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/

Zendy Plus

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

Zendy Tools

Zendy Open

Measurements of the slope current at twolocations north-west of Ireland have been made between April and December 1994,40 m above the seabed in a water depth of 660 m. A persistent polewardalong-slope current was observed at both locations, with measured means of 10and 21cms–1 respectively. A CTD transect across the slope near onemooring indicated the presence of a light, warm, saline core of water at theshelf edge. Peak currents were O(50)cms–1, with strongest meanflow at the location with steeper slope. Variability at sub-tidal periods,principally 2–5 and 11–12 days, was apparent. The shorter-period variability waswell correlated with coastal sea-level variations measured at a land point nearto one of the moorings. The variability in the slope current at this periodappeared to be a result of the warm current core movement up/down slope,probably as a result of interaction with higher-mode shelf waves. Somesuggestion of a bottom-trapped diurnal wave was also found at one location

The shelf-edge current north-west of Ireland