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Dimethylsulfide and Coral Bleaching: Links to Solar Radiation, Low Level Cloud and the Regulation of Seawater Temperatures and Climate in the Great Barrier Reef

  • Jones G
  • Curran M
  • Swan H
  • et al.
American Journal of Climate Change (2017) 06(02) 328-359
DOI: 10.4236/ajcc.2017.62017
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Abstract

Coral reefs produce atmospheric dimethylsulfide (DMS a) which oxidises to non-sea-salt (nss) sulfate aerosols, precursors of cloud condensation nuclei (CCN) and low level cloud (LLC), reducing solar radiation and regulating sea surface temperatures (SSTs). Here we report measurements of solar radiation, SST, LLC, DMS flux, 4

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APA

Jones, G., Curran, M., Swan, H., & Deschaseaux, E. (2017). Dimethylsulfide and Coral Bleaching: Links to Solar Radiation, Low Level Cloud and the Regulation of Seawater Temperatures and Climate in the Great Barrier Reef. American Journal of Climate Change, 06(02), 328–359. https://doi.org/10.4236/ajcc.2017.62017

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