Merge pull request #12 from RyuLandA24/add-new-notebook

Hope this is right.
ProjectPythia · May 24, 2024 · 2cb3fd5 · 2cb3fd5
2 parents 86878a0 + 5ea9e25
commit 2cb3fd5
Showing 1 changed file with 8 additions and 11 deletions.
diff --git a/KR_Project.ipynb → notebooks/ForcingLTKE.ipynb b/KR_Project.ipynb → notebooks/ForcingLTKE.ipynb
@@ -3,13 +3,11 @@
   {
    "cell_type": "markdown",
    "id": "e760bf9f-4601-4521-9f4c-c2be10101c18",
-   "metadata": {},
+   "metadata": {
+    "jp-MarkdownHeadingCollapsed": true
+   },
    "source": [
-    "# The impact of large-scale forcing scales on clouds.\n",
-    "\n",
-    "# Feel free to add your insights to my approach!\n",
-    "# It is fun to learn new things!\n",
-    "# May 22, 2024"
+    "# The impact of large-scale forcing scales on clouds.\n"
    ]
   },
   {
@@ -742,7 +740,7 @@
    "id": "079f44d4-a9d8-4a30-9c34-089a642497e0",
    "metadata": {},
    "source": [
-    "# cloud core fraction profiles"
+    "# Cloud Core Fraction Profiles"
    ]
   },
   {
@@ -781,12 +779,11 @@
    "id": "56c3c08f-b177-4647-a6f0-c584139d1496",
    "metadata": {},
    "source": [
-    "# Based on the above figures, We can see that Simulation 6 produces more cloud core fractions, and Simulation 7 is the closest one to the observation. What we learned today. \n",
-    "\n",
+    "## Based on the above figures, We can see that Simulation 6 produces more cloud core fractions, and Simulation 7 is the closest one to the observation. What we learned today. \n",
     "\n",
-    "# Based on them, I assume the different large-scale forcing lengths impact turbulence and thus cloud core fraction.\n",
+    "## Based on them, I assume the different large-scale forcing lengths impact turbulence and thus cloud core fraction.\n",
     "\n",
-    "# I know you all know this, but just to recap, TKE is the turbulent kinematic energy and thus it is the energy for turbulence from the surface to the atmospheric boundary layer. TKE = (U^2 + V^2 + W^2)/2\n"
+    "## I know you all know this, but just to recap, TKE is the turbulent kinematic energy and thus it is the energy for turbulence from the surface to the atmospheric boundary layer. TKE = (U^2 + V^2 + W^2)/2\n"
    ]
   },
   {