Articles | Volume 11, issue 16
Biogeosciences, 11, 4459–4476, 2014
Biogeosciences, 11, 4459–4476, 2014

Research article 22 Aug 2014

Research article | 22 Aug 2014

Methyl iodide production in the open ocean

I. Stemmler1,3, I. Hense1, B. Quack2, and E. Maier-Reimer3 I. Stemmler et al.
  • 1Institute for Hydrobiology and Fisheries Science, University of Hamburg, CEN, Hamburg, Germany
  • 2Geomar, Helmholtz Centre for Ocean Research, Kiel, Germany
  • 3Max Planck Institute for Meteorology, Hamburg, Germany

Abstract. Production pathways of the prominent volatile organic halogen compound methyl iodide (CH3I) are not fully understood. Based on observations, production of CH3I via photochemical degradation of organic material or via phytoplankton production has been proposed. Additional insights could not be gained from correlations between observed biological and environmental variables or from biogeochemical modeling to identify unambiguously the source of methyl iodide. In this study, we aim to address this question of source mechanisms with a three-dimensional global ocean general circulation model including biogeochemistry (MPIOM–HAMOCC (MPIOM – Max Planck Institute Ocean Model HAMOCC – HAMburg Ocean Carbon Cycle model)) by carrying out a series of sensitivity experiments. The simulated fields are compared with a newly available global data set. Simulated distribution patterns and emissions of CH3I differ largely for the two different production pathways. The evaluation of our model results with observations shows that, on the global scale, observed surface concentrations of CH3I can be best explained by the photochemical production pathway. Our results further emphasize that correlations between CH3I and abiotic or biotic factors do not necessarily provide meaningful insights concerning the source of origin. Overall, we find a net global annual CH3I air–sea flux that ranges between 70 and 260 Gg yr−1. On the global scale, the ocean acts as a net source of methyl iodide for the atmosphere, though in some regions in boreal winter, fluxes are of the opposite direction (from the atmosphere to the ocean).

Final-revised paper