Commit 0e452b89 authored by Mahé Perrette's avatar Mahé Perrette
Browse files

remove world and time ranking value

parent 6f43bf82
......@@ -67,7 +67,9 @@ However, at today’s level of 1°C global warming Cape Verde’s annual land ar
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 0 km<sup>2</sup> (1.0% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 0 km<sup>2</sup> (1.0% of the land area). By the middle of the century, changes reach 0 km<sup>2</sup> under RCP2.6 and 0 km<sup>2</sup> under RCP6.0.
Cape Verde is the (ranking-value: land-abs-temp_CPV value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in land area affected by droughts towards the end of the century under a high-emissions scenario (RCP6.0), Cape Verde’s ranking is (ranking-value: land-abs-time_CPV value: position time:2081-2100 scenario:rcp60).
Cape Verde is the (ranking-value: land-abs-temp_CPV value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### Population exposed to droughts
......@@ -84,7 +86,8 @@ However, at today’s level of 1°C of global warming Cape Verde’s annual popu
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.0 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 0.0 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.
Cape Verde is the (ranking-value: pop-abs-temp_CPV value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in population exposed to droughts towards the end of the century under a higher-emissions scenario (RCP6.0), Cape Verde’s ranking is (ranking-value: pop-abs-time_CPV value: position time:2081-2100 scenario:rcp60).
Cape Verde is the (ranking-value: pop-abs-temp_CPV value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### How is soil moisture calculated?
......
......@@ -67,7 +67,9 @@ However, at today’s level of 1°C global warming Costa Rica’s annual land ar
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 0 km<sup>2</sup> (0.1% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 0 km<sup>2</sup> (0.1% of the land area). By the middle of the century, changes reach 400 km<sup>2</sup> under RCP2.6 and -100 km<sup>2</sup> under RCP6.0.
Costa Rica is the (ranking-value: land-abs-temp_CRI value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in land area affected by droughts towards the end of the century under a high-emissions scenario (RCP6.0), Costa Rica’s ranking is (ranking-value: land-abs-time_CRI value: position time:2081-2100 scenario:rcp60).
Costa Rica is the (ranking-value: land-abs-temp_CRI value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### Population exposed to droughts
......@@ -84,7 +86,8 @@ However, at today’s level of 1°C of global warming Costa Rica’s annual popu
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.
Costa Rica is the (ranking-value: pop-abs-temp_CRI value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in population exposed to droughts towards the end of the century under a higher-emissions scenario (RCP6.0), Costa Rica’s ranking is (ranking-value: pop-abs-time_CRI value: position time:2081-2100 scenario:rcp60).
Costa Rica is the (ranking-value: pop-abs-temp_CRI value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### How is soil moisture calculated?
......
......@@ -67,7 +67,9 @@ However, at today’s level of 1°C global warming Cuba’s annual land area aff
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 3000 km<sup>2</sup> (2.9% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 0 km<sup>2</sup> (2.9% of the land area). By the middle of the century, changes reach 300 km<sup>2</sup> under RCP2.6 and 200 km<sup>2</sup> under RCP6.0.
Cuba is the (ranking-value: land-abs-temp_CUB value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in land area affected by droughts towards the end of the century under a high-emissions scenario (RCP6.0), Cuba’s ranking is (ranking-value: land-abs-time_CUB value: position time:2081-2100 scenario:rcp60).
Cuba is the (ranking-value: land-abs-temp_CUB value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### Population exposed to droughts
......@@ -84,7 +86,8 @@ However, at today’s level of 1°C of global warming Cuba’s annual population
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.1 million (0.7% 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 (0.0% 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.
Cuba is the (ranking-value: pop-abs-temp_CUB value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in population exposed to droughts towards the end of the century under a higher-emissions scenario (RCP6.0), Cuba’s ranking is (ranking-value: pop-abs-time_CUB value: position time:2081-2100 scenario:rcp60).
Cuba is the (ranking-value: pop-abs-temp_CUB value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### How is soil moisture calculated?
......
......@@ -67,7 +67,9 @@ However, at today’s level of 1°C global warming Cyprus’ annual land area af
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 1600 km<sup>2</sup> (16.7% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 800 km<sup>2</sup> (16.7% of the land area). By the middle of the century, changes reach 1000 km<sup>2</sup> under RCP2.6 and 600 km<sup>2</sup> under RCP6.0.
Cyprus is the (ranking-value: land-abs-temp_CYP value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in land area affected by droughts towards the end of the century under a high-emissions scenario (RCP6.0), Cyprus’ ranking is (ranking-value: land-abs-time_CYP value: position time:2081-2100 scenario:rcp60).
Cyprus is the (ranking-value: land-abs-temp_CYP value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### Population exposed to droughts
......@@ -84,7 +86,8 @@ However, at today’s level of 1°C of global warming Cyprus’ annual populatio
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.1 million (9.5% of the total population) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would expose 0.0 million people (4.3% 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.
Cyprus is the (ranking-value: pop-abs-temp_CYP value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in population exposed to droughts towards the end of the century under a higher-emissions scenario (RCP6.0), Cyprus’ ranking is (ranking-value: pop-abs-time_CYP value: position time:2081-2100 scenario:rcp60).
Cyprus is the (ranking-value: pop-abs-temp_CYP value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### How is soil moisture calculated?
......
......@@ -67,7 +67,9 @@ However, at today’s level of 1°C global warming Czech Republic’s annual lan
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 500 km<sup>2</sup> (0.7% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 300 km<sup>2</sup> (0.7% of the land area). By the middle of the century, changes reach 0 km<sup>2</sup> under RCP2.6 and 200 km<sup>2</sup> under RCP6.0.
Czech Republic is the (ranking-value: land-abs-temp_CZE value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in land area affected by droughts towards the end of the century under a high-emissions scenario (RCP6.0), Czech Republic’s ranking is (ranking-value: land-abs-time_CZE value: position time:2081-2100 scenario:rcp60).
Czech Republic is the (ranking-value: land-abs-temp_CZE value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### Population exposed to droughts
......@@ -84,7 +86,8 @@ However, at today’s level of 1°C of global warming Czech Republic’s annual
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.0 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 (0.1% 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.
Czech Republic is the (ranking-value: pop-abs-temp_CZE value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in population exposed to droughts towards the end of the century under a higher-emissions scenario (RCP6.0), Czech Republic’s ranking is (ranking-value: pop-abs-time_CZE value: position time:2081-2100 scenario:rcp60).
Czech Republic is the (ranking-value: pop-abs-temp_CZE value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### How is soil moisture calculated?
......
......@@ -67,7 +67,9 @@ However, at today’s level of 1°C global warming Germany’s annual land area
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to decrease by 0 km<sup>2</sup> (0.0% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 900 km<sup>2</sup> (0.0% of the land area). By the middle of the century, changes reach 0 km<sup>2</sup> under RCP2.6 and 0 km<sup>2</sup> under RCP6.0.
Germany is the (ranking-value: land-abs-temp_DEU value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in land area affected by droughts towards the end of the century under a high-emissions scenario (RCP6.0), Germany’s ranking is (ranking-value: land-abs-time_DEU value: position time:2081-2100 scenario:rcp60).
Germany is the (ranking-value: land-abs-temp_DEU value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### Population exposed to droughts
......@@ -84,7 +86,8 @@ However, at today’s level of 1°C of global warming Germany’s annual populat
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 0.1 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.
Germany is the (ranking-value: pop-abs-temp_DEU value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in population exposed to droughts towards the end of the century under a higher-emissions scenario (RCP6.0), Germany’s ranking is (ranking-value: pop-abs-time_DEU value: position time:2081-2100 scenario:rcp60).
Germany is the (ranking-value: pop-abs-temp_DEU value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### How is soil moisture calculated?
......
......@@ -67,7 +67,9 @@ However, at today’s level of 1°C global warming Djibouti’s annual land area
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 100 km<sup>2</sup> under RCP6.0.
Djibouti is the (ranking-value: land-abs-temp_DJI value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in land area affected by droughts towards the end of the century under a high-emissions scenario (RCP6.0), Djibouti’s ranking is (ranking-value: land-abs-time_DJI value: position time:2081-2100 scenario:rcp60).
Djibouti is the (ranking-value: land-abs-temp_DJI value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### Population exposed to droughts
......@@ -84,7 +86,8 @@ However, at today’s level of 1°C of global warming Djibouti’s annual popula
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.
Djibouti is the (ranking-value: pop-abs-temp_DJI value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in population exposed to droughts towards the end of the century under a higher-emissions scenario (RCP6.0), Djibouti’s ranking is (ranking-value: pop-abs-time_DJI value: position time:2081-2100 scenario:rcp60).
Djibouti is the (ranking-value: pop-abs-temp_DJI value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### How is soil moisture calculated?
......
......@@ -67,7 +67,9 @@ However, at today’s level of 1°C global warming Denmark’s annual land area
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to decrease by 0 km<sup>2</sup> (-0.1% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 0 km<sup>2</sup> (-0.1% of the land area). By the middle of the century, changes reach 0 km<sup>2</sup> under RCP2.6 and 0 km<sup>2</sup> under RCP6.0.
Denmark is the (ranking-value: land-abs-temp_DNK value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in land area affected by droughts towards the end of the century under a high-emissions scenario (RCP6.0), Denmark’s ranking is (ranking-value: land-abs-time_DNK value: position time:2081-2100 scenario:rcp60).
Denmark is the (ranking-value: land-abs-temp_DNK value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### Population exposed to droughts
......@@ -84,7 +86,8 @@ However, at today’s level of 1°C of global warming Denmark’s annual populat
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.
Denmark is the (ranking-value: pop-abs-temp_DNK value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in population exposed to droughts towards the end of the century under a higher-emissions scenario (RCP6.0), Denmark’s ranking is (ranking-value: pop-abs-time_DNK value: position time:2081-2100 scenario:rcp60).
Denmark is the (ranking-value: pop-abs-temp_DNK value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### How is soil moisture calculated?
......
......@@ -67,7 +67,9 @@ However, at today’s level of 1°C global warming Dominican Republic’s annual
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 100 km<sup>2</sup> (0.2% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 0 km<sup>2</sup> (0.2% of the land area). By the middle of the century, changes reach 700 km<sup>2</sup> under RCP2.6 and 0 km<sup>2</sup> under RCP6.0.
Dominican Republic is the (ranking-value: land-abs-temp_DOM value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in land area affected by droughts towards the end of the century under a high-emissions scenario (RCP6.0), Dominican Republic’s ranking is (ranking-value: land-abs-time_DOM value: position time:2081-2100 scenario:rcp60).
Dominican Republic is the (ranking-value: land-abs-temp_DOM value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### Population exposed to droughts
......@@ -84,7 +86,8 @@ However, at today’s level of 1°C of global warming Dominican Republic’s ann
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.
Dominican Republic is the (ranking-value: pop-abs-temp_DOM value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in population exposed to droughts towards the end of the century under a higher-emissions scenario (RCP6.0), Dominican Republic’s ranking is (ranking-value: pop-abs-time_DOM value: position time:2081-2100 scenario:rcp60).
Dominican Republic is the (ranking-value: pop-abs-temp_DOM value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### How is soil moisture calculated?
......
......@@ -67,7 +67,9 @@ However, at today’s level of 1°C global warming Algeria’s annual land area
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 305400 km<sup>2</sup> (12.8% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 80900 km<sup>2</sup> (12.8% of the land area). By the middle of the century, changes reach 58500 km<sup>2</sup> under RCP2.6 and 175400 km<sup>2</sup> under RCP6.0.
Algeria is the (ranking-value: land-abs-temp_DZA value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in land area affected by droughts towards the end of the century under a high-emissions scenario (RCP6.0), Algeria’s ranking is (ranking-value: land-abs-time_DZA value: position time:2081-2100 scenario:rcp60).
Algeria is the (ranking-value: land-abs-temp_DZA value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### Population exposed to droughts
......@@ -84,7 +86,8 @@ However, at today’s level of 1°C of global warming Algeria’s annual populat
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 1.8 million (4.8% 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 (1.0% of the total population). By mid of the century changes expose 0.5 million people under RCP2.6 and 0.7 million people under RCP6.0.
Algeria is the (ranking-value: pop-abs-temp_DZA value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in population exposed to droughts towards the end of the century under a higher-emissions scenario (RCP6.0), Algeria’s ranking is (ranking-value: pop-abs-time_DZA value: position time:2081-2100 scenario:rcp60).
Algeria is the (ranking-value: pop-abs-temp_DZA value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### How is soil moisture calculated?
......
......@@ -67,7 +67,9 @@ However, at today’s level of 1°C global warming Ecuador’s annual land area
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 100 km<sup>2</sup> (0.1% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 0 km<sup>2</sup> (0.1% of the land area). By the middle of the century, changes reach 600 km<sup>2</sup> under RCP2.6 and 0 km<sup>2</sup> under RCP6.0.
Ecuador is the (ranking-value: land-abs-temp_ECU value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in land area affected by droughts towards the end of the century under a high-emissions scenario (RCP6.0), Ecuador’s ranking is (ranking-value: land-abs-time_ECU value: position time:2081-2100 scenario:rcp60).
Ecuador is the (ranking-value: land-abs-temp_ECU value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### Population exposed to droughts
......@@ -84,7 +86,8 @@ However, at today’s level of 1°C of global warming Ecuador’s annual populat
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.
Ecuador is the (ranking-value: pop-abs-temp_ECU value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in population exposed to droughts towards the end of the century under a higher-emissions scenario (RCP6.0), Ecuador’s ranking is (ranking-value: pop-abs-time_ECU value: position time:2081-2100 scenario:rcp60).
Ecuador is the (ranking-value: pop-abs-temp_ECU value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### How is soil moisture calculated?
......
......@@ -67,7 +67,9 @@ However, at today’s level of 1°C global warming Egypt’s annual land area af
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 109300 km<sup>2</sup> (11.0% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 39100 km<sup>2</sup> (11.0% of the land area). By the middle of the century, changes reach 47200 km<sup>2</sup> under RCP2.6 and 43700 km<sup>2</sup> under RCP6.0.
Egypt is the (ranking-value: land-abs-temp_EGY value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in land area affected by droughts towards the end of the century under a high-emissions scenario (RCP6.0), Egypt’s ranking is (ranking-value: land-abs-time_EGY value: position time:2081-2100 scenario:rcp60).
Egypt is the (ranking-value: land-abs-temp_EGY value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### Population exposed to droughts
......@@ -84,7 +86,8 @@ However, at today’s level of 1°C of global warming Egypt’s annual populatio
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 2.3 million (2.6% of the total population) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would expose 0.4 million people (0.5% of the total population). By mid of the century changes expose 1.3 million people under RCP2.6 and 1.4 million people under RCP6.0.
Egypt is the (ranking-value: pop-abs-temp_EGY value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in population exposed to droughts towards the end of the century under a higher-emissions scenario (RCP6.0), Egypt’s ranking is (ranking-value: pop-abs-time_EGY value: position time:2081-2100 scenario:rcp60).
Egypt is the (ranking-value: pop-abs-temp_EGY value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### How is soil moisture calculated?
......
......@@ -67,7 +67,9 @@ However, at today’s level of 1°C global warming Eritrea’s annual land area
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 600 km<sup>2</sup> (0.6% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 700 km<sup>2</sup> (0.6% of the land area). By the middle of the century, changes reach 1000 km<sup>2</sup> under RCP2.6 and 1700 km<sup>2</sup> under RCP6.0.
Eritrea is the (ranking-value: land-abs-temp_ERI value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in land area affected by droughts towards the end of the century under a high-emissions scenario (RCP6.0), Eritrea’s ranking is (ranking-value: land-abs-time_ERI value: position time:2081-2100 scenario:rcp60).
Eritrea is the (ranking-value: land-abs-temp_ERI value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### Population exposed to droughts
......@@ -84,7 +86,8 @@ However, at today’s level of 1°C of global warming Eritrea’s annual populat
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.0 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 0.0 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.
Eritrea is the (ranking-value: pop-abs-temp_ERI value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in population exposed to droughts towards the end of the century under a higher-emissions scenario (RCP6.0), Eritrea’s ranking is (ranking-value: pop-abs-time_ERI value: position time:2081-2100 scenario:rcp60).
Eritrea is the (ranking-value: pop-abs-temp_ERI value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### How is soil moisture calculated?
......
......@@ -67,7 +67,9 @@ However, at today’s level of 1°C global warming Western Sahara’s annual lan
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 0 km<sup>2</sup> (4.1% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 0 km<sup>2</sup> (4.1% of the land area). By the middle of the century, changes reach 0 km<sup>2</sup> under RCP2.6 and 0 km<sup>2</sup> under RCP6.0.
Western Sahara is the (ranking-value: land-abs-temp_ESH value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in land area affected by droughts towards the end of the century under a high-emissions scenario (RCP6.0), Western Sahara’s ranking is (ranking-value: land-abs-time_ESH value: position time:2081-2100 scenario:rcp60).
Western Sahara is the (ranking-value: land-abs-temp_ESH value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### Population exposed to droughts
......@@ -84,7 +86,8 @@ However, at today’s level of 1°C of global warming Western Sahara’s annual
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by nan million (0.7% 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 (0.3% of the total population). By mid of the century changes expose nan million people under RCP2.6 and nan million people under RCP6.0.
Western Sahara is the (ranking-value: pop-abs-temp_ESH value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in population exposed to droughts towards the end of the century under a higher-emissions scenario (RCP6.0), Western Sahara’s ranking is (ranking-value: pop-abs-time_ESH value: position time:2081-2100 scenario:rcp60).
Western Sahara is the (ranking-value: pop-abs-temp_ESH value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### How is soil moisture calculated?
......
......@@ -67,7 +67,9 @@ However, at today’s level of 1°C global warming Spain’s annual land area af
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.
Spain is the (ranking-value: land-abs-temp_ESP value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in land area affected by droughts towards the end of the century under a high-emissions scenario (RCP6.0), Spain’s ranking is (ranking-value: land-abs-time_ESP value: position time:2081-2100 scenario:rcp60).
Spain is the (ranking-value: land-abs-temp_ESP value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### Population exposed to droughts
......@@ -84,7 +86,8 @@ However, at today’s level of 1°C of global warming Spain’s annual populatio
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.9 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 (0.2% of the total population). By mid of the century changes expose 0.2 million people under RCP2.6 and 0.2 million people under RCP6.0.
Spain is the (ranking-value: pop-abs-temp_ESP value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in population exposed to droughts towards the end of the century under a higher-emissions scenario (RCP6.0), Spain’s ranking is (ranking-value: pop-abs-time_ESP value: position time:2081-2100 scenario:rcp60).
Spain is the (ranking-value: pop-abs-temp_ESP value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### How is soil moisture calculated?
......
......@@ -67,7 +67,9 @@ However, at today’s level of 1°C global warming Estonia’s annual land area
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.
Estonia is the (ranking-value: land-abs-temp_EST value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in land area affected by droughts towards the end of the century under a high-emissions scenario (RCP6.0), Estonia’s ranking is (ranking-value: land-abs-time_EST value: position time:2081-2100 scenario:rcp60).
Estonia is the (ranking-value: land-abs-temp_EST value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### Population exposed to droughts
......@@ -84,7 +86,8 @@ However, at today’s level of 1°C of global warming Estonia’s annual populat
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to decrease 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.
Estonia is the (ranking-value: pop-abs-temp_EST value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in population exposed to droughts towards the end of the century under a higher-emissions scenario (RCP6.0), Estonia’s ranking is (ranking-value: pop-abs-time_EST value: position time:2081-2100 scenario:rcp60).
Estonia is the (ranking-value: pop-abs-temp_EST value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### How is soil moisture calculated?
......
......@@ -67,7 +67,9 @@ However, at today’s level of 1°C global warming Ethiopia’s annual land area
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.
Ethiopia is the (ranking-value: land-abs-temp_ETH value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in land area affected by droughts towards the end of the century under a high-emissions scenario (RCP6.0), Ethiopia’s ranking is (ranking-value: land-abs-time_ETH value: position time:2081-2100 scenario:rcp60).
Ethiopia is the (ranking-value: land-abs-temp_ETH value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### Population exposed to droughts
......@@ -84,7 +86,8 @@ However, at today’s level of 1°C of global warming Ethiopia’s annual popula
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.2 million (0.3% of the total population) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would expose 0.2 million people (0.2% of the total population). By mid of the century changes expose 0.2 million people under RCP2.6 and 0.2 million people under RCP6.0.
Ethiopia is the (ranking-value: pop-abs-temp_ETH value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in population exposed to droughts towards the end of the century under a higher-emissions scenario (RCP6.0), Ethiopia’s ranking is (ranking-value: pop-abs-time_ETH value: position time:2081-2100 scenario:rcp60).
Ethiopia is the (ranking-value: pop-abs-temp_ETH value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### How is soil moisture calculated?
......
......@@ -67,7 +67,9 @@ However, at today’s level of 1°C global warming Finland’s annual land area
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to decrease 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 -600 km<sup>2</sup> (-0.2% of the land area). By the middle of the century, changes reach -1000 km<sup>2</sup> under RCP2.6 and -1000 km<sup>2</sup> under RCP6.0.
Finland is the (ranking-value: land-abs-temp_FIN value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in land area affected by droughts towards the end of the century under a high-emissions scenario (RCP6.0), Finland’s ranking is (ranking-value: land-abs-time_FIN value: position time:2081-2100 scenario:rcp60).
Finland is the (ranking-value: land-abs-temp_FIN value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### Population exposed to droughts
......@@ -84,7 +86,8 @@ However, at today’s level of 1°C of global warming Finland’s annual populat
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.
Finland is the (ranking-value: pop-abs-temp_FIN value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in population exposed to droughts towards the end of the century under a higher-emissions scenario (RCP6.0), Finland’s ranking is (ranking-value: pop-abs-time_FIN value: position time:2081-2100 scenario:rcp60).
Finland is the (ranking-value: pop-abs-temp_FIN value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### How is soil moisture calculated?
......
......@@ -67,7 +67,9 @@ However, at today’s level of 1°C global warming Fiji’s annual land area aff
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.
Fiji is the (ranking-value: land-abs-temp_FJI value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in land area affected by droughts towards the end of the century under a high-emissions scenario (RCP6.0), Fiji’s ranking is (ranking-value: land-abs-time_FJI value: position time:2081-2100 scenario:rcp60).
Fiji is the (ranking-value: land-abs-temp_FJI value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### Population exposed to droughts
......@@ -84,7 +86,8 @@ However, at today’s level of 1°C of global warming Fiji’s annual population
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to decrease 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.
Fiji is the (ranking-value: pop-abs-temp_FJI value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in population exposed to droughts towards the end of the century under a higher-emissions scenario (RCP6.0), Fiji’s ranking is (ranking-value: pop-abs-time_FJI value: position time:2081-2100 scenario:rcp60).
Fiji is the (ranking-value: pop-abs-temp_FJI value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### How is soil moisture calculated?
......
......@@ -67,7 +67,9 @@ However, at today’s level of 1°C global warming Falkland Islands’ annual la
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.
Falkland Islands is the (ranking-value: land-abs-temp_FLK value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in land area affected by droughts towards the end of the century under a high-emissions scenario (RCP6.0), Falkland Islands’ ranking is (ranking-value: land-abs-time_FLK value: position time:2081-2100 scenario:rcp60).
Falkland Islands is the (ranking-value: land-abs-temp_FLK value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### Population exposed to droughts
......@@ -84,7 +86,8 @@ However, at today’s level of 1°C of global warming Falkland Islands’ annual
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to decrease by nan 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 nan million people (0.0% of the total population). By mid of the century changes expose nan million people under RCP2.6 and nan million people under RCP6.0.
Falkland Islands is the (ranking-value: pop-abs-temp_FLK value: position temperature:2) strongest affected by droughts at 2°C of global warming. For the absolute change in population exposed to droughts towards the end of the century under a higher-emissions scenario (RCP6.0), Falkland Islands’ ranking is (ranking-value: pop-abs-time_FLK value: position time:2081-2100 scenario:rcp60).
Falkland Islands is the (ranking-value: pop-abs-temp_FLK value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### How is soil moisture calculated?
......
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