日本海の衛星海面高度偏差を用いた海面冷却駆動流の抽出

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書誌事項

タイトル別名
  • Extraction of cooling-induced current from the satellite sea surface height anomaly in the Japan Sea

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抄録

To extract “Cooling-Induced Current (CIC)” component of the Tsushima Warm Current from the satellite sea surface height anomaly (SSHA) data, harmonic analysis of SSHA in spring (February to April) is conducted for 8- and 5-year period, with respect to similarities in the year-to-year variation of Asian Monsoon Index (MOI). In the long-term response of 8-year period, north-eastward flow off shelf edge along the Japanese island is intensified just at the most severe cooling year, which is suggested by the maximum MOI. Such intensified flow, i.e., CIC, gradually migrates offshore during 2 years, and then connects to inflow in the Tsushima/Korean strait via the east coast of Korean peninsula with time lag of about 3 years.

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詳細情報 詳細情報について

  • CRID
    1390290699772575872
  • NII論文ID
    120006712020
  • NII書誌ID
    AA11547977
  • DOI
    10.14943/bull.fish.69.1.19
  • HANDLE
    2115/75195
  • ISSN
    13461842
  • 本文言語コード
    ja
  • データソース種別
    • JaLC
    • IRDB
    • CiNii Articles
  • 抄録ライセンスフラグ
    使用可

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