Tracking Interannual‐ to Multidecadal‐Scale Climate Variability in the Atlantic Warm Pool Using Central Caribbean Coral Data. Issue 4 (26th April 2018)

• Record Type: Journal Article
• Authors: von Reumont, J.; Hetzinger, S.; Garbe‐Schönberg, D.; Manfrino, C.; Dullo, C.
• Is Part Of: Paleoceanography and paleoclimatology. Volume 33:Issue 4(2018)
• Page Start: 395
• Page End: 411
• Publication Date: 2018-04-26
• Subjects: coral δ18O -- coral Sr/Ca -- Atlantic Warm Pool -- North Atlantic Oscillation -- Diploria strigosa -- Caribbean; Paleoceanography -- Periodicals; Paleoclimatology -- Periodicals; 551.46
• DOI: 10.1002/2018PA003321
• Languages: English
• ISSNs: 2572-4517

Abstract

Abstract: Atlantic Warm Pool (AWP) climate variability is subject to multiple influences of remote and local forcing. However, shortage of observational data before the midtwentieth century and of long‐term sea surface temperature (SST) and climate records has hampered the detection and investigation of decadal‐ and longer‐scale variability. We present new seasonally resolved 125‐year records of coral δ 18 O and Sr/Ca variations in the Central Caribbean Sea (Little Cayman, Cayman Islands; Diploria strigosa ). Both geochemical proxies show decreasing long‐term trends, indicating long‐term warming. Sr/Ca indicates much stronger regional warming than large‐scale grid‐SST data, while δ 18 O tracks large‐scale SST changes in the Atlantic Warm Pool. Seawater δ 18 O variations are reconstructed, indicating a drying trend over the past century. High spatial correlation between coral δ 18 O and SST in the region of the Loop Current and Gulf Stream system suggests that Little Cayman is a sensitive location for detecting past large‐scale temperature variability beyond the Central Caribbean region. More specifically, our δ 18 O data track changes in North Atlantic Oscillation variability on decadal and multidecadal time scales providing insights into the temporal and spatial nonstationarity of the North Atlantic Oscillation. A combination of our δ 18 O record with two coral records from different Caribbean sites reveals high spatial correspondence between coral δ 18 O and SST variability in the North Atlantic subtropical gyre, where few instrumental measurements and proxies are available prior to the twentieth century. Our results clearly demonstrate the potential of combining proxy data to provide information from sparsely sampled areas, helping to reduce uncertainty in model‐based projections. Key Points: Caribbean coral proxy records show stronger regional warming than grid‐SST data and a drying trend over the past century Coral δ 18 O tracks decadal and multidecadal North Atlantic Oscillation variability in the region of the Loop Current and Gulf Stream system Combined Caribbean coral proxy records provide SST information for large sparsely sampled Atlantic regions beyond the Caribbean