Quick search Find article
Quick search
Find article

Allowable CO2 concentrations under the United Nations Framework Convention on Climate Change as a function of the climate sensitivity probability distribution function

L D Danny Harvey

Show affiliations


Article 2 of the United Nations Framework Convention on Climate Change (UNFCCC) calls for stabilization of greenhouse gas (GHG) concentrations at levels that prevent dangerous anthropogenic interference (DAI) in the climate system. Until recently, the consensus viewpoint was that the climate sensitivity (the global mean equilibrium warming for a doubling of atmospheric CO2 concentration) was 'likely' to fall between 1.5 and 4.5 K. However, a number of recent studies have generated probability distribution functions (pdfs) for climate sensitivity with the 95th percentile of the expected climate sensitivity as large as 10 K, while some studies suggest that the climate sensitivity is likely to fall in the lower half of the long-standing 1.5–4.5 K range. This paper examines the allowable CO2 concentration as a function of the 95th percentile of the climate sensitivity pdf (ranging from 2 to 8 K) and for the following additional assumptions: (i) the 50th percentile for the pdf of the minimum sustained global mean warming that causes unacceptable harm equal to 1.5 or 2.5 K; and (ii) 1%, 5% or 10% allowable risks of unacceptable harm. For a 1% risk tolerance and the more stringent harm-threshold pdf, the allowable CO2 concentration ranges from 323 to 268 ppmv as the 95th percentile of the climate sensitivity pdf increases from 2 to 8 K, while for a 10% risk tolerance and the less stringent harm-threshold pdf, the allowable CO2 concentration ranges from 531 to 305 ppmv. In both cases it is assumed that non-CO2 GHG radiative forcing can be reduced to half of its present value, otherwise; the allowable CO2 concentration is even smaller. Accounting for the fact that the CO2 concentration will gradually fall if emissions are reduced to zero, and that peak realized warming will then be less than the peak equilibrium warming (related to peak radiative forcing) allows the CO2 concentration to peak at 10–40 ppmv higher than the limiting values given above for a climate sensitivity 95th percentile at 4.5 K. Even allowing for the difference between peak realized and peak equilibrium warming, and assuming that present non-CO2 GHG forcing can be cut in half, a CO2 concentration of 410 ppmv or less constitutes DAI for every combination of harm-threshold pdf and risk tolerance considered here if the 95th percentile of the climate sensitivity pdf is 4.5 K or greater.


PACS

92.60.Ry Climatology

92.60.Sz Air quality and air pollution

92.60.hf Tropospheric composition and chemistry, constituent transport and chemistry

92.60.Vb Solar radiation

Subjects

Environmental and Earth science

Dates

Issue 1 (January–March 2007)

Received 6 July 2006, accepted for publication 2 February 2007

Published 16 February 2007


A Perspective for this article has been published in 2007 Environ. Res. Lett. 2 011001


Related review articles

What's this?
View review articles related to this research to gain an insight into the key trends in this subject area. Related review articles are selected based on PACS/MSC codes, and are no more than three years old.

  1. Solar radiation transport in the cloudy atmosphere: a 3D perspective on observations and climate impacts
  2. Nucleation in the atmosphere

View by subject




Export








Please login to access our web services, or create an account if you don't yet have one.

You must have cookies enabled in your web browser to be able to login.

Username
Password

Forgotten your password? Get a new one here.