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 Plus annual

Presents the access of premium content as premium feature

Premium Content

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 Plus monthly

Global: Zendy Tools annual

Global: Zendy Tools monthly

Global: Zendy Free Plan

The cold water region in the offing of Enshfmada is generated by the overflow of the intermediate water upwelling in the sea off the coast of TOkaidO. And when the Kuroshio is strong, the overflowing of the intermediate water is stopped and the cold water region is pushed away and disappear. From the mean values of actual sounding, no cold water region can be seen when the maximum velocity of the Kuroshio is larger than 2. 5 knots.

A Theory of the Mechanism of the Generation of the Cold Water Region in the Offing of Ensh&ucirc;nada

A Theory of the Mechanism of the Generation of the Cold Water Region in the Offing of Enshûnada