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 Haiti’s annual land area af
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.
Haiti is the (ranking-value: land-abs-temp_HTI 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), Haiti’s ranking is (ranking-value: land-abs-time_HTI value: position time:2081-2100 scenario:rcp60).
Haiti is the (ranking-value: land-abs-temp_HTI 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 Haiti’s annual populatio
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.
Haiti is the (ranking-value: pop-abs-temp_HTI 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), Haiti’s ranking is (ranking-value: pop-abs-time_HTI value: position time:2081-2100 scenario:rcp60).
Haiti is the (ranking-value: pop-abs-temp_HTI 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 Hungary’s annual land area
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 3400 km<sup>2</sup> (3.8% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 100 km<sup>2</sup> (3.8% of the land area). By the middle of the century, changes reach 1100 km<sup>2</sup> under RCP2.6 and 900 km<sup>2</sup> under RCP6.0.
Hungary is the (ranking-value: land-abs-temp_HUN 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), Hungary’s ranking is (ranking-value: land-abs-time_HUN value: position time:2081-2100 scenario:rcp60).
Hungary is the (ranking-value: land-abs-temp_HUN 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 Hungary’s annual populat
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.1 million (1.5% 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 (0.1% 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.
Hungary is the (ranking-value: pop-abs-temp_HUN 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), Hungary’s ranking is (ranking-value: pop-abs-time_HUN value: position time:2081-2100 scenario:rcp60).
Hungary is the (ranking-value: pop-abs-temp_HUN 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 Indonesia’s annual land are
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 300 km<sup>2</sup> (0.0% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 2900 km<sup>2</sup> (0.0% of the land area). By the middle of the century, changes reach 4000 km<sup>2</sup> under RCP2.6 and -800 km<sup>2</sup> under RCP6.0.
Indonesia is the (ranking-value: land-abs-temp_IDN 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), Indonesia’s ranking is (ranking-value: land-abs-time_IDN value: position time:2081-2100 scenario:rcp60).
Indonesia is the (ranking-value: land-abs-temp_IDN 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 Indonesia’s annual popul
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.3 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 0.5 million people (0.2% 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.
Indonesia is the (ranking-value: pop-abs-temp_IDN 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), Indonesia’s ranking is (ranking-value: pop-abs-time_IDN value: position time:2081-2100 scenario:rcp60).
Indonesia is the (ranking-value: pop-abs-temp_IDN 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 India’s annual land area af
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 34300 km<sup>2</sup> (1.2% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 30900 km<sup>2</sup> (1.2% of the land area). By the middle of the century, changes reach 2900 km<sup>2</sup> under RCP2.6 and 13400 km<sup>2</sup> under RCP6.0.
India is the (ranking-value: land-abs-temp_IND 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), India’s ranking is (ranking-value: land-abs-time_IND value: position time:2081-2100 scenario:rcp60).
India is the (ranking-value: land-abs-temp_IND 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 India’s annual populatio
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 8.3 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 8.0 million people (0.6% of the total population). By mid of the century changes expose -0.2 million people under RCP2.6 and 5.4 million people under RCP6.0.
India is the (ranking-value: pop-abs-temp_IND 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), India’s ranking is (ranking-value: pop-abs-time_IND value: position time:2081-2100 scenario:rcp60).
India is the (ranking-value: pop-abs-temp_IND 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 Ireland’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 0 km<sup>2</sup> under RCP6.0.
Ireland is the (ranking-value: land-abs-temp_IRL 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), Ireland’s ranking is (ranking-value: land-abs-time_IRL value: position time:2081-2100 scenario:rcp60).
Ireland is the (ranking-value: land-abs-temp_IRL 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 Ireland’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.
Ireland is the (ranking-value: pop-abs-temp_IRL 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), Ireland’s ranking is (ranking-value: pop-abs-time_IRL value: position time:2081-2100 scenario:rcp60).
Ireland is the (ranking-value: pop-abs-temp_IRL 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 Iran’s annual land area aff
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 154100 km<sup>2</sup> (9.5% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 40000 km<sup>2</sup> (9.5% of the land area). By the middle of the century, changes reach 46800 km<sup>2</sup> under RCP2.6 and 56800 km<sup>2</sup> under RCP6.0.
Iran is the (ranking-value: land-abs-temp_IRN 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), Iran’s ranking is (ranking-value: land-abs-time_IRN value: position time:2081-2100 scenario:rcp60).
Iran is the (ranking-value: land-abs-temp_IRN 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 Iran’s annual population
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 2.3 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 0.7 million people (1.0% of the total population). By mid of the century changes expose 0.6 million people under RCP2.6 and 1.0 million people under RCP6.0.
Iran is the (ranking-value: pop-abs-temp_IRN 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), Iran’s ranking is (ranking-value: pop-abs-time_IRN value: position time:2081-2100 scenario:rcp60).
Iran is the (ranking-value: pop-abs-temp_IRN 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 Iraq’s annual land area aff
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 35700 km<sup>2</sup> (8.2% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 17200 km<sup>2</sup> (8.2% of the land area). By the middle of the century, changes reach 10600 km<sup>2</sup> under RCP2.6 and 29800 km<sup>2</sup> under RCP6.0.
Iraq is the (ranking-value: land-abs-temp_IRQ 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), Iraq’s ranking is (ranking-value: land-abs-time_IRQ value: position time:2081-2100 scenario:rcp60).
Iraq is the (ranking-value: land-abs-temp_IRQ 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 Iraq’s annual population
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 1.0 million (3.1% of the total population) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would expose 0.3 million people (0.9% of the total population). By mid of the century changes expose 0.2 million people under RCP2.6 and 0.7 million people under RCP6.0.
Iraq is the (ranking-value: pop-abs-temp_IRQ 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), Iraq’s ranking is (ranking-value: pop-abs-time_IRQ value: position time:2081-2100 scenario:rcp60).
Iraq is the (ranking-value: pop-abs-temp_IRQ 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 Iceland’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 -100 km<sup>2</sup> under RCP2.6 and 0 km<sup>2</sup> under RCP6.0.
Iceland is the (ranking-value: land-abs-temp_ISL 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), Iceland’s ranking is (ranking-value: land-abs-time_ISL value: position time:2081-2100 scenario:rcp60).
Iceland is the (ranking-value: land-abs-temp_ISL 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 Iceland’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.
Iceland is the (ranking-value: pop-abs-temp_ISL 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), Iceland’s ranking is (ranking-value: pop-abs-time_ISL value: position time:2081-2100 scenario:rcp60).
Iceland is the (ranking-value: pop-abs-temp_ISL 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 Israel’s annual land area a
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 4200 km<sup>2</sup> (19.3% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 1200 km<sup>2</sup> (19.3% of the land area). By the middle of the century, changes reach 1300 km<sup>2</sup> under RCP2.6 and 2100 km<sup>2</sup> under RCP6.0.
Israel is the (ranking-value: land-abs-temp_ISR 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), Israel’s ranking is (ranking-value: land-abs-time_ISR value: position time:2081-2100 scenario:rcp60).
Israel is the (ranking-value: land-abs-temp_ISR 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 Israel’s annual populati
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.6 million (7.7% 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 (1.4% 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.
Israel is the (ranking-value: pop-abs-temp_ISR 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), Israel’s ranking is (ranking-value: pop-abs-time_ISR value: position time:2081-2100 scenario:rcp60).
Israel is the (ranking-value: pop-abs-temp_ISR 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 Italy’s annual land area af
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 15300 km<sup>2</sup> (5.2% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 6900 km<sup>2</sup> (5.2% of the land area). By the middle of the century, changes reach 4100 km<sup>2</sup> under RCP2.6 and 5000 km<sup>2</sup> under RCP6.0.
Italy is the (ranking-value: land-abs-temp_ITA 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), Italy’s ranking is (ranking-value: land-abs-time_ITA value: position time:2081-2100 scenario:rcp60).
Italy is the (ranking-value: land-abs-temp_ITA 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 Italy’s annual populatio
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.7 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 0.2 million people (0.4% 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.
Italy is the (ranking-value: pop-abs-temp_ITA 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), Italy’s ranking is (ranking-value: pop-abs-time_ITA value: position time:2081-2100 scenario:rcp60).
Italy is the (ranking-value: pop-abs-temp_ITA 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 Jamaica’s annual land area
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 0 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 0 km<sup>2</sup> (0.3% of the land area). By the middle of the century, changes reach 0 km<sup>2</sup> under RCP2.6 and 0 km<sup>2</sup> under RCP6.0.
Jamaica is the (ranking-value: land-abs-temp_JAM 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), Jamaica’s ranking is (ranking-value: land-abs-time_JAM value: position time:2081-2100 scenario:rcp60).
Jamaica is the (ranking-value: land-abs-temp_JAM 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 Jamaica’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.
Jamaica is the (ranking-value: pop-abs-temp_JAM 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), Jamaica’s ranking is (ranking-value: pop-abs-time_JAM value: position time:2081-2100 scenario:rcp60).
Jamaica is the (ranking-value: pop-abs-temp_JAM 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 Jordan’s annual land area a
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 8800 km<sup>2</sup> (9.9% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 4500 km<sup>2</sup> (9.9% of the land area). By the middle of the century, changes reach 4200 km<sup>2</sup> under RCP2.6 and 4700 km<sup>2</sup> under RCP6.0.
Jordan is the (ranking-value: land-abs-temp_JOR 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), Jordan’s ranking is (ranking-value: land-abs-time_JOR value: position time:2081-2100 scenario:rcp60).
Jordan is the (ranking-value: land-abs-temp_JOR 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 Jordan’s annual populati
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.3 million (3.5% 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 (1.2% 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.
Jordan is the (ranking-value: pop-abs-temp_JOR 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), Jordan’s ranking is (ranking-value: pop-abs-time_JOR value: position time:2081-2100 scenario:rcp60).
Jordan is the (ranking-value: pop-abs-temp_JOR 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 Japan’s annual land area af
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 1100 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 0 km<sup>2</sup> (0.3% of the land area). By the middle of the century, changes reach 1000 km<sup>2</sup> under RCP2.6 and 1400 km<sup>2</sup> under RCP6.0.
Japan is the (ranking-value: land-abs-temp_JPN 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), Japan’s ranking is (ranking-value: land-abs-time_JPN value: position time:2081-2100 scenario:rcp60).
Japan is the (ranking-value: land-abs-temp_JPN 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 Japan’s annual populatio
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.2 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 0.1 million people under RCP2.6 and 0.4 million people under RCP6.0.
Japan is the (ranking-value: pop-abs-temp_JPN 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), Japan’s ranking is (ranking-value: pop-abs-time_JPN value: position time:2081-2100 scenario:rcp60).
Japan is the (ranking-value: pop-abs-temp_JPN 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 Kazakhstan’s annual land ar
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 17300 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 -1300 km<sup>2</sup> (0.6% of the land area). By the middle of the century, changes reach 8300 km<sup>2</sup> under RCP2.6 and 9300 km<sup>2</sup> under RCP6.0.
Kazakhstan is the (ranking-value: land-abs-temp_KAZ 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), Kazakhstan’s ranking is (ranking-value: land-abs-time_KAZ value: position time:2081-2100 scenario:rcp60).
Kazakhstan is the (ranking-value: land-abs-temp_KAZ 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 Kazakhstan’s annual popu
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.0 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 -0.0 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.
Kazakhstan is the (ranking-value: pop-abs-temp_KAZ 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), Kazakhstan’s ranking is (ranking-value: pop-abs-time_KAZ value: position time:2081-2100 scenario:rcp60).
Kazakhstan is the (ranking-value: pop-abs-temp_KAZ 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 Kenya’s annual land area af
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 400 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 2100 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 700 km<sup>2</sup> under RCP6.0.
Kenya is the (ranking-value: land-abs-temp_KEN 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), Kenya’s ranking is (ranking-value: land-abs-time_KEN value: position time:2081-2100 scenario:rcp60).
Kenya is the (ranking-value: land-abs-temp_KEN 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 Kenya’s annual populatio
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.
Kenya is the (ranking-value: pop-abs-temp_KEN 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), Kenya’s ranking is (ranking-value: pop-abs-time_KEN value: position time:2081-2100 scenario:rcp60).
Kenya is the (ranking-value: pop-abs-temp_KEN 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 Kyrgyzstan’s annual land ar
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 2800 km<sup>2</sup> (1.5% of the land area) towards the end of the century (2081-2100). Following the low emission scenario (RCP2.6) the change would only reach 1600 km<sup>2</sup> (1.5% of the land area). By the middle of the century, changes reach 2500 km<sup>2</sup> under RCP2.6 and 600 km<sup>2</sup> under RCP6.0.
Kyrgyzstan is the (ranking-value: land-abs-temp_KGZ 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), Kyrgyzstan’s ranking is (ranking-value: land-abs-time_KGZ value: position time:2081-2100 scenario:rcp60).
Kyrgyzstan is the (ranking-value: land-abs-temp_KGZ 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 Kyrgyzstan’s annual popu
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.
Kyrgyzstan is the (ranking-value: pop-abs-temp_KGZ 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), Kyrgyzstan’s ranking is (ranking-value: pop-abs-time_KGZ value: position time:2081-2100 scenario:rcp60).
Kyrgyzstan is the (ranking-value: pop-abs-temp_KGZ 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 Cambodia’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 500 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 400 km<sup>2</sup> under RCP6.0.
Cambodia is the (ranking-value: land-abs-temp_KHM 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), Cambodia’s ranking is (ranking-value: land-abs-time_KHM value: position time:2081-2100 scenario:rcp60).
Cambodia is the (ranking-value: land-abs-temp_KHM 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 Cambodia’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 (0.1% 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.
Cambodia is the (ranking-value: pop-abs-temp_KHM 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), Cambodia’s ranking is (ranking-value: pop-abs-time_KHM value: position time:2081-2100 scenario:rcp60).
Cambodia is the (ranking-value: pop-abs-temp_KHM 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 Kiribati’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 0 km<sup>2</sup> under RCP6.0.
Kiribati is the (ranking-value: land-abs-temp_KIR 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), Kiribati’s ranking is (ranking-value: land-abs-time_KIR value: position time:2081-2100 scenario:rcp60).
Kiribati is the (ranking-value: land-abs-temp_KIR 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 Kiribati’s annual popula
Following the higher-emissions scenario (RCP6.0) the population exposed to droughts is expected to increase by 0.1 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 0.1 million people (100.0% 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.
Kiribati is the (ranking-value: pop-abs-temp_KIR 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), Kiribati’s ranking is (ranking-value: pop-abs-time_KIR value: position time:2081-2100 scenario:rcp60).
Kiribati is the (ranking-value: pop-abs-temp_KIR 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 Republic of Korea’s annual
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 200 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 200 km<sup>2</sup> under RCP2.6 and -100 km<sup>2</sup> under RCP6.0.
Republic of Korea is the (ranking-value: land-abs-temp_KOR 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), Republic of Korea’s ranking is (ranking-value: land-abs-time_KOR value: position time:2081-2100 scenario:rcp60).
Republic of Korea is the (ranking-value: land-abs-temp_KOR 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 Republic of Korea’s annu
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 0.1 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.
Republic of Korea is the (ranking-value: pop-abs-temp_KOR 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), Republic of Korea’s ranking is (ranking-value: pop-abs-time_KOR value: position time:2081-2100 scenario:rcp60).
Republic of Korea is the (ranking-value: pop-abs-temp_KOR 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 Kuwait’s annual land area a
Following the higher-emissions scenario (RCP6.0) the land area affected by droughts is expected to increase by 1300 km<sup>2</sup> (7.2% 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> (7.2% of the land area). By the middle of the century, changes reach 100 km<sup>2</sup> under RCP2.6 and 200 km<sup>2</sup> under RCP6.0.
Kuwait is the (ranking-value: land-abs-temp_KWT 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), Kuwait’s ranking is (ranking-value: land-abs-time_KWT value: position time:2081-2100 scenario:rcp60).
Kuwait is the (ranking-value: land-abs-temp_KWT 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 Kuwait’s annual populati
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.
Kuwait is the (ranking-value: pop-abs-temp_KWT 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), Kuwait’s ranking is (ranking-value: pop-abs-time_KWT value: position time:2081-2100 scenario:rcp60).
Kuwait is the (ranking-value: pop-abs-temp_KWT value: position temperature:2) strongest affected by droughts at 2°C of global warming.
### How is soil moisture calculated?
......
Markdown is supported
0% or .
You are about to add 0 people to the discussion. Proceed with caution.
Finish editing this message first!
Please register or to comment