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OEWG, Bangkok, Thailand 22 April 2015 The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014 From CFCs to HCFCs to HFCs Co-Chairs: Ayité-Lô Ajavon Paul A. Newman John Pyle A.R. Ravishankara Scientific Steering Committee: Co-Chairs & David Karoly Malcolm Ko Theodore Shepherd Susan Solomon Coordinating Editor: Christine Ennis
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OEWG, Bangkok, Thailand 22 April 2015 The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014.

Dec 18, 2015

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Page 1: OEWG, Bangkok, Thailand 22 April 2015 The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014.

OEWG, Bangkok, Thailand22 April 2015

The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014

From CFCs to HCFCs to HFCs

Co-Chairs:

Ayité-Lô AjavonPaul A. NewmanJohn PyleA.R. Ravishankara

Scientific Steering Committee:Co-Chairs &David KarolyMalcolm KoTheodore ShepherdSusan Solomon

Coordinating Editor:Christine Ennis

Page 2: OEWG, Bangkok, Thailand 22 April 2015 The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014.

Ozone-depleting substances (ODSs) are decreasing

312 ppt (9%) decline of chlorine

Page 3: OEWG, Bangkok, Thailand 22 April 2015 The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014.

Ozone-depleting substances (ODSs) are decreasing

2 ppt (12%) decline of Br

Page 4: OEWG, Bangkok, Thailand 22 April 2015 The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014.

In spite of lifetime and bank changes from 2011, the WMO (2015) scenario is about the same

Page 5: OEWG, Bangkok, Thailand 22 April 2015 The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014.

Stopping all future production of HCFCs has only a limited effect on the 2015 scenario

Page 6: OEWG, Bangkok, Thailand 22 April 2015 The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014.

Destruction of all ODS banks by 2020 also has limited impact on the evolution of ODSs

Page 7: OEWG, Bangkok, Thailand 22 April 2015 The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014.

Stopping all future emissions advances ODS recovery by about 11 years

Page 8: OEWG, Bangkok, Thailand 22 April 2015 The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014.

CFCs emissions continue to decline, but other compounds are increasing

Let’s zoom in

Page 9: OEWG, Bangkok, Thailand 22 April 2015 The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014.

In 2013, the emissions of CFCs, HCFCs, and HFCs were about equal in G tonnes CO2-equivalent

Page 10: OEWG, Bangkok, Thailand 22 April 2015 The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014.

HFCs are increasing in the atmosphere

HFC-23 global abundance is growing, and emissions continue to increase

Page 11: OEWG, Bangkok, Thailand 22 April 2015 The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014.

ODS contributions to climate forcing were large, but are declining as ODS levels decrease

Page 12: OEWG, Bangkok, Thailand 22 April 2015 The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014.

HFC contributions are growing because of the MP, and will eventually offset the climate gains achieved by the regulation of ODSs

Page 13: OEWG, Bangkok, Thailand 22 April 2015 The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014.

The combined radiative impact of CFCs, HCFCs, and HFCs will continue to grow over the next few decades

Page 14: OEWG, Bangkok, Thailand 22 April 2015 The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014.

By mid-century, HFCs are beginning to dominate the total radiative forcing

Page 15: OEWG, Bangkok, Thailand 22 April 2015 The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014.

By mid-century, HFCs are beginning to dominate the total radiative forcing

Page 16: OEWG, Bangkok, Thailand 22 April 2015 The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014.

Summary

• ODSs are declining in our atmosphere• The radiative forcing by CFCs and

HCFCs will decline over the course of

the 21st century• Radiative forcing by future HFC

emissions can be ~25% of that of CO2

future emissions.• Future HFC emissions may hinder the

450 ppm CO2 stabilization target.