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Title: Dynamical Links between the Decadal Variability of the Oyashio and Kuroshio Extensions

Journal Article · · Journal of Climate
 [1];  [1];  [1]
  1. Department of Oceanography, University of Hawai‘i at Mānoa, Honolulu, Hawaii

Rather than a single and continuous boundary current outflow, long-term satellite observations reveal that the Oyashio Extension (OE) in the North Pacific Subarctic Gyre comprises two independent, northeast–southwest-slanted front systems. With a mean latitude along 40°N, the western OE front exists primarily west of 153°E and is a continuation of the subarctic gyre western boundary current. The eastern OE front, also appearing along 40°N, is located between 153° and 170°E, whose entity is disconnected from its western counterpart. During 1982–2016, both of the OE fronts exhibit prominent decadal fluctuations, although their signals show little contemporaneous correlation. An upper-ocean temperature budget analysis based on the Estimating the Circulation and Climate of the Ocean, phase II (ECCO2), state estimate reveals that the advective temperature flux convergence plays a critical role in determining the low-frequency temperature changes relating to the OE fronts. Specifically, the western OE front variability is controlled by the decadal mesoscale eddy modulations in the upstream Kuroshio Extension (KE). An enhanced eddy activity increases the poleward heat transport and works to strengthen the western OE front. The eastern OE front variability, on the other hand, is dictated by both the meridional shift of the KE position and the circulation intensity change immediately north of the eastern OE. Different baroclinic adjustment speeds for the KE and OE are found to cause the in-phase changes between these latter two processes. Lack of contemporaneous correlation between the decadal western and eastern OE variability is found to be related to the interaction of the meridionally migrating KE jet with the Shatsky Rise near 159°E.

Research Organization:
Univ. of Hawaii, Honolulu, HI (United States)
Sponsoring Organization:
USDOE Office of Science (SC)
Grant/Contract Number:
SC0005111; SC006766
OSTI ID:
1407454
Alternate ID(s):
OSTI ID: 1541842
Journal Information:
Journal of Climate, Journal Name: Journal of Climate Vol. 30 Journal Issue: 23; ISSN 0894-8755
Publisher:
American Meteorological SocietyCopyright Statement
Country of Publication:
United States
Language:
English
Citation Metrics:
Cited by: 49 works
Citation information provided by
Web of Science

Cited By (7)

Mesoscale SST perturbation-induced impacts on climatological precipitation in the Kuroshio-Oyashio extension region, as revealed by the WRF simulations journal September 2018
Identification of the fronts from the Kuroshio Extension to the Subarctic Current using absolute dynamic topographies in satellite altimetry products journal March 2018
Meridional Shift of the Oyashio Extension Front in the Past 36 Years journal September 2018
The Signature of Oceanic Processes in Decadal Extratropical SST Anomalies journal August 2018
Interannual Eddy Kinetic Energy Modulations in the Agulhas Return Current journal September 2018
Low ocean-floor rises regulate subpolar sea surface temperature by forming baroclinic jets journal March 2018
Enhanced Warming and Intensification of the Kuroshio Extension, 1999–2013 journal January 2019