Earth system commitments due to delayed mitigation
Using an Earth System Model of Intermediate Complexity, we show that the current emission increase rate causes a ΔTmax increase roughly 3–7.5 times as fast as observed warming, and a millenial steric sea level rise (SSLR) 7–25 times as fast as observed SSLR, depending on the achievable rate of emission reductions after the peak of emissions.