FIELD MEASUREMENTS OF CURRENTS AND MATERIAL TRANSPORT AT TOKYO-BAY MOUTH IN THE CONDITION OF KUROSHIO WARM WATER INTRUSION IN WINTER

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  • 黒潮系暖水波及時における冬季東京湾湾口部の流動構造と熱・物質フラックス
  • クロシオケイダンスイ ハキュウジ ニ オケル トウキ トウキョウワン ワンコウブ ノ リュウドウ コウゾウ ト ネツ ブッシツ フラックス

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Abstract

Field measurements were performed to investigate the effects of Kuroshio Warm Water Intrusion (KWWI) to the mouth of Tokyo Bay on the three dimensional characteristics of currents and material transport in the bay mouth in winter. When KWWI occurs, the bay water with low temperature and low salinity flows toward the ocean in the surface layer, the Kuroshio Warm water with high temperature and high salinity intrudes into the bay in the intermediate layer and the coastal water with low temperature and high salinity flows toward the ocean in the bottom layer. The depth of the KWW intrusions into the bay depends on its density relative to the vertical density profile at the bay. The KWWI transports heat into the bay effectively which is five times as large as the winter-averaged heat flux.

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