Growth of climate change commitments from HFC banks and emissions
Author:
Velders G. J. M.ORCID, Solomon S., Daniel J. S.
Abstract
Abstract. Chlorofluorocarbons (CFCs) are the primary cause of ozone depletion, and they also contribute to global climate change. With the global phaseout of CFCs and the coming phaseout of hydrochlorofluorocarbons (HCFCs), the substitute hydrofluorocarbons (HFCs) are increasingly used. While CFCs were originally used mainly in applications such as spray cans and were released within a year after production, concern about the ozone layer led to reductions in rapid-release applications, and the relative importance of slower-release applications grew. HFCs are now mainly used in refrigerators and air-conditioners (AC) and are released over years to a decade after production. Their containment in such equipment represents banks, which are building up as production grows. A key finding of our work is that the increases of HFC banks represent a substantial unseen commitment to further radiative forcing of climate change after production of the chemicals ceases. We show that earlier phaseouts of HFCs would provide greater benefits for climate protection than previously recognized, due to the avoided buildup of the banks. If, for example, HFC production were to be phased out in 2020 instead of 2050, not only would about 91–146 GtCO2eq of cumulative emission be avoided from 2020 to 2050, but an additional bank of about 39–64 GtCO2eq is also avoided in 2050. Choices of later phaseout dates lead to larger commitments to climate change unless growing banks of HFCs from millions of dispersed locations are collected and destroyed.
Publisher
Copernicus GmbH
Reference23 articles.
1. AFEAS: Production, Sales and Atmospheric Release of Fluorocarbons Through 2006, Alternative Fluorocarbons Environmental Acceptability Study, available at: http://www.afeas.org (last access: February 2009), Arlington, VA, USA, 2009. 2. Daniel, J. S., Velders, G. J. M., Solomon, S., McFarland, M., and Montzka, S. A.: Present and future sources and emissions of halocarbons: towards new constraints, J. Geophys. Res., 112, D02301, https://doi.org/10.1029/2006JD007275, 2007. 3. Fisher, D. A. and Midgley, P. M.: Uncertainties in the calculation of atmospheric releases of chlorofluorocarbons, J. Geophys. Res., 99, 16643–16650, 1994. 4. Gamlen, P. H., Lane, B. C., Midgley, P. M., and Steed, J. M.: The production and release to the atmosphere of CCl3F and CCl2F2 (chlorofluorocarbons CFC 11 and CFC 12), Atmos. Environ., 20, 1077–1085, 1986. 5. Gschrey, B., Schwarz, W., Elsner, C., and Engelhardt, R.: High increase of global F-gas emissions until 2050, Greenhouse Gas Measurement & Management, 1, 85–92, 2011.
Cited by
1 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献
|
|