Carbon dioxide equivalent (CDE) and equivalent carbon dioxide (CO 2e and CO 2eq) are two related but distinct measures for estimating how much global warming a given type and amount of greenhouse gas may cause, using the functionally equivalent amount or concentration of carbon dioxide (CO 2) as the reference. CO 2e calculations depend on the time-scale chosen, typically 100 years but occasionally 20 years or less. They also depend on assumptions about the amount of time a given pollutant will remain in the atmosphere, which rely on other assumptions such as the amount of carbon sequestration that will occur in the future.
Carbon dioxide equivalency is a quantity that describes, for a given mixture and amount of greenhouse gas, the amount of CO 2 that would have the same global warming potential (GWP), when measured over a specified timescale (typically 100 years). Carbon dioxide equivalency thus reflects the time-integrated radiative forcing of a quantity of emissions or rate of greenhouse gas emission—a flow into the atmosphere—rather than the instantaneous value of the radiative forcing of the stock (concentration) of greenhouse gases in the atmosphere described by CO 2e.
The carbon dioxide equivalency for a gas is obtained by multiplying the mass and the GWP of the gas. The following units are commonly used:
By the UN climate change panel (IPCC): n×109tonnes of CO2 equivalent (GtCO2eq).
In industry: million metric tonnes of carbon dioxide equivalents (MMTCDE).
For vehicles: g of carbon dioxide equivalents / km (gCDE/km).
For example, the GWP for methane over 100 years is 34, and for nitrous oxide, 298. This means that emissions of 1 million tonnes of methane or nitrous oxide are equivalent to emissions of 34 or 298 million tonnes of carbon dioxide, respectively.
The radiative forcing for pure CO 2 is approximated by where C is the present concentration, is a constant, 5.35, and is the pre-industrial concentration, 280 ppm. Hence the value of CO 2e for an arbitrary gas mixture with a known radiative forcing is given by in ppmv.
To calculate the radiative forcing for a 1998 gas mixture, IPCC 2001 gives the radiative forcing (relative to 1750) of various gases as: CO 2=1.46 (corresponding to a concentration of 365 ppmv), CH4=0.48, N2O=0.15 and other minor gases =0.01 W/m2. The sum of these is 2.10 W/m2. Inserting this to the above formula, we obtain CO 2e = 412 ppmv.
To calculate the CO 2e of the additional radiative forcing calculated from April 2016's updated data: ∑ RF(GHGs) = 3.3793, thus CO 2e = 280 e3.3793/5.35 ppmv = 526.6 ppmv.
^Ocko, Ilissa B.; Hamburg, Steven P.; Jacob, Daniel J.; Keith, David W.; Keohane, Nathaniel O.; Oppenheimer, Michael; Roy-Mayhew, Joseph D.; Schrag, Daniel P.; Pacala, Stephen W. (2017). "Unmask temporal trade-offs in climate policy debates". Science. 356 (6337): 492–493. doi:10.1126/science.aaj2350. ISSN0036-8075.