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 Morocco’s annual land area affected by droughts is, on average, already larger and amount to 20000 km<sup>2</sup> (4.5% of the land area). The level of change ranges from 0.1% to 40.6% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Morocco’s annual land area affected by droughts is projected to increase by 54600 km<sup>2</sup> (i.e. 12.2% of the land area) on average in comparison to a world without climate change. Under these conditions, 30.6% 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 400 to 181100 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 87300 km<sup>2</sup> (19.6% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 21300 km<sup>2</sup> (19.6% of the land area). By the middle of the century, changes reach 28400 km<sup>2</sup> under RCP2.6 and 36100 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 87300 km<sup>2</sup> (19.6% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 21300 km<sup>2</sup> (4.8% of the land area). By the middle of the century, changes reach 28400 km<sup>2</sup> under RCP2.6 and 36100 km<sup>2</sup> under RCP6.0.
......
......@@ -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 Moldova’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 -1.2% to 27.7% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Moldova’s annual land area affected by droughts is projected to increase 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, 0.6% 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 -300 to 8000 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 100 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 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 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 100 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 100 km<sup>2</sup> under RCP6.0.
......
......@@ -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 Madagascar’s annual land area affected by droughts is, on average, already larger and amount to 1900 km<sup>2</sup> (0.3% of the land area). The level of change ranges from 0.0% to 8.2% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Madagascar’s annual land area affected by droughts is projected to increase by 7400 km<sup>2</sup> (i.e. 1.3% of the land area) on average in comparison to a world without climate change. Under these conditions, 0.4% 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 200 to 47700 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 20800 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 4700 km<sup>2</sup> (3.6% of the land area). By the middle of the century, changes reach 6600 km<sup>2</sup> under RCP2.6 and 3400 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 20800 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 4700 km<sup>2</sup> (0.8% of the land area). By the middle of the century, changes reach 6600 km<sup>2</sup> under RCP2.6 and 3400 km<sup>2</sup> under RCP6.0.
......
......@@ -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 Mexico’s annual land area affected by droughts is, on average, already larger and amount to 30000 km<sup>2</sup> (1.5% of the land area). The level of change ranges from -0.2% to 10.7% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Mexico’s annual land area affected by droughts is projected to increase by 56400 km<sup>2</sup> (i.e. 2.9% of the land area) on average in comparison to a world without climate change. Under these conditions, 3.9% 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 -3100 to 208900 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 96000 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 42200 km<sup>2</sup> (4.9% of the land area). By the middle of the century, changes reach 35200 km<sup>2</sup> under RCP2.6 and 68000 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 96000 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 42200 km<sup>2</sup> (2.2% of the land area). By the middle of the century, changes reach 35200 km<sup>2</sup> under RCP2.6 and 68000 km<sup>2</sup> under RCP6.0.
......
......@@ -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 Macedonia’s annual land area affected by droughts is, on average, already larger and amount to 200 km<sup>2</sup> (1.0% of the land area). The level of change ranges from 0.0% to 13.9% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Macedonia’s annual land area affected by droughts is projected to increase by 700 km<sup>2</sup> (i.e. 2.9% of the land area) on average in comparison to a world without climate change. Under these conditions, 1.6% 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 3500 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 1100 km<sup>2</sup> (4.5% 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> (4.5% 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 1100 km<sup>2</sup> (4.5% 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> (3.3% 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.
......
......@@ -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 Mali’s annual land area affected by droughts is, on average, already larger and amount to 16300 km<sup>2</sup> (1.3% of the land area). The level of change ranges from -1.7% to 12.4% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Mali’s annual land area affected by droughts is projected to increase by 23500 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, 12.9% 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 -20600 to 151400 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 46600 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 39900 km<sup>2</sup> (3.8% of the land area). By the middle of the century, changes reach 35800 km<sup>2</sup> under RCP2.6 and 21200 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 46600 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 39900 km<sup>2</sup> (3.3% of the land area). By the middle of the century, changes reach 35800 km<sup>2</sup> under RCP2.6 and 21200 km<sup>2</sup> under RCP6.0.
......
......@@ -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 Myanmar’s annual land area affected by droughts is, on average, already larger and amount to 3000 km<sup>2</sup> (0.5% of the land area). The level of change ranges from -0.4% to 10.6% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Myanmar’s annual land area affected by droughts is projected to increase by 4700 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, 0.5% 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 -2600 to 69000 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> (0.5% 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> (0.5% of the land area). By the middle of the century, changes reach 3200 km<sup>2</sup> under RCP2.6 and 1200 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> (0.5% 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> (1.2% of the land area). By the middle of the century, changes reach 3200 km<sup>2</sup> under RCP2.6 and 1200 km<sup>2</sup> under RCP6.0.
......
......@@ -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 Montenegro’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 -0.3% to 1.8% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Montenegro’s annual land area affected by droughts is projected to increase 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% 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 200 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> (0.4% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 0 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 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> (0.4% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 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.
......
......@@ -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 Mongolia’s annual land area affected by droughts is, on average, already larger and amount to 24400 km<sup>2</sup> (1.6% of the land area). The level of change ranges from -0.7% to 25.1% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Mongolia’s annual land area affected by droughts is projected to increase by 45900 km<sup>2</sup> (i.e. 2.9% of the land area) on average in comparison to a world without climate change. Under these conditions, 8.0% 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 -11100 to 391000 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 71100 km<sup>2</sup> (4.6% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 32000 km<sup>2</sup> (4.6% of the land area). By the middle of the century, changes reach 34600 km<sup>2</sup> under RCP2.6 and 24100 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 71100 km<sup>2</sup> (4.6% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 32000 km<sup>2</sup> (2.1% of the land area). By the middle of the century, changes reach 34600 km<sup>2</sup> under RCP2.6 and 24100 km<sup>2</sup> under RCP6.0.
......
......@@ -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 Mozambique’s annual land area affected by droughts is, on average, already larger and amount to 2600 km<sup>2</sup> (0.3% of the land area). The level of change ranges from -0.0% to 12.1% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Mozambique’s annual land area affected by droughts is projected to increase by 3900 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, 0.4% 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 -100 to 95200 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 6600 km<sup>2</sup> (0.8% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 5500 km<sup>2</sup> (0.8% of the land area). By the middle of the century, changes reach 2400 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 6600 km<sup>2</sup> (0.8% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 5500 km<sup>2</sup> (0.7% of the land area). By the middle of the century, changes reach 2400 km<sup>2</sup> under RCP2.6 and 100 km<sup>2</sup> under RCP6.0.
......
......@@ -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 Mauritania’s annual land area affected by droughts is, on average, already larger and amount to 15100 km<sup>2</sup> (1.5% of the land area). The level of change ranges from -6.0% to 8.5% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Mauritania’s annual land area affected by droughts is projected to increase by 26900 km<sup>2</sup> (i.e. 2.6% of the land area) on average in comparison to a world without climate change. Under these conditions, 18.4% 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 -61500 to 87300 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 32700 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 38100 km<sup>2</sup> (3.2% of the land area). By the middle of the century, changes reach 21700 km<sup>2</sup> under RCP2.6 and 17600 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 32700 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 38100 km<sup>2</sup> (3.7% of the land area). By the middle of the century, changes reach 21700 km<sup>2</sup> under RCP2.6 and 17600 km<sup>2</sup> under RCP6.0.
......
......@@ -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 Mauritius’ annual land area affected by droughts is, on average, already larger and amount to 0 km<sup>2</sup> (0.0% of the land area). The level of change ranges from -0.4% to 2.4% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Mauritius’ 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, 0.6% 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 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> (1.3% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 0 km<sup>2</sup> (1.3% 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.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 0 km<sup>2</sup> (1.3% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 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.
......
......@@ -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 Malawi’s annual land area affected by droughts is, on average, already larger and amount to 300 km<sup>2</sup> (0.3% of the land area). The level of change ranges from -0.3% to 21.0% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Malawi’s annual land area affected by droughts is projected to increase by 700 km<sup>2</sup> (i.e. 0.8% 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 -300 to 19800 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> (0.5% 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> (0.5% of the land area). By the middle of the century, changes reach 400 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 500 km<sup>2</sup> (0.5% 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> (0.3% of the land area). By the middle of the century, changes reach 400 km<sup>2</sup> under RCP2.6 and 0 km<sup>2</sup> under RCP6.0.
......
......@@ -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 Malaysia’s annual land area affected by droughts is, on average, already larger and amount to 800 km<sup>2</sup> (0.2% of the land area). The level of change ranges from -0.0% to 2.4% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Malaysia’s annual land area affected by droughts is projected to increase by 500 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 0 to 7800 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> (0.2% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 400 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 increase by 500 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 400 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.
......
......@@ -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 Namibia’s annual land area affected by droughts is, on average, already larger and amount to 9400 km<sup>2</sup> (1.1% of the land area). The level of change ranges from -0.5% to 29.1% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Namibia’s annual land area affected by droughts is projected to increase by 15500 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, 3.5% 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 -4500 to 238800 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 17000 km<sup>2</sup> (2.1% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 9900 km<sup>2</sup> (2.1% of the land area). By the middle of the century, changes reach 2600 km<sup>2</sup> under RCP2.6 and 13900 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 17000 km<sup>2</sup> (2.1% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 9900 km<sup>2</sup> (1.2% of the land area). By the middle of the century, changes reach 2600 km<sup>2</sup> under RCP2.6 and 13900 km<sup>2</sup> under RCP6.0.
......
......@@ -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 New Caledonia’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 -0.2% to 4.6% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, New Caledonia’s annual land area affected by droughts is projected to increase by 0 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, 0.5% 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 0 to 800 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 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 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.
......
......@@ -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 Niger’s annual land area affected by droughts is, on average, already larger and amount to 7400 km<sup>2</sup> (0.6% of the land area). The level of change ranges from -16.4% to 25.9% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Niger’s annual land area affected by droughts is projected to increase by 20900 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, 14.1% 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 -207800 to 328300 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 81500 km<sup>2</sup> (6.4% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 26500 km<sup>2</sup> (6.4% of the land area). By the middle of the century, changes reach 18100 km<sup>2</sup> under RCP2.6 and 25000 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 81500 km<sup>2</sup> (6.4% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 26500 km<sup>2</sup> (2.1% of the land area). By the middle of the century, changes reach 18100 km<sup>2</sup> under RCP2.6 and 25000 km<sup>2</sup> under RCP6.0.
......
......@@ -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 Nigeria’s annual land area affected by droughts is, on average, already larger and amount to 8200 km<sup>2</sup> (0.9% of the land area). The level of change ranges from 0.0% to 26.1% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Nigeria’s annual land area affected by droughts is projected to increase by 8700 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, 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 0 to 238000 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 24900 km<sup>2</sup> (2.7% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 34800 km<sup>2</sup> (2.7% of the land area). By the middle of the century, changes reach 13700 km<sup>2</sup> under RCP2.6 and 12800 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 24900 km<sup>2</sup> (2.7% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 34800 km<sup>2</sup> (3.8% of the land area). By the middle of the century, changes reach 13700 km<sup>2</sup> under RCP2.6 and 12800 km<sup>2</sup> under RCP6.0.
......
......@@ -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 Nicaragua’s annual land area affected by droughts is, on average, already smaller and amount to -100 km<sup>2</sup> (-0.1% of the land area). The level of change ranges from -1.5% to 3.9% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Nicaragua’s 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, 0.4% 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 -1800 to 4600 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 400 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.
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 400 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 -100 km<sup>2</sup> under RCP6.0.
......
......@@ -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 Norway’s annual land area affected by droughts is, on average, already smaller and amount to -500 km<sup>2</sup> (-0.1% of the land area). The level of change ranges from -1.3% to 4.8% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Norway’s annual land area affected by droughts is projected to decrease by -1100 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, 0.8% 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 -4900 to 17400 km<sup>2</sup>.
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to decrease by -1200 km<sup>2</sup> (-0.3% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach -1600 km<sup>2</sup> (-0.3% of the land area). By the middle of the century, changes reach -1200 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 decrease by -1200 km<sup>2</sup> (-0.3% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach -1600 km<sup>2</sup> (-0.4% of the land area). By the middle of the century, changes reach -1200 km<sup>2</sup> under RCP2.6 and -1100 km<sup>2</sup> under RCP6.0.
......
Markdown is supported
0% or .
You are about to add 0 people to the discussion. Proceed with caution.
Finish editing this message first!
Please register or to comment