Derivation of tropospheric methane from TCCON CH<sub>4</sub> and HF total column observations

oleh: K. M. Saad, D. Wunch, G. C. Toon, P. Bernath, C. Boone, B. Connor, N. M. Deutscher, D. W. T. Griffith, R. Kivi, J. Notholt, C. Roehl, M. Schneider, V. Sherlock, P. O. Wennberg

Format: Article
Diterbitkan: Copernicus Publications 2014-09-01

Deskripsi

The Total Carbon Column Observing Network (TCCON) is a global ground-based network of Fourier transform spectrometers that produce precise measurements of column-averaged dry-air mole fractions of atmospheric methane (CH<sub>4</sub>). Temporal variability in the total column of CH<sub>4</sub> due to stratospheric dynamics obscures fluctuations and trends driven by tropospheric transport and local surface fluxes that are critical for understanding CH<sub>4</sub> sources and sinks. We reduce the contribution of stratospheric variability from the total column average by subtracting an estimate of the stratospheric CH<sub>4</sub> derived from simultaneous measurements of hydrogen fluoride (HF). HF provides a proxy for stratospheric CH<sub>4</sub> because it is strongly correlated to CH<sub>4</sub> in the stratosphere, has an accurately known tropospheric abundance (of zero), and is measured at most TCCON stations. The stratospheric partial column of CH<sub>4</sub> is calculated as a function of the zonal and annual trends in the relationship between CH<sub>4</sub> and HF in the stratosphere, which we determine from ACE-FTS satellite data. We also explicitly take into account the CH<sub>4</sub> column averaging kernel to estimate the contribution of stratospheric CH<sub>4</sub> to the total column. The resulting tropospheric CH<sub>4</sub> columns are consistent with in situ aircraft measurements and augment existing observations in the troposphere.