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The severe storm surge was occurred at the eastern part (Atsumi Bay) of Mikawa Bay due to Typhoon 0918. The high water level region was simultaneously induced in the western part (Chita Bay) of the bay. The formative mechanism of the region was investigated in this study. The high water level condition around Chita Bay occurred prior to the storm surge in Atsumi Bay by easterly winds of typhoon approaching. Strong currents, which are a part of counter-clockwise circulation in Mikawa Bay, were generated at the mouth of Chita Bay during the surge. It is inferred the currents pushed sea water into Chita Bay and weakened that the water flows out of the bay. Consequently, the high water level condition in the bay persisted during the surge in Mikawa Bay.

Formative Mechanism of High Water Level Region in Chita Bay due to Storm Surge in Mikawa Bay