Intraseasonal oscillation of deep currents influenced by mesoscale eddies in the Kuroshio Extension Region

Yansong Liu,Wenzheng Zhou,Feng Nan,Fei Yu

doi:10.1038/s41598-019-39567-7

Abstract

Intraseasonal oscillation of deep currents in the Kuroshio Extension region is examined using observations from a collection of current meter moorings. The moored observations reveal variability with characteristic time scales of 23–38 days for velocity time series and of 38–99 days for temperature time series. The time series of normalized temperature (NT) in the deep ocean change correspondingly with sea level anomaly (SLA). The maximum correlation coefficient between NT in the deep ocean and SLA is also up to 0.7. Positive correlation is observed between deep currents and surface geostrophic current. Furthermore, the influence of mesoscale eddies on deep currents is examined by analyzing the data collected when cyclonic and anticyclonic eddies crossed the current meter mooring. Whether anticyclonic or cyclonic eddy intensified the deep currents from 2000 m to 4000 m in the same direction and increased the amplitude. These results provide observational evidence of intraseasonal oscillation in the deep ocean and the effect of mesoscale eddies on deep currents in the Kuroshio Extension region.

Highlights

The responses in the deep ocean to mesoscale eddies in the upper ocean were investigated by using the satellite observational data
The results of our power spectral analysis, applied to the uninterrupted current meter mooring data of more than two years, revealed 23–38 day peak in both zonal and meridional velocities, and 38–99 day peak in temperature. It means that there existed the intraseasonal (20–100 days) oscillation of deep currents in the Kuroshio Extension region
The locations of the CMs were in the Kuroshio Extension region, where mesoscale eddy often occurs

Summary

Introduction

The intraseasonal oscillation of deep currents in the Kuroshio Extension region was investigated using current meter mooring data. The responses in the deep ocean to mesoscale eddies in the upper ocean were investigated by using the satellite observational data. It means that there existed the intraseasonal (20–100 days) oscillation of deep currents in the Kuroshio Extension region. The SLA and NT in the deep ocean had high correlation (~0.7).

Results

Conclusion