1

Online Supplemental Material

Integrated IR absorption intensities and calibration.

From Beer-Lambert’s law, the absorption cross-section of a compound J at a specific wavenumber is given by , where is the napierian absorbance,  is the transmittance, nJ is the number density of J and l is the path length over which the absorption takes place. The integrated absorption intensity, Sint, is given by:

The integrated cross-sections of the absorption bands of the compounds under study were determined by plotting the integrated absorbance intensities against the product of the number density and pathlength. Conservative estimates of systematic errors are: pressure measurements (0.5%), path length (1%), temperature (1%), and definition of the baseline in the integration procedure (1%). Tables Supplemental Tables 4 1 and 5 2 summarizes the calibration results while Figure 5Supplemental Figure 1 (see Supplemental Digital Content 1, see Figure 1 legend at end of supplement) displays the linear relationship between number density times pathlength and the measured integrated absorbance.

The integrated absorption cross-section (often referred to as the integrated band intensity, or IBI) of the 2000-450 cm-1 region of isoflurane has previously been reported by Sihra et al.(1) who gave a value of 27.44×1017 cm2 molecules-1 cm-1. The two results for IBI2000-450 are within the estimated systematic errors in the two studies. Brown et al.(2) have reported a value of (15.9 ± 0.8) ×1017 cm2 molecules-1 cm-1 for the 1200-800 cm-1 region of isoflurane. For the same region the present result is IBI1200-800 = (16.2 ± 0.2) ×1017 cm2 molecules-1 cm-1.

For sevoflurane Brown et al.(2) reported a value of IBI1200-800 = (10.4 ± 0.6) ×1017 cm2 molecules-1 cm-1 for sevoflurane. The present result is somewhat larger, (11.6 ± 0.3) ×1017 cm2 molecules-1 cm-1. However, it should be noted that that one of the integration limits used in the study of Brown et al.(2) fall in a cluster of bands and we therefore consider the two results consistent. For desflurane, Imasu et al. (3) reported a value of IBI2000-500 = (29.9 ± 0.7) ×1017 cm2 molecules-1 cm-1 in perfect agreement with the present result.

IR absorption cross-sections and radiative forcing.

The infrared absorption cross-sections were derived from the absorbance spectra assuming that the gases were ideal. The absorption cross-sections (base e) of isoflurane and sevoflurane in the 1600 – 400 cm-1 region are shown in Supplemental Figures 6 2 (see Supplemental Digital Content 2, see Figure 2 legend at end of supplement) and 73 (see Supplemental Digital Content 3, see Figure 3 legend at end of supplement). We routinely use the absorption cross-section of HCFC-22, which has been critically evaluated by Ballard et al. ,(4) as a benchmark (5-12). Our measurements of HCFC-22 (CHClF2) are constantly within 5% of the absorption intensities reported by Ballard and co-workers. As can be seen in Supplemental Table 36, the statistical variance in the integrated absorption cross-section of the compounds is at most 2%. Adding to this the above-mentioned systematic errors allows us to suggest that our spectroscopic results are accurate to within 5%.

Pinnock et al.(13) have provided a simple method for estimating the instantaneous cloudy-sky radiative forcing (IF) directly from a molecule’s absorption cross-sections. The instantaneous cloudy-sky radiative forcings are summarised in Supplemental Table 36 in which the previously reported results for desflurane (14) have been included for comparison.

It is interesting that sevoflurane, which has the largest integrated absorption cross section of the three anaesthetics, has the smallest instantaneous radiative forcing. This is due to the fact that several of the strongest absorption bands in sevoflurane fall in wavenumber regions where the CO2, O3 and water vapour dominates the radiative transfer properties of the atmosphere. Supplemental Figures 6-82 ( see Figure 2 legend at end of supplement), 3 ( see Figure 3 legend at end of supplement), and -4(see Supplemental Digital Content 4, see Figure 4 legend at end of supplement) illustrate this point.

Atmospheric Lifetimes and Global Warming Potentials.

The main atmospheric removal process for the compounds under investigation is the reaction with OH radicals. For isoflurane there are several reports of the rate coefficient for this reaction. In 1990 Brown et al. (2) reported a value of kOH+Isoflurane = (2.1 ± 0.7) × 10-14 cm3 molecule–1 s–1 in a study employing the discharge-flow resonance-fluorescence technique. In 1999 appeared three kinetic studies of the OH reaction with isoflurane. Tokuhashi et al.(15) studied the temperature dependency of the reaction rate constant using the flash photolysis, laser photolysis, and discharge-flow methods combined with the laser induced fluorescence technique to monitor the OH radical concentration and reported kOH+Isoflurane(T) = (1.12 ± 0.18) × 10-12 × exp(-1280 ± 50 K/T) cm3 molecule–1 s–1. Langbein et al.(16) reported kOH+Isoflurane = (2.3 ± 0.19) × 10-14 cm3 molecule–1 s–1 from the pseudo first-order decay of OH using the laser long-path absorption technique. Nolan et al.(17) reported kOH+Isoflurane = (2.3 ± 0.19) × 10-14 cm3 molecule–1 s–1 from relative rate experiments employing GC separation and flame ionisation detection. Finally, Beach et al.(18)determined the temperature dependency of the reaction rate constant using the discharge-flow resonance-fluorescence technique and reported kOH+Isoflurane(T) = (4.5 ± 1.3) × 10-13×exp(-940 ± 100 K/T) cm3 molecule–1 s–1. The available kinetic data are summarised in Supplemental Figure 5 (see Supplemental Digital Content 5, see Figure 5 legend at end of supplement)9. The data are generally in good agreement although it can be seen that the k(298 K) data of Beach et al. (18), Brown et al. (2) and Nolan et al. (17) apparently are 25-40% higher than the other data. A fit of the Arrhenius expression to the other data give kOH+Isoflurane(T) = (1.11 ± 0.12) × 10-12 × exp(-1275 K/T) cm3 molecule–1 s–1.

There are only two sets of kinetic data for the OH reaction with sevoflurane. Brown et al.(2) reported results for two temperatures from a study employing the discharge-flow resonance-fluorescence technique and gave kOH+Sevoflurane = 1.53 × 10-12 × exp(-900 ± 500 K/T) cm3 molecule–1 s–1. The other study is by Langbein et al.(16) who reported kOH+Sevoflurane = (2.7 ± 0.5) × 10-14 cm3 molecule–1 s–1 at 298 K from the pseudo first-order decay of OH using the laser long-path absorption technique. The scatter in the available data, Supplemental Figure 5 ( see Figure 5 legend at end of supplement)9, only allows a rough estimate of the reaction rate constant. Assuming Ea/R to be the same in sevoflurane as in isoflurane results in kOH+Sevoflurane(T) = 3.3 × 10-12 × exp(-1275 K/T) cm3 molecule–1 s–1 as a first approximation.

For comparison we include literature data for desflurane, CF3CHF-O-CHF2.(14) There are only two kinetic studies of the OH radical reaction with this compound, both carried out at room temperature. Langbein et al.(16) reported kOH+Desflurane = (4.4 ± 0.8) × 10-15 cm3 molecule–1 s–1 from the pseudo first-order decay of OH using the laser long-path absorption technique. Oyaro et al.(14) reported kOH+Desflurane = (6.5 ± 0.8) × 10-15 cm3 molecule–1 s–1 from relative rate measurements employing GS-MS detection. Taking the average of these and assuming Ea/R to be the same as in sevoflurane and isoflurane results in kOH+Desflurane(T) = 3.9 × 10-13 × exp(-1275 K/T) cm3 molecule–1 s–1 as a first approximation.

The atmospheric lifetime of a long-lived compound due to removal by reaction by OH radicals may be estimated once its rate coefficient for reaction with OH is known. Assuming that the compounds studied here (fluorinated ethers, FE) will have the same atmospheric distribution as CH3CCl3 their atmospheric lifetimes, , may be calculated relative to that of CH3CCl3 from:(19)

where years (20) is the atmospheric lifetime of CH3CCl3 with respect to reaction with OH, and the scaling temperature of 272 K is chosen to compensate for the tropospheric OH distribution.(21) Using kOH+CH3CCl3(272 K) = 6.14  10-15 cm3 molecule–1 s–1 from the latest JPL evaluation,(22) the following lifetimes in the gas-phase are found: ~3.6 years, ~1.2 years, ~ 10 years.

Global warming potentials for the FEs relative to CFC-11 (CCl3F), HGWP(t), can then be calculated from the following expression:(23)

where M is the molecular mass and t is the time horizon over which the instantaneous forcing is integrated. Global warming potentials for a 20-year, 100-year and 500-year time horizon for the FEs are summarized in Supplemental Table 47. The data on CFC-11 were taken from the IPCC 2007 report. (24) For compounds with atmospheric lifetimes in excess of 1 year, the Global warming potentials relative to CO2, GWP(t), were estimated from that of CFC-11 referenced to CO2:(25)

GWPFE(t) = HGWPFE(t) × GWPCFC-11(t)

Pinnock et al.(13) has reported that their model for estimating the instantaneous radiative forcing generally overestimates the real forcing when calculating the instantaneous radiative forcing directly from the absorption cross-sections. It is therefore likely that the present results provide upper estimates for the global warming potentials of the three FEs studied here. For comparison the values listed in the latest IPPC report for the GWP of isoflurane are included in Supplemental Table 47. The present estimates of the GWP for isoflurane compares quite well with the results of the more elaborate calculations behind the IPPC recommendation (24) suggesting that the more simplified estimation method gives reliable values. The slightly lower values in GWP for desflurane in the present work than in the previous study by Oyaro et al. (14) is due to a lowering of the estimated atmospheric lifetime from 10.288 to 10.08 years.

Supplemental Table 1. Integrated absorption intensity and absorption cross-section (base e) of the 2000-450 cm-1 region of isoflurane.

Table 4. Integrated absorption intensity and absorption cross-section (base e) of the 2000-450 cm-1 region of isoflurane.

Pressure Number densityIntegrated absorption Integrated absorption Pathlength intensity (base e) cross-section (base e)

/mbar/1017molecules cm-2/cm-1/1017 cm2 molecules-1cm-1

1.08 ± 0.012.62 ± 0.0474.08 ± 1.1728.24 ± 0.4

1.52 ± 0.023.69 ± 0.05104.66 ± 0.3628.35 ± 0.4

1.89 ± 0.024.59 ± 0.06129.58 ± 0.6128.23 ± 0.4

2.55 ± 0.036.19 ± 0.09174.93 ± 0.6728.25 ± 0.4

2.66 ± 0.036.46 ± 0.09186.53 ± 2.5328.88 ± 0.4

2.67 ± 0.036.48 ± 0.09184.61 ± 0.4628.47 ± 0.4

3.01 ± 0.037.31 ± 0.10206.38 ± 1.2628.23 ± 0.4

4.67 ± 0.0511.3 ± 0.2325.12 ± 2.7728.67 ± 0.4

9.93 ± 0.1024.1 ± 0.3694.74 ± 1.9428.81 ± 0.4

28.5 ± 0.3 (average)

Supplemental Table 1. Integrated absorption intensity and absorption cross-section (base e) of the 2000-450 cm-1 region of isoflurane.

Supplemental Table 2. Integrated absorption intensity and absorption cross-section (base e) of the 2000-475 cm-1 region of sevoflurane.

Table 5. Integrated absorption intensity and absorption cross-section (base e) of the 2000-475 cm-1 region of sevoflurane.

Pressure Number densityIntegrated absorption Integrated absorption Pathlength intensity (base e) cross-section (base e)

/mbar/1017molecules cm-2/cm-1/1017 cm2 molecules-1cm

1.05 ± 0.012.55 ± 0.0478.29 ± 0.8230.70 ± 0.4

1.41 ± 0.023.42 ± 0.05106.73 ± 0.6331.17 ± 0.4

1.49 ± 0.023.62 ± 0.06112.93 ± 0.4131.21 ± 0.4

1.90 ± 0.034.61 ± 0.09139.15 ± 0.5630.16 ± 0.4

2.50 ± 0.036.07 ± 0.09187.18 ± 0.2430.83 ± 0.4

2.69 ± 0.036.53 ± 0.09202.04 ± 0.3030.93 ± 0.4

3.34 ± 0.038.11 ± 0.10241.50 ± 0.9829.77 ± 0.4

4.16 ± 0.0510.1 ± 0.2299.03 ± 0.4929.60 ± 0.4

4.62 ± 0.1011.2 ± 0.3343.06 ± 0.4930.58 ± 0.4

30.6 ± 0.6 (average)

Supplemental Table 2. Integrated absorption intensity and absorption cross-section (base e) of the 2000-475 cm-1 region of sevoflurane.

Supplemental Table 3. Instantaneous radiative forcing (IF) of isoflurane, sevoflurane and desflurane. a Data from Oyaro et al.((26))

Table 6. Instantaneous radiative forcing (IF) of isoflurane, sevoflurane and desflurane.

CompoundMInt. absorption cross sectionIF

/g mol-1/10-17 cm2 molecule-1 cm-1/W m-2

Isoflurane184.528.5 ± 0.30.453

Sevoflurane200.030.6 ± 0.60.365

Desflurane a168.030.3 ± 0.70.447

Supplemental Table 3. Instantaneous radiative forcing (IF) of isoflurane, sevoflurane and desflurane.

a Data from Oyaro et al.((26))

Supplemental Table 4. Estimated Global Warming Potentials HGWP(t) and GWP(t) for 20-year, 100-year and 500-year Time Horizons relative to CFC-11 and CO2, respectively.

a From IPPC 2007, (24). b From Brown et al. (2). c From Oyaro et al., (14) d From Imasu et al. (3)

Table 7. Estimated Global Warming Potentials HGWP(t) and GWP(t) for 20-year, 100-year and 500-year Time Horizons relative to CFC-11 and CO2, respectively.

CompoundLifetimeHGWP20HGWP100HGWP500GWP20GWP100GWP500

/year

CFC-11 a45111630046001600

Sevoflurane1.190.0700.0270.02334910632

Isoflurane3.570.2800.1070.0931401429130

2.6 b1100 a340 a110 a

Desflurane10.080.7430.3280.28437141314398

10.288 c0.753 c0.335 c3766 c1341 c

5.8d3100a960a300a

Supplemental Table 4. Estimated Global Warming Potentials HGWP(t) and GWP(t) for 20-year, 100-year and 500-year Time Horizons relative to CFC-11 and CO2, respectively.

a From IPPC 2007, (24). b From Brown et al. (2). c From Oyaro et al., (14) d From Imasu et al. (3)

Figure Legend

Supplemental Figure 1. Integrated absorption intensities (base e) of the 2000-450 cm-1 region in isoflurane and the 2000-475 cm-1 region in sevoflurane. The sevoflurane data have been shifted by 100 for the sake of clarity.

Figure 5. Integrated absorption intensities (base e) of the 2000-450 cm-1 region in isoflurane and the 2000-475 cm-1 region in sevoflurane. The sevoflurane data have been shifted by 100 for the sake of clarity.

Figure 6Supplemental Figure 2. Absorption cross section of isoflurane and radiative forcing per unit cross section for a 0 to 1 ppbv increase in mixing ratio.

Figure 7Supplemental Figure 3. Absorption cross section of sevoflurane and radiative forcing per unit cross section for a 0 to 1 ppbv increase in mixing ratio.

Figure 8Supplemental Figure 4. Absorption cross section of desflurane and radiative forcing per unit cross section for a 0 to 1 ppbv increase in mixing ratio. Infrared data from Ref. (26).

Figure 9Supplemental Figure 5. Arrhenius plots of rate constants for the reactions of OH radicals with isoflurane and sevoflurane. (×)Tokuhashi et al.(15); (●) Brown et al.(2); (o) Langbein et al.(16); (▲) Nolan et al.(17); (♦)Beach et al.(18) The dotted line corresponds to kOH+isoflurane(T) = 1.11 × 10-12 × exp(-1275 K/T) cm3 molecule–1 s–1, the full line corresponds to kOH+sevoflurane(T) = 3.3 × 10-12 × exp(-1275 K/T) cm3 molecule–1s–1. The data and curve for sevoflurane have been shifted by ln(10) for the sake of clarity.

15

1

References

1.Sihra K, Hurley MD, Shine KP, Wallington TJ. Updated radiative forcing estimates of 65 halocarbons and nonmethane hydrocarbons. Journal Title:Journal of Geophysical Research, [Atmospheres] 2001;106:20493-505.

2.Brown AC, Canosa-Mas CE, Parr AD, Wayne RP. Laboratory studies of some halogenated ethanes and ethers: measurements of rates of reaction with hydroxyl radical and of infrared absorption cross-sections. Atmospheric Environment, Part A 1990;24A:2499-511.

3.Imasu R, Suga A, Matsuno T. Radiative effects and halocarbon global warming potentials of replacement compounds for chlorofluorocarbons. Journal of the Meteorological Society of Japan 1995;73:1123-36.

4.Ballard J, Knight RJ, Newnham DA, Vander Auwera J, Herman M, Di Lonardo G, Masciarelli G, Nicolaisen FM, Beukes JA, Christensen LK, McPheat R, Duxbury G, Freckleton R, Shine KP. An intercomparison of laboratory measurements of absorption cross-sections and integrated absorption intensities for HCFC-22. J. Quant. Spectrosc. Radiat. Transfer 2000;66:109-28.

5.Myhre G, Nielsen CJ, Powell DL, Stordal F. Infrared absorption cross section, radiative forcing, and GWP of four hydrofluoro(poly)ethers. Atmospheric Environment 1999;33:4447-58.

6.Acerboni G, Beukes JA, Jensen NR, Hjorth J, Myhre G, Nielsen CJ, Sundet JK. Atmospheric degradation and global warming potentials of three perfluoroalkenes. Atmospheric Environment 2001;35:4113-23.

7.Sellevaag SR, Stenstrom Y, Helgaker T, Nielsen CJ. Atmospheric chemistry of CHF2CHO: Study of the IR and UV-Vis absorption cross sections, photolysis, and OH-, Cl-, and NO3-initiated oxidation. Journal of Physical Chemistry A 2005;109:3652-62.

8.Sellevaag SR, Kelly T, Sidebottom H, Nielsen CJ. A study of the IR and UV-Vis absorption cross-sections, photolysis and OH-initiated oxidation of CF3CHO and CF3CH2CHO. Physical Chemistry Chemical Physics 2004;6:1243-52.

9.D'Anna B, Sellevg SR, Wirtz K, Nielsen CJ. Photolysis Study of Perfluoro-2-methyl-3-pentanone under Natural Sunlight Conditions. Environmental Science and Technology 2005;39:8708-11.

10.Sellevaag SR, Nielsen CJ, Sovde OA, Myhre G, Sundet JK, Stordal F, Isaksen ISA. Atmospheric gas-phase degradation and global warming potentials of 2-fluoroethanol, 2,2-difluoroethanol, and 2,2,2-trifluoroethanol. Atmospheric Environment 2004;38:6725-35.

11.Myhre G, Stordal F, Gausemel I, Nielsen CJ, Mahieu E. Line-by-line calculations of thermal infrared radiation representative for global condition: CFC-12 as an example. Journal of Quantitative Spectroscopy & Radiative Transfer 2005;97:317-31.

12.Oyaro N, Sellevg SR, Nielsen CJ. Study of the OH and Cl-Initiated Oxidation, IR Absorption Cross-Section, Radiative Forcing, and Global Warming Potential of Four C4-Hydrofluoroethers. Environmental Science and Technology 2004;38:5567-76.

13.Pinnock S, Hurley MD, Shine KP, Wallington TJ, Smyth TJ. Radiative forcing of climate by hydrochlorofluorocarbons and hydrofluorocarbons. Journal of Geophysical Research, [Atmospheres] 1995;100:23227-38.

14.Oyaro N, Sellevag SR, Nielsen CJ. Atmospheric chemistry of hydrofluoroethers: Reaction of a series of hydrofluoroethers with OH radicals and Cl atoms, atmospheric lifetimes, and global warming potentials. J Phys Chem A 2005;109:337-46.

15.Tokuhashi K, Takahashi A, Kaise M, Kondo S. Rate constants for the reactions of OH radicals with CH3OCF2CHFCl, CHF2OCF2CHFCl, CHF2OCHClCF3, and CH3CH2OCF2CHF2. Journal of Geophysical Research, [Atmospheres] 1999;104:18681-8.

16.Langbein T, Sonntag H, Trapp D, Hoffmann A, Malms W, Roth EP, Mors V, Zellner R. Volatile anaesthetics and the atmosphere: atmospheric lifetimes and atmospheric effects of halothane, enflurane, isoflurane, desflurane and sevoflurane. Br J Anaesth 1999;82:66-73.

17.Nolan S, O'Sullivan N, Wenger J, Sidebottom H, Treacy J. Kinetics and mechanisms of the OH radical initiated degradation of a series of hydrofluoroethers. Proceedings of EUROTRAC Symposium '98: Transport and Chemical Transformation in the Troposphere, Garmisch-Partenkirchen, Germany, Mar. 23-27, 1998 1999;1:120-3.

18.Beach SD, Hickson KM, Smith IWM, Tuckett RP. Rate constants and Arrhenius parameters for the reactions of OH radicals and Cl atoms with CF3CH2OCHF2, CF3CHClOCHF2 and CF3CH2OCClF2, using the discharge-flow/resonance fluorescence method. Physical Chemistry Chemical Physics 2001;3:3064-9.

19.Kurylo MJ, Orkin VL. Determination of Atmospheric Lifetimes via the Measurement of OH Radical Kinetics. Chem. Rev. (Washington, DC, U. S.) FIELD Full Journal Title:Chemical Reviews (Washington, DC, United States) 2003;103:5049-76.

20.Prinn RG, Huang J, Weiss RF, Cunnold DM, Fraser PJ, Simmonds PG, McCulloch A, Harth C, Salameh P, O'Doherty S, Wang RHJ, Porter L, Miller BR. Evidence for substantial variations of atmospheric hydroxyl radicals in the past two decades. Science (Washington, DC, United States) 2001;292:1882-7.

21.Spivakovsky CM, Logan JA, Montzka SA, Balkanski YJ, Foreman-Fowler M, Jones DBA, Horowitz LW, Fusco AC, Brenninkmeijer CAM, Prather MJ, Wofsy SC, McElroy MB. Three-dimensional climatological distribution of tropospheric OH: update and evaluation. Journal of Geophysical Research, [Atmospheres] 2000;105:8931-80.

22.Sander SP, Friedl RR, Golden DM, Kurylo MJ, Moortgat GK, Wine PH, Ravishankara AR, Kolb CE, Molina MJ, Finlayson-Pitts BJ, Huie RE, Orkin VL. Chemical Kinetics and Photochemical Data for Use in Atmospheric Studies. Evaluation Number 15 Pasadena, California: National Aeronautics and Space Administration, Jet Propulsion Laboratory, California Institute of Technology, 2006.

23.Houghton JT, Meira Filho LG, Bruce J, Lee H, Callander BA, Haites E, Harris N, Maskell K. Climate Change 1994: Radiative Forcing of Climate Change and An Evaluation of the IPCC IS92 Emission Scenarios. Cambridge: Intergovernmental Panel on Climate Change, Cambridge University Press, 1995.

24.Forster P, Ramaswamy V, Artaxo P, Berntsen T, Betts R, Fahey DW, Haywood J, Lean J, Lowe DC, Myhre G, Nganga J, Prinn R, Raga G, Schulz M, Van Dorland R. Changes in Atmospheric Constituents and in Radiative Forcing. In: Solomon S, Qin D, Manning M et al. eds. Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change: Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, 2007.

25.Orkin VL, Guschin AG, Larin IK, Huie RE, Kurylo MJ. Measurements of the infrared absorption cross-sections of haloalkanes and their use in a simplified calculational approach for estimating direct global warming potentials. Journal of Photochemistry and Photobiology, A: Chemistry 2003;157:211-22.

26.Oyaro N, Sellevaag SR, Nielsen CJ. Atmospheric Chemistry of Hydrofluoroethers: Reaction of a Series of Hydrofluoroethers with OH Radicals and Cl Atoms, Atmospheric Lifetimes, and Global Warming Potentials. Journal of Physical Chemistry A 2005;109:337-46.

Figure Legends

Supplemental Figure 1. Integrated absorption intensities (base e) of the 2000-450 cm-1 region in isoflurane and the 2000-475 cm-1 region in sevoflurane. The sevoflurane data have been shifted by 100 for the sake of clarity.

Supplemental Figure 2. Absorption cross section of isoflurane and radiative forcing per unit cross section for a 0 to 1 ppbv increase in mixing ratio.

Supplemental Figure 3. Absorption cross section of sevoflurane and radiative forcing per unit cross section for a 0 to 1 ppbv increase in mixing ratio.

Supplemental Figure 4. Absorption cross section of desflurane and radiative forcing per unit cross section for a 0 to 1 ppbv increase in mixing ratio. Infrared data from Ref. (26).

Supplemental Figure 5. Arrhenius plots of rate constants for the reactions of OH radicals with isoflurane and sevoflurane. (×)Tokuhashi et al.(15); (●) Brown et al.(2); (o) Langbein et al.(16); (▲) Nolan et al.(17); (♦)Beach et al.(18) The dotted line corresponds to kOH+isoflurane(T) = 1.11 × 10-12 × exp(-1275 K/T) cm3 molecule–1 s–1, the full line corresponds to kOH+sevoflurane(T) = 3.3 × 10-12 × exp(-1275 K/T) cm3 molecule–1s–1. The data and curve for sevoflurane have been shifted by ln(10) for the sake of clarity.

15