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オゾン層
Sign in to saveAlso known as stratospheric ozone, ozone shield, atmospheric ozone, atmospheric ozone layer
地球の大気中でオゾンの濃度が高い部分
AI overview
The ozone layer is a region in Earth's upper atmosphere that absorbs most of the harmful ultraviolet radiation coming from the Sun. This protection matters because it shields life on Earth's surface from UV radiation that can damage living organisms.
AI-generated from the Wikipedia summary — may contain errors.
Research
3,115 papers- Anaesthetic agents and the ozone layer.ReviewAnaesthesia and intensive care · 1990Westhorpe R, Blutstein HDOI: 10.1177/0310057X9001800115
- Ozone depletion update.ReviewDermatologic surgery : official publication for American Society for Dermatologic Surgery [et al.] · 1996Coldiron BMDOI: 10.1111/j.1524-4725.1996.tb00321.x
- UV-induced DNA damage and repair: a review.ReviewPhotochemical & photobiological sciences : Official journal of the European Photochemistry Association and the European Society for Photobiology · 2002Sinha RP, Häder DPDOI: 10.1039/b201230h
- Australian wildfires depleted the ozone layer.Science (New York, N.Y.) · 2022Salawitch RJ, McBride LADOI: 10.1126/science.add2056
- How CubeSats could harm the ozone layer.Nature · 2023DOI: 10.1038/d41586-023-01281-w
- Stratospheric ozone depletion.ReviewPhilosophical transactions of the Royal Society of London. Series B, Biological sciences · 2006Rowland FSDOI: 10.1098/rstb.2005.1783
- CFCS and the ozone layer.British journal of clinical practice. Supplement · 1997Hayman GD
- Depletion of the ozone layer: consequences for non-infectious human diseases.ReviewParasitology · 1993Bentham GDOI: 10.1017/s0031182000086108
via PubMed
Wikidata facts
- Part of
- stratosphere
- Has part
- ozone
- Image
- Agujero en la capa de ozono 2008.jpg
Show 1 more fact
- Commons category
- Ozone layer
Sources (2)
via Wikidata · CC0
Article · 日本語
オゾン層(オゾンそう 独: Ozonschicht 英: ozone layer)とは地球の大気中でオゾンの濃度が高い部分のことである。オゾンは、高度約10 - 50 kmほどの成層圏に多く存在し、特に高度約25 kmで最も密度が高くなる。
Abstract from DBpedia / Wikipedia · CC BY-SA
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