The stratospheric ozone layer is a band of ozone (O₃) in the stratosphere, roughly 15-35 km up, that absorbs most of the sun's ultraviolet radiation. It is essential to the evolution of life on Earth and the continued health and survival of life on Earth.
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Lesson PreviewLesson 1 of 10 in this unit
9.1 Stratospheric Ozone Depletion
Part of Global Change in AP® Environmental Science. Read the opening section, then create a free account for the full interactive lesson, practice, and progress tracking.
In this unit
10 lessons
- 9.1Stratospheric Ozone DepletionThis lesson
- 9.2Reducing Ozone DepletionPreview lesson
- 9.3The Greenhouse EffectPreview lesson
- 9.4Increases in the Greenhouse GasesPreview lesson
- 9.5Global Climate ChangePreview lesson
- 9.6Ocean WarmingPreview lesson
- 9.7Ocean AcidificationPreview lesson
- 9.8Invasive SpeciesPreview lesson
- 9.9Endangered SpeciesPreview lesson
- 9.10Human Impacts on BiodiversityPreview lesson
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