Abstract
Profiles of CFC-11 (CCl3F), CFC-12 (CCl2F2) and HCFC-22 (CHF2Cl) have been obtained from Fourier transform infrared (FTIR) solar absorption measurements above the Saint-Denis (St Denis) and Maïdo sites at Réunion Island (21° S, 55° E) with low vertical
resolution. FTIR profile retrievals are performed by the well-established
SFIT4 program and the detail retrieval strategies along with the
systematic/random uncertainties of CFC-11, CFC-12 and HCFC-22 are discussed
in this study. The FTIR data of all three species are sensitive to the whole
troposphere and the lowermost stratosphere, with the peak sensitivity between
5 and 10 km.
The ground-based FTIR data have been compared with the collocated Michelson
Interferometer for Passive Atmospheric Sounding (MIPAS/ENVISAT) data and
found to be in good agreement: the observed mean relative biases and standard
deviations of the differences between the smoothed MIPAS and FTIR partial
columns (6–30 km) are (−4.3 and 4.4 %), (−2.9 and 4.6 %) and
(−0.7 and 4.8 %) for CFC-11, CFC-12 and HCFC-22, respectively, which
are within the combined error budgets from both measurements. The season
cycles of CFC-11, CFC-12 and HCFC-22 from FTIR measurements and MIPAS data
show a similar variation: concentration is highest in February–April and
lowest in August–October.
The trends derived from the combined St Denis and Maïdo FTIR time series
are −0.86 ± 0.12 and 2.84 ± 0.06 % year−1 for CFC-11
and HCFC-22, respectively, for the period 2004 to 2016, and
−0.76 ± 0.05 % year−1 for CFC-12 for 2009 to 2016. These
measurements are consistent with the trends observed by the National Oceanic
and Atmospheric Administration (NOAA) Global Monitoring Division's (GMD)
Halocarbons & other Atmospheric Trace Species Group (HATS) measurements at
Samoa (14.2° S, 170.5° W) for CFC-11
(−0.87 ± 0.04 % year−1), but slightly weaker for HCFC-22
(3.46 ± 0.05 %) year−1 and stronger for CFC-12
(−0.60 ± 0.02 % year−1).
Citation
ID:
188783
Ref Key:
zhou2016atmosphericcfc-11,