Preprints
https://doi.org/10.5194/egusphere-2022-1102
https://doi.org/10.5194/egusphere-2022-1102
 
28 Oct 2022
28 Oct 2022
Status: this preprint is open for discussion and under review for Climate of the Past (CP).

Indian Ocean variability changes in the Palaeoclimate Model Intercomparison Project

Chris Brierley1, Kaustubh Thirumalai2, Edward Grindrod1, and Jonathan Barnsley1 Chris Brierley et al.
  • 1Dept. Geography, University College London, London, United Kingdom
  • 2Dept. Geosciences, University of Arizona, Tucson, Arizona, USA

Abstract. The Indian Ocean exhibits multiple modes of interannual climate variability, whose future behaviour is uncertain. Recent analysis of glacial climates has uncovered an additional El Niño-like equatorial mode in the Indian Ocean, which could also emerge in future warm states. Here we explore changes in the tropical Indian Ocean simulated by the Palaeoclimate Model Intercomparison Project (PMIP4). These simulations are performed by an ensemble of models contributing to the Coupled Model Intercomparison Project 6, and over four coordinated experiments: three past periods - the mid-Holocene (6000 years5 ago), the last glacial maximum (21,000 years ago), the last interglacial (127,000 years ago) - and an idealised forcing scenario to examine the impact of greenhouse forcing. The two interglacial experiments are used to characterise the role of orbital variations on the seasonal cycle, whilst the other pair focus on responses to large changes in global temperature.

The Indian Ocean Basin Mode (IOBM) is damped in both the mid-Holocene and last interglacial, with the amount related to the damping of the El Niño-Southern Oscillation in the Pacific. No coherent changes in the strength of the IOBM are seen10 with global temperature changes; neither are changes in the Indian Ocean Dipole (IOD) nor the Niño-like mode. Under orbital forcing, the IOD robustly weakens during the mid-Holocene experiment, with only minor reductions in amplitude during the last interglacial. Orbital changes do impact the SST pattern of the Indian Ocean Dipole, with the cold pole reaching up to the Equator and extending along it. Induced changes in the regional seasonality are hypothesised to be important control on changes in the Indian Ocean variability.

Chris Brierley et al.

Status: open (until 23 Dec 2022)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2022-1102', Anonymous Referee #1, 06 Dec 2022 reply

Chris Brierley et al.

Model code and software

Indiabn Ocean Variability repository on GitHub Chris Brierley, Kau Thirulamai https://github.com/pmip4/IndianOceanVariability

Chris Brierley et al.

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Short summary
Year-to-year variations in the weather conditions over the Indian Ocean have important consequences for the substantial fraction of the Earth's population that live near it. This work looks at how these variations respond to climate change - both past and future. The models rarely agree, suggesting a weak, uncertain response to climate change.