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Arctic “ozone hole” in a cold volcanic stratosphere
Optical depth records indicate that volcanic aerosols from major eruptions often produce clouds that have greater surface area than typical Arctic polar stratospheric clouds (PSCs). A trajectory cloud–chemistry model is used to study how volcanic aerosols could affect springtime Arctic ozone loss pr...
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| Hoofdauteurs: | , , , , |
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| Formaat: | Artigo |
| Taal: | Inglês |
| Gepubliceerd in: |
The National Academy of Sciences
2002
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| Onderwerpen: | |
| Online toegang: | https://ncbi.nlm.nih.gov/pmc/articles/PMC122395/ https://ncbi.nlm.nih.gov/pubmed/11854461 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.052518199 |
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