These energetic neutral atom (ENA) panels show IBEX observations before (left) and after (right) the solar wind impacted the Earth's magnetosphere on April 5, 2010, and increased from one- to two-million miles-per-hour.
The magnetosphere, which is modeled in both panels, becomes compressed after the impact and shows a significant rise in the production of energetic neutral atoms (indicated by red).
For the first time, instrumentation aboard two NASA missions operating from complementary vantage points watched as a powerful solar storm spewed a two million-mile-per-hour stream of charged particles and interacted with the invisible magnetic field surrounding Earth, according to a paper published today in the Journal of Geophysical Research.
The spacecraft, NASA's Two Wide-angle Imaging Neutral-atom Spectrometers (TWINS) and Interstellar Boundary Explorer (IBEX), observed the impact from inside and outside the Earth's magnetosphere, respectively.
The energetic neutral atom (ENA) cameras aboard each spacecraft enabled global imaging of the magnetosphere, the invisible bubble that protects Earth from the majority of charged particles from the Sun, as it compressed in response to sharply faster solar wind.
The storm, observed April 5, 2010, also is thought to have caused an important communications satellite, Galaxy-15, to founder and drift, taking almost a year to return to its station.
These integrated images show energetic neutral atom (ENA) emissions as seen by TWINS.
Each circle represents five minutes of activity, with the start times listed at the top of the graph.
Each row shows a different energy band. The images in the last two columns (in red boxes) were taken roughly 20 minutes and one hour after the solar wind impact.
Each circle represents five minutes of activity, with the start times listed at the top of the graph.
Each row shows a different energy band. The images in the last two columns (in red boxes) were taken roughly 20 minutes and one hour after the solar wind impact.
"More likely, however, is that they will get too close together and their radio frequencies will interfere with the operation of nearby satellites, which could hamper activities on Earth."
The IBEX images (taken from a distance of around 180,000 miles) show an immediate compression of the magnetosphere as it was impacted by charged particles from the solar wind.
ENA global imaging enabled the team to determine the precise timing of the compression, to within ±9 seconds.
Minutes later, one of the TWINS spacecraft, carrying identical ENA sensors that provide stereoscopic imaging, observed changes in the inner magnetosphere (from a much-closer 28,000 miles).
A magnetospheric structure called the "ring current" traps charged particles that gyrate around magnetic field lines.
About 15 minutes after impact, the trapped particles propagated down the field lines toward the poles and into Earth's atmosphere, where they produced additional ENAs.
The brief time delay in losing particles to the atmosphere suggests that internal magnetospheric processes take some time after compression from the initial impact.
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