feat(story-12): content updates

* Auto content commit for story id: story-12 * Auto content commit for story id: story-12 * Auto content commit for story id: story-12 * Auto content commit for story id: story-12 * Auto content commit for story id: story-12 * Auto content commit for story id: story-12 * Auto content commit for story id: story-12 * Auto content commit for story id: story-12 Co-authored-by: StoryMapper <storyMapper@ubilabs.com> Co-authored-by: Katherina Marcenko <45818654+KatvonRivia@users.noreply.github.com>
ubilabs · Mar 3, 2021 · 58d6223 · 58d6223
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Showing 5 changed files with 40 additions and 60 deletions.
diff --git a/storage/stories/story-12/story-12-de.json b/storage/stories/story-12/story-12-de.json
@@ -23,7 +23,7 @@
         "Spare natural gas being burned off on an oil production platform in the North Sea. Carbon dioxide and water vapour are the main combustion products. Extracting and burning hydrocarbons pumps carbon from a rock reservoir into the atmosphere. (Varodrig)",
         "Atmospheric carbon dioxide concentration over the last 300 years, based on air samples from ice cores and, since 1958, direct measurements from Mauna Loa Observatory, Hawaii. Carbon dioxide has been accumulating in the atmosphere since the Industrial Revolution, its concentration increasing rapidly in the second half of the twentieth century. (source: Scripps Institute of Oceanography)",
         "The molecular structure of carbon dioxide and methane molecules allows them to absorb infrared radiation. Heat is absorbed by a molecule if the atoms inside can vibrate at the frequency of infrared radiation. More complex molecules have more vibrational modes, so more opportunities to absorb heat, making them more powerful greenhouse gases. A methane molecule, with one carbon atom (grey) bound to four hydrogen atoms (red), can absorb more heat than a carbon dioxide molecule, with one carbon atom bound to two oxygen atoms (blue). A chlorofluorocarbon like CFC-113 (green and yellow) has even more bonds, making it a very powerful greenhouse gas. (Planetary Visions)",
-        "Atmospheric carbon dioxide as a function of time and latitude, derived from the SCIAMACHY sensor on Envisat. The data surface shows the natural annual cycle of CO<sub>2</sub> uptake and release, which is particularly strong in the northern hemisphere, as well as a gradual increase over the years resulting from human activity. (ESA-CCI)"
+        "Atmospheric carbon dioxide as a function of time and latitude, derived from the SCIAMACHY sensor on Envisat. The data surface shows the natural annual cycle of carbon dioxide uptake and release, which is particularly strong in the northern hemisphere, as well as a gradual increase over the years resulting from human activity. (ESA-CCI)"
       ]
     },
     {
@@ -32,27 +32,23 @@
       "shortText": "## The Fast Carbon Cycle \r\n\r\nCycling of carbon through living things is known as the fast carbon cycle.\r\n\r\n- Plants take up CO2 from the atmosphere by photosynthesis as they grow in spring and summer.\r\n- Some returned when leaves die and by animals eating plants and breathing out carbon dioxide. \r\n- Atmospheric CO2 peaks at the end of the northern winter.\r\n- Rapidly-growing plants start absorbing CO2 in the spring. \r\n- Atmospheric carbon varies most in the northern hemisphere (more land, therefore more plants).\r\n- Year-to-year increase in CO2 shows the carbon cycle is out of balance (mainly from fossil fuel burning).\r\n\r\n## Carbon and the Land\r\n\r\n- Changes in land use and land cover also alter the carbon cycle. \r\n- Tropical forest clearance releases large amounts of CO2 by fire and removes trees that absorb and store carbon. \r\n- Thawing permafrost releases soil carbon by decomposition and potentially vast amounts of methane. \r\n- Warming and drying of northern lands exposes vast areas of forest, bush and peat to the risk of wildfires. \r\n- Fire is a key component of the carbon cycle, taking carbon from the biosphere into the atmosphere.",
       "flyTo": {
         "position": {
-          "longitude": 37.88,
-          "latitude": 15.08,
-          "height": 12754110.44
+          "longitude": 54.03,
+          "latitude": 26.9,
+          "height": 24997871.88
         },
         "orientation": {
-          "heading": 0,
-          "pitch": -89.95,
+          "heading": 360,
+          "pitch": -89.96,
           "roll": 0
         }
       },
       "layer": [
         {
           "id": "greenhouse.xco2",
-          "timestamp": "2010-07-08T00:00:00.000Z"
-        },
-        {
-          "id": "greenhouse.xch4",
-          "timestamp": "2010-07-08T00:00:00.000Z"
+          "timestamp": "2007-12-06T00:00:00.000Z"
         }
       ],
-      "layerDescription": "Atmospheric carbon dioxide compared with methane"
+      "layerDescription": "Atmospheric carbon dioxide concentration"
     },
     {
       "type": "video",

diff --git a/storage/stories/story-12/story-12-en.json b/storage/stories/story-12/story-12-en.json
@@ -23,7 +23,7 @@
         "Spare natural gas being burned off on an oil production platform in the North Sea. Carbon dioxide and water vapour are the main combustion products. Extracting and burning hydrocarbons pumps carbon from a rock reservoir into the atmosphere. (Varodrig)",
         "Atmospheric carbon dioxide concentration over the last 300 years, based on air samples from ice cores and, since 1958, direct measurements from Mauna Loa Observatory, Hawaii. Carbon dioxide has been accumulating in the atmosphere since the Industrial Revolution, its concentration increasing rapidly in the second half of the twentieth century. (source: Scripps Institute of Oceanography)",
         "The molecular structure of carbon dioxide and methane molecules allows them to absorb infrared radiation. Heat is absorbed by a molecule if the atoms inside can vibrate at the frequency of infrared radiation. More complex molecules have more vibrational modes, so more opportunities to absorb heat, making them more powerful greenhouse gases. A methane molecule, with one carbon atom (grey) bound to four hydrogen atoms (red), can absorb more heat than a carbon dioxide molecule, with one carbon atom bound to two oxygen atoms (blue). A chlorofluorocarbon like CFC-113 (green and yellow) has even more bonds, making it a very powerful greenhouse gas. (Planetary Visions)",
-        "Atmospheric carbon dioxide as a function of time and latitude, derived from the SCIAMACHY sensor on Envisat. The data surface shows the natural annual cycle of CO<sub>2</sub> uptake and release, which is particularly strong in the northern hemisphere, as well as a gradual increase over the years resulting from human activity. (ESA-CCI)"
+        "Atmospheric carbon dioxide as a function of time and latitude, derived from the SCIAMACHY sensor on Envisat. The data surface shows the natural annual cycle of carbon dioxide uptake and release, which is particularly strong in the northern hemisphere, as well as a gradual increase over the years resulting from human activity. (ESA-CCI)"
       ]
     },
     {
@@ -32,27 +32,23 @@
       "shortText": "## The Fast Carbon Cycle \r\n\r\nCycling of carbon through living things is known as the fast carbon cycle.\r\n\r\n- Plants take up CO2 from the atmosphere by photosynthesis as they grow in spring and summer.\r\n- Some returned when leaves die and by animals eating plants and breathing out carbon dioxide. \r\n- Atmospheric CO2 peaks at the end of the northern winter.\r\n- Rapidly-growing plants start absorbing CO2 in the spring. \r\n- Atmospheric carbon varies most in the northern hemisphere (more land, therefore more plants).\r\n- Year-to-year increase in CO2 shows the carbon cycle is out of balance (mainly from fossil fuel burning).\r\n\r\n## Carbon and the Land\r\n\r\n- Changes in land use and land cover also alter the carbon cycle. \r\n- Tropical forest clearance releases large amounts of CO2 by fire and removes trees that absorb and store carbon. \r\n- Thawing permafrost releases soil carbon by decomposition and potentially vast amounts of methane. \r\n- Warming and drying of northern lands exposes vast areas of forest, bush and peat to the risk of wildfires. \r\n- Fire is a key component of the carbon cycle, taking carbon from the biosphere into the atmosphere.",
       "flyTo": {
         "position": {
-          "longitude": 37.88,
-          "latitude": 15.08,
-          "height": 12754110.44
+          "longitude": 54.03,
+          "latitude": 26.9,
+          "height": 24997871.88
         },
         "orientation": {
-          "heading": 0,
-          "pitch": -89.95,
+          "heading": 360,
+          "pitch": -89.96,
           "roll": 0
         }
       },
       "layer": [
         {
           "id": "greenhouse.xco2",
-          "timestamp": "2010-07-08T00:00:00.000Z"
-        },
-        {
-          "id": "greenhouse.xch4",
-          "timestamp": "2010-07-08T00:00:00.000Z"
+          "timestamp": "2007-12-06T00:00:00.000Z"
         }
       ],
-      "layerDescription": "Atmospheric carbon dioxide compared with methane"
+      "layerDescription": "Atmospheric carbon dioxide concentration"
     },
     {
       "type": "video",

diff --git a/storage/stories/story-12/story-12-es.json b/storage/stories/story-12/story-12-es.json
@@ -23,7 +23,7 @@
         "Spare natural gas being burned off on an oil production platform in the North Sea. Carbon dioxide and water vapour are the main combustion products. Extracting and burning hydrocarbons pumps carbon from a rock reservoir into the atmosphere. (Varodrig)",
         "Atmospheric carbon dioxide concentration over the last 300 years, based on air samples from ice cores and, since 1958, direct measurements from Mauna Loa Observatory, Hawaii. Carbon dioxide has been accumulating in the atmosphere since the Industrial Revolution, its concentration increasing rapidly in the second half of the twentieth century. (source: Scripps Institute of Oceanography)",
         "The molecular structure of carbon dioxide and methane molecules allows them to absorb infrared radiation. Heat is absorbed by a molecule if the atoms inside can vibrate at the frequency of infrared radiation. More complex molecules have more vibrational modes, so more opportunities to absorb heat, making them more powerful greenhouse gases. A methane molecule, with one carbon atom (grey) bound to four hydrogen atoms (red), can absorb more heat than a carbon dioxide molecule, with one carbon atom bound to two oxygen atoms (blue). A chlorofluorocarbon like CFC-113 (green and yellow) has even more bonds, making it a very powerful greenhouse gas. (Planetary Visions)",
-        "Atmospheric carbon dioxide as a function of time and latitude, derived from the SCIAMACHY sensor on Envisat. The data surface shows the natural annual cycle of CO<sub>2</sub> uptake and release, which is particularly strong in the northern hemisphere, as well as a gradual increase over the years resulting from human activity. (ESA-CCI)"
+        "Atmospheric carbon dioxide as a function of time and latitude, derived from the SCIAMACHY sensor on Envisat. The data surface shows the natural annual cycle of carbon dioxide uptake and release, which is particularly strong in the northern hemisphere, as well as a gradual increase over the years resulting from human activity. (ESA-CCI)"
       ]
     },
     {
@@ -32,27 +32,23 @@
       "shortText": "## The Fast Carbon Cycle \r\n\r\nCycling of carbon through living things is known as the fast carbon cycle.\r\n\r\n- Plants take up CO2 from the atmosphere by photosynthesis as they grow in spring and summer.\r\n- Some returned when leaves die and by animals eating plants and breathing out carbon dioxide. \r\n- Atmospheric CO2 peaks at the end of the northern winter.\r\n- Rapidly-growing plants start absorbing CO2 in the spring. \r\n- Atmospheric carbon varies most in the northern hemisphere (more land, therefore more plants).\r\n- Year-to-year increase in CO2 shows the carbon cycle is out of balance (mainly from fossil fuel burning).\r\n\r\n## Carbon and the Land\r\n\r\n- Changes in land use and land cover also alter the carbon cycle. \r\n- Tropical forest clearance releases large amounts of CO2 by fire and removes trees that absorb and store carbon. \r\n- Thawing permafrost releases soil carbon by decomposition and potentially vast amounts of methane. \r\n- Warming and drying of northern lands exposes vast areas of forest, bush and peat to the risk of wildfires. \r\n- Fire is a key component of the carbon cycle, taking carbon from the biosphere into the atmosphere.",
       "flyTo": {
         "position": {
-          "longitude": 37.88,
-          "latitude": 15.08,
-          "height": 12754110.44
+          "longitude": 54.03,
+          "latitude": 26.9,
+          "height": 24997871.88
         },
         "orientation": {
-          "heading": 0,
-          "pitch": -89.95,
+          "heading": 360,
+          "pitch": -89.96,
           "roll": 0
         }
       },
       "layer": [
         {
           "id": "greenhouse.xco2",
-          "timestamp": "2010-07-08T00:00:00.000Z"
-        },
-        {
-          "id": "greenhouse.xch4",
-          "timestamp": "2010-07-08T00:00:00.000Z"
+          "timestamp": "2007-12-06T00:00:00.000Z"
         }
       ],
-      "layerDescription": "Atmospheric carbon dioxide compared with methane"
+      "layerDescription": "Atmospheric carbon dioxide concentration"
     },
     {
       "type": "video",

diff --git a/storage/stories/story-12/story-12-fr.json b/storage/stories/story-12/story-12-fr.json
@@ -23,7 +23,7 @@
         "Spare natural gas being burned off on an oil production platform in the North Sea. Carbon dioxide and water vapour are the main combustion products. Extracting and burning hydrocarbons pumps carbon from a rock reservoir into the atmosphere. (Varodrig)",
         "Atmospheric carbon dioxide concentration over the last 300 years, based on air samples from ice cores and, since 1958, direct measurements from Mauna Loa Observatory, Hawaii. Carbon dioxide has been accumulating in the atmosphere since the Industrial Revolution, its concentration increasing rapidly in the second half of the twentieth century. (source: Scripps Institute of Oceanography)",
         "The molecular structure of carbon dioxide and methane molecules allows them to absorb infrared radiation. Heat is absorbed by a molecule if the atoms inside can vibrate at the frequency of infrared radiation. More complex molecules have more vibrational modes, so more opportunities to absorb heat, making them more powerful greenhouse gases. A methane molecule, with one carbon atom (grey) bound to four hydrogen atoms (red), can absorb more heat than a carbon dioxide molecule, with one carbon atom bound to two oxygen atoms (blue). A chlorofluorocarbon like CFC-113 (green and yellow) has even more bonds, making it a very powerful greenhouse gas. (Planetary Visions)",
-        "Atmospheric carbon dioxide as a function of time and latitude, derived from the SCIAMACHY sensor on Envisat. The data surface shows the natural annual cycle of CO<sub>2</sub> uptake and release, which is particularly strong in the northern hemisphere, as well as a gradual increase over the years resulting from human activity. (ESA-CCI)"
+        "Atmospheric carbon dioxide as a function of time and latitude, derived from the SCIAMACHY sensor on Envisat. The data surface shows the natural annual cycle of carbon dioxide uptake and release, which is particularly strong in the northern hemisphere, as well as a gradual increase over the years resulting from human activity. (ESA-CCI)"
       ]
     },
     {
@@ -32,27 +32,23 @@
       "shortText": "## The Fast Carbon Cycle \r\n\r\nCycling of carbon through living things is known as the fast carbon cycle.\r\n\r\n- Plants take up CO2 from the atmosphere by photosynthesis as they grow in spring and summer.\r\n- Some returned when leaves die and by animals eating plants and breathing out carbon dioxide. \r\n- Atmospheric CO2 peaks at the end of the northern winter.\r\n- Rapidly-growing plants start absorbing CO2 in the spring. \r\n- Atmospheric carbon varies most in the northern hemisphere (more land, therefore more plants).\r\n- Year-to-year increase in CO2 shows the carbon cycle is out of balance (mainly from fossil fuel burning).\r\n\r\n## Carbon and the Land\r\n\r\n- Changes in land use and land cover also alter the carbon cycle. \r\n- Tropical forest clearance releases large amounts of CO2 by fire and removes trees that absorb and store carbon. \r\n- Thawing permafrost releases soil carbon by decomposition and potentially vast amounts of methane. \r\n- Warming and drying of northern lands exposes vast areas of forest, bush and peat to the risk of wildfires. \r\n- Fire is a key component of the carbon cycle, taking carbon from the biosphere into the atmosphere.",
       "flyTo": {
         "position": {
-          "longitude": 37.88,
-          "latitude": 15.08,
-          "height": 12754110.44
+          "longitude": 54.03,
+          "latitude": 26.9,
+          "height": 24997871.88
         },
         "orientation": {
-          "heading": 0,
-          "pitch": -89.95,
+          "heading": 360,
+          "pitch": -89.96,
           "roll": 0
         }
       },
       "layer": [
         {
           "id": "greenhouse.xco2",
-          "timestamp": "2010-07-08T00:00:00.000Z"
-        },
-        {
-          "id": "greenhouse.xch4",
-          "timestamp": "2010-07-08T00:00:00.000Z"
+          "timestamp": "2007-12-06T00:00:00.000Z"
         }
       ],
-      "layerDescription": "Atmospheric carbon dioxide compared with methane"
+      "layerDescription": "Atmospheric carbon dioxide concentration"
     },
     {
       "type": "video",