Thermohaline structure in the subarctic North Pacific simulated in a general circulation model

Takahiro Endoh, Humio Mitsudera, Shang Ping Xie, Bo Qiu

Research output: Contribution to journalArticle

16 Citations (Scopus)

Abstract

The Miami Isopycnic Coordinate Ocean Model configured with 1° horizontal resolution and 23 layers is used to examine processes that maintain the mesothermal structure, a subsurface temperature inversion, in the subarctic North Pacific. The model successfully reproduces the mesothermal structure consisting of a shallow temperature minimum and an underlying temperature maximum that are called the dichothermal and mesothermal waters, respectively. The mesothermal water is formed through cross-gyre exchange between the subtropical and subarctic gyres, whereas the dichothermal water originates from cold and low-salinity waters formed in the winter mixed layer. The horizontal distribution of the passive tracer injected into the subsurface layers south of Japan shows that warm and saline water of the Kuroshio in the density range of 26.8-27.0 σθ is the source of the mesothermal water. There are three pathways through which the Kuroshio waters enter the subarctic region. First, the Kuroshio waters that cross the gyre boundary in the western boundary region are carried to the Alaskan gyre by the northern part of the North Pacific Current. Second, the Kuroshio waters carried by the southern part of the North Pacific Current enter the Alaskan gyre through a cross-gyre window in the eastern basin. Third, the Kuroshio waters that diffuse along the isopycnal in the Kuroshio-Oyashio Extension enter the western subarctic gyre. The mesothermal water thus formed in the subarctic region is entrained into the winter mixed layer and returns to the subtropics as surface water by the southward Ekman drift, forming the subpolar cell.

Original languageEnglish
Pages (from-to)360-371
Number of pages12
JournalJournal of Physical Oceanography
Volume34
Issue number2
DOIs
Publication statusPublished - Feb 2004

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thermohaline structure
general circulation model
gyre
water
subarctic region
mixed layer
temperature inversion
winter
temperature
tracer

All Science Journal Classification (ASJC) codes

  • Oceanography

Cite this

Thermohaline structure in the subarctic North Pacific simulated in a general circulation model. / Endoh, Takahiro; Mitsudera, Humio; Xie, Shang Ping; Qiu, Bo.

In: Journal of Physical Oceanography, Vol. 34, No. 2, 02.2004, p. 360-371.

Research output: Contribution to journalArticle

Endoh, Takahiro ; Mitsudera, Humio ; Xie, Shang Ping ; Qiu, Bo. / Thermohaline structure in the subarctic North Pacific simulated in a general circulation model. In: Journal of Physical Oceanography. 2004 ; Vol. 34, No. 2. pp. 360-371.
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