diff --git a/notebooks/foundations/energy-balance-model.ipynb b/notebooks/foundations/energy-balance-model.ipynb
index 27a4e46..df07227 100644
--- a/notebooks/foundations/energy-balance-model.ipynb
+++ b/notebooks/foundations/energy-balance-model.ipynb
@@ -46,7 +46,7 @@
     "| TBD | Necessary | |\n",
     "\n",
     "\n",
-    "- **Time to learn**: 30 minutes?"
+    "- **Time to learn**: >30 minutes"
    ]
   },
   {
@@ -60,19 +60,7 @@
    "cell_type": "markdown",
    "metadata": {},
    "source": [
-    "## Imports\n",
-    "We will import commonly used scientific Python packages for this notebook."
-   ]
-  },
-  {
-   "cell_type": "code",
-   "execution_count": 8,
-   "metadata": {},
-   "outputs": [],
-   "source": [
-    "import numpy as np \n",
-    "import xarray as xr \n",
-    "import matplotlib.pyplot as plt "
+    "## Radiative Budget Analysis"
    ]
   },
   {
@@ -216,7 +204,9 @@
     "\n",
     "If we include the planetary emissivity $\\epsilon$, we will get $\\lambda_{Planck} \\approx -3.3Wm^{-2}K^{-1}$, which is close to observations {cite:p}`dessler:2013a` and global climate models {cite:p}`caldwell:2016a`). \n",
     "\n",
-    "Simply put, the more you heat, the more LW radiation go out.\n",
+    "**Simply put, the more you heat, the more LW radiation go out.**\n",
+    "\n",
+    "\n",
     "[TO BE POLISHED]\n",
     "*Kernel related: structural uncertainty in Planck feedback arises from differences in spatial pattern of surface warming and climatological distribution fo clodus and water vapor that determines planetary emissivity - affects radiative temperature kernel {cite:p}`sherwood:2020a`. \n",
     "\n",
@@ -285,7 +275,7 @@
    "cell_type": "markdown",
    "metadata": {},
    "source": [
-    "### 4. Cloud Feedback "
+    "### 5. Cloud Feedback "
    ]
   },
   {