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Corals record long-term Leeuwin current variability including Ningaloo Niño/Niña since 1795
J Zinke1, A Rountrey2, M Feng3
11] UWA Oceans Institute, 39 Fairway, Nedlands, Western Australia 6009, Australia [2] UWA School of Earth and Environment, 35 Stirling Highway, Crawley, Western Australia 6009, Australia [3] Australian Institute of Marine Science, PMB 3, Townsville MC, Queensland 4810, Australia.
The Leeuwin Current (LC) shows climate variations linked to the Indo-Pacific. Recent extreme events, like Ningaloo Niño, are unprecedented and amplified by global warming.
Area of Science:
- Oceanography
- Climate Science
- Paleoclimatology
Background:
- The Leeuwin Current (LC) variability reflects Indo-Pacific climate shifts.
- Extreme events, such as Ningaloo Niño, involve strengthened LC, high sea levels, and warm sea surface temperatures (SSTs).
- Understanding these events is limited by a lack of long-term data.
Observation:
- Coral SST records and El Niño-Southern Oscillation reconstructions were used to hindcast LC strength and SST from 1795 to 2010.
- Analysis covered 215 years of interannual and decadal variations in LC strength and SST.
Findings:
- Interannual and decadal variability in LC strength and SST were evident over the past 215 years.
- The most extreme sea level and SST anomalies occurred after 1980.
- Recent extreme events were unprecedented in severity.
Implications:
- Accelerated global ocean warming and sea-level rise likely contribute to the severity of recent extreme LC events.
- These findings highlight the sensitivity of the southeastern Indian Ocean to climate forcing.
- The study underscores the need for continued monitoring of the LC and its associated climate phenomena.
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