Lesson 4 of 8 · Dynamics explorer
Dynamics Explorer: connect the upper atmosphere with the magnetosphere
8 minute lesson · 3 checks along the way
Your goal for this lessonExplain how two spacecraft at different altitudes helped investigate interactions between Earth’s atmosphere, ionosphere and magnetosphere.
In this lesson 3 sections · 3 checks
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Observe connected regions from different heights
Dynamics Explorer 1 and Dynamics Explorer 2 launched together in August 1981. Their polar orbits lay in the same plane but reached different altitudes: DE-1 traveled much farther from Earth, while DE-2 sampled the upper atmosphere and ionosphere closer to the planet. This arrangement let scientists investigate connected regions with complementary measurements.
The ionosphere contains charged particles as well as neutral gas, and it interacts with the magnetosphere above. Electric fields, particle motion and atmospheric winds are linked through several processes rather than a single rigid connection. A low-altitude measurement can therefore supply a different part of the explanation from a measurement or auroral image taken at greater distance.
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Combine a wider view with local measurements
DE-1 included instruments for studying particles and fields, along with remote observations. DE-2 investigated conditions closer to Earth, including the neutral and charged environment. An auroral image can locate a broad pattern, while an in-situ detector samples conditions near the spacecraft. Combining these methods can connect visible or ultraviolet structure with the particles and fields involved.
Consider a fictional brightening in an auroral image and a particle change measured on the lower spacecraft. They are promising observations to compare, but similar times do not prove that both instruments observed exactly the same physical region. Investigators need the spacecraft positions, viewing geometry and a model of magnetic connectivity, with its uncertainty made explicit.
Dynamics Explorer: connected regions
Original teaching diagram. Higher observations. DE-1: particles and fields. Remote auroral observations. Lower observations. DE-2: ions and neutral gas. Upper-atmosphere conditions. Same orbital plane does not mean continuous alignment; diagram is not to scale.
Open full-size diagram in a new tab: Dynamics Explorer: connected regionsCheck 2 of 3
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Keep geometric alignment separate from complete coverage
mean that the orbital planes coincide; they do not guarantee that the spacecraft remain vertically aligned or observe every region together. Orbital motion changes their separation and opportunities for comparison. A useful event selection therefore identifies when the geometry supports the scientific question, rather than assuming every pair of timestamps is equally informative.
The original teaching diagram contrasts higher and lower observations without drawing them to scale. In a research analysis, actual position data replace that sketch. Check instrument response, time resolution and the relevant atmospheric conditions before joining datasets. Dynamics Explorer’s contribution was to make linked-region investigations possible while showing why observations at different heights still require careful physical interpretation.
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Explore further · Optional
Go to the source
Explore the evidence behind this lesson. These optional readings and videos open in a new tab.
- Read: NASA: Dynamics Explorer launchCompare the explanation and its assumptions with the worked example in this lesson.
- Read: LASP instrument team: Dynamics Explorer orbits and measurementsHistorical instrument-team description; mission end dates can refer to different operational or data milestones.
- Read: NASA: Dynamics Explorer mission reportCompare the explanation and its assumptions with the worked example in this lesson.