Bottom current at the equatorial gap of the Ninety East Ridge is revealed by long-term bottom mooring observations from 24 December 2019 to 2 April 2021. It is found that the observed bottom current has significant intraseasonal variability (ISV) with a dominant time scale of ∼33 days, which becomes enhanced in the boreal summer and winter. Variability of the bottom current was explored by using the Mercator Ocean outputs, which revealed that the enhancement of ISV of the bottom current is closely related to the westward propagation of Rossby waves originating from the eastern boundary, with their ray paths vertically propagating into the deep layer. Considering the importance of water mass transport through the gaps in the Ninety East Ridge to the renewal of deep water and modification of deep circulation in the Central Indian Basin (CIB) and West Australian Basin (WAB), our study provides in-situ evidence for previously unrevealed energetic variation of water mass exchange between the CIB and WAB, and it further helps us gain a comprehensive understanding of the pathway and variation of the deep meridional overturning circulation in the Indian Ocean.

中文翻译：

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基于系泊资料的印度洋东九十海岭赤道缺口高能底流

2019 年 12 月 24 日至 2021 年 4 月 2 日的长期底部系泊观测揭示了东九十岭赤道缺口处的底流。发现观测到的底流具有显着的季节内变化（ISV），主要时间尺度为~33天，在寒带夏季和冬季变得增强。利用墨卡托海洋输出探索了底流的变化，表明底流ISV的增强与源自东部边界的罗斯贝波向西传播密切相关，其射线路径垂直传播到深部层。