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Impact of the Changjiang River discharge on torrential rainfall events over Kyushu

Research Project

Project/Area Number 17K13006
Research Category

Grant-in-Aid for Young Scientists (B)

Allocation TypeMulti-year Fund
Research Field Natural disaster / Disaster prevention science
Research InstitutionKagoshima University

Principal Investigator

Kako Shin'ichiro  鹿児島大学, 理工学域工学系, 助教 (60709624)

Project Period (FY) 2017-04-01 – 2020-03-31
Project Status Completed (Fiscal Year 2019)
Budget Amount *help
¥4,160,000 (Direct Cost: ¥3,200,000、Indirect Cost: ¥960,000)
Fiscal Year 2019: ¥650,000 (Direct Cost: ¥500,000、Indirect Cost: ¥150,000)
Fiscal Year 2018: ¥650,000 (Direct Cost: ¥500,000、Indirect Cost: ¥150,000)
Fiscal Year 2017: ¥2,860,000 (Direct Cost: ¥2,200,000、Indirect Cost: ¥660,000)
Keywords長江希釈水 / 領域大気モデル / 海洋循環モデル / 水蒸気フラックス / 双子実験 / 感度実験 / moisture flux / Moisture flux / 集中豪雨 / 平成21年中国・九州北部豪雨 / 自然災害 / 大気海洋相互作用
Outline of Final Research Achievements

This study investigated the effects of the Changjiang River discharge (CRD) into the East China Sea (ECS) with regard to sea surface temperature (SST) and related atmospheric changes (such as torrential rainfall events) using the ocean general circulation model (OGCM) and regional climate model. Twin experiments, using a regional climate model with and without CRD used for the lower boundary conditions, revealed that the decrease in the SST dependent on the CRD contributes to the substantially increased precipitation in extreme events such as the one observed in July 2009 over Kyushu. This is because the change in SST related to the CRD significantly affects the field change of the moisture flux convergence. These results suggest that CRD significantly influences both ocean and atmosphere circulation systems over the ECS.

Academic Significance and Societal Importance of the Research Achievements

東シナ海への長江からの淡水流入をテーマにした既往研究は、ほとんどが塩分、海色・濁度、生態系への影響を議論しており、Kako et al. (2016)で示されたような長江希釈水に起因した水温分布の形成・変動過程が、その直上の大気に与える影響や、集中豪雨などの激甚災害に与えるインパクトへの言及は皆無であった。本研究は数値実験を通して、長江希釈水が夏季東シナ海陸棚域の海面水温を低下させ、その水温低下によって励起される東シナ海上の大気応答が、集中豪雨の発生・発達に対し、統計的な有意性が見出される程度に寄与することを初めて示した。これらの成果は、国内外の主要な学会で発表した。

Report

(4 results)
  • 2019 Annual Research Report   Final Research Report ( PDF )
  • 2018 Research-status Report
  • 2017 Research-status Report
  • Research Products

    (4 results)

All 2019 2017

All Presentation (4 results) (of which Int'l Joint Research: 1 results)

  • [Presentation] 長江希釈水と九州周辺で発生する集中豪雨の関係2019

    • Author(s)
      加古真一郎 高山勝巳
    • Organizer
      日本海洋学会秋季大会
    • Related Report
      2019 Annual Research Report
  • [Presentation] Impact of the Changjiang River discharge on sea surface temperature in the East China sea and torrential rainfall events over Kyushu2019

    • Author(s)
      Shin'ichiro Kako and Katsumi Takayama
    • Organizer
      20th Pacific Asian Marginal Seas (PAMS 2019)
    • Related Report
      2018 Research-status Report
    • Int'l Joint Research
  • [Presentation] 長江希釈水が平成21年7月中国・九州北部豪雨に与えた影響2017

    • Author(s)
      加古真一郎・有留晴香・高山勝巳
    • Organizer
      日本海洋学会秋季大会
    • Related Report
      2017 Research-status Report
  • [Presentation] 有留晴香・加古真一郎・高山勝巳2017

    • Author(s)
      長江希釈水が平成21年7月中国・九州北部豪雨に与えた影響
    • Organizer
      鹿児島県気象研究会
    • Related Report
      2017 Research-status Report

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Published: 2017-04-28   Modified: 2021-02-19  

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