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Stratospheric ozone depletion
Solar ultraviolet radiation creates an ozone layer in the atmosphere which in turn completely absorbs the most energetic fraction of this radiation. This process both warms the air, creating the stratosphere between 15 and 50 km altitude, and protects the biological activities at the Earth's su...
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| 第一著者: | |
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| フォーマット: | Artigo |
| 言語: | Inglês |
| 出版事項: |
The Royal Society
2006
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| 主題: | |
| オンライン･アクセス: | https://ncbi.nlm.nih.gov/pmc/articles/PMC1609402/ https://ncbi.nlm.nih.gov/pubmed/16627294 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1098/rstb.2005.1783 |
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