For most reasonable emissions pathways, temperature and linked physical effects depend only on cumulative emissions*. Delaying a given emission by some time therefore does not impact the amount of climate change it causes, so from a climate-focused perspective we don’t see any change in the harm of emissions with time (this may not be true at very low net emissions rates but is at rates similar to present-day). This would mean that the only time delaying emissions would have any climatic benefit would be if they are delayed until a time when net emissions are negative (in which case the world experiences a lower peak cumulative emissions than it would do when emitting without the delay, which we assume is less bad). It’s not clear if and when this will happen, and climate-based discounting would be 0 before that point.
This suggests that for all climatic ‘badness functions’ (effects on humans/ecology) no discounting is needed, however this may depend on the rate of change as well as the state of the system, and human impacts may also depend human development, equality and preparation for climate change. As we hope that the rate of emission will begin to decrease soon, this would mean that delayed emissions might be less impactful in the future. It’s going to be very assumption/IAM-dependent as to how much though. It’s also not clear that this generates a positive discount rate—it’s possible that people seeing more climate change sooner incentivises more research/investment in averting it, which takes time to pay off.
It’s important to distinguish two different factors that could be relevant when discussing this – one is the social cost of carbon (potentially measured in money lost, or in more egalitarian DALY losses), the other is the carbon market value of carbon. If one assumes the existence of a well-functioning global carbon market, then emissions at times after this may be largely absorbed by elasticity. However at times prior to this/if the market is not comprehensive, the ‘offsetting’ may be just displacing consumption.
A lower limit on the discount rate could come from the probability of catastrophic events (which may be a function of pure time, carbon concentration and derivative of concentration). In the event of a nuclear war, meteorite impact etc. our climate may no longer be determined primarily by emissions concentrations, hence carbon released after this period is of lower importance.
For most reasonable emissions pathways, temperature and linked physical effects depend only on cumulative emissions*. Delaying a given emission by some time therefore does not impact the amount of climate change it causes, so from a climate-focused perspective we don’t see any change in the harm of emissions with time (this may not be true at very low net emissions rates but is at rates similar to present-day). This would mean that the only time delaying emissions would have any climatic benefit would be if they are delayed until a time when net emissions are negative (in which case the world experiences a lower peak cumulative emissions than it would do when emitting without the delay, which we assume is less bad). It’s not clear if and when this will happen, and climate-based discounting would be 0 before that point.
This suggests that for all climatic ‘badness functions’ (effects on humans/ecology) no discounting is needed, however this may depend on the rate of change as well as the state of the system, and human impacts may also depend human development, equality and preparation for climate change. As we hope that the rate of emission will begin to decrease soon, this would mean that delayed emissions might be less impactful in the future. It’s going to be very assumption/IAM-dependent as to how much though. It’s also not clear that this generates a positive discount rate—it’s possible that people seeing more climate change sooner incentivises more research/investment in averting it, which takes time to pay off.
It’s important to distinguish two different factors that could be relevant when discussing this – one is the social cost of carbon (potentially measured in money lost, or in more egalitarian DALY losses), the other is the carbon market value of carbon. If one assumes the existence of a well-functioning global carbon market, then emissions at times after this may be largely absorbed by elasticity. However at times prior to this/if the market is not comprehensive, the ‘offsetting’ may be just displacing consumption.
A lower limit on the discount rate could come from the probability of catastrophic events (which may be a function of pure time, carbon concentration and derivative of concentration). In the event of a nuclear war, meteorite impact etc. our climate may no longer be determined primarily by emissions concentrations, hence carbon released after this period is of lower importance.
\* https://www.nature.com/articles/nature08019,
\* https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2019EF001312?fbclid=IwAR3nOrAs0l_WT6y7GibtOK-OYlktegmhaerDDu2_gArXh-lGZRT0ZzT8wFA