Derivation of tropospheric methane from TCCON CH<sub>4</sub> and HF total column observations
Author:
Saad K. M.ORCID, Wunch D.ORCID, Toon G. C., Bernath P., Boone C., Connor B., Deutscher N. M., Griffith D. W. T.ORCID, Kivi R.ORCID, Notholt J., Roehl C., Schneider M.ORCID, Sherlock V., Wennberg P. O.ORCID
Abstract
Abstract. 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 (CH4). Temporal variability in the total column of CH4 due to stratospheric dynamics obscures fluctuations and trends driven by tropospheric transport and local sources and sinks. We remove the contribution of stratospheric variability from the total column average by subtracting an estimate of the stratospheric CH4 derived from simultaneous measurements of hydrogen fluoride (HF). HF provides a proxy for stratospheric CH4 because it resides solely in the stratosphere, has a nearly linear inverse relationship with stratospheric CH4, and is measured at most TCCON stations. The stratospheric partial column of CH4 is calculated as a function of the zonal and annual trends in the relationship between CH4 and HF in the stratosphere, which we determine from ACE-FTS satellite data. We also explicitly take into account the CH4 column averaging kernel to estimate the contribution of stratospheric CH4 to the total column. The resulting tropospheric CH4 columns are consistent with in situ aircraft measurements and augment existing observations in the troposphere.
Funder
European Commission
Publisher
Copernicus GmbH
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