Potential controls of isoprene in the surface ocean. Issue 4 (11th April 2017)

• Record Type: Journal Article
• Authors: Hackenberg, S. C.; Andrews, S. J.; Airs, R.; Arnold, S. R.; Bouman, H. A.; Brewin, R. J. W.; Chance, R. J.; Cummings, D.; Dall'Olmo, G.; Lewis, A. C.; Minaeian, J. K.; Reifel, K. M.; Small, A.; Tarran, G. A.; Tilstone, G. H.; Carpenter, L. J.
• Is Part Of: Global biogeochemical cycles. Volume 31:Issue 4(2017:Apr.)
• Page Start: 644
• Page End: 662
• Publication Date: 2017-04-11
• Subjects: marine isoprene -- sea‐to‐air fluxes -- seawater concentrations -- atmospheric mixing ratios -- biogenic trace gas; Biogeochemical cycles -- Periodicals; Electronic journals; 577.1405
• DOI: 10.1002/2016GB005531
• Languages: English
• ISSNs: 0886-6236

Abstract

Abstract: Isoprene surface ocean concentrations and vertical distribution, atmospheric mixing ratios, and calculated sea‐to‐air fluxes spanning approximately 125° of latitude (80°N–45°S) over the Arctic and Atlantic Oceans are reported. Oceanic isoprene concentrations were associated with a number of concurrently monitored biological variables including chlorophyll a (Chl a ), photoprotective pigments, integrated primary production (intPP), and cyanobacterial cell counts, with higher isoprene concentrations relative to all respective variables found at sea surface temperatures greater than 20°C. The correlation between isoprene and the sum of photoprotective carotenoids, which is reported here for the first time, was the most consistent across all cruises. Parameterizations based on linear regression analyses of these relationships perform well for Arctic and Atlantic data, producing a better fit to observations than an existing Chl a ‐based parameterization. Global extrapolation of isoprene surface water concentrations using satellite‐derived Chl a and intPP reproduced general trends in the in situ data and absolute values within a factor of 2 between 60% and 85%, depending on the data set and algorithm used. Key Points: Isoprene water concentrations correlated well with Chl a, primary production, photoprotective pigments, and cyanobacterial cell counts Higher isoprene concentrations relative to all respective variables were found at sea surface temperatures greater than 20°C Predicted isoprene water concentrations based on satellite Chl a compared well with observations