feat(content): update story 30

Co-authored-by: StoryMapper <storyMapper@ubilabs.com>
Co-authored-by: Patrick Mast <mast@ubilabs.net>

storage/stories/story-30/story-30-de.json

@@ -77,13 +77,13 @@
         "High tide on Marakei Island, Kiribati (Diederik Veerman/Museon The Hague)",
         "The Mississippi Delta is losing land the size of a football field every hour to the sea. Proba-V satellite image from 10 February 2015. \r\n(ESA-BELSPO, produced by VITO)",
         "Copernicus Sentinel-2 Image of the 9km-long Eastern Scheldt Storm Surge Barrier (Oosterscheldekering) in the Netherlands.  \r\nCoastal defences like this will be severely challenged in a future world with higher sea level.\r\n(Modified Copernicus Sentinel data (2020), processed by ESA)",
-        "Since the early 1990s, satellite altimeters have revolutionised our understanding of sea-level rise. Global mean sea level has not only risen over the last 25 years – by about 3 cm per decade – but the rate at which it is rising is accelerating. ESA’s ERS and Envisat satellites carried radar altimeters, as do CryoSat and Copernicus Sentinel-3. Sentinel-6 provides continuity with the US-French Jason and Topex-Poseidon satellites. (ESA)",
+        "Since the early 1990s, satellite altimeters have revolutionised our understanding of sea-level rise. Global mean sea level has not only risen over the last 25 years – by about 3 cm per decade – but the rate at which it is rising is accelerating. ESA’s ERS and Envisat satellites carried radar altimeters, as do CryoSat and Copernicus Sentinel-3. Copernicus Sentinel-6 provides continuity with the US-French Jason and Topex-Poseidon satellites. (ESA)",
         "A map of regional sea level trends, derived from more than 20 years of satellite observations, shows where mean sea level is rising the most (red), dropping (blue), or remains unchanged (grey) (ESA-CCI)"
       ]
     },
     {
       "type": "video",
-      "text": "## The Sea Level Budget\r\n\r\nTo accurately measure sea level rise, attribute its causes and analyse the potential impacts, we need consistent data from observations across the globe. Identifying the individual contributors to sea level rise involves tracking water as it moves around the world in all its states – solid, liquid and gas – and this makes it one of the most complicated challenges in climate science. ESA’s Climate Change Initiative has examined records of satellite data collected since the 1990s covering sea level, the temperature of the sea surface and the thickness of the polar ice sheets, and information about the world’s glaciers going back to the 1960s. \r\n\r\nIt is estimated that in the decade 2003–2013, 36% of sea level rise was meltwater from the Greenland and Antarctic ice sheets; 30% was due to thermal expansion; 20% from melting glaciers; and 10% was due to groundwater extracted from aquifers for domestic, industrial and agricultural use that is ultimately discharged to the oceans. Although the contributions are all following an upward trend, they vary through time and don’t always add up to the observed total sea level rise. Bridging this gap in our knowledge is known as closing the sea level budget, and is an important focus for climate scientists. \r\n\r\nThe integration of new data from ESA satellites such as CryoSat, Copernicus Sentinel-3 and Sentinel-6 will improve our knowledge of this key climate variable. Consistent and continuous information from multiple sources will help us better understand sea level change and its impacts, and evaluate the adaptation options for the world’s coastal populations, including the inhabitants of Kiribati.",
+      "text": "## The Sea Level Budget\r\n\r\nTo accurately measure sea level rise, attribute its causes and analyse the potential impacts, we need consistent data from observations across the globe. Identifying the individual contributors to sea level rise involves tracking water as it moves around the world in all its states – solid, liquid and gas – and this makes it one of the most complicated challenges in climate science. ESA’s Climate Change Initiative has examined records of satellite data collected since the 1990s covering sea level, the temperature of the sea surface and the thickness of the polar ice sheets, and information about the world’s glaciers going back to the 1960s. \r\n\r\nIt is estimated that in the decade 2003–2013, 36% of sea level rise was meltwater from the Greenland and Antarctic ice sheets; 30% was due to thermal expansion; 20% from melting glaciers; and 10% was due to groundwater extracted from aquifers for domestic, industrial and agricultural use that is ultimately discharged to the oceans. Although the contributions are all following an upward trend, they vary through time and don’t always add up to the observed total sea level rise. Bridging this gap in our knowledge is known as closing the sea level budget, and is an important focus for climate scientists. \r\n\r\nThe integration of new data from ESA satellites such as CryoSat and Copernicus Sentinels-3 and -6 will improve our knowledge of this key climate variable. Consistent and continuous information from multiple sources will help us better understand sea level change and its impacts, and evaluate the adaptation options for the world’s coastal populations, including the inhabitants of Kiribati.",
       "shortText": "# The Sea Level Budget\r\n\r\nESA’s Climate Change Initiative uses satellite data to investigate individual contributors to sea level rise:\r\n\r\n- sea level and ice sheet thickness since 1990s\r\n- ocean temperature since 1980s\r\n- glacier information since 1960s\r\n\r\nIn the decade 2003–2013 sea level rise was:\r\n\r\n- 36% due to meltwater from Greenland and Antarctic ice sheets\r\n- 30% due to thermal expansion\r\n- 20% due to melting glaciers\r\n- 10% due to groundwater extraction\r\n\r\nContinuous information from satellite and other sources will help us better understand sea level change, and evaluate the adaptation options for Kiribati’s inhabitants and the world’s other coastal populations.",
       "videoId": "K7JmzmDoo4w"
     }

storage/stories/story-30/story-30-en.json

@@ -77,13 +77,13 @@
         "High tide on Marakei Island, Kiribati (Diederik Veerman/Museon The Hague)",
         "The Mississippi Delta is losing land the size of a football field every hour to the sea. Proba-V satellite image from 10 February 2015. \r\n(ESA-BELSPO, produced by VITO)",
         "Copernicus Sentinel-2 Image of the 9km-long Eastern Scheldt Storm Surge Barrier (Oosterscheldekering) in the Netherlands.  \r\nCoastal defences like this will be severely challenged in a future world with higher sea level.\r\n(Modified Copernicus Sentinel data (2020), processed by ESA)",
-        "Since the early 1990s, satellite altimeters have revolutionised our understanding of sea-level rise. Global mean sea level has not only risen over the last 25 years – by about 3 cm per decade – but the rate at which it is rising is accelerating. ESA’s ERS and Envisat satellites carried radar altimeters, as do CryoSat and Copernicus Sentinel-3. Sentinel-6 provides continuity with the US-French Jason and Topex-Poseidon satellites. (ESA)",
+        "Since the early 1990s, satellite altimeters have revolutionised our understanding of sea-level rise. Global mean sea level has not only risen over the last 25 years – by about 3 cm per decade – but the rate at which it is rising is accelerating. ESA’s ERS and Envisat satellites carried radar altimeters, as do CryoSat and Copernicus Sentinel-3. Copernicus Sentinel-6 provides continuity with the US-French Jason and Topex-Poseidon satellites. (ESA)",
         "A map of regional sea level trends, derived from more than 20 years of satellite observations, shows where mean sea level is rising the most (red), dropping (blue), or remains unchanged (grey) (ESA-CCI)"
       ]
     },
     {
       "type": "video",
-      "text": "## The Sea Level Budget\r\n\r\nTo accurately measure sea level rise, attribute its causes and analyse the potential impacts, we need consistent data from observations across the globe. Identifying the individual contributors to sea level rise involves tracking water as it moves around the world in all its states – solid, liquid and gas – and this makes it one of the most complicated challenges in climate science. ESA’s Climate Change Initiative has examined records of satellite data collected since the 1990s covering sea level, the temperature of the sea surface and the thickness of the polar ice sheets, and information about the world’s glaciers going back to the 1960s. \r\n\r\nIt is estimated that in the decade 2003–2013, 36% of sea level rise was meltwater from the Greenland and Antarctic ice sheets; 30% was due to thermal expansion; 20% from melting glaciers; and 10% was due to groundwater extracted from aquifers for domestic, industrial and agricultural use that is ultimately discharged to the oceans. Although the contributions are all following an upward trend, they vary through time and don’t always add up to the observed total sea level rise. Bridging this gap in our knowledge is known as closing the sea level budget, and is an important focus for climate scientists. \r\n\r\nThe integration of new data from ESA satellites such as CryoSat, Copernicus Sentinel-3 and Sentinel-6 will improve our knowledge of this key climate variable. Consistent and continuous information from multiple sources will help us better understand sea level change and its impacts, and evaluate the adaptation options for the world’s coastal populations, including the inhabitants of Kiribati.",
+      "text": "## The Sea Level Budget\r\n\r\nTo accurately measure sea level rise, attribute its causes and analyse the potential impacts, we need consistent data from observations across the globe. Identifying the individual contributors to sea level rise involves tracking water as it moves around the world in all its states – solid, liquid and gas – and this makes it one of the most complicated challenges in climate science. ESA’s Climate Change Initiative has examined records of satellite data collected since the 1990s covering sea level, the temperature of the sea surface and the thickness of the polar ice sheets, and information about the world’s glaciers going back to the 1960s. \r\n\r\nIt is estimated that in the decade 2003–2013, 36% of sea level rise was meltwater from the Greenland and Antarctic ice sheets; 30% was due to thermal expansion; 20% from melting glaciers; and 10% was due to groundwater extracted from aquifers for domestic, industrial and agricultural use that is ultimately discharged to the oceans. Although the contributions are all following an upward trend, they vary through time and don’t always add up to the observed total sea level rise. Bridging this gap in our knowledge is known as closing the sea level budget, and is an important focus for climate scientists. \r\n\r\nThe integration of new data from ESA satellites such as CryoSat and Copernicus Sentinels-3 and -6 will improve our knowledge of this key climate variable. Consistent and continuous information from multiple sources will help us better understand sea level change and its impacts, and evaluate the adaptation options for the world’s coastal populations, including the inhabitants of Kiribati.",
       "shortText": "# The Sea Level Budget\r\n\r\nESA’s Climate Change Initiative uses satellite data to investigate individual contributors to sea level rise:\r\n\r\n- sea level and ice sheet thickness since 1990s\r\n- ocean temperature since 1980s\r\n- glacier information since 1960s\r\n\r\nIn the decade 2003–2013 sea level rise was:\r\n\r\n- 36% due to meltwater from Greenland and Antarctic ice sheets\r\n- 30% due to thermal expansion\r\n- 20% due to melting glaciers\r\n- 10% due to groundwater extraction\r\n\r\nContinuous information from satellite and other sources will help us better understand sea level change, and evaluate the adaptation options for Kiribati’s inhabitants and the world’s other coastal populations.",
       "videoId": "K7JmzmDoo4w"
     }

storage/stories/story-30/story-30-es.json

@@ -77,13 +77,13 @@
         "High tide on Marakei Island, Kiribati (Diederik Veerman/Museon The Hague)",
         "The Mississippi Delta is losing land the size of a football field every hour to the sea. Proba-V satellite image from 10 February 2015. \r\n(ESA-BELSPO, produced by VITO)",
         "Copernicus Sentinel-2 Image of the 9km-long Eastern Scheldt Storm Surge Barrier (Oosterscheldekering) in the Netherlands.  \r\nCoastal defences like this will be severely challenged in a future world with higher sea level.\r\n(Modified Copernicus Sentinel data (2020), processed by ESA)",
-        "Since the early 1990s, satellite altimeters have revolutionised our understanding of sea-level rise. Global mean sea level has not only risen over the last 25 years – by about 3 cm per decade – but the rate at which it is rising is accelerating. ESA’s ERS and Envisat satellites carried radar altimeters, as do CryoSat and Copernicus Sentinel-3. Sentinel-6 provides continuity with the US-French Jason and Topex-Poseidon satellites. (ESA)",
+        "Since the early 1990s, satellite altimeters have revolutionised our understanding of sea-level rise. Global mean sea level has not only risen over the last 25 years – by about 3 cm per decade – but the rate at which it is rising is accelerating. ESA’s ERS and Envisat satellites carried radar altimeters, as do CryoSat and Copernicus Sentinel-3. Copernicus Sentinel-6 provides continuity with the US-French Jason and Topex-Poseidon satellites. (ESA)",
         "A map of regional sea level trends, derived from more than 20 years of satellite observations, shows where mean sea level is rising the most (red), dropping (blue), or remains unchanged (grey) (ESA-CCI)"
       ]
     },
     {
       "type": "video",
-      "text": "## The Sea Level Budget\r\n\r\nTo accurately measure sea level rise, attribute its causes and analyse the potential impacts, we need consistent data from observations across the globe. Identifying the individual contributors to sea level rise involves tracking water as it moves around the world in all its states – solid, liquid and gas – and this makes it one of the most complicated challenges in climate science. ESA’s Climate Change Initiative has examined records of satellite data collected since the 1990s covering sea level, the temperature of the sea surface and the thickness of the polar ice sheets, and information about the world’s glaciers going back to the 1960s. \r\n\r\nIt is estimated that in the decade 2003–2013, 36% of sea level rise was meltwater from the Greenland and Antarctic ice sheets; 30% was due to thermal expansion; 20% from melting glaciers; and 10% was due to groundwater extracted from aquifers for domestic, industrial and agricultural use that is ultimately discharged to the oceans. Although the contributions are all following an upward trend, they vary through time and don’t always add up to the observed total sea level rise. Bridging this gap in our knowledge is known as closing the sea level budget, and is an important focus for climate scientists. \r\n\r\nThe integration of new data from ESA satellites such as CryoSat, Copernicus Sentinel-3 and Sentinel-6 will improve our knowledge of this key climate variable. Consistent and continuous information from multiple sources will help us better understand sea level change and its impacts, and evaluate the adaptation options for the world’s coastal populations, including the inhabitants of Kiribati.",
+      "text": "## The Sea Level Budget\r\n\r\nTo accurately measure sea level rise, attribute its causes and analyse the potential impacts, we need consistent data from observations across the globe. Identifying the individual contributors to sea level rise involves tracking water as it moves around the world in all its states – solid, liquid and gas – and this makes it one of the most complicated challenges in climate science. ESA’s Climate Change Initiative has examined records of satellite data collected since the 1990s covering sea level, the temperature of the sea surface and the thickness of the polar ice sheets, and information about the world’s glaciers going back to the 1960s. \r\n\r\nIt is estimated that in the decade 2003–2013, 36% of sea level rise was meltwater from the Greenland and Antarctic ice sheets; 30% was due to thermal expansion; 20% from melting glaciers; and 10% was due to groundwater extracted from aquifers for domestic, industrial and agricultural use that is ultimately discharged to the oceans. Although the contributions are all following an upward trend, they vary through time and don’t always add up to the observed total sea level rise. Bridging this gap in our knowledge is known as closing the sea level budget, and is an important focus for climate scientists. \r\n\r\nThe integration of new data from ESA satellites such as CryoSat and Copernicus Sentinels-3 and -6 will improve our knowledge of this key climate variable. Consistent and continuous information from multiple sources will help us better understand sea level change and its impacts, and evaluate the adaptation options for the world’s coastal populations, including the inhabitants of Kiribati.",
       "shortText": "# The Sea Level Budget\r\n\r\nESA’s Climate Change Initiative uses satellite data to investigate individual contributors to sea level rise:\r\n\r\n- sea level and ice sheet thickness since 1990s\r\n- ocean temperature since 1980s\r\n- glacier information since 1960s\r\n\r\nIn the decade 2003–2013 sea level rise was:\r\n\r\n- 36% due to meltwater from Greenland and Antarctic ice sheets\r\n- 30% due to thermal expansion\r\n- 20% due to melting glaciers\r\n- 10% due to groundwater extraction\r\n\r\nContinuous information from satellite and other sources will help us better understand sea level change, and evaluate the adaptation options for Kiribati’s inhabitants and the world’s other coastal populations.",
       "videoId": "K7JmzmDoo4w"
     }