Infrared spectroscopy of halogen-containing species for atmospheric remote sensing Jeremy J. Harrison University of York
FTS: 750 to 4400 cm -1 Radiance of sun gives high S/N Long pathlengths ~ 300 km (limb sounding) Measurements at many altitudes ACE detects more trace organic molecules than any other satellite instrument. Atmospheric Chemistry Experiment (ACE)
Halocarbons Strong greenhouse gases Many are ozone depleting substances –Regulated by the Montreal Protocol Many are increasing in the atmosphere Many have long atmospheric lifetimes
GEISA and HITRAN contain a number of absorption cross section datasets for Cl- and F-containing molecules Dataset requirements for remote sensing: –Accurate band intensities –Accurate wavenumber scale –Wide P-T coverage for best interpolation –Appropriate resolution (Doppler-limited) A number of GEISA / HITRAN datasets fail in many of these respects. Laboratory Spectroscopy
Bruker IFS 125 HR MSF at RAL 26-cm absorption cell
CFC-12 (CCl 2 F 2 ) Most abundant anthropogenic halocarbon in the atmosphere Was used in refrigeration and air conditioning Banned under the Montreal Protocol Atmospheric lifetime ~ 100 years MIPAS: Kellmann et al., ACP, 12, 11857–11875, 2012
CFC-12 absorption cross sections in HITRAN / GEISA
CCl 2 F 2 (CFC-12) Main problems with old dataset: –Strong Q branch near 1160 cm -1 often saturated. –Wavenumber calibration error CCl 2 F 2 cross sections
Carbon tetrachloride CCl 4 accounted for 359 ppt (about 11%) of total tropospheric Cl in 2008 CCl 4 tropospheric abundances have declined less rapidly than expected Atmospheric lifetime 26 years Top-down emissions 40–80 Gg/yr (2005–2008) Bottom-up emissions 0–30 Gg/yr (2005–2008) Errors in reporting, errors in the analysis of reported data, and/or unknown sources? ACE-FTS CCl 4 data product biased ~20% high
CCl 4 absorption cross sections in HITRAN / GEISA
CCl 4 CCl 4 cross sections Main problems with old dataset: –Spectra under-resolved –Wavenumber calibration error
CCl 4 cross sections
HCFC-22 (CHClF 2 ) Most abundant HCFC (substitutes for long-lived ozone-depleting substances) Lifetime 11.9 years HCFC-22 increased at a rate of about 8 ppt/yr (4.3%/yr) during 2007–2008, more than 50% faster than observed in 2003–2004 –Rapidly increasing HCFC-22 production in developing countries Emissions are projected to begin to decline during the coming decade due to measures already agreed to under the Montreal Protocol
HCFC-22 absorption cross sections in HITRAN / GEISA
CHClF 2 (HCFC-22) CHClF 2 cross sections Main problems with old dataset: –Poor P-T coverage –Wavenumber calibration error
CHClF 2 cross sections
Hydrofluorocarbons (HFCs) are replacements for CFCs and HCFCs –Not regulated by Montreal Protocol Trifluoromethane (HFC-23, CHF 3 ) –Second most abundant HFC in atmosphere –Lifetime of 222 years –100-year GWP of 14,200 –Formed as a by-product of HCFC-22 (CHClF 2 ) production 1,1,1,2-Tetrafluoroethane (HFC-134a, CF 3 CH 2 F) –Most abundant HFC in atmosphere –Lifetime of 13.4 years –100-year GWP of 1,370 –The preferred refrigerant in refrigeration and mobile air conditioning (replacement for CFC-12) Hydrofluorocarbons (HFCs)
Previous HFC-23 absorption cross sections
Harrison et al., First remote-sensing observations of trifluoromethane (HFC-23) in the upper troposphere and lower stratosphere, J. Geophys. Res., 2012, 117, D05308, doi: /2011JD Remote-sensing observations of HFC-23
CHF 3 cross sections CHF 3 (HFC-23) Main problems with old dataset: –Very poor P-T coverage –Spectra under-resolved –Inconsistent baselines –Wavenumber calibration error New dataset: Harrison, JQSRT 130, (2013)
Nassar et al., J. Geophys. Res., 2006, 111, D22313, doi: /2006JD Remote-sensing observations of HFC-134a
HFC-134a absorption cross sections in HITRAN / GEISA
CF 3 CH 2 F cross sections CF 3 CH 2 F (HFC-134a) Main problems with old dataset: –Poor P-T coverage –Wavenumber calibration error
CF 3 CH 2 F cross sections
Acknowledgements Funding from NERC (UK) & NCEO RAL – Gary Williams & Robert McPheat NCEO – John Remedios ACE – Chris Boone & Peter Bernath