In Situ Measurements of Long-Lived Trace Gases in the Lower Stratosphere by Gas Chromatography

Abstract Detailed information on the four-channel Airborne Chromatograph for Atmospheric Trace Species (ACATS-IV), used to measure long-lived atmospheric trace gases, is presented. Since ACATS-IV was last described in the literature, the temporal resolution of some measurements was tripled during 1997–99, chromatography was significantly changed, and data processing improved. ACATS-IV presently measures CCl3F [chlorofluorocarbon (CFC)-11], CCl2FCClF2 (CFC-113), CH3CCl3 (methyl chloroform), CCl4 (carbon tetrachloride), CH4 (methane), H2 (hydrogen), and CHCl3 (chloroform) every 140 s, and N2O (nitrous oxide), CCl2F2 (CFC-12), CBrClF2 (halon-1211), and SF6 (sulfur hexafluoride) every 70 s. An in-depth description of the instrument operation, standardization, calibration, and data processing is provided, along with a discussion of precision and uncertainties of ambient air measurements for several airborne missions.

[1]  Michael R. Gunson,et al.  Evaluation of source gas lifetimes from stratospheric observations , 1997 .

[2]  D. Fahey,et al.  Quantifying Transport Between the Tropical and Mid-Latitude Lower Stratosphere , 1996, Science.

[3]  R. Prinn,et al.  Evaluating chemical transport models: Comparison of effects of different CFC‐11 emission scenarios , 1996 .

[4]  James W. Elkins,et al.  Decline in the Tropospheric Abundance of Halogen from Halocarbons: Implications for Stratospheric Ozone Depletion , 1996, Science.

[5]  R. Weiss,et al.  Lifetime and emission estimates of 1,1,2-trichlorotrifluorethane (CFC-113) from daily global background observations , 1996 .

[6]  S. J. Ciciora,et al.  Airborne gas chromatograph for in situ measurements of long‐lived species in the upper troposphere and lower stratosphere , 1996 .

[7]  D. Fahey,et al.  Estimates of total organic and inorganic chlorine in the lower stratosphere from in situ and flask measurements during AASE II , 1995 .

[8]  S. W. Bowen,et al.  In situ observations in aircraft exhaust plumes in the lower stratosphere at midlatitudes , 1995 .

[9]  J. Butler,et al.  Decrease in the growth rates of atmospheric chlorofluorocarbons 11 and 12 , 1993, Nature.

[10]  S. Montzka,et al.  Global tropospheric distribution and calibration scale of HCFC‐22 , 1993 .

[11]  R. Stolarski,et al.  Episodic total ozone minima and associated effects on heterogeneous chemistry and lower stratospheric transport , 1992 .

[12]  P. Novelli,et al.  The development and evaluation of a gravimetric reference scale for measurements of atmospheric carbon monoxide , 1991 .

[13]  Adrian F. Tuck,et al.  In situ ozone measurements within the 1987 Antarctic ozone hole from a high-altitude ER-2 aircraft , 1989 .

[14]  F. Singleton,et al.  Possible meridional circulations in the stratosphere and mesosphere , 1961 .

[15]  G. Dobson Origin and distribution of the polyatomic molecules in the atmosphere , 1956, Proceedings of the Royal Society of London. Series A. Mathematical and Physical Sciences.

[16]  A. W. Brewer Evidence for a world circulation provided by the measurements of helium and water vapour distribution in the stratosphere , 1949 .