This new paper published in Science suggests that as the tropical oceans get warmer, ocean emissions of methyl bromide (CH3Br) and other short-lived ozone-depleting substances will increase, slowing down the ongoing ozone recovery.
Image credit: Scientific assessment of ozone depletion 2014
http://science.sciencemag.org/content/358/6368/1257
https://www.esrl.noaa.gov/research/themes/o3/
http://science.sciencemag.org/content/353/6296/269
Leave a Reply