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C A R B O NG L O B A LP R O J E C T
Laboratoiredes sciences du climatet de l’environnement
CARBONATLAS.ORG
supported byA project led by
designed by
Explore and download global and country level carbon
Explore and visualize research carbon data and get access through data providers.
Take a journey through the history and future of human development and carbon. OUTREACH
RESEARCH
EMISSIONS
400
300
200
100
0
ppm
-796,501
-763,724
-735,255
-700,370
-682,408
-624,204
-578,008
-556,382
-522,398
-486,257
-441,551
-396,075
-327,464
-284,117
-235,283
-196,961
-134,000
-105,568
-17,336
-9,327
-4,827 80
18791929
19792013
500 508 516 524 532 540 556 564 572 580
WHERE DO CARBON EMISSIONS COME FROM?
a platform to explore and visualizethe most up-to-date data on carbon fluxes
2100207020501950190010001000 BC5000 BC10 000 BC20 000 BC100 000 BC
100 PPM
200 PPM
300 PPM
400 PPM
500 PPM
600 PPM
700 PPM
800 PPM
900 PPM
2015
CO2 CONCENTRATION IN THE ATMOSPHERE
OCEAN LAND ATMOSPHERE + 3.2°C to + 5.4°C5.9°F – 9.7°F
We keep on relying on fossil fuels as the primary source of energyWe live in an energy-intensive world based on the use of ever more expensive and scarce fossil fuels. There is large transformation and damage to the natural environment and to the human enterprise. The cost of adaptation far exceeds the cost of climate mitigation.
+ 2.0°C to + 3.7°C3.6°F – 6.7°F
Slow but existing policy developmentA range of technologies and strategies for reducing greenhouse gas emissions are adopted : CO² emissions begin to decrease after 2100. The pace of mitigation is too slow to prevent very large changes in the natural and human environments across the globe.
+ 1.7°C to + 3.2°C3.1°F – 5.8°F
Big leaps towards a green economyThe nations have loosened their dependence on fossil fuels. Climate policies now also value natural vegetation for their carbon stores. But by 2100, global mean temperature will rise beyond 2°C with large consequences for natural and human environments.
+ 0.9°C to + 2.3°C1.6°F – 4.1°F
A fully decarbonized worldBy 2020, carbon emissions peak and then begin to rapidly fall, with emission reductions of about 50% by 2050. Society becomes fully decarbonized by the end of this century with the possible need for technologies that remove carbon dioxide from the atmosphere.
Sea level rises Permafrost shrinking
Significant negative impact on crop yields
Existing rainfall patterns will intensify at the regional level
Extreme precipitation events are more intense and frequent
Major species extinction
Vegetation losing efficiency in removing CO²
Coral reef subject to long-term degradation
Heat waves increase very significantly
Arctic sea ice could disappear in summer
TODAY’S CHOICE, TOMORROW’S IMPACTS
Uzbek
istan
Pakist
an
Vietnam
Malaysi
a
Taiw
an
Kazakh
stan
Thailan
d
Indonesia
South Korea
Japan
IndiaChina
Algeria
Egypt
S. Afri
ca
Czech
Republic
Netherl
ands
Spain
Ukraine
Poland
France
Italy
United Kingd
om
German
y
Russian
Federa
tion
Kuwait
Iraq
UAETu
rkey
Saudi A
rabia
Iran
Mexico
Canad
aUnite
d State
s
Argentina
Venez
uela
Brazil
Australi
a
AFR
ICA
ASI
AEU
ROPE
MID
DLE
EAST
NO
RTH
AM
ERIC
AO
CEA
NIA
LATI
NA
MER
ICA
&C
AR
RIB
EAN
Carbon emissions from land use and land-cover change
Land useChange
Gas flaring
Cement
Gas
Oil
Coal
EMISSIONS SOURCESWorld carbon emissions
in 2014 per source
REGIONAL EMISSIONSWorld carbon emissions
in 2014 per regionEmitters above
100 Mt CO² per year
MAJOR EMITTERS