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  4. El Ni?o-Southern Oscillation and internal sea surface temperature variability in the tropical Indian Ocean since 1675
 
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El Ni?o-Southern Oscillation and internal sea surface temperature variability in the tropical Indian Ocean since 1675

Journal
Climate of the Past
Journal Volume
17
Journal Issue
1
Pages
151-170
Date Issued
2021
Author(s)
Leupold M
Pfeiffer M
Watanabe T.K
Reuning L
Garbe-Sch?nberg D
CHUAN-CHOU SHEN  
Brummer G.-J.A.
DOI
10.5194/cp-17-151-2021
URI
https://www.scopus.com/inward/record.uri?eid=2-s2.0-85099539005&doi=10.5194%2fcp-17-151-2021&partnerID=40&md5=d9af93d62ee0c813b6a64f1d8b6128f3
https://scholars.lib.ntu.edu.tw/handle/123456789/571625
Abstract
The dominant modes of climate variability on interannual timescales in the tropical Indian Ocean are the El Ni?o Southern Oscillation (ENSO) and the Indian Ocean Dipole. El Ni?o events have occurred more frequently during recent decades, and it has been suggested that an asymmetric ENSO teleconnection (warming during El Ni?o events is stronger than cooling during La Ni?a events) caused the pronounced warming of the western Indian Ocean. In this study, we test this hypothesis using coral Sr=Ca records from the central Indian Ocean (Chagos Archipelago) to reconstruct past sea surface temperatures (SSTs) in time windows from the mid-Little Ice Age (1675 1716) to the present. Three sub-fossil massive Porites corals were dated to the 17 18th century (one coral) and the 19 20th century (two corals). Their records were compared with a published modern coral Sr=Ca record from the same site. All corals were subsampled at a monthly resolution for Sr=Ca measurements, which were measured using a simultaneous inductively coupled plasma optical emission spectrometer (ICP-OES). Wavelet coherence analysis shows that interannual variability in the four coral records is driven by ENSO, suggesting that the ENSO SST teleconnection in the central Indian Ocean has been stationary since the 17th century. To determine the symmetry of El Ni?o and La Ni?a events, we compiled composite records of positive and negative ENSO-driven SST anomaly events. We find similar magnitudes of warm and cold anomalies, indicating a symmetric ENSO response in the tropical Indian Ocean. This suggests that ENSO is not the main driver of central Indian Ocean warming. ? 2021 Author(s).
Subjects
Anthozoa; Porites; Porites porites; Porites porites porites
SDGs

[SDGs]SDG13

[SDGs]SDG14

Other Subjects
Anthozoa; Porites; Porites porites; Porites porites porites
Type
journal article

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