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| Funder | Swedish National Space Agency |
|---|---|
| Recipient Organization | Swedish Institute of Space Physics |
| Country | Sweden |
| Start Date | Mar 01, 2025 |
| End Date | May 31, 2025 |
| Duration | 91 days |
| Number of Grantees | 2 |
| Roles | Principal Investigator; Co-Investigator |
| Data Source | Swedish Research Council |
| Grant ID | 2025-00072_SNSB |
The Venus magnetotail is highly dynamic, much more so than was previously expected.
Indeed, many scientists in this field still consider it to be relatively stable; however, our measurements by the Analyzer of Space Plasmas and Energetic Atoms (ASPERA-4) instrument, developed by the Swedish Institute of Space Physics (IRF) on Venus Express (VEX), along with many other instruments on VEX, Solar Orbiter, BepiColombo, and Parker Solar Probe, reveal its dynamic nature.
While ions in the magnetotail generally flow away from the planet, ASPERA-4 frequently measured a "return flow", a global ion flow pattern in the tail directed toward Venus.The plasma process that alters the flow direction is still unknown.
Magnetic reconnection and its associated phenomena were identified experimentally, but the link to the return flow is another key open question to understand convection in the Venusian magnetotail.
No global numerical model has reproduced this large-scale convection in the induced magnetotail of Venus, emphasizing the lack of current knowledge about this phenomenon.The Dungey-V mission concept aims to answer the following science questions.How does the ion return flow impact the global energy, momentum, and mass flow at Venus?What is the fate of the ions in the return flows and reconnected magnetic flux?How does the magnetic reconnection process work with the draped field?The Dungey-V spacecraft will be inserted into a heliocentric orbit and conduct at least 10 flybys with a resonant orbit.
A flyby mission concept would prove more beneficial than an orbiter for multiple reasons.
First, controlled flybys will allow exploration of various tail regions in the magnetotail, not easily achieved with an orbiter. Observing dynamic processes requires advanced instrument suites capable of high-time resolution measurement (~100 ms).
Such measurements will create a large data volume; however, the flyby mission provides opportunities for data downlink when the spacecraft is close to Earth, simplifying telemetry requirements.The Dungey-V instrument suite will include ion spectrometers, electron spectrometers, a magnetometer, electromagnetic wave analyzers, and a nightglow camera, subject to future trade-off.
The innovation of this mission concept is the very high time resolution for plasma measurements, never achieved before near Venus.
This capability is comparable to that of state-of-the-art terrestrial magnetospheric missions (e.g., MMS), which have provided extensive insight into Earth’s magnetosphere.
Given the unique nature of Venus as the only truly non-magnetized terrestrial magnetosphere, we expect similarly significant scientific insights from Dungey-V.Here, IRF needs professional industry support fortheDungey-V missionproof-of-concept.
The main focus will beonmission analysistoenable our science.We anticipate a trade-off assessment of flyby configurations, includingapros/cons analysis compared to an orbiter.
We additionally expect analysis of the mission operation scenario and telemetry budget, as well as a basic spacecraft conceptual design.
Swedish Institute of Space Physics
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