Planetary Ecologist<p>Ozone–oxygen cycle (Biogeochemical cycle 🔄)</p><p>The ozone–oxygen cycle is the process by which ozone is continually regenerated in Earth's stratosphere, converting ultraviolet radiation 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...</p><p><a href="https://en.wikipedia.org/wiki/Ozone–oxygen_cycle" rel="nofollow noopener" translate="no" target="_blank"><span class="invisible">https://</span><span class="ellipsis">en.wikipedia.org/wiki/Ozone–ox</span><span class="invisible">ygen_cycle</span></a></p><p><a href="https://mastodon.social/tags/OzoneOxygenCycle" class="mention hashtag" rel="nofollow noopener" target="_blank">#<span>OzoneOxygenCycle</span></a> <a href="https://mastodon.social/tags/Oxygen" class="mention hashtag" rel="nofollow noopener" target="_blank">#<span>Oxygen</span></a> <a href="https://mastodon.social/tags/OzoneDepletion" class="mention hashtag" rel="nofollow noopener" target="_blank">#<span>OzoneDepletion</span></a> <a href="https://mastodon.social/tags/BiogeochemicalCycle" class="mention hashtag" rel="nofollow noopener" target="_blank">#<span>BiogeochemicalCycle</span></a> <a href="https://mastodon.social/tags/AtmosphericChemistry" class="mention hashtag" rel="nofollow noopener" target="_blank">#<span>AtmosphericChemistry</span></a></p>