日本周辺海域における透明度の季節変動と臨界深度との関係

DOI

書誌事項

タイトル別名
  • Seasonal Variability of Transparency and its Relationship to the Critical Depth in the Seas Adjacent to Japan.

抄録

Aim of this paper is to reveal major causes of seasonal variability of phytoplankton biomass in the seas adjacent to Japan by relating changes of transparency to those of environmental factors. Generally, phytoplankton biomass begins to increase when the Sverdrup's critical depth exceeds the upper mixed layer depth in spring, and decreases in summer with development of the seasonal pycnocline. After the summer minimum, it increases temporally in early autumn when an upper mixed layer becomes deeper and yet shallower than the critical depth. Critical depth model is applicable to waters in the transitional/subarctic Pacific and the Japan Sea. On the other hand, in the Pacific off the southern midcoast of Japan and the East China Sea, seasonal variability of phytoplankton biomass is not fully explained by the critical depth model. These waters are characterized by low concentration and no seasonality of nutrients. Significant negative correlations were observed between surface nutrient concentrations and transparency. These facts indicate that the physical conditions such as critical depths, mixed layer depths and solar irradiance as well and the chemical condition like nutrients availability are responsible for the seasonal variability and annual level of phytoplankton biomass in the seas adjacent to Japan.

収録刊行物

  • 海の研究

    海の研究 6 (6), 351-360, 1997

    日本海洋学会

詳細情報 詳細情報について

  • CRID
    1390001204382587776
  • NII論文ID
    130004387787
  • DOI
    10.5928/kaiyou.6.351
  • ISSN
    21863105
    09168362
  • 本文言語コード
    ja
  • データソース種別
    • JaLC
    • Crossref
    • CiNii Articles
  • 抄録ライセンスフラグ
    使用不可

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