Commit b1c36b9d authored by Mahé Perrette's avatar Mahé Perrette
Browse files

fix comma for country's population

parent 685a858d
......@@ -78,7 +78,7 @@ Afghanistan is the (ranking-value: land-abs-temp_AFG value: position temperature
Our definition of “drought” is quite strict, such that, without climate change, only 0.0% of Afghanistan’s population would be exposed to droughts each year, on average.
However, at today’s level of 1°C of global warming Afghanistan’s annual population exposed to droughts is, on average, already 0.4 million (i.e. 1.1% of the total population) higher than without climate change and amount to 1.5% of the total population. The level of change ranges from 0.3 % to 13.3% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Afghanistan’s annual population exposed to droughts is projected to increase by 0 million (i.e. 1.7% of the population) on average in comparison to a world without climate change. Under these conditions, 2.1% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from 0.1 up to 3.7 million people.
However, at today’s level of 1°C of global warming Afghanistan’s annual population exposed to droughts is, on average, already 0.4 million (i.e. 1.1% of the total population) higher than without climate change and amount to 1.5% of the total population. The level of change ranges from 0.3 % to 13.3% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Afghanistan’s annual population exposed to droughts is projected to increase by 0.5 million (i.e. 1.7% of the population) on average in comparison to a world without climate change. Under these conditions, 2.1% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from 0.1 up to 3.7 million people.
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 1.6 million (5.0% of the total population) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would expose 0.2 million people (0.7% of the total population). By mid of the century changes expose 0.4 million people under RCP2.6 and 0.5 million people under RCP6.0.
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......@@ -78,7 +78,7 @@ Angola is the (ranking-value: land-abs-temp_AGO value: position temperature:2) s
Our definition of “drought” is quite strict, such that, without climate change, only 0.0% of Angola’s population would be exposed to droughts each year, on average.
However, at today’s level of 1°C of global warming Angola’s annual population exposed to droughts is, on average, already 0.0 million (i.e. 0.1% of the total population) higher than without climate change and amount to 0.2% of the total population. The level of change ranges from -0.1 % to 12.6% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Angola’s annual population exposed to droughts is projected to increase by 0 million (i.e. 0.1% of the population) on average in comparison to a world without climate change. Under these conditions, 0.1% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -0.0 up to 1.0 million people.
However, at today’s level of 1°C of global warming Angola’s annual population exposed to droughts is, on average, already 0.0 million (i.e. 0.1% of the total population) higher than without climate change and amount to 0.2% of the total population. The level of change ranges from -0.1 % to 12.6% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Angola’s annual population exposed to droughts is projected to increase by 0.0 million (i.e. 0.1% of the population) on average in comparison to a world without climate change. Under these conditions, 0.1% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -0.0 up to 1.0 million people.
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.1 million (0.2% of the total population) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would expose 0.0 million people (0.2% of the total population). By mid of the century changes expose 0.0 million people under RCP2.6 and 0.0 million people under RCP6.0.
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......@@ -78,7 +78,7 @@ Albania is the (ranking-value: land-abs-temp_ALB value: position temperature:2)
Our definition of “drought” is quite strict, such that, without climate change, only 0.0% of Albania’s population would be exposed to droughts each year, on average.
However, at today’s level of 1°C of global warming Albania’s annual population exposed to droughts is, on average, already 0.0 million (i.e. 0.1% of the total population) higher than without climate change and amount to 0% of the total population. The level of change ranges from 0.0 % to 7.0% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Albania’s annual population exposed to droughts is projected to increase by 0 million (i.e. 0.4% of the population) on average in comparison to a world without climate change. Under these conditions, 0.0% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from 0.0 up to 0.1 million people.
However, at today’s level of 1°C of global warming Albania’s annual population exposed to droughts is, on average, already 0.0 million (i.e. 0.1% of the total population) higher than without climate change and amount to 0% of the total population. The level of change ranges from 0.0 % to 7.0% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Albania’s annual population exposed to droughts is projected to increase by 0.0 million (i.e. 0.4% of the population) on average in comparison to a world without climate change. Under these conditions, 0.0% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from 0.0 up to 0.1 million people.
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.0 million (0.6% of the total population) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would expose 0.0 million people (0.1% of the total population). By mid of the century changes expose 0.0 million people under RCP2.6 and 0.0 million people under RCP6.0.
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......@@ -78,7 +78,7 @@ United Arab Emirates is the (ranking-value: land-abs-temp_ARE value: position te
Our definition of “drought” is quite strict, such that, without climate change, only 0.0% of United Arab Emirates’ population would be exposed to droughts each year, on average.
However, at today’s level of 1°C of global warming United Arab Emirates’ annual population exposed to droughts is, on average, already 0.0 million (i.e. 0.0% of the total population) higher than without climate change and amount to 1.0% of the total population. The level of change ranges from 0.0 % to 35.3% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, United Arab Emirates’ annual population exposed to droughts is projected to increase by 0 million (i.e. 0.1% of the population) on average in comparison to a world without climate change. Under these conditions, 0.8% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -0.0 up to 0.4 million people.
However, at today’s level of 1°C of global warming United Arab Emirates’ annual population exposed to droughts is, on average, already 0.0 million (i.e. 0.0% of the total population) higher than without climate change and amount to 1.0% of the total population. The level of change ranges from 0.0 % to 35.3% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, United Arab Emirates’ annual population exposed to droughts is projected to increase by 0.0 million (i.e. 0.1% of the population) on average in comparison to a world without climate change. Under these conditions, 0.8% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -0.0 up to 0.4 million people.
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.0 million (0.1% of the total population) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would expose 0.0 million people (0.0% of the total population). By mid of the century changes expose 0.0 million people under RCP2.6 and 0.0 million people under RCP6.0.
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......@@ -78,7 +78,7 @@ Argentina is the (ranking-value: land-abs-temp_ARG value: position temperature:2
Our definition of “drought” is quite strict, such that, without climate change, only 0.0% of Argentina’s population would be exposed to droughts each year, on average.
However, at today’s level of 1°C of global warming Argentina’s annual population exposed to droughts is, on average, already 0.0 million (i.e. 0.0% of the total population) higher than without climate change and amount to 0.1% of the total population. The level of change ranges from 0.3 % to 7.9% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Argentina’s annual population exposed to droughts is projected to increase by 0 million (i.e. 0.1% of the population) on average in comparison to a world without climate change. Under these conditions, 0.1% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -0.1 up to 0.1 million people.
However, at today’s level of 1°C of global warming Argentina’s annual population exposed to droughts is, on average, already 0.0 million (i.e. 0.0% of the total population) higher than without climate change and amount to 0.1% of the total population. The level of change ranges from 0.3 % to 7.9% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Argentina’s annual population exposed to droughts is projected to increase by 0.0 million (i.e. 0.1% of the population) on average in comparison to a world without climate change. Under these conditions, 0.1% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -0.1 up to 0.1 million people.
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.1 million (0.1% of the total population) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would expose 0.0 million people (0.0% of the total population). By mid of the century changes expose 0.0 million people under RCP2.6 and 0.0 million people under RCP6.0.
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......@@ -78,7 +78,7 @@ Armenia is the (ranking-value: land-abs-temp_ARM value: position temperature:2)
Our definition of “drought” is quite strict, such that, without climate change, only 0.0% of Armenia’s population would be exposed to droughts each year, on average.
However, at today’s level of 1°C of global warming Armenia’s annual population exposed to droughts is, on average, already 0.0 million (i.e. 0.4% of the total population) higher than without climate change and amount to 1.6% of the total population. The level of change ranges from -0.1 % to 22.9% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Armenia’s annual population exposed to droughts is projected to increase by 0 million (i.e. 0.5% of the population) on average in comparison to a world without climate change. Under these conditions, 1.6% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -0.0 up to 0.3 million people.
However, at today’s level of 1°C of global warming Armenia’s annual population exposed to droughts is, on average, already 0.0 million (i.e. 0.4% of the total population) higher than without climate change and amount to 1.6% of the total population. The level of change ranges from -0.1 % to 22.9% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Armenia’s annual population exposed to droughts is projected to increase by 0.0 million (i.e. 0.5% of the population) on average in comparison to a world without climate change. Under these conditions, 1.6% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -0.0 up to 0.3 million people.
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.0 million (1.2% of the total population) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would expose 0.0 million people (0.1% of the total population). By mid of the century changes expose 0.0 million people under RCP2.6 and 0.0 million people under RCP6.0.
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......@@ -78,7 +78,7 @@ American Samoa is the (ranking-value: land-abs-temp_ASM value: position temperat
Our definition of “drought” is quite strict, such that, without climate change, only 0.0% of American Samoa’s population would be exposed to droughts each year, on average.
However, at today’s level of 1°C of global warming American Samoa’s annual population exposed to droughts is, on average, already 0.0 million (i.e. 0.0% of the total population) higher than without climate change and amount to 0% of the total population. The level of change ranges from -0.3 % to 4.7% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, American Samoa’s annual population exposed to droughts is projected to decrease by 0 million (i.e. 0.0% of the population) on average in comparison to a world without climate change. Under these conditions, 0% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -0.0 up to 0.0 million people.
However, at today’s level of 1°C of global warming American Samoa’s annual population exposed to droughts is, on average, already 0.0 million (i.e. 0.0% of the total population) higher than without climate change and amount to 0% of the total population. The level of change ranges from -0.3 % to 4.7% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, American Samoa’s annual population exposed to droughts is projected to decrease by 0.0 million (i.e. 0.0% of the population) on average in comparison to a world without climate change. Under these conditions, 0% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -0.0 up to 0.0 million people.
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to decrease by 0.0 million (0.0% of the total population) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would expose 0.0 million people (0.0% of the total population). By mid of the century changes expose 0.0 million people under RCP2.6 and 0.0 million people under RCP6.0.
......
......@@ -78,7 +78,7 @@ Antarctica is the (ranking-value: land-abs-temp_ATA value: position temperature:
Our definition of “drought” is quite strict, such that, without climate change, only 0.0% of Antarctica’s population would be exposed to droughts each year, on average.
However, at today’s level of 1°C of global warming Antarctica’s annual population exposed to droughts is, on average, already nan million (i.e. 0.0% of the total population) lower than without climate change and amount to 0% of the total population. The level of change ranges from 0.0 % to 0.0% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Antarctica’s annual population exposed to droughts is projected to decrease by 0 million (i.e. 0.0% of the population) on average in comparison to a world without climate change. Under these conditions, 0% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from nan up to nan million people.
However, at today’s level of 1°C of global warming Antarctica’s annual population exposed to droughts is, on average, already nan million (i.e. 0.0% of the total population) lower than without climate change and amount to 0% of the total population. The level of change ranges from 0.0 % to 0.0% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Antarctica’s annual population exposed to droughts is projected to decrease by nan million (i.e. 0.0% of the population) on average in comparison to a world without climate change. Under these conditions, 0% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from nan up to nan million people.
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by nan million (100.0% of the total population) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would expose nan million people (100.0% of the total population). By mid of the century changes expose nan million people under RCP2.6 and nan million people under RCP6.0.
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......@@ -78,7 +78,7 @@ French Southern and Antarctica Lands is the (ranking-value: land-abs-temp_ATF va
Our definition of “drought” is quite strict, such that, without climate change, only 0.0% of French Southern and Antarctica Lands’ population would be exposed to droughts each year, on average.
However, at today’s level of 1°C of global warming French Southern and Antarctica Lands’ annual population exposed to droughts is, on average, already nan million (i.e. 0.0% of the total population) lower than without climate change and amount to 0% of the total population. The level of change ranges from -0.6 % to 0.5% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, French Southern and Antarctica Lands’ annual population exposed to droughts is projected to decrease by 0 million (i.e. 0.0% of the population) on average in comparison to a world without climate change. Under these conditions, 0% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from nan up to nan million people.
However, at today’s level of 1°C of global warming French Southern and Antarctica Lands’ annual population exposed to droughts is, on average, already nan million (i.e. 0.0% of the total population) lower than without climate change and amount to 0% of the total population. The level of change ranges from -0.6 % to 0.5% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, French Southern and Antarctica Lands’ annual population exposed to droughts is projected to decrease by nan million (i.e. 0.0% of the population) on average in comparison to a world without climate change. Under these conditions, 0% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from nan up to nan million people.
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by nan million (100.0% of the total population) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would expose nan million people (100.0% of the total population). By mid of the century changes expose nan million people under RCP2.6 and nan million people under RCP6.0.
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......@@ -78,7 +78,7 @@ Australia is the (ranking-value: land-abs-temp_AUS value: position temperature:2
Our definition of “drought” is quite strict, such that, without climate change, only 0.0% of Australia’s population would be exposed to droughts each year, on average.
However, at today’s level of 1°C of global warming Australia’s annual population exposed to droughts is, on average, already 0.0 million (i.e. 0.1% of the total population) higher than without climate change and amount to 0.4% of the total population. The level of change ranges from 0.0 % to 10.0% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Australia’s annual population exposed to droughts is projected to increase by 0 million (i.e. 0.3% of the population) on average in comparison to a world without climate change. Under these conditions, 1.3% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from 0.0 up to 0.4 million people.
However, at today’s level of 1°C of global warming Australia’s annual population exposed to droughts is, on average, already 0.0 million (i.e. 0.1% of the total population) higher than without climate change and amount to 0.4% of the total population. The level of change ranges from 0.0 % to 10.0% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Australia’s annual population exposed to droughts is projected to increase by 0.1 million (i.e. 0.3% of the population) on average in comparison to a world without climate change. Under these conditions, 1.3% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from 0.0 up to 0.4 million people.
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.1 million (0.5% of the total population) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would expose 0.1 million people (0.5% of the total population). By mid of the century changes expose 0.0 million people under RCP2.6 and 0.0 million people under RCP6.0.
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......@@ -78,7 +78,7 @@ Austria is the (ranking-value: land-abs-temp_AUT value: position temperature:2)
Our definition of “drought” is quite strict, such that, without climate change, only 0.0% of Austria’s population would be exposed to droughts each year, on average.
However, at today’s level of 1°C of global warming Austria’s annual population exposed to droughts is, on average, already 0.0 million (i.e. 0.1% of the total population) higher than without climate change and amount to 0.1% of the total population. 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, Austria’s annual population exposed to droughts is projected to increase by 0 million (i.e. 0.1% of the population) on average in comparison to a world without climate change. Under these conditions, 0.1% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -0.1 up to 0.3 million people.
However, at today’s level of 1°C of global warming Austria’s annual population exposed to droughts is, on average, already 0.0 million (i.e. 0.1% of the total population) higher than without climate change and amount to 0.1% of the total population. 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, Austria’s annual population exposed to droughts is projected to increase by 0.0 million (i.e. 0.1% of the population) on average in comparison to a world without climate change. Under these conditions, 0.1% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -0.1 up to 0.3 million people.
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.0 million (0.1% of the total population) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would expose 0.0 million people (0.2% of the total population). By mid of the century changes expose -0.0 million people under RCP2.6 and 0.0 million people under RCP6.0.
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......@@ -78,7 +78,7 @@ Azerbaijan is the (ranking-value: land-abs-temp_AZE value: position temperature:
Our definition of “drought” is quite strict, such that, without climate change, only 0.0% of Azerbaijan’s population would be exposed to droughts each year, on average.
However, at today’s level of 1°C of global warming Azerbaijan’s annual population exposed to droughts is, on average, already 0.0 million (i.e. 0.3% of the total population) higher than without climate change and amount to 0.9% of the total population. The level of change ranges from 0.1 % to 13.3% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Azerbaijan’s annual population exposed to droughts is projected to increase by 0 million (i.e. 1.1% of the population) on average in comparison to a world without climate change. Under these conditions, 1.6% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from 0.0 up to 0.7 million people.
However, at today’s level of 1°C of global warming Azerbaijan’s annual population exposed to droughts is, on average, already 0.0 million (i.e. 0.3% of the total population) higher than without climate change and amount to 0.9% of the total population. The level of change ranges from 0.1 % to 13.3% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Azerbaijan’s annual population exposed to droughts is projected to increase by 0.1 million (i.e. 1.1% of the population) on average in comparison to a world without climate change. Under these conditions, 1.6% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from 0.0 up to 0.7 million people.
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.3 million (2.7% of the total population) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would expose 0.0 million people (0.5% of the total population). By mid of the century changes expose 0.1 million people under RCP2.6 and 0.1 million people under RCP6.0.
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......@@ -78,7 +78,7 @@ Burundi is the (ranking-value: land-abs-temp_BDI value: position temperature:2)
Our definition of “drought” is quite strict, such that, without climate change, only 0.0% of Burundi’s population would be exposed to droughts each year, on average.
However, at today’s level of 1°C of global warming Burundi’s annual population exposed to droughts is, on average, already 0.0 million (i.e. 0.0% of the total population) lower than without climate change and amount to 0% of the total population. The level of change ranges from -0.7 % to 12.7% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Burundi’s annual population exposed to droughts is projected to decrease by 0 million (i.e. 0.0% of the population) on average in comparison to a world without climate change. Under these conditions, 0% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -0.1 up to 1.2 million people.
However, at today’s level of 1°C of global warming Burundi’s annual population exposed to droughts is, on average, already 0.0 million (i.e. 0.0% of the total population) lower than without climate change and amount to 0% of the total population. The level of change ranges from -0.7 % to 12.7% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Burundi’s annual population exposed to droughts is projected to decrease by 0.0 million (i.e. 0.0% of the population) on average in comparison to a world without climate change. Under these conditions, 0% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -0.1 up to 1.2 million people.
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to decrease by 0.0 million (0.0% of the total population) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would expose 0.0 million people (0.0% of the total population). By mid of the century changes expose 0.0 million people under RCP2.6 and 0.0 million people under RCP6.0.
......
......@@ -78,7 +78,7 @@ Belgium is the (ranking-value: land-abs-temp_BEL value: position temperature:2)
Our definition of “drought” is quite strict, such that, without climate change, only 0.0% of Belgium’s population would be exposed to droughts each year, on average.
However, at today’s level of 1°C of global warming Belgium’s annual population exposed to droughts is, on average, already 0.0 million (i.e. 0.0% of the total population) lower than without climate change and amount to 0% of the total population. The level of change ranges from -0.5 % to 0.8% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Belgium’s annual population exposed to droughts is projected to decrease by 0 million (i.e. 0.0% of the population) on average in comparison to a world without climate change. Under these conditions, 0% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -0.0 up to 0.0 million people.
However, at today’s level of 1°C of global warming Belgium’s annual population exposed to droughts is, on average, already 0.0 million (i.e. 0.0% of the total population) lower than without climate change and amount to 0% of the total population. The level of change ranges from -0.5 % to 0.8% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Belgium’s annual population exposed to droughts is projected to decrease by 0.0 million (i.e. 0.0% of the population) on average in comparison to a world without climate change. Under these conditions, 0% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -0.0 up to 0.0 million people.
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to decrease by 0.0 million (0.0% of the total population) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would expose -0.0 million people (-0.0% of the total population). By mid of the century changes expose -0.0 million people under RCP2.6 and -0.0 million people under RCP6.0.
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......@@ -78,7 +78,7 @@ Benin is the (ranking-value: land-abs-temp_BEN value: position temperature:2) st
Our definition of “drought” is quite strict, such that, without climate change, only 0.0% of Benin’s population would be exposed to droughts each year, on average.
However, at today’s level of 1°C of global warming Benin’s annual population exposed to droughts is, on average, already 0.1 million (i.e. 0.7% of the total population) higher than without climate change and amount to 0.6% of the total population. The level of change ranges from 0.1 % to 27.0% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Benin’s annual population exposed to droughts is projected to increase by 0 million (i.e. 0.9% of the population) on average in comparison to a world without climate change. Under these conditions, 0.7% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -0.0 up to 2.7 million people.
However, at today’s level of 1°C of global warming Benin’s annual population exposed to droughts is, on average, already 0.1 million (i.e. 0.7% of the total population) higher than without climate change and amount to 0.6% of the total population. The level of change ranges from 0.1 % to 27.0% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Benin’s annual population exposed to droughts is projected to increase by 0.1 million (i.e. 0.9% of the population) on average in comparison to a world without climate change. Under these conditions, 0.7% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -0.0 up to 2.7 million people.
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.4 million (3.7% of the total population) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would expose 0.1 million people (1.3% of the total population). By mid of the century changes expose 0.0 million people under RCP2.6 and 0.1 million people under RCP6.0.
......
......@@ -78,7 +78,7 @@ Burkina Faso is the (ranking-value: land-abs-temp_BFA value: position temperatur
Our definition of “drought” is quite strict, such that, without climate change, only 0.0% of Burkina Faso’s population would be exposed to droughts each year, on average.
However, at today’s level of 1°C of global warming Burkina Faso’s annual population exposed to droughts is, on average, already 0.1 million (i.e. 0.6% of the total population) higher than without climate change and amount to 2.4% of the total population. The level of change ranges from -0.4 % to 22.5% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Burkina Faso’s annual population exposed to droughts is projected to increase by 0 million (i.e. 1.5% of the population) on average in comparison to a world without climate change. Under these conditions, 4.4% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -0.1 up to 3.1 million people.
However, at today’s level of 1°C of global warming Burkina Faso’s annual population exposed to droughts is, on average, already 0.1 million (i.e. 0.6% of the total population) higher than without climate change and amount to 2.4% of the total population. The level of change ranges from -0.4 % to 22.5% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Burkina Faso’s annual population exposed to droughts is projected to increase by 0.3 million (i.e. 1.5% of the population) on average in comparison to a world without climate change. Under these conditions, 4.4% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -0.1 up to 3.1 million people.
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.6 million (3.3% of the total population) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would expose 0.4 million people (2.5% of the total population). By mid of the century changes expose 0.1 million people under RCP2.6 and 0.2 million people under RCP6.0.
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......@@ -78,7 +78,7 @@ Bangladesh is the (ranking-value: land-abs-temp_BGD value: position temperature:
Our definition of “drought” is quite strict, such that, without climate change, only 0.0% of Bangladesh’s population would be exposed to droughts each year, on average.
However, at today’s level of 1°C of global warming Bangladesh’s annual population exposed to droughts is, on average, already 0.2 million (i.e. 0.1% of the total population) higher than without climate change and amount to 0.1% of the total population. The level of change ranges from -0.4 % to 4.9% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Bangladesh’s annual population exposed to droughts is projected to increase by 0 million (i.e. 0.1% of the population) on average in comparison to a world without climate change. Under these conditions, 0.1% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -0.5 up to 2.7 million people.
However, at today’s level of 1°C of global warming Bangladesh’s annual population exposed to droughts is, on average, already 0.2 million (i.e. 0.1% of the total population) higher than without climate change and amount to 0.1% of the total population. The level of change ranges from -0.4 % to 4.9% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Bangladesh’s annual population exposed to droughts is projected to increase by 0.2 million (i.e. 0.1% of the population) on average in comparison to a world without climate change. Under these conditions, 0.1% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -0.5 up to 2.7 million people.
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.1 million (0.1% of the total population) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would expose 0.0 million people (0.0% of the total population). By mid of the century changes expose 0.0 million people under RCP2.6 and -0.1 million people under RCP6.0.
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......@@ -78,7 +78,7 @@ Bulgaria is the (ranking-value: land-abs-temp_BGR value: position temperature:2)
Our definition of “drought” is quite strict, such that, without climate change, only 0.0% of Bulgaria’s population would be exposed to droughts each year, on average.
However, at today’s level of 1°C of global warming Bulgaria’s annual population exposed to droughts is, on average, already 0.1 million (i.e. 0.7% of the total population) higher than without climate change and amount to 0.3% of the total population. The level of change ranges from 0.1 % to 23.7% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Bulgaria’s annual population exposed to droughts is projected to increase by 0 million (i.e. 1.3% of the population) on average in comparison to a world without climate change. Under these conditions, 0.5% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from 0.0 up to 0.6 million people.
However, at today’s level of 1°C of global warming Bulgaria’s annual population exposed to droughts is, on average, already 0.1 million (i.e. 0.7% of the total population) higher than without climate change and amount to 0.3% of the total population. The level of change ranges from 0.1 % to 23.7% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Bulgaria’s annual population exposed to droughts is projected to increase by 0.1 million (i.e. 1.3% of the population) on average in comparison to a world without climate change. Under these conditions, 0.5% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from 0.0 up to 0.6 million people.
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.1 million (2.0% of the total population) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would expose 0.1 million people (1.3% of the total population). By mid of the century changes expose 0.0 million people under RCP2.6 and 0.0 million people under RCP6.0.
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......@@ -78,7 +78,7 @@ Bahamas is the (ranking-value: land-abs-temp_BHS value: position temperature:2)
Our definition of “drought” is quite strict, such that, without climate change, only 0.0% of Bahamas’ population would be exposed to droughts each year, on average.
However, at today’s level of 1°C of global warming Bahamas’ annual population exposed to droughts is, on average, already 0.0 million (i.e. 0.0% of the total population) higher than without climate change and amount to 0.0% of the total population. The level of change ranges from -0.3 % to 20.4% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Bahamas’ annual population exposed to droughts is projected to increase by 0 million (i.e. 0.0% of the population) on average in comparison to a world without climate change. Under these conditions, 0.0% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -0.0 up to 0.0 million people.
However, at today’s level of 1°C of global warming Bahamas’ annual population exposed to droughts is, on average, already 0.0 million (i.e. 0.0% of the total population) higher than without climate change and amount to 0.0% of the total population. The level of change ranges from -0.3 % to 20.4% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Bahamas’ annual population exposed to droughts is projected to increase by 0.0 million (i.e. 0.0% of the population) on average in comparison to a world without climate change. Under these conditions, 0.0% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -0.0 up to 0.0 million people.
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.0 million (0.0% of the total population) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would expose 0.0 million people (0.0% of the total population). By mid of the century changes expose 0.0 million people under RCP2.6 and 0.0 million people under RCP6.0.
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......@@ -78,7 +78,7 @@ Bosnia and Herzegovina is the (ranking-value: land-abs-temp_BIH value: position
Our definition of “drought” is quite strict, such that, without climate change, only 0.0% of Bosnia and Herzegovina’s population would be exposed to droughts each year, on average.
However, at today’s level of 1°C of global warming Bosnia and Herzegovina’s annual population exposed to droughts is, on average, already 0.0 million (i.e. 0.5% of the total population) higher than without climate change and amount to 0.1% of the total population. The level of change ranges from -0.1 % to 15.4% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Bosnia and Herzegovina’s annual population exposed to droughts is projected to increase by 0 million (i.e. 0.7% of the population) on average in comparison to a world without climate change. Under these conditions, 0.5% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -0.0 up to 0.4 million people.
However, at today’s level of 1°C of global warming Bosnia and Herzegovina’s annual population exposed to droughts is, on average, already 0.0 million (i.e. 0.5% of the total population) higher than without climate change and amount to 0.1% of the total population. The level of change ranges from -0.1 % to 15.4% for the individual combinations of global hydrological models and global climate models. At 2°C of global warming, Bosnia and Herzegovina’s annual population exposed to droughts is projected to increase by 0.0 million (i.e. 0.7% of the population) on average in comparison to a world without climate change. Under these conditions, 0.5% of the total population would be affected by droughts, on average. Across the individual combinations of global hydrological models and global climate models this expected level of change ranges from -0.0 up to 0.4 million people.
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.1 million (1.7% of the total population) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would expose 0.0 million people (0.3% of the total population). By mid of the century changes expose 0.0 million people under RCP2.6 and 0.0 million people under RCP6.0.
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