A multi-control climate policy process for a trusted decision maker

Abstract

Persistent greenhouse gas (GHG) emissions threaten global climate goals and have prompted consideration of climate controls supplementary to emissions mitigation. We present an idealized model of optimally-controlled climate change, which is complementary to simpler analytical models and more comprehensive Integrated Assessment Models. We show that the four methods of controlling climate damage– mitigation, carbon dioxide removal, adaptation, and solar radiation modification– are not interchangeable, as they enter at different stages of the causal chain that connects GHG emissions to climate damages. Early and aggressive mitigation is always necessary to stabilize GHG concentrations at a tolerable level. The most cost-effective way of keeping warming below 2 degrees Celsius is a combination of all four controls; omitting solar radiation modification– a particularly contentious climate control– increases net control costs by 31%. At low discount rates, near-term mitigation and carbon dioxide removal are used to permanently reduce the warming effect of GHGs. At high discount rates, however, GHGs concentrations increase rapidly and future generations are required to use solar radiation modification to offset a large greenhouse effect. We propose a policy response process wherein climate policy decision-makers re-adjust their policy prescriptions over time based on evolving climate outcomes and revised model assumptions. We demonstrate the utility of the process by applying it to three hypothetical scenarios in which model biases in 1) baseline emissions, 2) geoengineering (CDR and SRM) costs, and 3) climate feedbacks are revealed over time and control policies are re-adjusted accordingly.

Control of the abyssal ocean overturning circulation by mixing-driven bottom boundary layers

“…For example, 90% of the heat trapped by anthropogenic forcing agents in the atmosphere has been stored in the ocean (Levitus et al, 2012). Including also carbon uptake, the uptake of atmospheric tracers by the deep ocean slows the transient rate of atmospheric global warming by up to 30%, buying society more time for climate mitigation and adaptation (Figure 1-1; Drake et al 2020b). In the absence of ocean mixing or circulation, these tracer exchanges would occur on an excessively long timescale (2000 m) 2 set by the slow rate of molecular diffusion, e.g.…”

“…Figure 1-1: Decomposing the global warming response (solid black line) to a hypothetical highemissions scenario (RCP-bollox; thick brown line) in a simple climate model (Drake et al 2020b, based on Joos et al 2013and Geoffroy et al 2012. The thin grey line (left axis) shows the hypothetical equilibrium response to the instantaneous radiative forcing in a given year (i.e.…”