Deploy preview for PR 114 🛫

Author: malmans2

pr-preview/pr-114/Satellite_ECVs/Cryosphere/satellite_satellite-sea-ice-edge-type_intercomparison_q01.html

@@ -481,11 +481,14 @@ <h2>❓ Quality assessment question<a class="headerlink" href="#quality-assessme
 </section>
 <section id="quality-assessment-statement">
 <h2>📢 Quality assessment statement<a class="headerlink" href="#quality-assessment-statement" title="Link to this heading">#</a></h2>
+<div class="admonition-these-are-the-key-outcomes-of-this-assessment admonition">
+<p class="admonition-title">These are the key outcomes of this assessment</p>
 <ul class="simple">
 <li><p>Both the CDS and the NERSC datasets reveal an overall decrease in multi-year sea ice extent over Arctic since 1991, with the most significant reductions occurring in the Beaufort Sea, the Chukchi Sea, and the Eurasian Basin.</p></li>
 <li><p>Despite their consistent conclusion, notable differences exist between the two datasets. Specifically, the CDS dataset tends to overestimate multi-year sea ice presence in the Beaufort Sea and underestimate it in the Greenland Sea when compared to the NERSC dataset. It is shown that these discrepancies tend to be minimum in October and to become more pronounced as each winter progresses.</p></li>
 <li><p>The inclusion of ‘ambiguous’ data points in the CDS dataset has two main implications on the estimates of multi-year sea ice extent in the Arctic. At first, it affects the total amount of multi-year sea ice in the region, even though it only little alters its geographic distribution. Secondly, it increases its day-to-day variability.</p></li>
 </ul>
+</div>
 </section>
 <section id="methodology">
 <h2>📋 Methodology<a class="headerlink" href="#methodology" title="Link to this heading">#</a></h2>

pr-preview/pr-114/_sources/Satellite_ECVs/Cryosphere/satellite_satellite-sea-ice-edge-type_intercomparison_q01.ipynb

@@ -2,7 +2,7 @@
  "cells": [
   {
    "cell_type": "markdown",
-   "id": "0b61e87b",
+   "id": "c2e5e6ba",
    "metadata": {
     "tags": []
    },
@@ -12,7 +12,7 @@
   },
   {
    "cell_type": "markdown",
-   "id": "29793f13",
+   "id": "78158632",
    "metadata": {
     "tags": [
      "disclaimer"
@@ -82,11 +82,13 @@
    "source": [
     "## 📢 Quality assessment statement\n",
     "\n",
+    "```{admonition} These are the key outcomes of this assessment\n",
     "* Both the CDS and the NERSC datasets reveal an overall decrease in multi-year sea ice extent over Arctic since 1991, with the most significant reductions occurring in the Beaufort Sea, the Chukchi Sea, and the Eurasian Basin. \n",
     "\n",
     "* Despite their consistent conclusion, notable differences exist between the two datasets. Specifically, the CDS dataset tends to overestimate multi-year sea ice presence in the Beaufort Sea and underestimate it in the Greenland Sea when compared to the NERSC dataset. It is shown that these discrepancies tend to be minimum in October and to become more pronounced as each winter progresses. \n",
     "\n",
-    "* The inclusion of ‘ambiguous’ data points in the CDS dataset has two main implications on the estimates of multi-year sea ice extent in the Arctic. At first, it affects the total amount of multi-year sea ice in the region, even though it only little alters its geographic distribution. Secondly, it increases its day-to-day variability. "
+    "* The inclusion of ‘ambiguous’ data points in the CDS dataset has two main implications on the estimates of multi-year sea ice extent in the Arctic. At first, it affects the total amount of multi-year sea ice in the region, even though it only little alters its geographic distribution. Secondly, it increases its day-to-day variability.\n",
+    "```"
    ]
   },
   {

pr-preview/pr-114/_sources/templates/template.ipynb

@@ -2,7 +2,7 @@
  "cells": [
   {
    "cell_type": "markdown",
-   "id": "ed6a992f",
+   "id": "55cbb42e",
    "metadata": {
     "tags": []
    },
@@ -12,7 +12,7 @@
   },
   {
    "cell_type": "markdown",
-   "id": "63cb4751",
+   "id": "7b9a2f30",
    "metadata": {
     "tags": [
      "disclaimer"