The JUpiter Icy Moons Explorer (JUICE) is a European Space Agency (ESA) mission dedicated to investigating Jupiter's icy satellites and Jovian environment. The mission will be launched in 2022 from Kourou, French Guyana, on an Ariane 5 and it will arrive in the Jovian system in 2029. The mission will perform a series of flybys of the icy moons Europa, Callisto and Ganymede before being inserted into a 9-month orbit around Ganymede. The Ganymede orbital phase is divided into a 5-month elliptical orbit (GEO) and a 4-month circular orbit at an altitude of approximately 500 km (GCO-500). JUICE is endowed with a suite of instruments that will investigate the moon's icy crust, interior structure, magnetic field, and exosphere. The 3GM (Geodesy and Geophysics of Jupiter and the Galilean Moons) experiment on board the spacecraft will exploit accurate Doppler and range measurements to determine the moons' orbits, gravity fields, tides and therefore infer features of their internal structures. In this paper, we compare the expected results of the nominal GCO-500 phase with a possible extended mission to a 200 km circular orbit (GCO-200). The simulations of the nominal mission (GCO-500) reveals that 3GM can provide a gravity map of the moon's up to degree and order 40. The Love number k2, modelling the tidal response, is determined with an accuracy of 10-4 (1-s), which will allow us to set a constraint on the internal structure of the moon. The obliquity, f, and the libration at orbital period, ?, can be retrieved with a level of uncertainty of 1 and 2 µrad, respectively. In this paper, we compare the expected results of the nominal GCO-500 phase with a possible extended mission to a 200 km circular orbit (GCO-200). At a lower altitude, the gravity field can be recovered up to degree and order 80, thus, revealing more details about the superficial structures with a resolution of 207 km at the equator. The potential effect of spacecraft drag due to Ganymede's tenuous exosphere, which ranges between 10-17 - 10-16 kg/m3, in the GCO-500 phase is very faint making not possible for 3GM to estimate it. During the extended mission, the drag becomes 2 orders of magnitude higher, thus, 3GM will be able to provide an estimation of the exospheric density.

JUICE's 3GM gravity experiment around ganymede - Comparison between nominal and extended mission / Cappuccio, P.; Benedetto, M. D.; Iess, L.. - (2020). (Intervento presentato al convegno 71st International Astronautical Congress, IAC 2020 tenutosi a Online).

JUICE's 3GM gravity experiment around ganymede - Comparison between nominal and extended mission

Cappuccio P.
Primo
;
Iess L.
Ultimo
2020

Abstract

The JUpiter Icy Moons Explorer (JUICE) is a European Space Agency (ESA) mission dedicated to investigating Jupiter's icy satellites and Jovian environment. The mission will be launched in 2022 from Kourou, French Guyana, on an Ariane 5 and it will arrive in the Jovian system in 2029. The mission will perform a series of flybys of the icy moons Europa, Callisto and Ganymede before being inserted into a 9-month orbit around Ganymede. The Ganymede orbital phase is divided into a 5-month elliptical orbit (GEO) and a 4-month circular orbit at an altitude of approximately 500 km (GCO-500). JUICE is endowed with a suite of instruments that will investigate the moon's icy crust, interior structure, magnetic field, and exosphere. The 3GM (Geodesy and Geophysics of Jupiter and the Galilean Moons) experiment on board the spacecraft will exploit accurate Doppler and range measurements to determine the moons' orbits, gravity fields, tides and therefore infer features of their internal structures. In this paper, we compare the expected results of the nominal GCO-500 phase with a possible extended mission to a 200 km circular orbit (GCO-200). The simulations of the nominal mission (GCO-500) reveals that 3GM can provide a gravity map of the moon's up to degree and order 40. The Love number k2, modelling the tidal response, is determined with an accuracy of 10-4 (1-s), which will allow us to set a constraint on the internal structure of the moon. The obliquity, f, and the libration at orbital period, ?, can be retrieved with a level of uncertainty of 1 and 2 µrad, respectively. In this paper, we compare the expected results of the nominal GCO-500 phase with a possible extended mission to a 200 km circular orbit (GCO-200). At a lower altitude, the gravity field can be recovered up to degree and order 80, thus, revealing more details about the superficial structures with a resolution of 207 km at the equator. The potential effect of spacecraft drag due to Ganymede's tenuous exosphere, which ranges between 10-17 - 10-16 kg/m3, in the GCO-500 phase is very faint making not possible for 3GM to estimate it. During the extended mission, the drag becomes 2 orders of magnitude higher, thus, 3GM will be able to provide an estimation of the exospheric density.
2020
71st International Astronautical Congress, IAC 2020
JUICE; planetary science; precise orbit determination; radio science
04 Pubblicazione in atti di convegno::04b Atto di convegno in volume
JUICE's 3GM gravity experiment around ganymede - Comparison between nominal and extended mission / Cappuccio, P.; Benedetto, M. D.; Iess, L.. - (2020). (Intervento presentato al convegno 71st International Astronautical Congress, IAC 2020 tenutosi a Online).
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11573/1542845
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