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Northeastern Caribbean rainfall variability linked to solar and volcanic forcing

We present a 500-year precipitation-sensitive record based on co-varying speleothem δ18O values and Mg/Ca ratios from Larga cave in Puerto Rico. This multi-proxy record shows that the evolution of rainfall in the northeastern Caribbean was characterized by alternating centennial dry and wet phases c...

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Main Authors: Vieten, Rolf (Author) , Warken, Sophie F. (Author) , Zanchettin, Davide (Author) , Winter, Amos (Author) , Scholz, Denis (Author) , Black, David (Author) , Koltai, Gabriella (Author) , Spötl, Christoph (Author)
Format: Article (Journal)
Language:English
Published: 12 April 2024
In: Paleoceanography and paleoclimatology
Year: 2024, Volume: 39, Issue: 4, Pages: 1-17
ISSN:2572-4525
DOI:10.1029/2023PA004720
Online Access:Verlag, lizenzpflichtig, Volltext: https://doi.org/10.1029/2023PA004720
Verlag, lizenzpflichtig, Volltext: https://onlinelibrary.wiley.com/doi/abs/10.1029/2023PA004720
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Author Notes:Rolf Vieten, Sophie F. Warken, Davide Zanchettin, Amos Winter, Denis Scholz, David Black, Gabriella Koltai, and Christoph Spötl
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Summary:We present a 500-year precipitation-sensitive record based on co-varying speleothem δ18O values and Mg/Ca ratios from Larga cave in Puerto Rico. This multi-proxy record shows that the evolution of rainfall in the northeastern Caribbean was characterized by alternating centennial dry and wet phases corresponding to reduced versus enhanced convective activity. These phases occurred synchronous with relatively cool and warm tropical Atlantic sea-surface temperatures (SSTs), respectively. While the observed pattern suggests a close link of northeastern Caribbean rainfall to the Atlantic Multidecadal Variability, a regional comparison reveals intermittent regional heterogeneity especially on decadal timescales, which may be related to a superimposing influence of the Pacific and Atlantic basins. Furthermore, the speleothem-based hydroclimate reconstruction indicates a significant volcanic impact during the past two centuries, and further reveals a potential solar signal in the preceding three centuries. We posit that the forcing likely shifted from solar to volcanic during the eighteenth century in being an important source of multidecadal to centennial Caribbean rainfall variability. The link between convective rainfall and natural forcing may be explained through a modulation of SST variations in the tropical Atlantic and Pacific oceans.
Item Description:Gesehen am 25.09.2024
Physical Description:Online Resource
ISSN:2572-4525
DOI:10.1029/2023PA004720

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