Localisation of the Cluster satellites

We contributed to classifying 24 years of Cluster measurements by determining in which region of the magnetosphere the satellites are located at any given time. This is not obvious as the shape and dimensions of these regions are constantly changing due to the interaction with the solar wind.
Localisation of the Cluster satellites
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The Cluster mission

The European Space Agency's (ESA) Cluster mission was launched in summer 2000. It consisted of 4 identical satellites orbiting Earth in a choreographed dance, aptly named Rumba, Salsa, Samba and Tango. The mission ended in September 2024 with the re-entry of Salsa in the Earth’s atmosphere; the others will follow in November 2025 and August 2026.

The goal of this mission was to study the interaction between the solar wind and the magnetic bubble surrounding the Earth, the magnetosphere. Cluster collected unique data on the Earth's magnetosphere and the near-Earth solar wind using 11 scientific instruments over a period of more than 24 years.  

Figure 1 Artist's impression of the Cluster constellation. ESA's mission Cluster consists of four identical spacecraft flying in formation between 19 000 and 119 000 km above the Earth. They study the interaction between the solar wind and Earth’s magnetosphere, or the Sun-Earth connection in 3D.
Figure 1 Artist's impression of the Cluster constellation. ESA's mission Cluster consists of four identical spacecraft flying in formation between 19 000 and 119 000 km above the Earth. They study the interaction between the solar wind and Earth’s magnetosphere, or the Sun-Earth connection in 3D.

The GRMB project

Thanks to their high-inclination elongated orbit, the Cluster spacecraft traversed almost all the regions of the magnetosphere. Since the shape and the size of the magnetosphere are continuously changing due to various space weather effects, knowing the position of the spacecraft is not sufficient to identify the region in which the satellite is situated.

Correctly classifying the measurements and identifying the corresponding regions and boundaries crossed by the Cluster satellites add value to the huge quantity of data acquired over more than 24 years. Being able to assign the data to specific magnetospheric regions enables statistical studies regarding the fundamental processes occurring in a particular region, such as plasmasphere refilling, reconnection at the magnetopause, turbulence or wave propagation in the magnetosphere.

ESA proposed a project whose goal was to do exactly this: the GRMB project, or Geospace Region and Magnetospheric Boundary dataset identification. This project started in October 2022 for a duration of 2 years under the responsibility of two partner institutes:  BIRA-IASB (Royal Belgian Institute for Space Aeronomy) in Brussels, Belgium  and  IAP (Institute of Atmospheric Physics) in Prague, Czech Republic. This project has been extended by 2 more years to include the Cluster data recorded in 2023 and 2024.

The GRMB dataset

The first step of the project consisted in defining the geospace regions that serve as categories for the classification, their properties, and the relevant Cluster data products to identify them. A tool has been developed to be used by human operators to manually identify the regions and the boundaries between them.

This manual classification, based on pre-generated plots of 44 Cluster data products coming from 6 different instruments, covers 15 labelled regions, spanning from the plasmasphere to the solar wind: 4 labels cover the regions outside the magnetosphere, 9 regions inside the magnetosphere, and 2 categories reflect data gaps or intervals where the classification cannot be made (mostly due to insufficient data). This classification has been thoroughly validated in several ways, e.g. by checking for some physical quantities whether their values are compatible with the region associated to it.

The GRMB dataset is now also publicly available in the ESA Cluster Science Archive.

This paper describes the methodology used to build this dataset in full details. It describes the validation of the approach through different types of comparisons. One check consists of comparing the GRMB locations of some specific magnetospheric features with their predicted positions.


Figure 2 Location of the bow shock and the magnetopause (top) from a prediction based on a simple model and (bottom) from the GRMB dataset for Cluster 1 in 2003. The bottom horizontal axis corresponds to the orbit number and the vertical axis to the location of the spacecraft along its orbit. (Credit: Grison et al., 2025)

An example is shown on Figure 2 for the bow shock (shock wave formed where the supersonic solar wind starts to deviate around the Earth’s magnetosphere) and the magnetopause (boundary between the Earth’s magnetosphere and the shocked solar wind) for Cluster 1 (Rumba) in 2003, highlighting that the GRMB locations and the expected positions match very well.

Figure 3 summarises how often each Cluster spacecraft visited the different regions between year 2001 and 2007. The first two years contain a larger proportion of N/A data as the mission was still operating in a non-continuous observation mode. From 2003 to 2007, the Cluster satellites spent ~40% of the time in the 4 regions located outside the magnetosphere and ~60% in the 9 regions located inside.

Figure 3 Frequency with which the geospace regions were visited by each of the 4 Cluster spacecraft from 2001 to 2007. The labels correspond to those of the GRMB dataset. The OUT label refers to regions located outside of the magnetosphere while the IN regions correspond to regions located inside the magnetosphere. (Credit: Grison et al., 2025)

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Plasma Physics
Physical Sciences > Physics and Astronomy > Plasma Physics
Magnetospheric Physics
Physical Sciences > Physics and Astronomy > Astronomy, Cosmology and Space Sciences > Planetary Science > Magnetospheric Physics
Magnetospheric Physics
Physical Sciences > Earth and Environmental Sciences > Earth Sciences > Planetary Science > Magnetospheric Physics

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