Impact of Aleutian Low activity on the STMW formation in the Kuroshio recirculation gyre region

Shusaku Sugimoto, Kimio Hanawa

研究成果: Article査読

36 被引用数 (Scopus)

抄録

To understand the formation of North Pacific subtropical mode water (STMW) in the Kuroshio recirculation gyre region, the cause of STMW thickness variation is investigated using temperature profiles in a historically archived data set. The thickness variation is predominantly controlled by the main thermocline depth (MTD). When the main thermocline deepens (shoals), the wintertime mixed layer depth can develop (not develop), and consequently, thicker (thinner) STMW is observed in summer. The large-scale atmospheric forcing controlling the MTD is explored using a wind-driven hindcast ocean model. The MTD variation stems primarily from a baroclinic response in the ocean to the Aleutian Low (AL) activity; especially, the meridional movement of the AL exerts a remarkable influence.

本文言語English
論文番号L03606
ジャーナルGeophysical Research Letters
37
3
DOI
出版ステータスPublished - 2010 2月

ASJC Scopus subject areas

  • 地球物理学
  • 地球惑星科学(全般)

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