Spinning Tethered Systems: Opportunities for Improved Earth Observation and Planetary Exploration
Highlights
- A feasibility study of CubeSat-scale spinning tethered systems for Earth and planetary observation.
- Analytical and mission-level analyses assess achievable configurations and system performance.
- Applicability of spinning tethered systems to multiple sensing approaches, including stereo imaging, radar sounders, and SAR interferometry.
- The proposed architecture enables observation missions with flexible baselines and system configurations at the CubeSat scale.
Abstract
1. Introduction
2. Tether System
2.1. System Description and Modelling
- Orbit: the orbital parameters are selected based on the regions of interest to ensure adequate coverage. Moreover, the orbital altitude directly affects the achievable imaging resolution.
- Length of the tether: it determines the system baseline and, consequently, the performance of the remote sensing measurements. A longer tether is generally desirable; however, increasing the tether length also increases the volume occupied by the coiled tether within the system. Therefore, a detailed trade-off study is required to satisfy both baseline and volume constraints.
- Spin vector: the spin vector is crucial both in terms of direction and magnitude, resulting in different baselines and periodicity of the signal.
2.2. Mission Phases and System Stability
2.3. System Configuration
- Spin axis lying on the orbital plane, see Figure 5. Due to geometrical constraints, in this inertially fixed configuration, the spin axis is, clearly, not always nadir-pointing, unless a constant thrust is applied. This configuration allows baseline projection variations both along and across the velocity. The baseline projection variations evolve more slowly compared with the other configuration, and the maximum baseline projection length can be achieved only twice per orbit: when the spin axis is aligned with the orbital radial direction.
- Spin axis perpendicular to the orbital plane, see Figure 6. The main advantage of this configuration lies in the ability to achieve the maximum baseline projection as a function of the system spin rate, and more frequently than in the previous configuration. Since the motion of the masses lies entirely within the orbital plane, this configuration allows the baseline projection to vary only along the velocity direction.
2.4. System Sizing
3. Possible Applications for Earth and Moon Observation
3.1. Stereo Imaging
- The two images are taken at the same time, allowing it to observe even very fast phenomena, as well as simplifying the matching procedure between the two images by reducing temporal decorrelation;
- It is possible to easily vary the baseline of the system, by just reeling the tether in or out, allowing a much greater flexibility in operations.
3.2. Distributed Radar Sounder
- 4.2 cm (X-band)—analogous to the wavelength used by the Mini-RF instrument aboard NASA’s Lunar Reconnaissance Orbiter (LRO) [39], designed for polar ice detection;
- 70 cm (P-band)—consistent with the radar wavelength planned for the BIOMASS mission [40] by the the European Space Agency (ESA), aimed at global forest biomass observation;
- 33 m (HF-band)—corresponding to the wavelength of the RIME instrument on board ESA’s JUICE mission [41], designed for subsurface geological analysis of icy moons.
3.3. SAR Interferometry
4. Conclusions and Future Developments
Author Contributions
Funding
Data Availability Statement
Conflicts of Interest
References
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| Wavelength | |||||||
|---|---|---|---|---|---|---|---|
| [rpm] | |||||||
| ct | at | ct | at | ct | at | ||
| Earth—400 km | 1 | 86.35 | 78.13 | 84.05 | 75.14 | 43.20 | 42.42 |
| 0.1 | 86.23 | 77.70 | 83.89 | 75.48 | 42.16 | 41.30 | |
| Moon—100 km | 1 | 96.61 | 92.88 | 96.04 | 91.93 | 87.51 | 76.65 |
| 0.1 | 96.56 | 95.19 | 96.07 | 94.52 | 87.50 | 79.13 | |
| Moon—50 km | 1 | 98.30 | 96.12 | 98.06 | 95.50 | 93.78 | 88.28 |
| 0.1 | 98.32 | 97.12 | 98.03 | 96.76 | 93.72 | 89.67 | |
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Trabacchin, N.; Trevisanuto, G.; Enzo, S.; Anese, G.; Olivieri, L.; Valmorbida, A.; Colombatti, G.; Bettanini, C.; Lorenzini, E.C. Spinning Tethered Systems: Opportunities for Improved Earth Observation and Planetary Exploration. Remote Sens. 2026, 18, 706. https://doi.org/10.3390/rs18050706
Trabacchin N, Trevisanuto G, Enzo S, Anese G, Olivieri L, Valmorbida A, Colombatti G, Bettanini C, Lorenzini EC. Spinning Tethered Systems: Opportunities for Improved Earth Observation and Planetary Exploration. Remote Sensing. 2026; 18(5):706. https://doi.org/10.3390/rs18050706
Chicago/Turabian StyleTrabacchin, Nicolò, Giovanni Trevisanuto, Samuele Enzo, Giovanni Anese, Lorenzo Olivieri, Andrea Valmorbida, Giacomo Colombatti, Carlo Bettanini, and Enrico C. Lorenzini. 2026. "Spinning Tethered Systems: Opportunities for Improved Earth Observation and Planetary Exploration" Remote Sensing 18, no. 5: 706. https://doi.org/10.3390/rs18050706
APA StyleTrabacchin, N., Trevisanuto, G., Enzo, S., Anese, G., Olivieri, L., Valmorbida, A., Colombatti, G., Bettanini, C., & Lorenzini, E. C. (2026). Spinning Tethered Systems: Opportunities for Improved Earth Observation and Planetary Exploration. Remote Sensing, 18(5), 706. https://doi.org/10.3390/rs18050706

