LONG-TERM TREND OF CARBON TETRACHLORIDE (CCl$_{4}$) FROM GROUND-BASED HIGH RESOLUTION INFRARED SOLAR SPECTRA RECRODED AT THE JUNGFRAUJOCH

Author Institution: NASA Langley Research Center, Hampton, VA USA; Institute of Astrophysics and Geophysics, University of Liege, Liege, Belgium; Science Systems and Applications, Inc, Hampton, VA USA; Laboratoire Inter-universitaire des Systemes Atmospheriques (LISA) UMR, CNRS/INSU 7583, Universites Paris VII et Paris XII, 94010 Creteil Cedex, France Spectroscopie de l'Atmosphere, Service de Chimie Quantique et de PhotophysiqueThe long-term trend of carbon tetrachloride (CCl$_{4}$) has been retrieved from infrared high resolution solar absorption spectra encompassing the 1999 to 2010 time period. The measurements were recorded with a Fourier transform spectrometer at the northern mid-latitude, high altitude Jungfraujoch station in Switzerland ($46.5^irc}$N latitude, $8.0^irc}$E longitude, 3580 m altitude). Total columns were derived from the region of the strong CCl$_{4}$ $\upsilon_{3}$ band at 794 cm$^{-1}$ accounting for all interfering molecules (e.g. H$_{2}$O, O$_{3}$) with significant improvement in the residuals obtained by also taking into account the line mixing in a nearby CO$_{2}$ Q branch, a procedure not implemented in previous remote sensing CCl$_{4}$ retrievals though its importance has been noted in several papers. The time series shows a statistically-significant long-term decrease in the CCl$_{4}$ total atmospheric burden of (-1.18?ñ0.10 \%/yr), at the 95\% confidence level, using 2005 as reference. Furthermore, fit to the total column data set also reveals a seasonal cycle with a peak-to-peak amplitude of 10.2\%, with minimum and maximum values found in mid-February and early August, respectively. This seasonal modulation can however be attributed to tropopause height changes throughout the season. The results quantify the continued impact of the regulations implemented by the Montreal Protocol and its strengthening amendments and adjustments for a molecule with high global warming potential. Although a statistically significant decrease in the total column is inferred, the CCl$_{4}$ molecule remains an important contributor to the stratospheric chlorine budget and burden