An El Niño Mode in the Glacial Indian Ocean?. Issue 8 (14th August 2019)

• Record Type: Journal Article
• Authors: Thirumalai, Kaustubh; DiNezio, Pedro N.; Tierney, Jessica E.; Puy, Martin; Mohtadi, Mahyar
• Is Part Of: Paleoceanography and paleoclimatology. Volume 34:Issue 8(2019)
• Page Start: 1316
• Page End: 1327
• Publication Date: 2019-08-14
• Subjects: Paleoceanography -- Periodicals; Paleoclimatology -- Periodicals; 551.46
• DOI: 10.1029/2019PA003669
• Languages: English
• ISSNs: 2572-4517

Abstract

Abstract: Despite minor variations in sea surface temperature (SST) compared to other tropical regions, coupled ocean‐atmosphere dynamics in the Indian Ocean cause widespread drought, wildfires, and flooding. It is unclear whether changes in the Indian Ocean mean state can support stronger SST variability and climatic extremes. Here we focus on the Last Glacial Maximum (19, 000–21, 000 years before present) when background oceanic conditions could have been favorable for stronger variability. Using individual foraminiferal analyses and climate model simulations, we find that seasonal and interannual SST variations in the eastern equatorial Indian Ocean were much larger during this glacial period relative to modern conditions. The increase in year‐to‐year variance is consistent with the emergence of an equatorial mode of climate variability, which strongly resembles the Pacific El Niño and is currently not active in the Indian Ocean. Key Points: Individual foraminiferal δ 18 O reveal intensified climate variability in the Indian Ocean during the Last Glacial Maximum (LGM) Climate simulations indicate enhanced seasonal and interannual variability consistent with mean‐state changes tied to shelf exposure We propose that an equatorial mode of variability was active in the LGM Indian Ocean, with dynamics mirroring modern El Niño in the Pacific