EGU22-13270
https://doi.org/10.5194/egusphere-egu22-13270
EGU General Assembly 2022
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.

The combined assimilation of MIPAS carbonyl sulfide (COS) and NOAA surface observations in TM5-4DVAR: Consequences for the global COS budget.

Maarten Krol1,2, Jin Ma2, Stelios Myriokefalitakis3, Norbert Glatthor4, Marc von Hobe5, and Steve Montzka6
Maarten Krol et al.
  • 1Meteorology and Air Quality group, Wageningen University and Research, the Netherlands
  • 2Institute for Marine and Atmospheric Research Utrecht, Utrecht University, the Netherlands
  • 3Atmospheric Physics and Chemistry Group, National Observatory Athens, Greece
  • 4Forschungszentrum Jülich GmbH, Germany
  • 5Karlsruher Institut für Technologie, Institut für Meteorologie und Klimaforschung, Karlsruhe, Germany
  • 6Global Monitoring Laboratory, NOAA, US

The atmospheric budget of carbonyl sulfide (COS, lifetime ~2 years) is primarily determined by emissions from anthropogenic and oceanic sources and uptake by the biosphere. Once the budget of COS is adequately understood, COS could be a suitable tracer to estimate Gross Primary Productivity (GPP), since stomatal uptake by plants is basically a one-way process, unlike the assimilation of CO2. However, currently the global budget of COS is not closed. Here, we will report progress on the use of inverse modelling to better constrain the atmospheric COS budget. To that end, we assimilate data from the MIPAS instrument that flew onboard the ENVISAT satellite (2002–2012). MIPAS is a limb sounder that measures atmospheric emission profiles down to the upper troposphere. Tropospheric COS retrievals are assimilated together with NOAA COS surface observations, and a bias correction scheme is employed to correct for potential calibration differences. Using the 4DVAR-TM5 model, we derive a consistent global COS budget. However, evaluation with independent data reveals that TM5 remains biased low in the free troposphere. We will show that this underestimate may be resolved by accounting for an aqueous-phase oxidation process of the newly discovered HydroPeroxyMethylThioFormate (HPMTF) intermediate in the DMS oxidation chain.

How to cite: Krol, M., Ma, J., Myriokefalitakis, S., Glatthor, N., von Hobe, M., and Montzka, S.: The combined assimilation of MIPAS carbonyl sulfide (COS) and NOAA surface observations in TM5-4DVAR: Consequences for the global COS budget., EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-13270, https://doi.org/10.5194/egusphere-egu22-13270, 2022.