“…On seasonal and interannual time scales, ocean currents can be significantly influenced by ENSO, IOD, and Indian Ocean basin‐wide warming by modulating equatorial winds and oceanic internal variations (Nyadjro & McPhaden, 2014; Sachidanandan et al., 2017; Wang, 2019). The multiscale variabilities in these currents can lead to heat convergence/divergence in the IPWP, which not only likely feedbacks to the MISO over the Pacific Ocean (Lee et al., 2022; Yang et al., 2020) but also has profound implications for the climate and local environment. For example, warm water volume in the western Pacific (WWV W ; the volume of water above the 20°C isotherm within 120°E−155°W, 5°S–5°N) is the main precursor of ENSO events and plays a crucial role in these events by propagating eastward and triggering sea–air interactions (Ballester et al., 2016; Izumo et al., 2019; Larson & Kirtman, 2019; Petrova et al., 2017; Planton et al., 2018).…”