Journal
CORAL REEFS
Volume 28, Issue 2, Pages 399-403Publisher
SPRINGER
DOI: 10.1007/s00338-009-0476-x
Keywords
Seawater temperature; Coral bleaching; Refuges; Diego Garcia; Indian Ocean
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Funding
- United Kingdom's OTEP
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Seawater temperature was recorded at two-hourly intervals for two years (March 2006-March 2008) by six data loggers in Diego Garcia atoll, central Indian Ocean. Loggers were substrate mounted, in two transects of 5, 15 and 25 m depth on a seaward reef and in a lagoonal pass. During the season of mixed but predominantly northwest winds, regular plunges of temperature of 5-7A degrees C occurred with a periodicity of 1-4 days. This partly coincided with the period of greatest annual warming. Temperature fluctuations increased with increasing depth. Temperature traces are compared with HadISST1 and AVHRR satellite-derived temperature data which do not capture the deeper water temperature plunges. Reasons for the regular temperature plunges appear to include both tidal cycles and unidentified, internal waves. This is important for issues of coral refuges, complicating use of satellite-derived temperature data for planning optimal coral reef conservation areas.
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