the information contained in this report largely derives from the scientific assessment of ozone...

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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 Report of the Scientific Assessment Panel Open-Ended Working Group Meeting 20 July 2015 - Paris

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Page 1: The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014 From CFCs to HCFCs to HFCs World Meteorological

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

Report of the Scientific Assessment PanelOpen-Ended Working Group Meeting

20 July 2015 - Paris

Page 2: The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014 From CFCs to HCFCs to HFCs World Meteorological

Ozone-depleting substances (ODSs) are decreasing

312 ppt (9%) decline of chlorine

20 July 2015 OEWG meeting Paris 2

Page 3: The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014 From CFCs to HCFCs to HFCs World Meteorological

Ozone-depleting substances (ODSs) are decreasing

2 ppt (12%) decline of Br

20 July 2015 OEWG meeting Paris 3

Page 4: The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014 From CFCs to HCFCs to HFCs World Meteorological

Ozone levels seems to have improved, but cannot say they are

statistically significant

20 July 2015 OEWG meeting Paris 4

We have previously reported on the response of the ozone layer to the changes in ODSs.

Ozone in the upper stratosphere is increasing, as expected. Both CO2 increases and ODSs decreases contribute to this increase

The global ozone and the ozone hole are not getting worse; they appear to be slightly better but it is too early to tell.

Page 5: The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014 From CFCs to HCFCs to HFCs World Meteorological

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

20 July 2015 OEWG meeting Paris 5

Page 6: The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014 From CFCs to HCFCs to HFCs World Meteorological

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

20 July 2015 OEWG meeting Paris 6

Page 7: The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014 From CFCs to HCFCs to HFCs World Meteorological

Stopping all future emissions advances ODS recovery by about 11 years

20 July 2015 OEWG meeting Paris 7

Page 8: The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014 From CFCs to HCFCs to HFCs World Meteorological

CFCs emissions continue to decline, but other compounds are increasing

Let’s zoom in

20 July 2015 OEWG meeting Paris 8

Page 9: The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014 From CFCs to HCFCs to HFCs World Meteorological

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

20 July 2015 OEWG meeting Paris 9

Page 10: The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014 From CFCs to HCFCs to HFCs World Meteorological

Evolution of strategy to eliminate ozone depleting substances

Some HFCs are potent greenhouse gases.e.g., HCFC-134a- GWP~1300 (compare with CFC-12 with GWP ~10,000)

20 July 2015 OEWG meeting Paris 10

HFCs are the main replacements in many ODS applications. HFCs growth is primarily due to their uses as ODS-substitutes. HFCs are increasing rapidly.

UNEP HFC

reportCons

umpti

on

(mill

ion

tonn

es C

O2-e

q.)

0

200

400

600

800

1000

1990 2002 2010

Page 11: The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014 From CFCs to HCFCs to HFCs World Meteorological

Atmospheric observations show increases in HFCs

All HFCs are increasing. Most HFCs are increasing rapidly… Current HFC abundances are still small – together their

abundance is roughly < 115 ppt (excluding HFC-23), i.e.,

20% of the current CFC-12 abundance.

WMO/UNEP 2014 SAP report

20 July 2015 OEWG meeting Paris 11

Page 12: The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014 From CFCs to HCFCs to HFCs World Meteorological

Emissions of HFCs are increasing

HFC emissions are increasing. Recent HFC-23 emission changes are consistent with effectiveness

of the CDM in recapture and destruction.

Total

HFC-23

HFCs used as ODS substitutesUsing data from

WMO/UNEP 2014 SAP report

20 July 2015 OEWG meeting Paris 12

Page 13: The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014 From CFCs to HCFCs to HFCs World Meteorological

Uses of HFCs (ODS substitutes)

MAC, refrigeration, and other uses are roughly the same. Emissions from all uses are increasing at roughly the same

rate.

From Montzka et al. 2014/2015

20 July 2015 OEWG meeting Paris 13

Page 14: The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014 From CFCs to HCFCs to HFCs World Meteorological

Increases are consistent with estimates

Emissions from countries not expected to report to UNFCCC are increasing very rapidly.

From Montzka et al., 2014/2015

20 July 2015 OEWG meeting Paris 14

Consistent with Velders et al. 2009 Projections

Emissions from countries not reporting to UNFCCC

HFCs-

*

* HFCs other than 134a and 23, i.e., -125, -43a, -32, -152a, -227ea, 365mfc

Emissions are consistent with Velders et al. 2009 estimates for total and individual chemicals…. Lends confidence to projections

Page 15: The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014 From CFCs to HCFCs to HFCs World Meteorological

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

20 July 2015 OEWG meeting Paris 15

Page 16: The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014 From CFCs to HCFCs to HFCs World Meteorological

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

20 July 2015 OEWG meeting Paris 16

Page 17: The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014 From CFCs to HCFCs to HFCs World Meteorological

Future emissions of HFCs could make a large contribution to climate change

Future HFC contribution to climate change (as measured by

radiative forcing) can be large.o Radiative forcing by future HFC emissions can be ~25%

of that of CO2 future emissions.

CFCs and HCFCs

Various HFCScenarios

WMO/UNEP 2014 SAP report

20 July 2015 OEWG meeting Paris 17

Page 18: The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014 From CFCs to HCFCs to HFCs World Meteorological

HFCs contribution to climate change by future emissions can be large

Radiative forcing by future HFC emissions can be ~25% of

that of CO2 future emissions (scenarios from SRES).

Future HFC emissions can significantly undermine

achievements of the 450 ppm stabilization targets.

From UNEP HFC report

20 July 2015 OEWG meeting Paris 18

Page 19: The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014 From CFCs to HCFCs to HFCs World Meteorological

There are ways to avoid large climate effects of HFCs

Possible to retain a <1% contribution in 2050 if HFCs with GWP <20 and other alternatives are used, even for the upper range emissions scenarios.

Such alternatives appear to be available.

Impacts of TFA from HFO-1234yf, a potential substitute, are negligible over the the next decade. Longer-term impacts require future evaluations.

Rad

iativ

e F

orci

ng

(W m

-2)

2000 2010 2020 2030 2040 2050 Year

Progressively lower GWPFrom UNEP

HFC report

20 July 2015 OEWG meeting Paris 19

Page 20: The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014 From CFCs to HCFCs to HFCs World Meteorological

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.

• Alternatives to use of high GWP HFCs are

available

20 July 2015 OEWG meeting Paris 20

Page 21: The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014 From CFCs to HCFCs to HFCs World Meteorological

Thank you for

your attention.

20 July 2015 OEWG meeting Paris 21

Page 22: The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014 From CFCs to HCFCs to HFCs World Meteorological

HFC emissions projections by sectors

Velders et al., 2015 (to be

published)

Emission projections for various geographical regions and usage sectors are becoming available

Regional Emissions Sectoral Emissions

20 July 2015 OEWG meeting Paris 22

Page 23: The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014 From CFCs to HCFCs to HFCs World Meteorological

20 July 2015 OEWG meeting Paris 23

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

Page 24: The information contained in this report largely derives from the Scientific Assessment of Ozone Depletion: 2014 From CFCs to HCFCs to HFCs World Meteorological

Evolution of strategy to eliminate ozone depleting substances

MP successfully phased out CFCs and is phasing out HCFCs. Phase out done via use of substitute chemicals or other

approaches.

CFCs,Halons,CH3Br,CCl4, MCF,etc.

HCFCsHigh GWP HFCs

Low GWP HFCs

Alternate technologies

Burkholder, Cox, and Ravishankara, 2015

20 July 2015 OEWG meeting Paris 24