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Thermosphere: composition and chemistry

A view of Earth’s thin atmosphere from the International Space Station.
Posted inAGU News

Paying Attention to the “Ignorosphere”

by Heather Goss 22 April 20213 November 2021

Scientists discuss geospace and what we could learn if we put some more eyes on this region in the atmosphere. Read more in our special themed issue.

Two plots showing percent changes in TIME-GCM zonally averaged [O+] and [H+] as a function of latitude and altitude in the Northern Hemisphere between the “disturbed” and “pre-disturbance” time periods in 2012–2013
Posted inEditors' Highlights

Stratospheric Weather Impacts Light Species at Great Heights

by Michael P. Hickey 14 December 202010 December 2020

Sudden stratospheric warmings in the high latitude wintertime can drive changes in light species (H, He and O) all the way though the thermosphere, likely influencing ion densities in the exosphere.

Researchers trace long-term changes in the ionosphere back to Sun cycles, not greenhouse gas emissions.
Posted inResearch Spotlights

Is There a Greenhouse Effect in the Ionosphere, Too? Likely Not

by Mark Zastrow 13 October 2017

Controversial observations of long-term changes in the ionosphere appear to be explained by the Sun’s 11-year cycle of activity, not human greenhouse gas emissions.

Researchers unravel the mystery of an anomaly in Earth’s ionosphere
Posted inResearch Spotlights

Auroras May Explain an Anomaly in Earth’s Ionosphere

by E. Underwood 7 August 201715 August 2017

A new study finds that the ionospheric anomaly over the Weddell Sea is likely influenced by proximity to auroral energy input, rather than by tilting magnetic fields.

Posted inResearch Spotlights

What Drives Variation in the Ionosphere’s Electron Density?

by K. J. Knizhnik 22 September 201622 September 2016

The long-term trend in the electron density of the ionospheric F layer may be natural, not man-made.

Posted inResearch Spotlights

What Causes Nitric Oxide to Infiltrate the Ozone Layer?

by JoAnna Wendel 9 December 20147 September 2016

Processes in the polar atmosphere can cause nitric oxide (NO)-enriched air to descend and destroy stratospheric ozone. Scientists explore one cause of these NO fluxes, stratospheric sudden warming.

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