English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Tools annual

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Tools monthly

Global: Zendy Plus monthly

Presents the access of premium content as premium feature

Premium Content

Global: Zendy Plus annual

Global: Zendy Free Plan

In this study, the field observations were carried out along Konagai-Mizuho observation line at a spring tide in summer to investigate the characteristics of tidal flow and water quality in Isahaya Bay. A strong density-stratification and the anoxic water in the lower layer were observed and were not broken in one tidal period. The velocity profiles were appreciably different between the upper layer and the lower layer because of the stratification and the action of the south wind. The upwelling of water mass with low dissolved oxygen was observed at the south coast of Isahaya Bay during the ebb tide. It was caused by the superposition of the density stratification and the wind stress to transport the water mass in the lower layer toward the south coast on the unique tidal flow attributed to the geographical feature of Isahaya Bay.

The Upwelling of Water Mass with Low Dissolved Oxygen Induced at the South Coast of Isahaya Bay by the South Wind