Century of Ocean Warming on Florida Keys Coral Reefs: Historic In Situ Observations

• Published in: Estuaries and coasts Vol. 38; no. 3; pp. 1085 - 1096
• Main Authors: Kuffner, Ilsa B, Lidz, Barbara H, Hudson, J. Harold, Anderson, Jeffrey S
• Format: Journal Article
• Language: English
• Published: Boston Springer-Verlag 01.05.2015; Springer Science+Business Media; Springer US; Springer Nature B.V
• Subjects: Climate change; Coastal Sciences; Coasts; Coral reefs; corals; data collection; Earth and Environmental Science; Ecology; ecosystems; Environment; Environmental Management; Freshwater & Marine Ecology; Ocean temperature; population growth; prognosis; surface water temperature; thermography; Water and Health; Florida; ASW, USA, Florida, Florida Keys; ASW, USA, Florida, Florida Reef; Coral growth; Sea surface temperature; Global climate change; Coral reef degradation; Florida reef tract; In situ temperature
• ISSN: 1559-2723; 1559-2731
• DOI: 10.1007/s12237-014-9875-5

There is strong evidence that global climate change over the last several decades has caused shifts in species distributions, species extinctions, and alterations in the functioning of ecosystems. However, because of high variability on short (i.e., diurnal, seasonal, and annual) timescales as well as the recency of a comprehensive instrumental record, it is difficult to detect or provide evidence for long-term, site-specific trends in ocean temperature. Here we analyze five in situ datasets from Florida Keys coral reef habitats, including historic measurements taken by lighthouse keepers, to provide three independent lines of evidence supporting approximately 0.8 °C of warming in sea surface temperature (SST) over the last century. Results indicate that the warming observed in the records between 1878 and 2012 can be fully accounted for by the warming observed in recent decades (from 1975 to 2007), documented using in situ thermographs on a mid-shore patch reef. The magnitude of warming revealed here is similar to that found in other SST datasets from the region and to that observed in global mean surface temperature. The geologic context and significance of recent ocean warming to coral growth and population dynamics are discussed, as is the future prognosis for the Florida reef tract.