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Paul A. Newman (USA) SAP co-chair NASA/GSFC Greenbelt, MD 20771 [email protected] Primarily derived from WMO (2011) The Montreal Protocol and hydrochlorofluorocarbons (HCFCs) HFC Management Workshop Paris, 11-12 July 2014 July 11, 2014 1 Workshop on HFC Management

Paul A. Newman (USA) SAP co-chair NASA/GSFC Greenbelt, MD 20771 [email protected] Primarily derived from WMO (2011) The Montreal Protocol and hydrochlorofluorocarbons

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Page 1: Paul A. Newman (USA) SAP co-chair NASA/GSFC Greenbelt, MD 20771 paul.a.newman@nasa.gov Primarily derived from WMO (2011) The Montreal Protocol and hydrochlorofluorocarbons

Paul A. Newman (USA)SAP co-chairNASA/GSFC

Greenbelt, MD [email protected]

Primarily derived from WMO (2011)

The Montreal Protocol and hydrochlorofluorocarbons

(HCFCs)

HFC Management Workshop Paris, 11-12 July 2014

July 11, 2014 1Workshop on HFC Management

Page 2: Paul A. Newman (USA) SAP co-chair NASA/GSFC Greenbelt, MD 20771 paul.a.newman@nasa.gov Primarily derived from WMO (2011) The Montreal Protocol and hydrochlorofluorocarbons

Montreal Protocol signed

Em

issi

on

sC

FC

-11

equ

ival

ent

Meg

ato

nn

es/y

r

1960 1970 1980 1990 2000 2010 20200

1

2

HCFC accelerated phase-out(Montreal – 2007 adjustment)

Emissions of ozone depleting substances has declined under the

Montreal Protocol

July 11, 2014 2Workshop on HFC Management

Page 3: Paul A. Newman (USA) SAP co-chair NASA/GSFC Greenbelt, MD 20771 paul.a.newman@nasa.gov Primarily derived from WMO (2011) The Montreal Protocol and hydrochlorofluorocarbons

What are HCFCs?

• Hydroclorofluorocarbons (HCFCs) first appeared in the atmosphere in the 1960s to the 1980s.

• HCFCs were adopted as “interim” substitutes for CFCs following the Montreal Protocol.

• HCFCs are primarily destroyed in the troposphere by reaction with the OH molecule, and some small losses by reactions with oxygen atoms and sunlight.

July 11, 2014 3Workshop on HFC Management

Page 4: Paul A. Newman (USA) SAP co-chair NASA/GSFC Greenbelt, MD 20771 paul.a.newman@nasa.gov Primarily derived from WMO (2011) The Montreal Protocol and hydrochlorofluorocarbons

  FormulaLifetime

(yr) ODPRadiative

Efficiency100-y GWP

CFC-11 CFCl3 52 1.00 0.25 4750

HCFC-21 CHCl2F 1.7 0.04 0.14 151

HCFC-22 CHClF2 12.0 0.05 0.20 1790

HCFC-123 CHCl2CF3 1.3 0.02 0.14 77

HCFC-124 CHClFCF3 5.9 0.02 0.22 619

HCFC-141b CH3CCl2F 9.4 0.11 0.14 717

HCFC-142b CH3CClF2 18.0 0.06 0.20 2220

HCFC-225ca CHCl2CF2CF3 1.9 0.02 0.20 122

HCFC-225cb CHClFCF2CClF2 5.9 0.03 0.32 606

HCFCs contribute to ozone depletion, and climate change

HCFC-142b

HCFC-22

HCFC-141b

190.0 ppb

19.4 ppb18.7 ppb

PrincipalHCFCs

Low ODPs w/r to CFC-11High GWPsJuly 11, 2014 4Workshop on HFC Management

Page 5: Paul A. Newman (USA) SAP co-chair NASA/GSFC Greenbelt, MD 20771 paul.a.newman@nasa.gov Primarily derived from WMO (2011) The Montreal Protocol and hydrochlorofluorocarbons

Emissions are expected to grow over the next decade, but will be phased out in

response to Montreal (2007)

HCFC emissions should soon

begin to decline

Growth of CFCs without MP

HFC emissions are currently expected to

substantially increase in the coming decades to

replace HCFCs (see Dr. Ravishankara talk).

July 11, 2014 5Workshop on HFC Management

Page 6: Paul A. Newman (USA) SAP co-chair NASA/GSFC Greenbelt, MD 20771 paul.a.newman@nasa.gov Primarily derived from WMO (2011) The Montreal Protocol and hydrochlorofluorocarbons

HCFCs contributed about 7.5% of the total chlorine to the stratosphere in 2008

Includes HCFC-22, -141b, -142b,

-124

July 11, 2014 6Workshop on HFC Management

Page 7: Paul A. Newman (USA) SAP co-chair NASA/GSFC Greenbelt, MD 20771 paul.a.newman@nasa.gov Primarily derived from WMO (2011) The Montreal Protocol and hydrochlorofluorocarbons

HCFCs continue to increase, but are projected to decrease starting in about 2030

July 11, 2014 7Workshop on HFC Management

The 2007 HCFC Amendment leads to a HCFC decrease that

begins in the late 2020s

The 2007 HCFC Amendment leads to a HCFC decrease that

begins in the late 2020s

Observa

tions

Observa

tions

Obs

erva

tions

Page 8: Paul A. Newman (USA) SAP co-chair NASA/GSFC Greenbelt, MD 20771 paul.a.newman@nasa.gov Primarily derived from WMO (2011) The Montreal Protocol and hydrochlorofluorocarbons

HCFCs now comprise a considerable bank of ODSs and greenhouse gases

July 11, 2014 8Workshop on HFC Management

Page 9: Paul A. Newman (USA) SAP co-chair NASA/GSFC Greenbelt, MD 20771 paul.a.newman@nasa.gov Primarily derived from WMO (2011) The Montreal Protocol and hydrochlorofluorocarbons

HCFC GWP weighted emissions grow in importance

until about 2020

HCFCs are beginning to dominate GWP weighted emissions

Total radiative forcing falls off after about

2020, consistent with the shorter lifetimes of

HCFCs

July 11, 2014 9Workshop on HFC Management

Page 10: Paul A. Newman (USA) SAP co-chair NASA/GSFC Greenbelt, MD 20771 paul.a.newman@nasa.gov Primarily derived from WMO (2011) The Montreal Protocol and hydrochlorofluorocarbons

Summary

• HCFCs are interim compounds that have served as replacements for CFCs

• HCFCs are weaker ODSs than CFCs, but still contribute a significant contribution to chlorine in the stratosphere. They are also significant GHGs

• HCFCs are still increasing in the atmosphere, but should stop increasing in the mid-to-late 2020s.

• The 2007 phase-out will successfully reduce 2011-50 HCFC emissions by – 0.6–0.8 ODP-Mt - total– 0.4–0.6 GtCO2-eq per year– The effective chlorine return to 1980 levels is earlier by 4-5 years.

July 11, 2014 10Workshop on HFC Management