1Department of Earth, Atmospheric, and Planetary Sciences, MIT, Cambridge, MA 02139, USA
2Center for Australian Weather and Climate Research, CSIRO Marine and Atmospheric Research, Aspendale, Victoria, 3195, Australia
3School of Chemistry, University of Bristol, Bristol, UK
4Scripps Institution of Oceanography, University of California, San Diego, La Jolla, CA 92093, USA
5Center for Australian Weather and Climate Research, Bureau of Meteorology, Melbourne, Victoria, 3000, Australia
6Georgia Institute of Technology, Atlanta, GA, USA
7ESRL, NOAA, Boulder, CO, USA
8Swiss Federal Institute for Materials Science and Technology, Laboratory for Air Pollution/Environmental Technology, Duebendorf, Switzerland
9Norwegian Institute for Air Research, Kjeller, Norway
10University of Urbino, Urbino, Le Marche, 61029, Italy
11National Institute for Environmental Studies, Tsukuba, Ibaraki, Japan
*now at: Civil & Environmental Engineering, Rice University, Houston, TX 77005, USA
Received: 28 Sep 2009 – Discussion started: 23 Dec 2009
Abstract. Methyl chloride (CH3Cl) is a chlorine-containing trace gas in the atmosphere contributing significantly to stratospheric ozone depletion. Large uncertainties in estimates of its source and sink magnitudes and temporal and spatial variations currently exist. GEIA inventories and other bottom-up emission estimates are used to construct a priori maps of the surface fluxes of CH3Cl. The Model of Atmospheric Transport and Chemistry (MATCH), driven by NCEP interannually varying meteorological data, is then used to simulate CH3Cl mole fractions and quantify the time series of sensitivities of the mole fractions at each measurement site to the surface fluxes of various regional and global sources and sinks. We then implement the Kalman filter (with the unit pulse response method) to estimate the surface fluxes on regional/global scales with monthly resolution from January 2000 to December 2004. High frequency observations from the AGAGE, SOGE, NIES, and NOAA/ESRL HATS in situ networks and low frequency observations from the NOAA/ESRL HATS flask network are used to constrain the source and sink magnitudes. The inversion results indicate global total emissions around 4100 ± 470 Gg yr−1 with very large emissions of 2200 ± 390 Gg yr−1 from tropical plants, which turn out to be the largest single source in the CH3Cl budget. Relative to their a priori annual estimates, the inversion increases global annual fungal and tropical emissions, and reduces the global oceanic source. The inversion implies greater seasonal and interannual oscillations of the natural sources and sink of CH3Cl compared to the a priori. The inversion also reflects the strong effects of the 2002/2003 globally widespread heat waves and droughts on global emissions from tropical plants, biomass burning and salt marshes, and on the soil sink.
Revised: 03 Jun 2010 – Accepted: 04 Jun 2010 – Published: 22 Jun 2010
Xiao, X., Prinn, R. G., Fraser, P. J., Simmonds, P. G., Weiss, R. F., O'Doherty, S., Miller, B. R., Salameh, P. K., Harth, C. M., Krummel, P. B., Porter, L. W., Mühle, J., Greally, B. R., Cunnold, D., Wang, R., Montzka, S. A., Elkins, J. W., Dutton, G. S., Thompson, T. M., Butler, J. H., Hall, B. D., Reimann, S., Vollmer, M. K., Stordal, F., Lunder, C., Maione, M., Arduini, J., and Yokouchi, Y.: Optimal estimation of the surface fluxes of methyl chloride using a 3-D global chemical transport model, Atmos. Chem. Phys., 10, 5515-5533, doi:10.5194/acp-10-5515-2010, 2010.