Abstract

In the stratified ocean, vertical eddy diffusivity in the subsurface pycnocline plays a major role in new production through transporting nutrients upwards from the darker/nutrient-rich layer. In order to evaluate the diffusivity that was less available in the subsurface layers where indirect estimations are difficult, we conducted direct microstructure measurements in the upper 300 m of the open Pacific during summer, from 40°S to 50°N along 170°W and from 137°E to 120°W across the subtropical North Pacific (21°30′N–23°N). The subsurface pycnocline in the mid- and low-latitude regions was occupied primarily by the Subtropical Underwaters characterized by high salinity, and the Subtropical Mode Waters appeared with an increasing depth and latitude. In the North Pacific, low-salinity subarctic water with shallow seasonal pycnocline was observed in the high-latitude region. The base level of the diffusivity was 0.14–0.47 × 10–5 m2 s–1, while elevations up to 0.51–13 × 10–5 m2 s–1 were observed at the equator where the Equatorial Undercurrents formed the strong shear in the subsurface layer, and in areas high internal tide energy such as the Hawaiian Ridge. The effect of wind on the diffusivity was less clear, probably because the wind energy is generally low during summer. The shear-to-strain ratio showed dome-shaped profiles with respect to latitude and an increasing trend from west to east in the subtropical North Pacific. The geographical distributions of the diffusivity presented in this study will contribute to better understanding biogeochemical cycles in the stratified upper ocean through improving estimations of the material transport.

Highlights

  • In the open ocean, the subsurface pycnocline develops seasonally in mid- and high-latitude regions and is sustained throughout most of the year in low-latitude regions

  • In the mid- and low-latitude South Pacific, subsurface pycnoclines were mostly occupied by the high salinity water of > 35.0, which is defined as the South Pacific Subtropical Underwater (STUW) in the upper part and the South Pacific Subtropical Mode Water (STMW) in the lower part (Talley et al 2011; Fig. 3a)

  • In the North Pacific, the occurrence of the North Pacific STUW was confined in the upper layer/ lower latitude, and the North Pacific STMW and the North Pacific Central Mode Water (CMW) characterized by the thick layer were more clearly observed in 25–40°N than the South Pacific (Oka and Qiu 2011)

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Summary

Introduction

The subsurface pycnocline develops seasonally in mid- and high-latitude regions and is sustained throughout most of the year in low-latitude regions. The order of magnitude of the vertical eddy diffusivity in the pycnocline In addition to the general consensus on its order of magnitude, at least in the open ocean under calm conditions, the vertical eddy diffusivity is known to have substantial temporal and spatial variability. This is attributed in part to the intermittent nature of turbulence (e.g., Baker and Gibson 1987), geographical variability related to differences in various forcing and background conditions is important. While the globally averaged vertical diffusivity above 1000 m was O ­(10–5) ­m2 ­s–1, regional variability was evident, explained in part by the levels of local power input by internal tides and wind-driven

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