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

Simultaneous measurements of temperature and wind profiles in the surface boundary layer (below 10-m elevation over a beach and below 100-m elevation over an inland site) under the effect of the sea breeze were made near Fort Walton Beach, Fla. We found that the sea breeze in the atmospheric boundary layer is in the free convection regime and that observed sea-breeze wind and temperature profiles behave according to minus one-third power laws. These experiments also substantiate evidence that the Prandtl-Obukhov-Priestley prediction of the free convection regime is a valid one under appropriate atmospheric conditions.

Dynamics of the Sea Breeze in the Atmospheric Boundary Layer: A Case Study of the Free Convection Regime