Article in Nature by Becky Alexander
Isotopic evidence of multiple controls on atmospheric oxidants over climate transitions. The abundance of tropospheric oxidants, such as ozone (O3) and hydroxyl (OH) and peroxy radicals (HO2 + RO2), determines the lifetimes of reduced trace gases such as methane and the production of particulate matter important for climate and human health...Read more from UW Today: http://www.washington.edu/news/2017/05/17/earths-atmosphere-more-chemically-reactive-in-cold-climates/
Read the paper: https://www.nature.com/articles/nature22340
Last updated: 2021-06-03 23:01:47