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 Belarus’ annual land area a
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 -500 km<sup>2</sup> (-0.2% of the land area). By the middle of the century, changes reach 0 km<sup>2</sup> under RCP2.6 and 0 km<sup>2</sup> under RCP6.0.
Belarus is the (ranking-value: land-abs-temp_BLR 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), Belarus’ ranking is (ranking-value: land-abs-time_BLR value: position time:2081-2100 scenario:rcp60).
Belarus is the (ranking-value: land-abs-temp_BLR 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 Belarus’ annual populati
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 (-0.1% 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.
Belarus is the (ranking-value: pop-abs-temp_BLR 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), Belarus’ ranking is (ranking-value: pop-abs-time_BLR value: position time:2081-2100 scenario:rcp60).
Belarus is the (ranking-value: pop-abs-temp_BLR 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 Belize’s annual land area a
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 500 km<sup>2</sup> (2.2% 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> (2.2% of the land area). By the middle of the century, changes reach 0 km<sup>2</sup> under RCP2.6 and 0 km<sup>2</sup> under RCP6.0.
Belize is the (ranking-value: land-abs-temp_BLZ 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), Belize’s ranking is (ranking-value: land-abs-time_BLZ value: position time:2081-2100 scenario:rcp60).
Belize is the (ranking-value: land-abs-temp_BLZ 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 Belize’s annual populati
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.0 million (1.3% of the total population) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would expose -0.0 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.
Belize is the (ranking-value: pop-abs-temp_BLZ 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), Belize’s ranking is (ranking-value: pop-abs-time_BLZ value: position time:2081-2100 scenario:rcp60).
Belize is the (ranking-value: pop-abs-temp_BLZ 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 Bolivia’s annual land area
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 82400 km<sup>2</sup> (7.6% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 45300 km<sup>2</sup> (7.6% of the land area). By the middle of the century, changes reach 25200 km<sup>2</sup> under RCP2.6 and 22500 km<sup>2</sup> under RCP6.0.
Bolivia is the (ranking-value: land-abs-temp_BOL 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), Bolivia’s ranking is (ranking-value: land-abs-time_BOL value: position time:2081-2100 scenario:rcp60).
Bolivia is the (ranking-value: land-abs-temp_BOL 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 Bolivia’s annual populat
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.2 million (2.1% of the total population) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would expose 0.1 million people (1.3% 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.
Bolivia is the (ranking-value: pop-abs-temp_BOL 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), Bolivia’s ranking is (ranking-value: pop-abs-time_BOL value: position time:2081-2100 scenario:rcp60).
Bolivia is the (ranking-value: pop-abs-temp_BOL 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 Brazil’s annual land area a
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 296400 km<sup>2</sup> (3.5% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 209400 km<sup>2</sup> (3.5% of the land area). By the middle of the century, changes reach 155900 km<sup>2</sup> under RCP2.6 and 91900 km<sup>2</sup> under RCP6.0.
Brazil is the (ranking-value: land-abs-temp_BRA 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), Brazil’s ranking is (ranking-value: land-abs-time_BRA value: position time:2081-2100 scenario:rcp60).
Brazil is the (ranking-value: land-abs-temp_BRA 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 Brazil’s annual populati
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.7 million (0.4% of the total population) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would expose 0.5 million people (0.3% of the total population). By mid of the century changes expose 0.5 million people under RCP2.6 and 0.3 million people under RCP6.0.
Brazil is the (ranking-value: pop-abs-temp_BRA 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), Brazil’s ranking is (ranking-value: pop-abs-time_BRA value: position time:2081-2100 scenario:rcp60).
Brazil is the (ranking-value: pop-abs-temp_BRA 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 Brunei Darussalam’s annual
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.
Brunei Darussalam is the (ranking-value: land-abs-temp_BRN 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), Brunei Darussalam’s ranking is (ranking-value: land-abs-time_BRN value: position time:2081-2100 scenario:rcp60).
Brunei Darussalam is the (ranking-value: land-abs-temp_BRN 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 Brunei Darussalam’s annu
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.
Brunei Darussalam is the (ranking-value: pop-abs-temp_BRN 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), Brunei Darussalam’s ranking is (ranking-value: pop-abs-time_BRN value: position time:2081-2100 scenario:rcp60).
Brunei Darussalam is the (ranking-value: pop-abs-temp_BRN 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 Bhutan’s annual land area a
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 1400 km<sup>2</sup> (3.6% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 0 km<sup>2</sup> (3.6% of the land area). By the middle of the century, changes reach 200 km<sup>2</sup> under RCP2.6 and 0 km<sup>2</sup> under RCP6.0.
Bhutan is the (ranking-value: land-abs-temp_BTN 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), Bhutan’s ranking is (ranking-value: land-abs-time_BTN value: position time:2081-2100 scenario:rcp60).
Bhutan is the (ranking-value: land-abs-temp_BTN 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 Bhutan’s annual populati
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.0 million (0.9% 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.
Bhutan is the (ranking-value: pop-abs-temp_BTN 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), Bhutan’s ranking is (ranking-value: pop-abs-time_BTN value: position time:2081-2100 scenario:rcp60).
Bhutan is the (ranking-value: pop-abs-temp_BTN 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 Botswana’s annual land area
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 5600 km<sup>2</sup> (1.0% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 2800 km<sup>2</sup> (1.0% of the land area). By the middle of the century, changes reach 1400 km<sup>2</sup> under RCP2.6 and 2500 km<sup>2</sup> under RCP6.0.
Botswana is the (ranking-value: land-abs-temp_BWA 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), Botswana’s ranking is (ranking-value: land-abs-time_BWA value: position time:2081-2100 scenario:rcp60).
Botswana is the (ranking-value: land-abs-temp_BWA 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 Botswana’s annual popula
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.0 million (0.4% 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.
Botswana is the (ranking-value: pop-abs-temp_BWA 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), Botswana’s ranking is (ranking-value: pop-abs-time_BWA value: position time:2081-2100 scenario:rcp60).
Botswana is the (ranking-value: pop-abs-temp_BWA 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 Central African Republic’s
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 3600 km<sup>2</sup> (0.6% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 4400 km<sup>2</sup> (0.6% of the land area). By the middle of the century, changes reach 1000 km<sup>2</sup> under RCP2.6 and 2600 km<sup>2</sup> under RCP6.0.
Central African Republic is the (ranking-value: land-abs-temp_CAF 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), Central African Republic’s ranking is (ranking-value: land-abs-time_CAF value: position time:2081-2100 scenario:rcp60).
Central African Republic is the (ranking-value: land-abs-temp_CAF 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 Central African Republic
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 (0.4% 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.
Central African Republic is the (ranking-value: pop-abs-temp_CAF 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), Central African Republic’s ranking is (ranking-value: pop-abs-time_CAF value: position time:2081-2100 scenario:rcp60).
Central African Republic is the (ranking-value: pop-abs-temp_CAF 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 Canada’s annual land area a
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 64900 km<sup>2</sup> (0.7% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 11400 km<sup>2</sup> (0.7% of the land area). By the middle of the century, changes reach -14400 km<sup>2</sup> under RCP2.6 and 4800 km<sup>2</sup> under RCP6.0.
Canada is the (ranking-value: land-abs-temp_CAN 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), Canada’s ranking is (ranking-value: land-abs-time_CAN value: position time:2081-2100 scenario:rcp60).
Canada is the (ranking-value: land-abs-temp_CAN 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 Canada’s annual populati
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 (0.1% 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.
Canada is the (ranking-value: pop-abs-temp_CAN 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), Canada’s ranking is (ranking-value: pop-abs-time_CAN value: position time:2081-2100 scenario:rcp60).
Canada is the (ranking-value: pop-abs-temp_CAN 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 Cayman Islands’ annual land
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to decrease by 0 km<sup>2</sup> (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% 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.
Cayman Islands is the (ranking-value: land-abs-temp_CAY 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), Cayman Islands’ ranking is (ranking-value: land-abs-time_CAY value: position time:2081-2100 scenario:rcp60).
Cayman Islands is the (ranking-value: land-abs-temp_CAY 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 Cayman Islands’ annual p
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to decrease by nan million (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% of the total population). By mid of the century changes expose nan million people under RCP2.6 and nan million people under RCP6.0.
Cayman Islands is the (ranking-value: pop-abs-temp_CAY 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), Cayman Islands’ ranking is (ranking-value: pop-abs-time_CAY value: position time:2081-2100 scenario:rcp60).
Cayman Islands is the (ranking-value: pop-abs-temp_CAY 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 Switzerland’s annual land a
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 100 km<sup>2</sup> (0.2% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 0 km<sup>2</sup> (0.2% of the land area). By the middle of the century, changes reach 0 km<sup>2</sup> under RCP2.6 and 0 km<sup>2</sup> under RCP6.0.
Switzerland is the (ranking-value: land-abs-temp_CHE 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), Switzerland’s ranking is (ranking-value: land-abs-time_CHE value: position time:2081-2100 scenario:rcp60).
Switzerland is the (ranking-value: land-abs-temp_CHE 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 Switzerland’s annual pop
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.
Switzerland is the (ranking-value: pop-abs-temp_CHE 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), Switzerland’s ranking is (ranking-value: pop-abs-time_CHE value: position time:2081-2100 scenario:rcp60).
Switzerland is the (ranking-value: pop-abs-temp_CHE 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 Chile’s annual land area af
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 86300 km<sup>2</sup> (11.6% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 25000 km<sup>2</sup> (11.6% of the land area). By the middle of the century, changes reach 35400 km<sup>2</sup> under RCP2.6 and 52800 km<sup>2</sup> under RCP6.0.
Chile is the (ranking-value: land-abs-temp_CHL 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), Chile’s ranking is (ranking-value: land-abs-time_CHL value: position time:2081-2100 scenario:rcp60).
Chile is the (ranking-value: land-abs-temp_CHL 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 Chile’s annual populatio
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.5 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 0.1 million people (0.3% 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.
Chile is the (ranking-value: pop-abs-temp_CHL 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), Chile’s ranking is (ranking-value: pop-abs-time_CHL value: position time:2081-2100 scenario:rcp60).
Chile is the (ranking-value: pop-abs-temp_CHL 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 China’s annual land area af
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 407600 km<sup>2</sup> (4.3% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 357300 km<sup>2</sup> (4.3% of the land area). By the middle of the century, changes reach 229500 km<sup>2</sup> under RCP2.6 and 197200 km<sup>2</sup> under RCP6.0.
China is the (ranking-value: land-abs-temp_CHN 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), China’s ranking is (ranking-value: land-abs-time_CHN value: position time:2081-2100 scenario:rcp60).
China is the (ranking-value: land-abs-temp_CHN 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 China’s annual populatio
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 25.4 million (1.9% of the total population) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would expose 20.5 million people (1.5% of the total population). By mid of the century changes expose 11.8 million people under RCP2.6 and 7.7 million people under RCP6.0.
China is the (ranking-value: pop-abs-temp_CHN 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), China’s ranking is (ranking-value: pop-abs-time_CHN value: position time:2081-2100 scenario:rcp60).
China is the (ranking-value: pop-abs-temp_CHN 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 Cote dIvoire’s annual land
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 12500 km<sup>2</sup> (3.9% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 8000 km<sup>2</sup> (3.9% of the land area). By the middle of the century, changes reach 6800 km<sup>2</sup> under RCP2.6 and 6900 km<sup>2</sup> under RCP6.0.
Cote dIvoire is the (ranking-value: land-abs-temp_CIV 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), Cote dIvoire’s ranking is (ranking-value: land-abs-time_CIV value: position time:2081-2100 scenario:rcp60).
Cote dIvoire is the (ranking-value: land-abs-temp_CIV 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 Cote dIvoire’s annual po
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.6 million (3.0% of the total population) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would expose 0.4 million people (1.8% of the total population). By mid of the century changes expose 0.4 million people under RCP2.6 and 0.4 million people under RCP6.0.
Cote dIvoire is the (ranking-value: pop-abs-temp_CIV 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), Cote dIvoire’s ranking is (ranking-value: pop-abs-time_CIV value: position time:2081-2100 scenario:rcp60).
Cote dIvoire is the (ranking-value: pop-abs-temp_CIV 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 Cameroon’s annual land area
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 8500 km<sup>2</sup> (1.8% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 7900 km<sup>2</sup> (1.8% of the land area). By the middle of the century, changes reach 3100 km<sup>2</sup> under RCP2.6 and 3700 km<sup>2</sup> under RCP6.0.
Cameroon is the (ranking-value: land-abs-temp_CMR 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), Cameroon’s ranking is (ranking-value: land-abs-time_CMR value: position time:2081-2100 scenario:rcp60).
Cameroon is the (ranking-value: land-abs-temp_CMR 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 Cameroon’s annual popula
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.2 million (0.9% 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 (1.0% 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.
Cameroon is the (ranking-value: pop-abs-temp_CMR 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), Cameroon’s ranking is (ranking-value: pop-abs-time_CMR value: position time:2081-2100 scenario:rcp60).
Cameroon is the (ranking-value: pop-abs-temp_CMR 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 Democratic Republic of Congo
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 7300 km<sup>2</sup> (0.3% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 7000 km<sup>2</sup> (0.3% of the land area). By the middle of the century, changes reach 15600 km<sup>2</sup> under RCP2.6 and 10000 km<sup>2</sup> under RCP6.0.
Democratic Republic of Congo is the (ranking-value: land-abs-temp_COD 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), Democratic Republic of Congo’s ranking is (ranking-value: land-abs-time_COD value: position time:2081-2100 scenario:rcp60).
Democratic Republic of Congo is the (ranking-value: land-abs-temp_COD 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 Democratic Republic of Con
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 0.1 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.
Democratic Republic of Congo is the (ranking-value: pop-abs-temp_COD 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), Democratic Republic of Congo’s ranking is (ranking-value: pop-abs-time_COD value: position time:2081-2100 scenario:rcp60).
Democratic Republic of Congo is the (ranking-value: pop-abs-temp_COD 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 Congo’s annual land area af
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 3300 km<sup>2</sup> (1.0% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 3200 km<sup>2</sup> (1.0% of the land area). By the middle of the century, changes reach 3100 km<sup>2</sup> under RCP2.6 and 2300 km<sup>2</sup> under RCP6.0.
Congo is the (ranking-value: land-abs-temp_COG 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), Congo’s ranking is (ranking-value: land-abs-time_COG value: position time:2081-2100 scenario:rcp60).
Congo is the (ranking-value: land-abs-temp_COG 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 Congo’s annual populatio
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 (0.0% 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.
Congo is the (ranking-value: pop-abs-temp_COG 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), Congo’s ranking is (ranking-value: pop-abs-time_COG value: position time:2081-2100 scenario:rcp60).
Congo is the (ranking-value: pop-abs-temp_COG 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 Cook Islands’ annual land a
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.
Cook Islands is the (ranking-value: land-abs-temp_COK 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), Cook Islands’ ranking is (ranking-value: land-abs-time_COK value: position time:2081-2100 scenario:rcp60).
Cook Islands is the (ranking-value: land-abs-temp_COK 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 Cook Islands’ annual pop
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.
Cook Islands is the (ranking-value: pop-abs-temp_COK 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), Cook Islands’ ranking is (ranking-value: pop-abs-time_COK value: position time:2081-2100 scenario:rcp60).
Cook Islands is the (ranking-value: pop-abs-temp_COK 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 Colombia’s annual land area
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 9900 km<sup>2</sup> (0.9% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 9600 km<sup>2</sup> (0.9% of the land area). By the middle of the century, changes reach 5400 km<sup>2</sup> under RCP2.6 and -300 km<sup>2</sup> under RCP6.0.
Colombia is the (ranking-value: land-abs-temp_COL 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), Colombia’s ranking is (ranking-value: land-abs-time_COL value: position time:2081-2100 scenario:rcp60).
Colombia is the (ranking-value: land-abs-temp_COL 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 Colombia’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 0.1 million people (0.2% of the total population). By mid of the century changes expose 0.1 million people under RCP2.6 and 0.0 million people under RCP6.0.
Colombia is the (ranking-value: pop-abs-temp_COL 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), Colombia’s ranking is (ranking-value: pop-abs-time_COL value: position time:2081-2100 scenario:rcp60).
Colombia is the (ranking-value: pop-abs-temp_COL 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 Comoros’ annual land area a
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.
Comoros is the (ranking-value: land-abs-temp_COM 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), Comoros’ ranking is (ranking-value: land-abs-time_COM value: position time:2081-2100 scenario:rcp60).
Comoros is the (ranking-value: land-abs-temp_COM 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 Comoros’ annual populati
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.
Comoros is the (ranking-value: pop-abs-temp_COM 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), Comoros’ ranking is (ranking-value: pop-abs-time_COM value: position time:2081-2100 scenario:rcp60).
Comoros is the (ranking-value: pop-abs-temp_COM value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### How is soil moisture calculated?
......
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