diff --git a/storage/stories/story-16/story-16-de.json b/storage/stories/story-16/story-16-de.json
index 9fd741b5e..38b9aa9c4 100644
--- a/storage/stories/story-16/story-16-de.json
+++ b/storage/stories/story-16/story-16-de.json
@@ -5,7 +5,9 @@
       "type": "splashscreen",
       "text": "# Planetary Heat Pumps\r\n\r\nThe ocean and the atmosphere both redistribute energy around the planet. While it is the atmosphere that brings us our weather, the oceans can store much more heat, making them a more stable indicator of climate trends.",
       "shortText": "# Planetary Heat Pumps\r\n\r\nThe ocean and the atmosphere both redistribute energy around the planet. While it is the atmosphere that brings us our weather, the oceans can store much more heat, making them a more stable indicator of climate trends.",
-      "images": ["assets/sst.jpg"]
+      "images": [
+        "assets/sst.jpg"
+      ]
     },
     {
       "type": "image",
@@ -62,24 +64,24 @@
       "shortText": "## Fisherman’s Friend\r\n\r\nMaps of SST show where deep cold water is upwelling, bringing nutrients to the surface.\r\n\r\nModern fishing fleets use SST maps from satellites to help find and follow fish. \r\n\r\nThe interactive globe shows:\r\n\r\n- a comparison between SST and ocean chlorophyll (in phytoplankton)\r\n- high chlorophyll concentrations associated with areas of cold water upwelling off the coasts of Peru, Argentina and Namibia. \r\n\r\nPhytoplankton are the base of the oceanic food chain, but also play a key role in the climate by absorbing carbon dioxide through photosynthesis.",
       "flyTo": {
         "position": {
-          "longitude": -30.74,
-          "latitude": 23.32,
-          "height": 15145050.29
+          "longitude": -60.11,
+          "latitude": -19.14,
+          "height": 10614832.84
         },
         "orientation": {
           "heading": 360,
-          "pitch": -89.86,
+          "pitch": -89.83,
           "roll": 0
         }
       },
       "layer": [
         {
           "id": "sst.analysed_sst",
-          "timestamp": "2002-05-12T00:00:00.000Z"
+          "timestamp": "2009-03-30T12:00:00.000Z"
         },
         {
           "id": "oc.chlor_a",
-          "timestamp": "2002-05-12T00:00:00.000Z"
+          "timestamp": "2009-03-30T12:00:00.000Z"
         }
       ],
       "layerDescription": "Sea Surface Temperature compared with Chlorophyll-a Concentration"
@@ -121,4 +123,4 @@
       "videoId": "uPxXMA1heIY"
     }
   ]
-}
+}
\ No newline at end of file
diff --git a/storage/stories/story-16/story-16-en.json b/storage/stories/story-16/story-16-en.json
index d3ca0495f..38b9aa9c4 100644
--- a/storage/stories/story-16/story-16-en.json
+++ b/storage/stories/story-16/story-16-en.json
@@ -64,24 +64,24 @@
       "shortText": "## Fisherman’s Friend\r\n\r\nMaps of SST show where deep cold water is upwelling, bringing nutrients to the surface.\r\n\r\nModern fishing fleets use SST maps from satellites to help find and follow fish. \r\n\r\nThe interactive globe shows:\r\n\r\n- a comparison between SST and ocean chlorophyll (in phytoplankton)\r\n- high chlorophyll concentrations associated with areas of cold water upwelling off the coasts of Peru, Argentina and Namibia. \r\n\r\nPhytoplankton are the base of the oceanic food chain, but also play a key role in the climate by absorbing carbon dioxide through photosynthesis.",
       "flyTo": {
         "position": {
-          "longitude": -30.74,
-          "latitude": 23.32,
-          "height": 15145050.29
+          "longitude": -60.11,
+          "latitude": -19.14,
+          "height": 10614832.84
         },
         "orientation": {
           "heading": 360,
-          "pitch": -89.86,
+          "pitch": -89.83,
           "roll": 0
         }
       },
       "layer": [
         {
           "id": "sst.analysed_sst",
-          "timestamp": "2002-05-12T00:00:00.000Z"
+          "timestamp": "2009-03-30T12:00:00.000Z"
         },
         {
           "id": "oc.chlor_a",
-          "timestamp": "2002-05-12T00:00:00.000Z"
+          "timestamp": "2009-03-30T12:00:00.000Z"
         }
       ],
       "layerDescription": "Sea Surface Temperature compared with Chlorophyll-a Concentration"
diff --git a/storage/stories/story-16/story-16-es.json b/storage/stories/story-16/story-16-es.json
index 9fd741b5e..38b9aa9c4 100644
--- a/storage/stories/story-16/story-16-es.json
+++ b/storage/stories/story-16/story-16-es.json
@@ -5,7 +5,9 @@
       "type": "splashscreen",
       "text": "# Planetary Heat Pumps\r\n\r\nThe ocean and the atmosphere both redistribute energy around the planet. While it is the atmosphere that brings us our weather, the oceans can store much more heat, making them a more stable indicator of climate trends.",
       "shortText": "# Planetary Heat Pumps\r\n\r\nThe ocean and the atmosphere both redistribute energy around the planet. While it is the atmosphere that brings us our weather, the oceans can store much more heat, making them a more stable indicator of climate trends.",
-      "images": ["assets/sst.jpg"]
+      "images": [
+        "assets/sst.jpg"
+      ]
     },
     {
       "type": "image",
@@ -62,24 +64,24 @@
       "shortText": "## Fisherman’s Friend\r\n\r\nMaps of SST show where deep cold water is upwelling, bringing nutrients to the surface.\r\n\r\nModern fishing fleets use SST maps from satellites to help find and follow fish. \r\n\r\nThe interactive globe shows:\r\n\r\n- a comparison between SST and ocean chlorophyll (in phytoplankton)\r\n- high chlorophyll concentrations associated with areas of cold water upwelling off the coasts of Peru, Argentina and Namibia. \r\n\r\nPhytoplankton are the base of the oceanic food chain, but also play a key role in the climate by absorbing carbon dioxide through photosynthesis.",
       "flyTo": {
         "position": {
-          "longitude": -30.74,
-          "latitude": 23.32,
-          "height": 15145050.29
+          "longitude": -60.11,
+          "latitude": -19.14,
+          "height": 10614832.84
         },
         "orientation": {
           "heading": 360,
-          "pitch": -89.86,
+          "pitch": -89.83,
           "roll": 0
         }
       },
       "layer": [
         {
           "id": "sst.analysed_sst",
-          "timestamp": "2002-05-12T00:00:00.000Z"
+          "timestamp": "2009-03-30T12:00:00.000Z"
         },
         {
           "id": "oc.chlor_a",
-          "timestamp": "2002-05-12T00:00:00.000Z"
+          "timestamp": "2009-03-30T12:00:00.000Z"
         }
       ],
       "layerDescription": "Sea Surface Temperature compared with Chlorophyll-a Concentration"
@@ -121,4 +123,4 @@
       "videoId": "uPxXMA1heIY"
     }
   ]
-}
+}
\ No newline at end of file
diff --git a/storage/stories/story-16/story-16-fr.json b/storage/stories/story-16/story-16-fr.json
index 9fd741b5e..38b9aa9c4 100644
--- a/storage/stories/story-16/story-16-fr.json
+++ b/storage/stories/story-16/story-16-fr.json
@@ -5,7 +5,9 @@
       "type": "splashscreen",
       "text": "# Planetary Heat Pumps\r\n\r\nThe ocean and the atmosphere both redistribute energy around the planet. While it is the atmosphere that brings us our weather, the oceans can store much more heat, making them a more stable indicator of climate trends.",
       "shortText": "# Planetary Heat Pumps\r\n\r\nThe ocean and the atmosphere both redistribute energy around the planet. While it is the atmosphere that brings us our weather, the oceans can store much more heat, making them a more stable indicator of climate trends.",
-      "images": ["assets/sst.jpg"]
+      "images": [
+        "assets/sst.jpg"
+      ]
     },
     {
       "type": "image",
@@ -62,24 +64,24 @@
       "shortText": "## Fisherman’s Friend\r\n\r\nMaps of SST show where deep cold water is upwelling, bringing nutrients to the surface.\r\n\r\nModern fishing fleets use SST maps from satellites to help find and follow fish. \r\n\r\nThe interactive globe shows:\r\n\r\n- a comparison between SST and ocean chlorophyll (in phytoplankton)\r\n- high chlorophyll concentrations associated with areas of cold water upwelling off the coasts of Peru, Argentina and Namibia. \r\n\r\nPhytoplankton are the base of the oceanic food chain, but also play a key role in the climate by absorbing carbon dioxide through photosynthesis.",
       "flyTo": {
         "position": {
-          "longitude": -30.74,
-          "latitude": 23.32,
-          "height": 15145050.29
+          "longitude": -60.11,
+          "latitude": -19.14,
+          "height": 10614832.84
         },
         "orientation": {
           "heading": 360,
-          "pitch": -89.86,
+          "pitch": -89.83,
           "roll": 0
         }
       },
       "layer": [
         {
           "id": "sst.analysed_sst",
-          "timestamp": "2002-05-12T00:00:00.000Z"
+          "timestamp": "2009-03-30T12:00:00.000Z"
         },
         {
           "id": "oc.chlor_a",
-          "timestamp": "2002-05-12T00:00:00.000Z"
+          "timestamp": "2009-03-30T12:00:00.000Z"
         }
       ],
       "layerDescription": "Sea Surface Temperature compared with Chlorophyll-a Concentration"
@@ -121,4 +123,4 @@
       "videoId": "uPxXMA1heIY"
     }
   ]
-}
+}
\ No newline at end of file
diff --git a/storage/stories/story-16/story-16-nl.json b/storage/stories/story-16/story-16-nl.json
index 9fd741b5e..38b9aa9c4 100644
--- a/storage/stories/story-16/story-16-nl.json
+++ b/storage/stories/story-16/story-16-nl.json
@@ -5,7 +5,9 @@
       "type": "splashscreen",
       "text": "# Planetary Heat Pumps\r\n\r\nThe ocean and the atmosphere both redistribute energy around the planet. While it is the atmosphere that brings us our weather, the oceans can store much more heat, making them a more stable indicator of climate trends.",
       "shortText": "# Planetary Heat Pumps\r\n\r\nThe ocean and the atmosphere both redistribute energy around the planet. While it is the atmosphere that brings us our weather, the oceans can store much more heat, making them a more stable indicator of climate trends.",
-      "images": ["assets/sst.jpg"]
+      "images": [
+        "assets/sst.jpg"
+      ]
     },
     {
       "type": "image",
@@ -62,24 +64,24 @@
       "shortText": "## Fisherman’s Friend\r\n\r\nMaps of SST show where deep cold water is upwelling, bringing nutrients to the surface.\r\n\r\nModern fishing fleets use SST maps from satellites to help find and follow fish. \r\n\r\nThe interactive globe shows:\r\n\r\n- a comparison between SST and ocean chlorophyll (in phytoplankton)\r\n- high chlorophyll concentrations associated with areas of cold water upwelling off the coasts of Peru, Argentina and Namibia. \r\n\r\nPhytoplankton are the base of the oceanic food chain, but also play a key role in the climate by absorbing carbon dioxide through photosynthesis.",
       "flyTo": {
         "position": {
-          "longitude": -30.74,
-          "latitude": 23.32,
-          "height": 15145050.29
+          "longitude": -60.11,
+          "latitude": -19.14,
+          "height": 10614832.84
         },
         "orientation": {
           "heading": 360,
-          "pitch": -89.86,
+          "pitch": -89.83,
           "roll": 0
         }
       },
       "layer": [
         {
           "id": "sst.analysed_sst",
-          "timestamp": "2002-05-12T00:00:00.000Z"
+          "timestamp": "2009-03-30T12:00:00.000Z"
         },
         {
           "id": "oc.chlor_a",
-          "timestamp": "2002-05-12T00:00:00.000Z"
+          "timestamp": "2009-03-30T12:00:00.000Z"
         }
       ],
       "layerDescription": "Sea Surface Temperature compared with Chlorophyll-a Concentration"
@@ -121,4 +123,4 @@
       "videoId": "uPxXMA1heIY"
     }
   ]
-}
+}
\ No newline at end of file
diff --git a/storage/stories/story-30/story-30-en.json b/storage/stories/story-30/story-30-en.json
index 91c9c1247..bbdc1e4df 100644
--- a/storage/stories/story-30/story-30-en.json
+++ b/storage/stories/story-30/story-30-en.json
@@ -3,8 +3,8 @@
   "slides": [
     {
       "type": "splashscreen",
-      "text": "# A Country Under Threat\r\n\r\nMean sea level is rising across the globe, threatening coastal communities everywhere and the very existence of low-lying nations such as Kiribati and the Maldives. Sea level acts as an index of climate change because it depends on several components of the climate system, including ocean temperature and the behaviour of glaciers and ice sheets.",
-      "shortText": "# A Country Under Threat\r\n\r\nMean sea level is rising across the globe, threatening coastal communities everywhere and the very existence of low-lying nations such as Kiribati and the Maldives. Sea level acts as an index of climate change because it depends on several components of the climate system, including ocean temperature and the behaviour of glaciers and ice sheets.",
+      "text": "# Coasts Under Threat\r\n\r\nMean sea level is rising across the globe, threatening coastal communities everywhere and the very existence of low-lying nations such as Kiribati and the Maldives. Sea level acts as an index of climate change because it depends on several components of the climate system, including ocean temperature and the behaviour of glaciers and ice sheets.",
+      "shortText": "# Coasts Under Threat\r\n\r\nMean sea level is rising across the globe, threatening coastal communities everywhere and the very existence of low-lying nations such as Kiribati and the Maldives. Sea level acts as an index of climate change because it depends on several components of the climate system, including ocean temperature and the behaviour of glaciers and ice sheets.",
       "images": [
         "assets/sealevel.jpg"
       ]