Abstract

The Indo-Pacific warm pool (IPWP) is enclosed by a 28 °C isotherm and plays a vital role in controlling atmospheric circulations. However, the effects of changes in regional warm pool sea surface temperatures (SSTs) remain unexplored. We divided the IPWP into the Indian and Pacific sectors and distinguished their responses to natural variability and global warming. Furthermore, we examined the impacts of the interannual variability (IAV) in warm pool SST on the tropical Hadley, Walker, and monsoon circulations. The Hadley circulation was affected by warm pool SST warming, i.e., warmer SSTs over the warm pool strengthened the upward branch of Hadley circulation, whereas the downward branch was respectively weakened and strengthened in the Northern and Southern Hemispheres. Walker circulation was strengthened (weakened) in the warming (natural) mode. Consequently, the Walker circulation is weakened since the natural variability of warm pool SST plays a more dominant role rather than the warming trend of SSTs over the warm pool. Furthermore, our analysis displays that warm pool warming has little impact on the monsoon circulation. Our findings highlight the different roles of the IAV of warm pool regions in each tropical circulation as part of the warming trend and natural variability.

Highlights

  • The Indo-Pacific warm pool (IPWP), comprising the eastern tropical Indian and western tropicalPacific Oceans, straddles the equator and adjacent regions

  • Three rows indicate that the regression is against (a,d) Indo-Pacific warm pool (IPWP), (b,e) Indian warm pool (IWP), and (c,f) Pacific warm pool (PWP)

  • This study demonstrated that the modulation of tropical circulations was associated with interannual variability (IAV) in warm pool intensity in warming and natural modes

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Summary

Introduction

The Indo-Pacific warm pool (IPWP), comprising the eastern tropical Indian and western tropical. The IPWP plays a key role as a major energy source, supplying heat and water vapor through deep convection, which leads to intense air–sea interactions [6,7,8] This warm pool can elucidate ocean–atmosphere couplings [9,10]. Even small variations in IPWP SST can bring about considerable changes in the global climate and may directly affect Hadley and Walker circulations [12,15,16,17]. Several studies have examined the seasonal variations and IAV in warm pool properties and compared the Pacific and Indian Oceans [28,29].

Data and Methods
Hadley Circulation
Regression
Walker Circulation
Monsoon Circulation
Findings
Conclusions and Discussion

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