Japan Geoscience Union Meeting 2019

Presentation information

[E] Oral

A (Atmospheric and Hydrospheric Sciences ) » A-OS Ocean Sciences & Ocean Environment

[A-OS12] Marine ecosystems and biogeochemical cycles: theory, observation and modeling

Mon. May 27, 2019 9:00 AM - 10:30 AM 302 (3F)

convener:Shin-ichi Ito(Atmosphere and Ocean Research Institute, The University of Tokyo), Takafumi Hirata(Faculty of Environmental Earth Science, Hokkaido University), Enrique N Curchitser(Rutgers University New Brunswick), Eileen E Hofmann(Old Dominion University), Chairperson:Shin-Ichi Ito(The University of Tokyo)

9:30 AM - 9:45 AM

[AOS12-02] Decadal salinity variation in the western North Pacific correlated with the strength of the Oyashio and the Kuroshio Extension

*Hitoshi Kaneko1, Takeshi Okunishi2, Shinya Kouketsu3, Sachihiko Itoh1, Takashi Seto4, Hiroshi Kuroda5, Yugo Shimizu4 (1.Atmosphere and Ocean Research Institute, The University of Tokyo, 2.Tohoku National Fisheries Research Institute, Japan Fisheries Research and Education Agency, 3.Japan Agency for Marine-Earth Science and Technology, 4.National Research Institute of Fisheries Science, Japan Fisheries Research and Education Agency, 5.Hokkaido National Fisheries Research Institute, Japan Fisheries Research and Education Agency)

Keywords:North Pacific Intermediate Water , Decadal variation, Oyashio, Kuroshio Extension

Decadal changes in salinity around the density (~1026.8 kg m–3) of North Pacific Intermediate Water (NPIW) were investigated in the regions from the Oyashio to the Kuroshio Extension (KE), called as the Mixed Water Region (MWR), based on the long-term-data-sets provided from numerical reanalysis. Based on the reanalysis data provided by an ocean forecast system of the Japan Fisheries Research and Education Agency (FRA-ROMS; 1992–2012, horizontal resolutions of 0.1°), we found that during increase of the Oyashio velocity in the upstream region, negative salinity anomaly accompanied with the southward velocity at the density was enhanced between 144–145°E just south of 40°N. In addition, to examine influences from the downstream region of the Oyashio, we made a lag-correlation analysis focusing on the decadal variation of KE stability calculated from the zonal average (142–165°E) of the meridional gradient of the sea surface height (34.5–37.0°E) as the KE strength (KES). The result showed that signals of significant negative correlation appeared around the density from Hokkaido to the north region of KE. Through the composite analysis based on the KE stability, we found that the stable KE could also lead similar anomaly distribution around the north region of KE. We examined relationships between decadal tendency and each component of salinity fluxes at the density along the north-south boundary of the region of 38–40°N, and 142–145°E. Concerning estimation of the salinity fluxes, we employed time-mean components (S, V) and eddy components (s’, v’), and then, we calculated products of them (Sv’, s’V, s’v’). Decadal tendency of salinity (ds'/dt) was negatively correlated with the meridional difference of Sv’ (–0.5 < r< –0.47, 95% confidence interval). Whereas Sv’ at northern boundary was also negatively correlated with ds'/dt (–0.45 < r< –0.42), the correlation between ds'/dt and Sv’ at southern boundary was small (0.03 < r< 0.07). The result suggested that the southward Oyashio would play an important role for decadal salinity variation in the MWR.