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The Flux and Emission of Dimethylsulfide From the Great Barrier Reef Region and Potential Influence on the Climate of NE Australia
Author(s) -
Jones Graham,
Curran Mark,
Deschaseaux Elisabeth,
Omori Yuko,
Tanimoto Hiroshi,
Swan Hilton,
Eyre Bradley,
Ivey John,
McParland Erin,
Gabric Albert,
Cropp Roger
Publication year - 2018
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
eISSN - 2169-8996
pISSN - 2169-897X
DOI - 10.1029/2018jd029210
Subject(s) - dimethylsulfoniopropionate , reef , oceanography , coral reef , environmental science , coral , flux (metallurgy) , seawater , coral bleaching , great barrier reef , atmospheric sciences , geology , chemistry , ecology , biology , phytoplankton , nutrient , organic chemistry
Concentrations of dimethylsulfoniopropionate (DMSP), dimethylsulfide (DMS), and DMS flux are reported for the Great Barrier Reef (GBR), Great Barrier Reef Lagoon (GBRL), and Coral Sea. Generally higher concentrations of dimethylsulfoniopropionate and DMS occurred in coral reef waters, compared with GBRL concentrations. DMS flux from GBR coral reefs in summer ranged from nondetectable to 153 μmol m −2 d −1 (mean 6.4), while winter fluxes ranged from 0.02 to 15 μmol m −2 d −1 (mean 2.4). No significant seasonal difference in DMS flux occurred for the GBRL. High DMS w concentrations and DMS fluxes periodically occur at coral reefs during very low tides and elevated sea surface temperatures (SSTs). For the GBRL and GBR coral reefs there was a significant correlation between seawater DMS w concentrations and SST ( p < 0.001), up to temperatures of 30 °C. During coral bleaching DMS flux from reefs almost completely shuts down when SSTs are >30 °C. The GBRL and associated coral reefs emit 439 and 32 MmolS per year, respectively. Cyclones on average produce 170 MmolS to the GBR atmosphere in summer. This amount can markedly increase during severe cyclones such as severe tropical Cyclone Debbie in March 2017. Overall, the annual DMS emission estimate from the GBRL and coral reefs in the GBR is 0.64 GmolS, with cyclones contributing 27% or greater of the annual emission estimate, depending on the cyclone intensity. Oxidation of atmospheric DMS can potentially affect solar radiation, SSTs, low‐level cloud cover, and rainfall causing cooling and warming of the climate in the GBR region as recent modeling predicts.