Commit df4457ff authored by Mahé Perrette's avatar Mahé Perrette
Browse files

fixed typo % land rcp2.6 end of century

parent 57afbcaa
......@@ -64,7 +64,7 @@ Our definition of “drought” is quite strict, such that, without climate chan
However, at today’s level of 1°C global warming Central African Republic’s annual land area affected by droughts is, on average, already larger and amount to 1800 km<sup>2</sup> (0.3% of the land area). The level of change ranges from -0.4% to 10.9% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Central African Republic’s annual land area affected by droughts is projected to increase by 1200 km<sup>2</sup> (i.e. 0.2% of the land area) on average in comparison to a world without climate change. Under these conditions, 0.3% of the land area would be affected by droughts each year, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -2600 to 68100 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 3600 km<sup>2</sup> (0.6% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 4400 km<sup>2</sup> (0.6% of the land area). By the middle of the century, changes reach 1000 km<sup>2</sup> under RCP2.6 and 2600 km<sup>2</sup> under RCP6.0.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 3600 km<sup>2</sup> (0.6% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 4400 km<sup>2</sup> (0.7% of the land area). By the middle of the century, changes reach 1000 km<sup>2</sup> under RCP2.6 and 2600 km<sup>2</sup> under RCP6.0.
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......@@ -64,7 +64,7 @@ Our definition of “drought” is quite strict, such that, without climate chan
However, at today’s level of 1°C global warming Canada’s annual land area affected by droughts is, on average, already larger and amount to 6200 km<sup>2</sup> (0.1% of the land area). The level of change ranges from -2.1% to 10.2% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Canada’s annual land area affected by droughts is projected to increase by 94500 km<sup>2</sup> (i.e. 1.0% of the land area) on average in comparison to a world without climate change. Under these conditions, 11.1% of the land area would be affected by droughts each year, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -187200 to 928500 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 64900 km<sup>2</sup> (0.7% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 11400 km<sup>2</sup> (0.7% of the land area). By the middle of the century, changes reach -14400 km<sup>2</sup> under RCP2.6 and 4800 km<sup>2</sup> under RCP6.0.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 64900 km<sup>2</sup> (0.7% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 11400 km<sup>2</sup> (0.1% of the land area). By the middle of the century, changes reach -14400 km<sup>2</sup> under RCP2.6 and 4800 km<sup>2</sup> under RCP6.0.
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......@@ -64,7 +64,7 @@ Our definition of “drought” is quite strict, such that, without climate chan
However, at today’s level of 1°C global warming Switzerland’s annual land area affected by droughts is, on average, already larger and amount to 100 km<sup>2</sup> (0.2% of the land area). The level of change ranges from -0.1% to 5.6% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Switzerland’s annual land area affected by droughts is projected to increase by 100 km<sup>2</sup> (i.e. 0.2% of the land area) on average in comparison to a world without climate change. Under these conditions, 0.1% of the land area would be affected by droughts each year, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -100 to 2200 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 100 km<sup>2</sup> (0.2% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 0 km<sup>2</sup> (0.2% of the land area). By the middle of the century, changes reach 0 km<sup>2</sup> under RCP2.6 and 0 km<sup>2</sup> under RCP6.0.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 100 km<sup>2</sup> (0.2% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 0 km<sup>2</sup> (0.0% of the land area). By the middle of the century, changes reach 0 km<sup>2</sup> under RCP2.6 and 0 km<sup>2</sup> under RCP6.0.
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......@@ -64,7 +64,7 @@ Our definition of “drought” is quite strict, such that, without climate chan
However, at today’s level of 1°C global warming Chile’s annual land area affected by droughts is, on average, already larger and amount to 22500 km<sup>2</sup> (3.0% of the land area). The level of change ranges from 0.5% to 15.7% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Chile’s annual land area affected by droughts is projected to increase by 40100 km<sup>2</sup> (i.e. 5.4% of the land area) on average in comparison to a world without climate change. Under these conditions, 16.4% of the land area would be affected by droughts each year, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from 3700 to 116500 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 86300 km<sup>2</sup> (11.6% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 25000 km<sup>2</sup> (11.6% of the land area). By the middle of the century, changes reach 35400 km<sup>2</sup> under RCP2.6 and 52800 km<sup>2</sup> under RCP6.0.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 86300 km<sup>2</sup> (11.6% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 25000 km<sup>2</sup> (3.4% of the land area). By the middle of the century, changes reach 35400 km<sup>2</sup> under RCP2.6 and 52800 km<sup>2</sup> under RCP6.0.
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......@@ -64,7 +64,7 @@ Our definition of “drought” is quite strict, such that, without climate chan
However, at today’s level of 1°C global warming China’s annual land area affected by droughts is, on average, already larger and amount to 107500 km<sup>2</sup> (1.1% of the land area). The level of change ranges from 0.0% to 14.6% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, China’s annual land area affected by droughts is projected to increase by 209200 km<sup>2</sup> (i.e. 2.2% of the land area) on average in comparison to a world without climate change. Under these conditions, 5.9% of the land area would be affected by droughts each year, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from 2200 to 1366400 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 407600 km<sup>2</sup> (4.3% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 357300 km<sup>2</sup> (4.3% of the land area). By the middle of the century, changes reach 229500 km<sup>2</sup> under RCP2.6 and 197200 km<sup>2</sup> under RCP6.0.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 407600 km<sup>2</sup> (4.3% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 357300 km<sup>2</sup> (3.8% of the land area). By the middle of the century, changes reach 229500 km<sup>2</sup> under RCP2.6 and 197200 km<sup>2</sup> under RCP6.0.
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......@@ -64,7 +64,7 @@ Our definition of “drought” is quite strict, such that, without climate chan
However, at today’s level of 1°C global warming Cote dIvoire’s annual land area affected by droughts is, on average, already larger and amount to 4900 km<sup>2</sup> (1.5% of the land area). The level of change ranges from -0.1% to 31.4% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Cote dIvoire’s annual land area affected by droughts is projected to increase by 11500 km<sup>2</sup> (i.e. 3.6% of the land area) on average in comparison to a world without climate change. Under these conditions, 2.8% of the land area would be affected by droughts each year, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -300 to 99800 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 12500 km<sup>2</sup> (3.9% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 8000 km<sup>2</sup> (3.9% of the land area). By the middle of the century, changes reach 6800 km<sup>2</sup> under RCP2.6 and 6900 km<sup>2</sup> under RCP6.0.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 12500 km<sup>2</sup> (3.9% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 8000 km<sup>2</sup> (2.5% of the land area). By the middle of the century, changes reach 6800 km<sup>2</sup> under RCP2.6 and 6900 km<sup>2</sup> under RCP6.0.
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......@@ -64,7 +64,7 @@ Our definition of “drought” is quite strict, such that, without climate chan
However, at today’s level of 1°C global warming Cameroon’s annual land area affected by droughts is, on average, already larger and amount to 2300 km<sup>2</sup> (0.5% of the land area). The level of change ranges from -0.1% to 7.3% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Cameroon’s annual land area affected by droughts is projected to increase by 2600 km<sup>2</sup> (i.e. 0.6% of the land area) on average in comparison to a world without climate change. Under these conditions, 1.0% of the land area would be affected by droughts each year, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -300 to 34700 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 8500 km<sup>2</sup> (1.8% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 7900 km<sup>2</sup> (1.8% of the land area). By the middle of the century, changes reach 3100 km<sup>2</sup> under RCP2.6 and 3700 km<sup>2</sup> under RCP6.0.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 8500 km<sup>2</sup> (1.8% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 7900 km<sup>2</sup> (1.7% of the land area). By the middle of the century, changes reach 3100 km<sup>2</sup> under RCP2.6 and 3700 km<sup>2</sup> under RCP6.0.
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......@@ -64,7 +64,7 @@ Our definition of “drought” is quite strict, such that, without climate chan
However, at today’s level of 1°C global warming Congo’s annual land area affected by droughts is, on average, already larger and amount to 1300 km<sup>2</sup> (0.4% of the land area). The level of change ranges from -0.2% to 17.8% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Congo’s annual land area affected by droughts is projected to increase by 1400 km<sup>2</sup> (i.e. 0.4% of the land area) on average in comparison to a world without climate change. Under these conditions, 0.6% of the land area would be affected by droughts each year, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -600 to 60700 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 3300 km<sup>2</sup> (1.0% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 3200 km<sup>2</sup> (1.0% of the land area). By the middle of the century, changes reach 3100 km<sup>2</sup> under RCP2.6 and 2300 km<sup>2</sup> under RCP6.0.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 3300 km<sup>2</sup> (1.0% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 3200 km<sup>2</sup> (0.9% of the land area). By the middle of the century, changes reach 3100 km<sup>2</sup> under RCP2.6 and 2300 km<sup>2</sup> under RCP6.0.
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......@@ -64,7 +64,7 @@ Our definition of “drought” is quite strict, such that, without climate chan
However, at today’s level of 1°C global warming Cape Verde’s annual land area affected by droughts is, on average, already larger and amount to 0 km<sup>2</sup> (0.4% of the land area). The level of change ranges from -1.9% to 42.1% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Cape Verde’s annual land area affected by droughts is projected to increase by 0 km<sup>2</sup> (i.e. 0.4% of the land area) on average in comparison to a world without climate change. Under these conditions, 0% of the land area would be affected by droughts each year, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -100 to 1700 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 0 km<sup>2</sup> (1.0% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 0 km<sup>2</sup> (1.0% of the land area). By the middle of the century, changes reach 0 km<sup>2</sup> under RCP2.6 and 0 km<sup>2</sup> under RCP6.0.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 0 km<sup>2</sup> (1.0% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 0 km<sup>2</sup> (0.0% of the land area). By the middle of the century, changes reach 0 km<sup>2</sup> under RCP2.6 and 0 km<sup>2</sup> under RCP6.0.
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......@@ -64,7 +64,7 @@ Our definition of “drought” is quite strict, such that, without climate chan
However, at today’s level of 1°C global warming Costa Rica’s annual land area affected by droughts is, on average, already larger and amount to 100 km<sup>2</sup> (0.2% of the land area). The level of change ranges from -2.2% to 2.9% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Costa Rica’s annual land area affected by droughts is projected to increase by 0 km<sup>2</sup> (i.e. 0.0% of the land area) on average in comparison to a world without climate change. Under these conditions, 0.1% of the land area would be affected by droughts each year, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -1100 to 1500 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 0 km<sup>2</sup> (0.1% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 0 km<sup>2</sup> (0.1% of the land area). By the middle of the century, changes reach 400 km<sup>2</sup> under RCP2.6 and -100 km<sup>2</sup> under RCP6.0.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 0 km<sup>2</sup> (0.1% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 0 km<sup>2</sup> (0.0% of the land area). By the middle of the century, changes reach 400 km<sup>2</sup> under RCP2.6 and -100 km<sup>2</sup> under RCP6.0.
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......@@ -64,7 +64,7 @@ Our definition of “drought” is quite strict, such that, without climate chan
However, at today’s level of 1°C global warming Cuba’s annual land area affected by droughts is, on average, already larger and amount to 200 km<sup>2</sup> (0.2% of the land area). The level of change ranges from -0.0% to 17.4% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Cuba’s annual land area affected by droughts is projected to increase by 1000 km<sup>2</sup> (i.e. 0.9% of the land area) on average in comparison to a world without climate change. Under these conditions, 1.2% of the land area would be affected by droughts each year, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from 0 to 18300 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 3000 km<sup>2</sup> (2.9% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 0 km<sup>2</sup> (2.9% of the land area). By the middle of the century, changes reach 300 km<sup>2</sup> under RCP2.6 and 200 km<sup>2</sup> under RCP6.0.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 3000 km<sup>2</sup> (2.9% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 0 km<sup>2</sup> (0.0% of the land area). By the middle of the century, changes reach 300 km<sup>2</sup> under RCP2.6 and 200 km<sup>2</sup> under RCP6.0.
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......@@ -64,7 +64,7 @@ Our definition of “drought” is quite strict, such that, without climate chan
However, at today’s level of 1°C global warming Cyprus’ annual land area affected by droughts is, on average, already larger and amount to 300 km<sup>2</sup> (3.1% of the land area). The level of change ranges from 0.0% to 23.3% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Cyprus’ annual land area affected by droughts is projected to increase by 900 km<sup>2</sup> (i.e. 9.3% of the land area) on average in comparison to a world without climate change. Under these conditions, 15.3% of the land area would be affected by droughts each year, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from 0 to 2200 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 1600 km<sup>2</sup> (16.7% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 800 km<sup>2</sup> (16.7% of the land area). By the middle of the century, changes reach 1000 km<sup>2</sup> under RCP2.6 and 600 km<sup>2</sup> under RCP6.0.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 1600 km<sup>2</sup> (16.7% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 800 km<sup>2</sup> (8.7% of the land area). By the middle of the century, changes reach 1000 km<sup>2</sup> under RCP2.6 and 600 km<sup>2</sup> under RCP6.0.
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......@@ -64,7 +64,7 @@ Our definition of “drought” is quite strict, such that, without climate chan
However, at today’s level of 1°C global warming Czech Republic’s annual land area affected by droughts is, on average, already larger and amount to 0 km<sup>2</sup> (0.1% of the land area). The level of change ranges from -0.8% to 12.5% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Czech Republic’s annual land area affected by droughts is projected to increase by 200 km<sup>2</sup> (i.e. 0.2% of the land area) on average in comparison to a world without climate change. Under these conditions, 0.3% of the land area would be affected by droughts each year, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -600 to 9700 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 500 km<sup>2</sup> (0.7% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 300 km<sup>2</sup> (0.7% of the land area). By the middle of the century, changes reach 0 km<sup>2</sup> under RCP2.6 and 200 km<sup>2</sup> under RCP6.0.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 500 km<sup>2</sup> (0.7% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 300 km<sup>2</sup> (0.4% of the land area). By the middle of the century, changes reach 0 km<sup>2</sup> under RCP2.6 and 200 km<sup>2</sup> under RCP6.0.
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......@@ -64,7 +64,7 @@ Our definition of “drought” is quite strict, such that, without climate chan
However, at today’s level of 1°C global warming Germany’s annual land area affected by droughts is, on average, already larger and amount to 200 km<sup>2</sup> (0.0% of the land area). The level of change ranges from -0.7% to 1.6% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Germany’s annual land area affected by droughts is projected to increase by 800 km<sup>2</sup> (i.e. 0.2% of the land area) on average in comparison to a world without climate change. Under these conditions, 0.6% of the land area would be affected by droughts each year, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -2600 to 5600 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to decrease by 0 km<sup>2</sup> (0.0% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 900 km<sup>2</sup> (0.0% of the land area). By the middle of the century, changes reach 0 km<sup>2</sup> under RCP2.6 and 0 km<sup>2</sup> under RCP6.0.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to decrease by 0 km<sup>2</sup> (0.0% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 900 km<sup>2</sup> (0.3% of the land area). By the middle of the century, changes reach 0 km<sup>2</sup> under RCP2.6 and 0 km<sup>2</sup> under RCP6.0.
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......@@ -64,7 +64,7 @@ Our definition of “drought” is quite strict, such that, without climate chan
However, at today’s level of 1°C global warming Dominican Republic’s annual land area affected by droughts is, on average, already larger and amount to 100 km<sup>2</sup> (0.3% of the land area). The level of change ranges from -1.0% to 4.1% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Dominican Republic’s annual land area affected by droughts is projected to increase by 100 km<sup>2</sup> (i.e. 0.2% of the land area) on average in comparison to a world without climate change. Under these conditions, 0.9% of the land area would be affected by droughts each year, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -500 to 2000 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 100 km<sup>2</sup> (0.2% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 0 km<sup>2</sup> (0.2% of the land area). By the middle of the century, changes reach 700 km<sup>2</sup> under RCP2.6 and 0 km<sup>2</sup> under RCP6.0.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 100 km<sup>2</sup> (0.2% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 0 km<sup>2</sup> (0.0% of the land area). By the middle of the century, changes reach 700 km<sup>2</sup> under RCP2.6 and 0 km<sup>2</sup> under RCP6.0.
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......@@ -64,7 +64,7 @@ Our definition of “drought” is quite strict, such that, without climate chan
However, at today’s level of 1°C global warming Algeria’s annual land area affected by droughts is, on average, already larger and amount to 74100 km<sup>2</sup> (3.1% of the land area). The level of change ranges from 0.0% to 34.7% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Algeria’s annual land area affected by droughts is projected to increase by 135600 km<sup>2</sup> (i.e. 5.7% of the land area) on average in comparison to a world without climate change. Under these conditions, 22.6% of the land area would be affected by droughts each year, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from 0 to 825800 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 305400 km<sup>2</sup> (12.8% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 80900 km<sup>2</sup> (12.8% of the land area). By the middle of the century, changes reach 58500 km<sup>2</sup> under RCP2.6 and 175400 km<sup>2</sup> under RCP6.0.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 305400 km<sup>2</sup> (12.8% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 80900 km<sup>2</sup> (3.4% of the land area). By the middle of the century, changes reach 58500 km<sup>2</sup> under RCP2.6 and 175400 km<sup>2</sup> under RCP6.0.
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......@@ -64,7 +64,7 @@ Our definition of “drought” is quite strict, such that, without climate chan
However, at today’s level of 1°C global warming Ecuador’s annual land area affected by droughts is, on average, already smaller and amount to 0 km<sup>2</sup> (-0.0% of the land area). The level of change ranges from -0.5% to 7.8% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Ecuador’s annual land area affected by droughts is projected to increase by 200 km<sup>2</sup> (i.e. 0.1% of the land area) on average in comparison to a world without climate change. Under these conditions, 0.0% of the land area would be affected by droughts each year, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -1200 to 19400 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 100 km<sup>2</sup> (0.1% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 0 km<sup>2</sup> (0.1% of the land area). By the middle of the century, changes reach 600 km<sup>2</sup> under RCP2.6 and 0 km<sup>2</sup> under RCP6.0.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 100 km<sup>2</sup> (0.1% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 0 km<sup>2</sup> (0.0% of the land area). By the middle of the century, changes reach 600 km<sup>2</sup> under RCP2.6 and 0 km<sup>2</sup> under RCP6.0.
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......@@ -64,7 +64,7 @@ Our definition of “drought” is quite strict, such that, without climate chan
However, at today’s level of 1°C global warming Egypt’s annual land area affected by droughts is, on average, already larger and amount to 24100 km<sup>2</sup> (2.4% of the land area). The level of change ranges from 0.0% to 27.4% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Egypt’s annual land area affected by droughts is projected to increase by 51800 km<sup>2</sup> (i.e. 5.2% of the land area) on average in comparison to a world without climate change. Under these conditions, 39.7% of the land area would be affected by droughts each year, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from 0 to 273200 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 109300 km<sup>2</sup> (11.0% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 39100 km<sup>2</sup> (11.0% of the land area). By the middle of the century, changes reach 47200 km<sup>2</sup> under RCP2.6 and 43700 km<sup>2</sup> under RCP6.0.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 109300 km<sup>2</sup> (11.0% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 39100 km<sup>2</sup> (3.9% of the land area). By the middle of the century, changes reach 47200 km<sup>2</sup> under RCP2.6 and 43700 km<sup>2</sup> under RCP6.0.
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......@@ -64,7 +64,7 @@ Our definition of “drought” is quite strict, such that, without climate chan
However, at today’s level of 1°C global warming Eritrea’s annual land area affected by droughts is, on average, already larger and amount to 900 km<sup>2</sup> (0.9% of the land area). The level of change ranges from -1.8% to 14.5% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Eritrea’s annual land area affected by droughts is projected to increase by 600 km<sup>2</sup> (i.e. 0.5% of the land area) on average in comparison to a world without climate change. Under these conditions, 4.7% of the land area would be affected by droughts each year, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -1800 to 14700 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 600 km<sup>2</sup> (0.6% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 700 km<sup>2</sup> (0.6% of the land area). By the middle of the century, changes reach 1000 km<sup>2</sup> under RCP2.6 and 1700 km<sup>2</sup> under RCP6.0.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 600 km<sup>2</sup> (0.6% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 700 km<sup>2</sup> (0.7% of the land area). By the middle of the century, changes reach 1000 km<sup>2</sup> under RCP2.6 and 1700 km<sup>2</sup> under RCP6.0.
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......@@ -64,7 +64,7 @@ Our definition of “drought” is quite strict, such that, without climate chan
However, at today’s level of 1°C global warming Western Sahara’s annual land area affected by droughts is, on average, already larger and amount to 0 km<sup>2</sup> (1.0% of the land area). The level of change ranges from -0.1% to 46.0% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Western Sahara’s annual land area affected by droughts is projected to increase by 0 km<sup>2</sup> (i.e. 1.9% of the land area) on average in comparison to a world without climate change. Under these conditions, 13.1% of the land area would be affected by droughts each year, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from 0 to 0 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 0 km<sup>2</sup> (4.1% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 0 km<sup>2</sup> (4.1% of the land area). By the middle of the century, changes reach 0 km<sup>2</sup> under RCP2.6 and 0 km<sup>2</sup> under RCP6.0.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 0 km<sup>2</sup> (4.1% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 0 km<sup>2</sup> (4.3% of the land area). By the middle of the century, changes reach 0 km<sup>2</sup> under RCP2.6 and 0 km<sup>2</sup> under RCP6.0.
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