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 Spain’s annual land area affected by droughts is, on average, already larger and amount to 11500 km<sup>2</sup> (2.3% of the land area). The level of change ranges from 0.1% to 25.9% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Spain’s annual land area affected by droughts is projected to increase by 24500 km<sup>2</sup> (i.e. 4.9% of the land area) on average in comparison to a world without climate change. Under these conditions, 4.8% 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 600 to 129200 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 52000 km<sup>2</sup> (10.4% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 10800 km<sup>2</sup> (10.4% of the land area). By the middle of the century, changes reach 11400 km<sup>2</sup> under RCP2.6 and 12600 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 52000 km<sup>2</sup> (10.4% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 10800 km<sup>2</sup> (2.2% of the land area). By the middle of the century, changes reach 11400 km<sup>2</sup> under RCP2.6 and 12600 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 Estonia’s annual land area affected by droughts is, on average, already smaller and amount to 0 km<sup>2</sup> (-0.1% of the land area). The level of change ranges from -1.8% to 1.2% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Estonia’s annual land area affected by droughts is projected to decrease by 0 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, 0.5% 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 -800 to 500 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to decrease 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 -100 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 -100 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 -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 -100 km<sup>2</sup> (-0.1% of the land area). By the middle of the century, changes reach 0 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 Ethiopia’s annual land area affected by droughts is, on average, already larger and amount to 3500 km<sup>2</sup> (0.3% of the land area). The level of change ranges from -1.0% to 4.5% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Ethiopia’s annual land area affected by droughts is projected to increase by 1400 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, 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 -10100 to 44700 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 1800 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 4000 km<sup>2</sup> (0.2% of the land area). By the middle of the century, changes reach 3100 km<sup>2</sup> under RCP2.6 and 2500 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 1800 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 4000 km<sup>2</sup> (0.4% of the land area). By the middle of the century, changes reach 3100 km<sup>2</sup> under RCP2.6 and 2500 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 Fiji’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 -0.8% to 5.6% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Fiji’s annual land area affected by droughts is projected to increase by 0 km<sup>2</sup> (i.e. 0.3% 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 1000 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 0 km<sup>2</sup> (0.0% of the land area). By the middle of the century, changes reach -100 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 0 km<sup>2</sup> (0.1% of the land area). By the middle of the century, changes reach -100 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 France’s annual land area affected by droughts is, on average, already larger and amount to 1400 km<sup>2</sup> (0.3% of the land area). The level of change ranges from 0.0% to 5.8% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, France’s annual land area affected by droughts is projected to increase by 2600 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, 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 0 to 31600 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 5600 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 1400 km<sup>2</sup> (1.0% of the land area). By the middle of the century, changes reach 2400 km<sup>2</sup> under RCP2.6 and 800 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 5600 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 1400 km<sup>2</sup> (0.3% of the land area). By the middle of the century, changes reach 2400 km<sup>2</sup> under RCP2.6 and 800 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 Georgia’s annual land area affected by droughts is, on average, already larger and amount to 1000 km<sup>2</sup> (1.7% of the land area). The level of change ranges from -1.1% to 17.4% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Georgia’s annual land area affected by droughts is projected to increase by 900 km<sup>2</sup> (i.e. 1.7% of the land area) on average in comparison to a world without climate change. Under these conditions, 1.3% 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 9800 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 1700 km<sup>2</sup> (3.0% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 800 km<sup>2</sup> (3.0% of the land area). By the middle of the century, changes reach 700 km<sup>2</sup> under RCP2.6 and 800 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 1700 km<sup>2</sup> (3.0% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 800 km<sup>2</sup> (1.5% of the land area). By the middle of the century, changes reach 700 km<sup>2</sup> under RCP2.6 and 800 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 Ghana’s annual land area affected by droughts is, on average, already larger and amount to 3300 km<sup>2</sup> (1.5% of the land area). The level of change ranges from 0.3% to 37.1% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Ghana’s annual land area affected by droughts is projected to increase by 10300 km<sup>2</sup> (i.e. 4.5% of the land area) on average in comparison to a world without climate change. Under these conditions, 2.2% 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 600 to 84500 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 11100 km<sup>2</sup> (4.9% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 7700 km<sup>2</sup> (4.9% of the land area). By the middle of the century, changes reach 4000 km<sup>2</sup> under RCP2.6 and 7500 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 11100 km<sup>2</sup> (4.9% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 7700 km<sup>2</sup> (3.4% of the land area). By the middle of the century, changes reach 4000 km<sup>2</sup> under RCP2.6 and 7500 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 Guinea’s annual land area affected by droughts is, on average, already larger and amount to 800 km<sup>2</sup> (0.3% of the land area). The level of change ranges from -0.9% to 26.5% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Guinea’s annual land area affected by droughts is projected to increase by 1700 km<sup>2</sup> (i.e. 0.7% 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 -2100 to 65200 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 900 km<sup>2</sup> (0.4% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 2900 km<sup>2</sup> (0.4% of the land area). By the middle of the century, changes reach 1100 km<sup>2</sup> under RCP2.6 and 2800 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 900 km<sup>2</sup> (0.4% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 2900 km<sup>2</sup> (1.2% of the land area). By the middle of the century, changes reach 1100 km<sup>2</sup> under RCP2.6 and 2800 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 Gambia’s annual land area affected by droughts is, on average, already larger and amount to 100 km<sup>2</sup> (1.0% of the land area). The level of change ranges from -4.6% to 32.7% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Gambia’s annual land area affected by droughts is projected to increase by 200 km<sup>2</sup> (i.e. 1.7% of the land area) on average in comparison to a world without climate change. Under these conditions, 5.0% 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 -500 to 3300 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 300 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 200 km<sup>2</sup> (2.9% 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 300 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 200 km<sup>2</sup> (1.6% 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 Guinea-Bissau’s annual land area affected by droughts is, on average, already larger and amount to 100 km<sup>2</sup> (0.4% of the land area). The level of change ranges from -3.1% to 33.2% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Guinea-Bissau’s annual land area affected by droughts is projected to increase by 500 km<sup>2</sup> (i.e. 1.7% 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 -900 to 9300 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 800 km<sup>2</sup> (2.8% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 300 km<sup>2</sup> (2.8% of the land area). By the middle of the century, changes reach 500 km<sup>2</sup> under RCP2.6 and 1100 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 800 km<sup>2</sup> (2.8% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 300 km<sup>2</sup> (0.9% of the land area). By the middle of the century, changes reach 500 km<sup>2</sup> under RCP2.6 and 1100 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 Greece’s annual land area affected by droughts is, on average, already larger and amount to 2400 km<sup>2</sup> (1.9% of the land area). The level of change ranges from 0.0% to 27.1% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Greece’s annual land area affected by droughts is projected to increase by 4200 km<sup>2</sup> (i.e. 3.3% of the land area) on average in comparison to a world without climate change. Under these conditions, 1.8% 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 0 to 34900 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 12700 km<sup>2</sup> (9.9% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 4800 km<sup>2</sup> (9.9% of the land area). By the middle of the century, changes reach 3200 km<sup>2</sup> under RCP2.6 and 5100 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 12700 km<sup>2</sup> (9.9% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 4800 km<sup>2</sup> (3.8% of the land area). By the middle of the century, changes reach 3200 km<sup>2</sup> under RCP2.6 and 5100 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 Greenland’s annual land area affected by droughts is, on average, already larger and amount to 6000 km<sup>2</sup> (1.4% of the land area). The level of change ranges from -1.9% to 17.5% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Greenland’s annual land area affected by droughts is projected to increase by 7100 km<sup>2</sup> (i.e. 1.6% of the land area) on average in comparison to a world without climate change. Under these conditions, 2.7% 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 -8100 to 75100 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 9900 km<sup>2</sup> (2.3% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 9100 km<sup>2</sup> (2.3% of the land area). By the middle of the century, changes reach 7900 km<sup>2</sup> under RCP2.6 and 7300 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 9900 km<sup>2</sup> (2.3% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 9100 km<sup>2</sup> (2.1% of the land area). By the middle of the century, changes reach 7900 km<sup>2</sup> under RCP2.6 and 7300 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 Guatemala’s annual land area affected by droughts is, on average, already larger and amount to 300 km<sup>2</sup> (0.2% of the land area). The level of change ranges from 0.0% to 8.4% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Guatemala’s annual land area affected by droughts is projected to increase by 800 km<sup>2</sup> (i.e. 0.7% 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 0 to 9000 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 3500 km<sup>2</sup> (3.2% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach -200 km<sup>2</sup> (3.2% of the land area). By the middle of the century, changes reach 0 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 3500 km<sup>2</sup> (3.2% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach -200 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 -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 French Guiana’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 0.0% to 18.1% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, French Guiana’s annual land area affected by droughts is projected to increase by 0 km<sup>2</sup> (i.e. 1.4% of the land area) on average in comparison to a world without climate change. Under these conditions, 3.0% 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 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> (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 0 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> (1.6% 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 Guyana’s annual land area affected by droughts is, on average, already larger and amount to 1400 km<sup>2</sup> (0.7% of the land area). The level of change ranges from -0.0% to 23.6% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Guyana’s annual land area affected by droughts is projected to increase by 3200 km<sup>2</sup> (i.e. 1.6% of the land area) on average in comparison to a world without climate change. Under these conditions, 4.3% 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 -100 to 46600 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 8600 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 3100 km<sup>2</sup> (4.3% of the land area). By the middle of the century, changes reach 4500 km<sup>2</sup> under RCP2.6 and 1800 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 8600 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 3100 km<sup>2</sup> (1.6% of the land area). By the middle of the century, changes reach 4500 km<sup>2</sup> under RCP2.6 and 1800 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 Honduras’ annual land area affected by droughts is, on average, already larger and amount to 100 km<sup>2</sup> (0.0% of the land area). The level of change ranges from -0.6% to 13.7% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Honduras’ annual land area affected by droughts is projected to increase by 100 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, 1.4% 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 -700 to 15300 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 200 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 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 200 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 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 Croatia’s annual land area affected by droughts is, on average, already larger and amount to 400 km<sup>2</sup> (0.8% of the land area). The level of change ranges from -0.0% to 18.0% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Croatia’s annual land area affected by droughts is projected to increase by 1000 km<sup>2</sup> (i.e. 1.7% of the land area) on average in comparison to a world without climate change. Under these conditions, 0.7% 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 10100 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 2000 km<sup>2</sup> (3.6% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 200 km<sup>2</sup> (3.6% of the land area). By the middle of the century, changes reach 500 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 2000 km<sup>2</sup> (3.6% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 200 km<sup>2</sup> (0.4% of the land area). By the middle of the century, changes reach 500 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 Hungary’s annual land area affected by droughts is, on average, already larger and amount to 500 km<sup>2</sup> (0.6% of the land area). The level of change ranges from -0.4% to 22.9% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Hungary’s annual land area affected by droughts is projected to increase by 1700 km<sup>2</sup> (i.e. 1.8% of the land area) on average in comparison to a world without climate change. Under these conditions, 2.2% 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 -400 to 20800 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 3400 km<sup>2</sup> (3.8% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 100 km<sup>2</sup> (3.8% of the land area). By the middle of the century, changes reach 1100 km<sup>2</sup> under RCP2.6 and 900 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 3400 km<sup>2</sup> (3.8% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 100 km<sup>2</sup> (0.1% of the land area). By the middle of the century, changes reach 1100 km<sup>2</sup> under RCP2.6 and 900 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 Indonesia’s annual land area affected by droughts is, on average, already larger and amount to 2100 km<sup>2</sup> (0.1% of the land area). The level of change ranges from -0.2% to 2.4% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Indonesia’s annual land area affected by droughts is projected to increase by 3400 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 -3200 to 44300 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 300 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 2900 km<sup>2</sup> (0.0% of the land area). By the middle of the century, changes reach 4000 km<sup>2</sup> under RCP2.6 and -800 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 300 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 2900 km<sup>2</sup> (0.2% of the land area). By the middle of the century, changes reach 4000 km<sup>2</sup> under RCP2.6 and -800 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 India’s annual land area affected by droughts is, on average, already larger and amount to 8600 km<sup>2</sup> (0.3% of the land area). The level of change ranges from -0.7% to 8.1% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, India’s annual land area affected by droughts is projected to increase by 11400 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, 0.9% 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 -21200 to 241600 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 34300 km<sup>2</sup> (1.2% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 30900 km<sup>2</sup> (1.2% of the land area). By the middle of the century, changes reach 2900 km<sup>2</sup> under RCP2.6 and 13400 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 34300 km<sup>2</sup> (1.2% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 30900 km<sup>2</sup> (1.0% of the land area). By the middle of the century, changes reach 2900 km<sup>2</sup> under RCP2.6 and 13400 km<sup>2</sup> under RCP6.0.
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