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 Tools annual

Global: Zendy Free Plan

Global: Zendy Tools monthly

Global: Zendy Plus monthly

In August 2016, tropical cyclones formed over an area of enhanced convective activities to the southeast of Japan and moved westward or northward (Fig. 2d) with warm and moist air inflow, causing significant wet conditions in eastern and northern Japan (Fig. 1). Japan Meteorological Agency (JMA) performed climate diagnoses for the event and suggested that the Rossby wave-breaking (RWB) to the east of Japan might induce the enhanced convective activities to the southeast of Japan.

Relation between a Rossby Wave-Breaking Event and Enhanced Convective Activities in August 2016