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

a rather narrow zone immediately above and below t'hc point desig- nated as the tropopause. rlre mystery about the tropo- pause is, t'herefore, not primarily its location, bat rattwr the sharpness of the change of the temperature gradient' that is associated with it. The radiative processes and the other large-scale heat transport processes that cleter- mine the mean atmospheric temperature distribution probably also determine the large-scale features of the tropopause, such as its general location and its seasonal and large-scale spatial variations. Rut what is the reason for the often observed sharp change of the t'emperaturr gradient at the tropopause? What are the physical processes that are responsible for it's creation, maintenance,

The Probing of the Tropopause by Balloons that Follow It—A Suggestion1

The Probing of the Tropopause by Balloons that Follow It—A Suggestion¹