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Communicating Heliophysics at Different Levels

Whether you are a teacher answering a student question, a librarian planning a STEM day, or a scientist visiting a classroom, use this topic guide to help explain heliophysics concepts to your target audience at the appropriate level.

Atmosphere

What should learners know about this topic at each level?

Introductory: Our atmosphere consists of 21% oxygen, 78% nitrogen and 0.9% argon. There is also an important trace gas called carbon dioxide. Without it, our planet would be too cold for liquid water and life.

Intermediate: The atmosphere is a gaseous envelope surrounding and protecting our planet from the intense radiation of the Sun and serves as a key interface between the terrestrial and ocean cycles. Its inner layers closest to the surface are responsible for clouds and weather, while the outer layers above the stratosphere include the ozone layer, which protects life from ultraviolet light. Our atmosphere shields us from all solar radiation in the x-ray and gamma-ray bands of the EM spectrum, and some of the ultraviolet light. It also shields us from many forms of infrared and radio wavelength light.

Advanced: Our atmosphere does not have the same density and temperature at all heights. It is heated by absorbing radiation from the sun, and its ozoine layer blocks nearly all ultraviolet light. The upper stratosphere is strongly affected and heated by solar activity that produces x-rays. Its temperature and thickness is highest during sunspot maximum when the sun is most active.

An illustration showing the layers of Earth's atmosphere.
An illustration of the five different layers of Earth’s atmosphere.
NASA GSFC/Mary Pat Hrybyk-Keith

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