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2014 Fiscal Year Final Research Report

Elucidation of thermohaline/biogeochemical circulation systems connecting the Sea of Okhotsk with subarctic North Pacific Ocean

Research Project

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Project/Area Number 22221001
Research Category

Grant-in-Aid for Scientific Research (S)

Allocation TypeSingle-year Grants
Research Field Environmental dynamic analysis
Research InstitutionHokkaido University

Principal Investigator

WAKATSUCHI Masaaki  北海道大学, -, 名誉教授 (60002101)

Co-Investigator(Kenkyū-buntansha) MITSUDERA Humio  北海道大学, 低温科学研究所, 教授 (20360943)
NISHIOKA Jun  北海道大学, 低温科学研究所, 准教授 (90371533)
NAKAMURA Tomohiro  北海道大学, 低温科学研究所, 講師 (60400008)
EBUCHI Naoto  北海道大学, 低温科学研究所, 教授 (10203656)
WATANABE Yutaka  北海道大学, 地球環境科学研究院, 准教授 (90333640)
SUZUKI Koji  北海道大学, 地球環境科学研究院, 准教授 (40283452)
KURODA Hiroshi  独立行政法人水産総合研究センター, 北海道区水産研究所, 主任研究員 (30531107)
Co-Investigator(Renkei-kenkyūsha) OHSHIMA Keiichiro  北海道大学, 低温科学研究所, 教授 (30185251)
TSUMUNE Daisuke  電力中央研究所, 上席研究員 (10371494)
MATOBA Sumito  北海道大学, 低温科学研究所, 助教 (30391163)
Project Period (FY) 2010-04-01 – 2015-03-31
Keywords熱塩循環 / 物質循環 / 鉄 / 高密度水 / オホーツク海 / 親潮 / 植物プランクトン
Outline of Final Research Achievements

We investigated the thermohaline/biogeochemical circulation systems, connecting the Sea of Okhotsk with the North Pacific, to elucidate a ‘miraculous mechanism’ that supports abundant fisheries resources in the Okhotsk and Oyashio regions. Salinity of the dense shelf water (DSW) over the northern shelf of the Okhotsk Sea controls the strength of the thermohaline circulation of the North Pacific Ocean. DSW salinity is determined by relative contribution among the salinity anomaly that propagates long distance from the subarctic gyre, freshwater anomaly by precipitation, and saline water anomaly rejected during sea ice formation. DSW entrains nutrients such as iron, originating in the Amur River and deposited over the continental shelf, and spreads these materials to the North Pacific Ocean. This study has revealed an exquisite thermohaline-biogeochemical system coupled through DSW and tidal mixing, which controls primary production in the large area of the subarctic North Pacific.

Free Research Field

海洋物理学

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Published: 2016-06-03  

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