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

The foehn effect on the northwestern slopes of the White Carpathians has been by many scholars explained as the result of south and souteastern winds. No quantitative-based proofs, however, have so far acknowledged the existence of pseudoadiabatic processes in this region. This article analyses conditions for the rise and movement of foehn-type winds in the Moravian (northwestern) part of the White Carpathians. Data on air temperature and humidity from the period July 1987 - October 1988, recorded at 5 meteorological stations between the Váh and Morava Rivers, have been used.

Foehns on the Northwestern Slopes of the White Carpathians?