Between Earth and outer space, there is a critically important area. This is the atmosphere. Now, a NASA funded instrument has revealed some long-held secrets about the ionosphere.
The ionosphere stretches roughly 50 to 400 miles above Earth's surface. It is exactly at the edge of space. This is the dynamic region where the atmosphere meets space. Home to astronauts on the space station and to many satellites, the ionosphere constantly fluctuates and responds to changes from above and below.
A NASA-funded instrument is shedding new light on the invisible processes and rhythms at play in this intersection between Earth and space.
In the ionosphere, radiation from the Sun cooks some of the gases until they lose an electron or two. The result is a sea of electrically charged particles—ions—intermingled with the neutral upper atmosphere.
Not just energy from the Sun, but the ionosphere also responds to weather patterns that ripple up from the lower parts of Earth's atmosphere.
Such changes affect key communications systems such as high-frequency (HF) radio and GPS.
Atmospheric scientist Richard Eastes of the University of Colorado says the region is far more variable than scientists expected.
This is based on the insight from the Global-scale Observations of the Limb and Disk (GOLD) instrument, which images the ionosphere.
The image above was acquired by GOLD on December 19, 2018—a view of the entire Western Hemisphere as observed from geostationary orbit.
The left third of the sphere is still in daylight, while eastern North and South America were bathed in twilight or darkness.
The blue strips stretching across the Atlantic Ocean are known as the Appleton anomaly, a region of the ionosphere around the magnetic
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