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The influence of varying atmospheric CO2 on global warming potentials and carbon emission impulse response functions
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The influence of varying atmospheric CO2 on global warming potentials and carbon emission impulse response functions
The influence of varying atmospheric CO2 on global warming potentials and carbon emission impulse response functions
Journal Article

The influence of varying atmospheric CO2 on global warming potentials and carbon emission impulse response functions

2025
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Overview
Impulse response functions (IRF), the response in a climate parameter to an emission pulse of CO2, are used to characterize Earth system response timescales and to calculate Global Warming Potentials (GWPs). GWPs are widely used to compare emissions of different greenhouse gases and to compute CO2 equivalent emissions as reported by governments to the United Nations Framework Convention on Climate Change (UNFCCC). The GWP of any gas x is the absolute GWP of gas x Absolute and relative Global Warming Potential (AGWPx) divided by AGWP of CO2. Ideally, AGWP CO2 and GWPx would be independent of atmospheric CO2 and climate. However, AGWP CO2 , and, in turn, GWPx change under rising atmospheric CO2 and global warming, affecting the emission reporting under the UNFCCC. Here, we apply perturbed parameter ensemble simulations, constrained in a Bayesian approach by observational data, to investigate how AGWP CO2 and IRF vary under different atmospheric background CO2 levels (CO 2,bg ). We provide analytical formulations to compute AGWP CO2 and IRF for CO2, ocean and land carbon uptake, global mean surface air temperature, steric sea level, and ocean heat content, and to adjust these metrics to different CO 2,bg . AGWP CO2 , given by the time-integrated response in CO2 at year 100 multiplied by its radiative efficiency, is 101.8(±13.5) 10−15 yr W m−2 kg-CO 2−1 for CO 2,bg = 425 ppm and decreases by 7% for CO 2,bg = 500 ppm. The decrease is driven by a decrease in the radiative efficiency of CO2, partly canceled by a concomitant increase of IRF CO2 due to muted ocean and land carbon uptake under higher CO2 levels. We recommend regularly adjusting AGWP CO2 and, in turn, GWPs of long-lived gases to contemporary atmospheric CO2 and climate.