ipynb
@@ -106,8 +106,8 @@
    "metadata": {},
    "source": [
     "There are two ways to access data from the Copernicus Climate Data Store (CDS):\n",
-    "* [interactively](#access_manual) via the CDS web interface, or\n",
-    "* [programmatically](#access_programmatic) with the CDS API"
+    "* interactively via the CDS web interface, or\n",
+    "* programmatically with the CDS API"
    ]
   },
   {
@@ -196,7 +196,7 @@
     "**Note:** You need to be logged into the ADS portal and you have to accept the Terms and Conditions of the dataset before being able to download data.\n",
     "\n",
     "\n",
-    "You will need the `Show API request`, if you want to request data programmatically. See [Section 2.2](#access_programmatic) for further information. You will need the `Show Toolbox request`  if you want to request data via the CDS Toolbox. Learn more about the CDS Toolbox [here](https://cds.climate.copernicus.eu/cdsapp#!/toolbox).\n"
+    "You will need the `Show API request`, if you want to request data programmatically. See Section 2.2 for further information. You will need the `Show Toolbox request`  if you want to request data via the CDS Toolbox. Learn more about the CDS Toolbox [here](https://cds.climate.copernicus.eu/cdsapp#!/toolbox).\n"
    ]
   },
   {
@@ -435,13 +435,6 @@
     "#### Example: **ERA5-Land hourly data from 1950 to present**"
    ]
   },
-  {
-   "cell_type": "markdown",
-   "metadata": {},
-   "source": [
-    "> Data used in [113_c3s_climate_indices](./113_c3s_climate_indices.ipynb)"
-   ]
-  },
   {
    "cell_type": "markdown",
    "metadata": {},

diff --git a/_sources/ecv-notebooks/erb-outgoing-longwave-radiation.ipynb b/_sources/ecv-notebooks/erb-outgoing-longwave-radiation.ipynb
@@ -477,7 +477,7 @@
     "December 2018. The maximum values of the OLR are found in the tropics and it decreases toward the\n",
     "poles. The relative minimum near the equator, in yellow colour, corresponds to the ITCZ and the\n",
     "convection areas, where persistent and relatively high cloud cover reduces the LW radiation at the\n",
-    "TOA. Antarctica is cooler than the corresponding northern latitudes ([Harrison et al.](#harrison))."
+    "TOA. Antarctica is cooler than the corresponding northern latitudes (Harrison et al.)."
    ]
   },
   {
@@ -684,7 +684,7 @@
     "**Figure 3**, shows the evolution of the OLR in the Arctic region [70°N-90°N] for the period 1979-2019\n",
     "also using a yearly rolling mean. From the image, we can infer an increase in the OLR in the Arctic\n",
     "region with time. This increase is strongly marked as from 1998 and in line with the increase of\n",
-    "temperature in the Arctic ([Hansen et al, 2010](#hansen)), while the relative stability of the first part of the time\n",
+    "temperature in the Arctic (Hansen et al, 2010), while the relative stability of the first part of the time\n",
     "series is more difficult to interpret due to the major volcanic eruptions in this period."
    ]
   },
@@ -710,13 +710,6 @@
     "\n",
     "Harrison, E.F., Gurney, R. J., Foster, J. L., Gurney, R. J., & Parkinson, C. L. (1993). _Atlas of satellite observations related to global change_. Chapter: Radiation Budget at the top of the atmosphere. Cambridge University Press."
    ]
-  },
-  {
-   "cell_type": "markdown",
-   "metadata": {},
-   "source": [
-    "[Back to top the Page](#page-top)"
-   ]
   }
  ],
  "metadata": {

diff --git a/_sources/ecv-notebooks/srb-climatology-and-anomaly.ipynb b/_sources/ecv-notebooks/srb-climatology-and-anomaly.ipynb
@@ -1996,7 +1996,7 @@
    "cell_type": "markdown",
    "metadata": {},
    "source": [
-    "Please note that you need to open the dataset to be able to execute this usecase, as described in the previous section [\"Load dataset\"](#load).\n",
+    "Please note that you need to open the dataset to be able to execute this usecase, as described in the previous load data section.\n",
     "\n",
     "The spatial resolution of the CLARA-A3 radiation dataset is 0.25ºx0.25º that is roughly equal to 25x25 km. With this resolution, it is possible to conduct a regional analysis using the CLARA-A3 radiation datasets. Furthermore, we can use the CLARA-A3 radiation datasets to investigate recent meteorological events. This could be a research project for a student or provide complementary information on a special event, e.g., the analysis of recent heat waves. In recent years, a high number of heat waves appeared in Europe. Particularly interesting is the summer 2003."
    ]
@@ -2049,7 +2049,7 @@
   },
   {
    "cell_type": "code",
-   "execution_count": null,
+   "execution_count": 16,
    "metadata": {},
    "outputs": [
     {

diff --git a/_sources/reanalysis-climatology.ipynb b/_sources/reanalysis-climatology.ipynb
@@ -1476,7 +1476,7 @@
    "source": [
     "## 4. Calculate monthly climatology and anomalies\n",
     "\n",
-    "We will now calculate the monthly climatology of near-surface air temperature for the period 1991 to 2020. We will also view the anomalies with respect to the climatology for a particular month. To do this, we return to the data array created at the end of [section 1](#search_download).\n",
+    "We will now calculate the monthly climatology of near-surface air temperature for the period 1991 to 2020. We will also view the anomalies with respect to the climatology for a particular month. To do this, we return to the data array created at the end of section 1.\n",
     "\n",
     "We first create again a temporal subset for the period 1991 to 2020, but this time keeping the monthly temporal resolution."
    ]
@@ -1811,7 +1811,7 @@
    "cell_type": "markdown",
    "metadata": {},
    "source": [
-    "We will repeat the steps in [section 1](#search_download) to read the data into an xarray data array:"
+    "We will repeat the steps in section 1 to read the data into an xarray data array:"
    ]
   },
   {
@@ -1829,7 +1829,7 @@
    "cell_type": "markdown",
    "metadata": {},
    "source": [
-    "We will also repeat the steps in [section 1](#search_download) to convert the values from degrees Kelvin to Celsius:"
+    "We will also repeat the steps in section 1 to convert the values from degrees Kelvin to Celsius:"
    ]
   },
   {

diff --git a/_sources/sf-anomalies.ipynb b/_sources/sf-anomalies.ipynb
diff --git a/cds-tutorial.html b/cds-tutorial.html
@@ -32,7 +32,7 @@
     <link rel="stylesheet" type="text/css" href="_static/styles/sphinx-book-theme.css?v=a3416100" />
     <link rel="stylesheet" type="text/css" href="_static/togglebutton.css?v=13237357" />
     <link rel="stylesheet" type="text/css" href="_static/copybutton.css?v=76b2166b" />
-    <link rel="stylesheet" type="text/css" href="_static/mystnb.4510f1fc1dee50b3e5859aac5469c37c29e427902b24a333a5f9fcb2f0b3ac41.css" />
+    <link rel="stylesheet" type="text/css" href="_static/mystnb.4510f1fc1dee50b3e5859aac5469c37c29e427902b24a333a5f9fcb2f0b3ac41.css?v=be8a1c11" />
     <link rel="stylesheet" type="text/css" href="_static/sphinx-thebe.css?v=4fa983c6" />
     <link rel="stylesheet" type="text/css" href="_static/sphinx-design.min.css?v=95c83b7e" />
 
@@ -526,8 +526,8 @@ <h2>About<a class="headerlink" href="#about" title="Link to this heading">#</a><
 <h2>Data retrieval<a class="headerlink" href="#data-retrieval" title="Link to this heading">#</a></h2>
 <p>There are two ways to access data from the Copernicus Climate Data Store (CDS):</p>
 <ul class="simple">
-<li><p><a class="reference internal" href="#access_manual"><span class="xref myst">interactively</span></a> via the CDS web interface, or</p></li>
-<li><p><a class="reference internal" href="#access_programmatic"><span class="xref myst">programmatically</span></a> with the CDS API</p></li>
+<li><p>interactively via the CDS web interface, or</p></li>
+<li><p>programmatically with the CDS API</p></li>
 </ul>
 <section id="access-data-interactively-via-the-cds-web-interface">
 <h3>Access data interactively via the CDS web interface<a class="headerlink" href="#access-data-interactively-via-the-cds-web-interface" title="Link to this heading">#</a></h3>
@@ -550,7 +550,7 @@ <h4>Submit the <em>Download data</em> form<a class="headerlink" href="#submit-th
 </ul>
 <p>At the end of the <code class="docutils literal notranslate"><span class="pre">&quot;Download</span> <span class="pre">data&quot;</span> <span class="pre">form</span></code>, you get three options: <code class="docutils literal notranslate"><span class="pre">Show</span> <span class="pre">API</span> <span class="pre">request</span></code>, <code class="docutils literal notranslate"><span class="pre">Show</span> <span class="pre">Toolbox</span> <span class="pre">request</span></code> and <code class="docutils literal notranslate"><span class="pre">Submit</span> <span class="pre">Form</span></code>. If you want to download the data interactively, the data requests will be executed as soon as you click on the <code class="docutils literal notranslate"><span class="pre">Submit</span> <span class="pre">Form</span></code> button.</p>
 <p><strong>Note:</strong> You need to be logged into the ADS portal and you have to accept the Terms and Conditions of the dataset before being able to download data.</p>
-<p>You will need the <code class="docutils literal notranslate"><span class="pre">Show</span> <span class="pre">API</span> <span class="pre">request</span></code>, if you want to request data programmatically. See <a class="reference internal" href="#access_programmatic"><span class="xref myst">Section 2.2</span></a> for further information. You will need the <code class="docutils literal notranslate"><span class="pre">Show</span> <span class="pre">Toolbox</span> <span class="pre">request</span></code>  if you want to request data via the CDS Toolbox. Learn more about the CDS Toolbox <a class="reference external" href="https://cds.climate.copernicus.eu/cdsapp#!/toolbox">here</a>.</p>
+<p>You will need the <code class="docutils literal notranslate"><span class="pre">Show</span> <span class="pre">API</span> <span class="pre">request</span></code>, if you want to request data programmatically. See Section 2.2 for further information. You will need the <code class="docutils literal notranslate"><span class="pre">Show</span> <span class="pre">Toolbox</span> <span class="pre">request</span></code>  if you want to request data via the CDS Toolbox. Learn more about the CDS Toolbox <a class="reference external" href="https://cds.climate.copernicus.eu/cdsapp#!/toolbox">here</a>.</p>
 <div class="alert alert-block alert-success">
 <b>NOTE</b>: <br>
     Under the tab <code>Your requests</code> in the main menu, you can monitor the status of your data requests.</div>
@@ -636,9 +636,6 @@ <h3>Further resources<a class="headerlink" href="#further-resources" title="Link
 <h2>Example data request<a class="headerlink" href="#example-data-request" title="Link to this heading">#</a></h2>
 <section id="example-era5-land-hourly-data-from-1950-to-present">
 <h3>Example: <strong>ERA5-Land hourly data from 1950 to present</strong><a class="headerlink" href="#example-era5-land-hourly-data-from-1950-to-present" title="Link to this heading">#</a></h3>
-<blockquote>
-<div><p>Data used in <a class="reference internal" href="#./113_c3s_climate_indices.ipynb"><span class="xref myst">113_c3s_climate_indices</span></a></p>
-</div></blockquote>
 <p>CDS API name: <code class="docutils literal notranslate"><span class="pre">reanalysis-era5-land</span></code></p>
 <blockquote>
 <div><ul class="simple">

diff --git a/ci-windchill.html b/ci-windchill.html
@@ -32,7 +32,7 @@
     <link rel="stylesheet" type="text/css" href="_static/styles/sphinx-book-theme.css?v=a3416100" />
     <link rel="stylesheet" type="text/css" href="_static/togglebutton.css?v=13237357" />
     <link rel="stylesheet" type="text/css" href="_static/copybutton.css?v=76b2166b" />
-    <link rel="stylesheet" type="text/css" href="_static/mystnb.4510f1fc1dee50b3e5859aac5469c37c29e427902b24a333a5f9fcb2f0b3ac41.css" />
+    <link rel="stylesheet" type="text/css" href="_static/mystnb.4510f1fc1dee50b3e5859aac5469c37c29e427902b24a333a5f9fcb2f0b3ac41.css?v=be8a1c11" />
     <link rel="stylesheet" type="text/css" href="_static/sphinx-thebe.css?v=4fa983c6" />
     <link rel="stylesheet" type="text/css" href="_static/sphinx-design.min.css?v=95c83b7e" />
 

diff --git a/ecv-notebooks/erb-outgoing-longwave-radiation.html b/ecv-notebooks/erb-outgoing-longwave-radiation.html
@@ -32,7 +32,7 @@
     <link rel="stylesheet" type="text/css" href="../_static/styles/sphinx-book-theme.css?v=a3416100" />
     <link rel="stylesheet" type="text/css" href="../_static/togglebutton.css?v=13237357" />
     <link rel="stylesheet" type="text/css" href="../_static/copybutton.css?v=76b2166b" />
-    <link rel="stylesheet" type="text/css" href="../_static/mystnb.4510f1fc1dee50b3e5859aac5469c37c29e427902b24a333a5f9fcb2f0b3ac41.css" />
+    <link rel="stylesheet" type="text/css" href="../_static/mystnb.4510f1fc1dee50b3e5859aac5469c37c29e427902b24a333a5f9fcb2f0b3ac41.css?v=be8a1c11" />
     <link rel="stylesheet" type="text/css" href="../_static/sphinx-thebe.css?v=4fa983c6" />
     <link rel="stylesheet" type="text/css" href="../_static/sphinx-design.min.css?v=95c83b7e" />
 
@@ -777,7 +777,7 @@ <h4>Plot data<a class="headerlink" href="#plot-data" title="Link to this heading
 December 2018. The maximum values of the OLR are found in the tropics and it decreases toward the
 poles. The relative minimum near the equator, in yellow colour, corresponds to the ITCZ and the
 convection areas, where persistent and relatively high cloud cover reduces the LW radiation at the
-TOA. Antarctica is cooler than the corresponding northern latitudes (<a class="reference internal" href="#harrison"><span class="xref myst">Harrison et al.</span></a>).</p>
+TOA. Antarctica is cooler than the corresponding northern latitudes (Harrison et al.).</p>
 </section>
 </section>
 <section id="use-case-2-global-time-series-of-the-olr">
@@ -912,7 +912,7 @@ <h3><strong>Use case 3</strong>: OLR evolution in the Arctic<a class="headerlink
 <p><strong>Figure 3</strong>, shows the evolution of the OLR in the Arctic region [70°N-90°N] for the period 1979-2019
 also using a yearly rolling mean. From the image, we can infer an increase in the OLR in the Arctic
 region with time. This increase is strongly marked as from 1998 and in line with the increase of
-temperature in the Arctic (<a class="reference internal" href="#hansen"><span class="xref myst">Hansen et al, 2010</span></a>), while the relative stability of the first part of the time
+temperature in the Arctic (Hansen et al, 2010), while the relative stability of the first part of the time
 series is more difficult to interpret due to the major volcanic eruptions in this period.</p>
 </section>
 </section>
@@ -927,7 +927,6 @@ <h2>Get more information about Earth Radiation Budget:<a class="headerlink" href
 <h2>References<a class="headerlink" href="#references" title="Link to this heading">#</a></h2>
 <p>Hansen, J., Ruedy, R., Sato, M., &amp; Lo, K., (2010). <em>Global surface temperature change</em>. Reviews of Geophysics, 48(4).</p>
 <p>Harrison, E.F., Gurney, R. J., Foster, J. L., Gurney, R. J., &amp; Parkinson, C. L. (1993). <em>Atlas of satellite observations related to global change</em>. Chapter: Radiation Budget at the top of the atmosphere. Cambridge University Press.</p>
-<p><a class="reference internal" href="#page-top"><span class="xref myst">Back to top the Page</span></a></p>
 </section>
 </section>
 

diff --git a/ecv-notebooks/srb-climatology-and-anomaly.html b/ecv-notebooks/srb-climatology-and-anomaly.html
@@ -32,7 +32,7 @@
     <link rel="stylesheet" type="text/css" href="../_static/styles/sphinx-book-theme.css?v=a3416100" />
     <link rel="stylesheet" type="text/css" href="../_static/togglebutton.css?v=13237357" />
     <link rel="stylesheet" type="text/css" href="../_static/copybutton.css?v=76b2166b" />
-    <link rel="stylesheet" type="text/css" href="../_static/mystnb.4510f1fc1dee50b3e5859aac5469c37c29e427902b24a333a5f9fcb2f0b3ac41.css" />
+    <link rel="stylesheet" type="text/css" href="../_static/mystnb.4510f1fc1dee50b3e5859aac5469c37c29e427902b24a333a5f9fcb2f0b3ac41.css?v=be8a1c11" />
     <link rel="stylesheet" type="text/css" href="../_static/sphinx-thebe.css?v=4fa983c6" />
     <link rel="stylesheet" type="text/css" href="../_static/sphinx-design.min.css?v=95c83b7e" />
 
@@ -2241,7 +2241,7 @@ <h3>Plot of the temporal average of SIS<a class="headerlink" href="#plot-of-the-
 </section>
 <section id="use-case-2-relative-anomaly-hot-summer-of-the-year-2003-in-europe">
 <h2>Use case 2: Relative Anomaly. Hot summer of the year 2003 in Europe<a class="headerlink" href="#use-case-2-relative-anomaly-hot-summer-of-the-year-2003-in-europe" title="Link to this heading">#</a></h2>
-<p>Please note that you need to open the dataset to be able to execute this usecase, as described in the previous section <a class="reference internal" href="#load"><span class="xref myst">“Load dataset”</span></a>.</p>
+<p>Please note that you need to open the dataset to be able to execute this usecase, as described in the previous load data section.</p>
 <p>The spatial resolution of the CLARA-A3 radiation dataset is 0.25ºx0.25º that is roughly equal to 25x25 km. With this resolution, it is possible to conduct a regional analysis using the CLARA-A3 radiation datasets. Furthermore, we can use the CLARA-A3 radiation datasets to investigate recent meteorological events. This could be a research project for a student or provide complementary information on a special event, e.g., the analysis of recent heat waves. In recent years, a high number of heat waves appeared in Europe. Particularly interesting is the summer 2003.</p>
 <p>Firstly, we will select the data for year 2003 using <code class="docutils literal notranslate"><span class="pre">sel</span></code> argument.</p>
 <p>Then, we split the SRB data according to the seasons by using the <code class="docutils literal notranslate"><span class="pre">groupby()</span></code> method, with <code class="docutils literal notranslate"><span class="pre">'time.season'</span></code> as an argument, and then averaged over the years.

diff --git a/ecv-notebooks/total-column-water-vapour-combi.html b/ecv-notebooks/total-column-water-vapour-combi.html
@@ -32,7 +32,7 @@
     <link rel="stylesheet" type="text/css" href="../_static/styles/sphinx-book-theme.css?v=a3416100" />
     <link rel="stylesheet" type="text/css" href="../_static/togglebutton.css?v=13237357" />
     <link rel="stylesheet" type="text/css" href="../_static/copybutton.css?v=76b2166b" />
-    <link rel="stylesheet" type="text/css" href="../_static/mystnb.4510f1fc1dee50b3e5859aac5469c37c29e427902b24a333a5f9fcb2f0b3ac41.css" />
+    <link rel="stylesheet" type="text/css" href="../_static/mystnb.4510f1fc1dee50b3e5859aac5469c37c29e427902b24a333a5f9fcb2f0b3ac41.css?v=be8a1c11" />
     <link rel="stylesheet" type="text/css" href="../_static/sphinx-thebe.css?v=4fa983c6" />
     <link rel="stylesheet" type="text/css" href="../_static/sphinx-design.min.css?v=95c83b7e" />
 

diff --git a/ecv-notebooks/total-ozone-columns.html b/ecv-notebooks/total-ozone-columns.html
@@ -32,7 +32,7 @@
     <link rel="stylesheet" type="text/css" href="../_static/styles/sphinx-book-theme.css?v=a3416100" />
     <link rel="stylesheet" type="text/css" href="../_static/togglebutton.css?v=13237357" />
     <link rel="stylesheet" type="text/css" href="../_static/copybutton.css?v=76b2166b" />
-    <link rel="stylesheet" type="text/css" href="../_static/mystnb.4510f1fc1dee50b3e5859aac5469c37c29e427902b24a333a5f9fcb2f0b3ac41.css" />
+    <link rel="stylesheet" type="text/css" href="../_static/mystnb.4510f1fc1dee50b3e5859aac5469c37c29e427902b24a333a5f9fcb2f0b3ac41.css?v=be8a1c11" />
     <link rel="stylesheet" type="text/css" href="../_static/sphinx-thebe.css?v=4fa983c6" />
     <link rel="stylesheet" type="text/css" href="../_static/sphinx-design.min.css?v=95c83b7e" />
 

diff --git a/genindex.html b/genindex.html
@@ -31,7 +31,7 @@
     <link rel="stylesheet" type="text/css" href="_static/styles/sphinx-book-theme.css?v=a3416100" />
     <link rel="stylesheet" type="text/css" href="_static/togglebutton.css?v=13237357" />
     <link rel="stylesheet" type="text/css" href="_static/copybutton.css?v=76b2166b" />
-    <link rel="stylesheet" type="text/css" href="_static/mystnb.4510f1fc1dee50b3e5859aac5469c37c29e427902b24a333a5f9fcb2f0b3ac41.css" />
+    <link rel="stylesheet" type="text/css" href="_static/mystnb.4510f1fc1dee50b3e5859aac5469c37c29e427902b24a333a5f9fcb2f0b3ac41.css?v=be8a1c11" />
     <link rel="stylesheet" type="text/css" href="_static/sphinx-thebe.css?v=4fa983c6" />
     <link rel="stylesheet" type="text/css" href="_static/sphinx-design.min.css?v=95c83b7e" />