Our new infographic, based on IPCC data, depicts the likely consequences of various
emissions pathways ranging from a low - carbon future to a fossil fuel - intensive one.
The infographic below, based on IPCC data, depicts the likely consequences of various
emissions pathways ranging from a low - carbon future to a fossil fuel - intensive one.
Not exact matches
The What We Know report further states that «according to the IPCC, given the current
pathway for carbon
emissions the high end of the «likely»
range for the expected increase in global temperature is about 8 ˚ F by the end of the century.
When we adjust the TAR
emissions scenarios to include an atmospheric CO2
pathway that is based upon observed CO2 increases during the past 25 yr, we find a warming
range of 1.5 — 2.6 °C prior to the adjustments for the new findings.
In summary, transitioning toward a 2oC
pathway, as suggested by the
range of related 2040 performance levels shown on the chart, would imply that global
emissions peak and steadily fall to close to 1980 levels by 2040.
The chart also illustrates a
range of 2040 «performance levels» reflecting hypothetical combinations of global energy intensity and CO2
emission intensity levels that, if reached in 2040, might indicate the world was on a 2oC
pathway.
Therefore, across any reasonable
range of
pathways, two other factors remain critical to limiting CO2
emissions:
Whether you agree with it or not, the projections by 2050
range from a minimum of around 1.5 oC (if we choose to follow a very low
emission pathway) to around 2.6 oC (if we choose to follow a very high
emission pathway).
Given the
range for climate sensitivity, it is clear that it is possible that we could follow a reasonably high
emission pathway and not warm substantially (okay, this may not be true if we follow a particularly high
emission pathway, but let's agree that there is a possibility that warming will not be substantial for some reasonable
emission pathway).
A wider
range of functional forms to describe
emission pathways would be expected to reduce the strength of the relationship between 2050
emissions and peak warming.
Extending this analysis to include
pathways with cumulative
emissions of more than 3 TtC, a resultant warming of more than 3 — 4 °C, or cases in which temperatures fail to peak by 2500 would be possible in principle, but would take us outside the
range of
pathways for which such a simple model is appropriate.
We choose the
ranges of the parameters to give a
range of
emission pathways with cumulative
emissions to 2200 between 0.7 and 3 TtC.
Our method consists of deriving a
range of idealized CO2
emission pathways and using a simple coupled climate — carbon - cycle model to estimate the resulting climate change.
This limited
range of
pathways all have a rate of warming less than 0.2 °C per decade, which initially suggests that a cumulative
emissions target could be used to constrain rates of warming, assuming that rates of decline are kept at less than 4 per cent per year.
Projected global average temperature rise above pre-industrial levels under a
range of future scenarios, «business as usual» (BAU), which assumes no mitigation efforts are made (RCP8.5); «mitigation», which assumes moderate
emissions (RCP4.5) without negative
emissions, «carbon dioxide removal» (CDR), which assumes moderate
emissions with long - term CO2 removal; and «solar radiation management» (SRM), which is the same as the CDR
pathway but also includes enough SRM to limit temperatures to 1.5 C by 2100.
Representative Concentration
Pathways, are referred to as pathways in order to emphasize that they are not definitive scenarios, but rather internally consistent sets of time - dependent forcing projections that could potentially be realized with more than one underlying socioeconomic scenario... They are representative in that they are one of several different scenarios, sampling the full range of published scenarios (including mitigation scenarios) at the time they were defined, that have similar RF and emissions characte
Pathways, are referred to as
pathways in order to emphasize that they are not definitive scenarios, but rather internally consistent sets of time - dependent forcing projections that could potentially be realized with more than one underlying socioeconomic scenario... They are representative in that they are one of several different scenarios, sampling the full range of published scenarios (including mitigation scenarios) at the time they were defined, that have similar RF and emissions characte
pathways in order to emphasize that they are not definitive scenarios, but rather internally consistent sets of time - dependent forcing projections that could potentially be realized with more than one underlying socioeconomic scenario... They are representative in that they are one of several different scenarios, sampling the full
range of published scenarios (including mitigation scenarios) at the time they were defined, that have similar RF and
emissions characteristics.
To cover this vast amount of ground, it discusses, at a high level, subjects
ranging from observations of various parts of the climate system and climate modelling to the limits of economic assessments, the different
pathways of greenhouse gas
emissions considered, adaptation response strategies and methods of mitigation that include everything from from taxing greenhouse gas
emissions to removing carbon dioxide directly from the atmosphere.
When we adjust the TAR
emissions scenarios to include an atmospheric CO2
pathway that is based upon observed CO2 increases during the past 25 yr, we find a warming
range of 1.5 - 2.6 °C prior to the adjustments for the new findings.
The projected 2081 - 2100
range of even Representative Concentration
Pathway (RCP) 4.5 — an
emissions scenario which we are currently exceeding greatly, and the mildest one barring the sort active drawdown just mentioned — is 1.1 to 2.6 C, with a mean of 1.8 C.
Global carbon dioxide
emissions continue to track the high end of a
range of
emission scenarios, expanding the gap between current
emission trends and the
emission pathway required to keep the global - average temperature increase below 2 degrees Celsius.