Ozone–oxygen cycle
id:
ozone-oxygen-cycle-305-16665833
title:
Ozone–oxygen cycle
text:
The ozone–oxygen cycle is the process by which ozone is continually regenerated in Earth's stratosphere, converting ultraviolet radiation (UV) into heat. In 1930 Sydney Chapman resolved the chemistry involved. The process is commonly called the Chapman cycle by atmospheric scientists. Most of the ozone production occurs in the tropical upper stratosphere and mesosphere. The total mass of ozone produced per day over the globe is about 400 million metric tons. The global mass of ozone is relativel
brand slug:
wiki
category slug:
encyclopedia
description:
Biogeochemical cycle
original url:
https://en.wikipedia.org/wiki/Ozone%E2%80%93oxygen_cycle
date created:
date modified:
2024-04-01T19:03:51Z
main entity:
{"identifier":"Q673756","url":"https://www.wikidata.org/entity/Q673756"}
image:
{"content_url":"https://upload.wikimedia.org/wikipedia/commons/2/28/Ozone_cycle.svg","width":1052,"height":744}
fields total:
13
integrity:
15