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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

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Figure

Figure 1. The climate feedback involving production of DMS that can occur from coral sulfate aerosol particles grow to produce cloud condensation nuclei (CCN) forming low level cumulous and stratocumulous clouds, thus decreasing solar radiation levels, SST
Figure 2. Map of the study area showing locations of Nelly Bay fringing reef on the NE coast of Magnetic Island and the Pioneer Bay reef site at Orpheus Island north of Townsville
Figure 3. (a) Solar radiation levels in MJ·m−2·d−1, (b) Mean daily low level cloud cover (oktas), versus day of year (DOY), (c) SST (˚C), lowest nightime tides (m), LLC (oktas) and rainfall (mm) recorded from November to April by the BoM at Townsville airp
Figure 4. (a) DMSw (nM), DMS flux (µmol·m−2·d−1) and lowest nightime tide (m) at Nelly Bay reef
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