Ozone deposition to the sea surface: Chemical enhancement and wind speed dependence

Wonil Chang, Brian G. Heikes, Meehye Lee

Research output: Contribution to journalArticlepeer-review

70 Citations (Scopus)


Deposition of ozone to the sea surface is controlled by complex physical and chemical processes. There is a large variability in the observed deposition velocity of ozone vd needed to be better characterized. In addition, the existing formulations for estimating (vd) cannot explain a significant ozone loss, particularly, at low wind speed. By amalgamating previous works, a more general formula was developed to account for v d dependence on wind speed and chemical enhancement. The result shows that vd can be elevated from 0.016 to 0.078 cm s-1 by about a factor of 5 as wind speed increases from 0 to 20 m s-1, indicating the importance of wind-induced turbulent gas-transfer. To estimate molecular gas-transfer, represented by the surface reactivity of ozone, reaction rates of species known to react with ozone in seawater were investigated. Iodide was found to be capable of describing the substantial chemical destruction of ozone at low wind speed. Due to a wide range of distribution in the surface oceans (20-400 nM), iodide appears to be a candidate elucidating the variability of vd. This study suggests that the physical and chemical processes are coupled and both play significant roles in determining ozone deposition to the sea surface.

Original languageEnglish
Pages (from-to)1053-1059
Number of pages7
JournalAtmospheric Environment
Issue number7
Publication statusPublished - 2004 Mar


  • Air-sea exchange
  • Chemical enhancement
  • Deposition dry
  • Gas-transfer
  • Ozone

ASJC Scopus subject areas

  • Environmental Science(all)
  • Atmospheric Science


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