Concluded changes for September 2019 release.

ceos-seo · Oct 1, 2019 · a79af7b · a79af7b
1 parent 850eee9
commit a79af7b
Show file tree

Hide file tree

Showing 31 changed files with 5,672 additions and 8,545 deletions.
diff --git a/Chunking_Demo_Notebook_WOFS.ipynb b/Chunking_Demo_Notebook_WOFS.ipynb
diff --git a/Clustering_Notebook.ipynb b/Clustering_Notebook.ipynb
diff --git a/Coastal_Change_Classifier.ipynb b/Coastal_Change_Classifier.ipynb
diff --git a/Coastline_Classifier.ipynb b/Coastline_Classifier.ipynb
diff --git a/Composites_and_Shapefiles.ipynb b/Composites_and_Shapefiles.ipynb
diff --git a/DCAL/DCAL_Cloud_Statistics.ipynb b/DCAL/DCAL_Cloud_Statistics.ipynb
diff --git a/DCAL/DCAL_Custom_Mosaics.ipynb b/DCAL/DCAL_Custom_Mosaics.ipynb
diff --git a/DCAL/DCAL_Vegetation_Phenology.ipynb b/DCAL/DCAL_Vegetation_Phenology.ipynb
diff --git a/DCAL/DCAL_Water_Extents.ipynb b/DCAL/DCAL_Water_Extents.ipynb
diff --git a/Demo_Notebook.ipynb b/Demo_Notebook.ipynb
diff --git a/Export.ipynb b/Export.ipynb
diff --git a/GeoMedians+and+GeoMedoids+Compositing.ipynb b/GeoMedians+and+GeoMedoids+Compositing.ipynb
diff --git a/slip.ipynb → Landslide_Identification_SLIP.ipynb b/slip.ipynb → Landslide_Identification_SLIP.ipynb
@@ -272,14 +272,15 @@
    "cell_type": "markdown",
    "metadata": {},
    "source": [
-    "It is important to note that compositing will shorten the length of `baseline`'s time domain by the window size.(Since ranges less than the composite size are not computed). For a composite size of 5, `new`'s first 5 time values will not have composite values.  \n",
-    "<br>"
+    "It is important to note that compositing will shorten the length of `baseline`'s time domain by the window size.(Since ranges less than the composite size are not computed). For a composite size of 5, `new`'s first 5 time values will not have composite values.  "
    ]
   },
   {
    "cell_type": "code",
    "execution_count": 10,
-   "metadata": {},
+   "metadata": {
+    "scrolled": true
+   },
    "outputs": [
     {
      "data": {
@@ -300,7 +301,6 @@
    "cell_type": "markdown",
    "metadata": {},
    "source": [
-    "<br>\n",
     "#### What this composite looks like "
    ]
   },
@@ -415,12 +415,9 @@
    "cell_type": "markdown",
    "metadata": {},
    "source": [
-    "<br>\n",
     "#### How far NDWI filtering gets you  \n",
     "\n",
-    "A SLIP product is the result of a process of elimination.  NDWI is sufficient in eliminating a majority of non-contending areas early on in the process. Featured below is what is left of the original image after having filtered for changes in NDWI  \n",
-    "\n",
-    "<br>\n"
+    "A SLIP product is the result of a process of elimination.  NDWI is sufficient in eliminating a majority of non-contending areas early on in the process. Featured below is what is left of the original image after having filtered for changes in NDWI  "
    ]
   },
   {
@@ -477,7 +474,6 @@
    "cell_type": "markdown",
    "metadata": {},
    "source": [
-    "<br><br>\n",
     "The code is just as simple:"
    ]
   },
@@ -494,7 +490,6 @@
    "cell_type": "markdown",
    "metadata": {},
    "source": [
-    "<br>\n",
     "#### Filtering for RED reflectance increase\n",
     "Filtering RED reflectance change is just like the piecewise transformation used for filtering NDWI change.  \n",
     "  \n",
@@ -524,12 +519,8 @@
    "cell_type": "markdown",
    "metadata": {},
    "source": [
-    "<br>\n",
-    "\n",
     "#### How much further RED reflectance filtering gets you\n",
-    "Continuing SLIP's process of elimination, *Red increase* filtering will further refine the area of interest to areas that, upon visual inspection appear to be light brown in color.  \n",
-    "\n",
-    "<br><br>"
+    "Continuing SLIP's process of elimination, *Red increase* filtering will further refine the area of interest to areas that, upon visual inspection appear to be light brown in color.  "
    ]
   },
   {
@@ -556,7 +547,6 @@
    "cell_type": "markdown",
    "metadata": {},
    "source": [
-    "<br><br>  \n",
     "----\n",
     "\n",
     "## ASTER Global Elevation Models\n",
@@ -568,8 +558,7 @@
    "cell_type": "markdown",
    "metadata": {},
    "source": [
-    "#### Loading the elevation model  \n",
-    "<br>"
+    "#### Loading the elevation model  "
    ]
   },
   {
@@ -588,7 +577,6 @@
    "cell_type": "markdown",
    "metadata": {},
    "source": [
-    "<br>\n",
     "#### Calculating Angle of elevation   \n",
     "\n",
     "A gradient is generated for each pixel using the four pixels adjacent to it, as well as a rise/run formuala. \n",
@@ -611,8 +599,7 @@
     "  \n",
     "  <br><br>  \n",
     "  \n",
-    "The vagaries of implementation have been abstracted away by `dc_demutils`. It's used to derive a slope-mask. A slope-mask in this sense, is an array of `true` and `false` values based on whether or not that pixel meets a minimum angle of elevation requirement.  Its use is detailed below.  \n",
-    "<br><br>"
+    "The vagaries of implementation have been abstracted away by `dc_demutils`. It's used to derive a slope-mask. A slope-mask in this sense, is an array of `true` and `false` values based on whether or not that pixel meets a minimum angle of elevation requirement.  Its use is detailed below.  "
    ]
   },
   {
@@ -630,7 +617,6 @@
    "cell_type": "markdown",
    "metadata": {},
    "source": [
-    "<br>\n",
     "#### Filtering out pixels that don't meet requirements for steepness\n",
     "<br>\n",
     "Filtering based on slope is a peicewise transformation using a derived slopemask:   \n",
@@ -661,18 +647,14 @@
    "cell_type": "markdown",
    "metadata": {},
    "source": [
-    "<br><br>\n",
     "#### Visualising our final SLIP product"
    ]
   },
   {
    "cell_type": "markdown",
    "metadata": {},
    "source": [
-    "\n",
-    "The final results of SLIP are small regions of points with a high likelihood of landslides having occurred on them. Furthermore there is no possibility that detections are made in flat areas(areas with less than a $15^{\\circ}$ angle of elevation.  \n",
-    "  \n",
-    "<br>"
+    "The final results of SLIP are small regions of points with a high likelihood of landslides having occurred on them. Furthermore there is no possibility that detections are made in flat areas(areas with less than a $15^{\\circ}$ angle of elevation.  "
    ]
   },
   {
@@ -699,7 +681,6 @@
    "cell_type": "markdown",
    "metadata": {},
    "source": [
-    "<br><br>  \n",
     "## Reviewing the evolution of the SLIP product\n",
     "\n",
     "The following visualizations will detail the evolution of the SLIP product from the previous steps."
@@ -792,7 +773,7 @@
    "name": "python",
    "nbconvert_exporter": "python",
    "pygments_lexer": "ipython3",
-   "version": "3.5.2"
+   "version": "3.6.7"
   }
  },
  "nbformat": 4,