Atmospheric Chemistry and Physics Discussions www.atmos-chem-phys-discuss.net 1680-7367 1680-7375 6 5 2006 10.5194/acpd-6-9907-2006 http://www.atmos-chem-phys-discuss.net/6/9907/2006/ http://www.atmos-chem-phys-discuss.net/6/9907/2006/acpd-6-9907-2006.html http://www.atmos-chem-phys-discuss.net/6/9907/2006/acpd-6-9907-2006.pdf 9907 9935 2006-10-10 Air-sea fluxes of methanol, acetone, acetaldehyde, isoprene and DMS from a Norwegian fjord following a phytoplankton bloom in a mesocosm experiment V. Sinha J. Williams M. Meyerhöfer U. Riebesell A. I. Paulino A. Larsen Max Planck Institute for Chemistry, J. J. Becher Weg 27, 55128 Mainz, Germany Leibniz Institut für Meereswissenschaften, IFM-GEOMAR, Marine Biogeochemie, Düsternbrooker Weg 20, 24105 Kiel, Germany Department of Biology, Jahnebakken 5, University of Bergen, P. Box 7800, N-5020 Bergen, Norway The ocean's influence on volatile organic compounds (VOCs) in the atmosphere is poorly understood. This work characterises the oceanic emission and / or uptake of methanol, acetone, acetaldehyde, isoprene and dimethyl sulphide (DMS) as a function of photosynthetically active radiation (PAR) and a suite of biological parameters. The measurements were taken following a phytoplankton bloom, in May/June 2005 with a proton transfer reaction mass spectrometer (PTR-MS), from mesocosm enclosures anchored in the Raunefjord, Southern Norway. The net flux of methanol was always into the ocean, and was stronger at night. Isoprene and acetaldehyde were emitted from the ocean, correlating strongly with light (r_{avcorr, isoprene}=0.49; r_{avcorr, acetaldehyde}=0.70) and phytoplankton abundance. DMS was also emitted to the air but did not correlate significantly with light (r_{avcorr, dms}= 0.01). Under conditions of high biological activity and a PAR of ~450 µmol photons m^−2 s^−1, acetone was emitted from the ocean, otherwise it was uptaken. The mean fluxes for methanol, acetone, acetaldehyde, isoprene and DMS were −0.26 ng m^−2 s^−1, 0.21 ng m^−2s^−1, 0.23 ng m ^−2 s^−1, 0.12 ng m^−2 s^−1 and 0.3 ng m^−2 s^−1 respectively. This work shows that compound specific PAR and biological dependency should be used for estimating the influence of the global ocean on atmospheric VOC budgets.