618 / 2024-09-18 16:38:56
Variability in the Volume Transport of the Deep Overflow across the 10°S Saddle on the Ninetyeast Ridge
Ninetyeast Ridge,Volume Transport,Deep Overflow,Southeast Indian Ocean
Session 60 - Indian Ocean Dynamics, Air-sea Interaction and Biogeochemical Cycles
Abstract Accepted
Shanwu Zhang / Third Institute of Oceanography, Ministry of Natural Resources
Fuwen Qiu / Third Institute of Oceanography, Ministry of Natural Resources
Deep overflows across the saddles on the Ninetyeast Ridge are essential for the deep limb of the Indian Ocean meridional overturning circulation. However, the volume transport or temporal variability of these overflows remains poorly understood. Based on a 17-month moored record of velocity profiles, the time-averaged volume transport of the overflow across the saddle near 10°S is estimated to be 1.3 Sv (1 Sv = 1×106 m3/s) which closely aligns with the result diagnosed from a rotating hydraulic theory and early hydrographic observations. The overflow transport exhibits significant variabilities on intraseasonal (73 days) and semi-annual scales (170 days), and is closely correlated to the wind stress curl to the east of the Ninetyeast Ridge. These variabilities are attributed to vertically propagating Rossby waves generated by remote wind stress curl anomalies, which is indicated by the analysis on numerical model outputs utilizing spectral empirical orthogonal function decomposition and ray tracing techniques.