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Jupiter Icy Moons Explorer

The Jupiter Icy Moons Explorer () is a spacecraft mission led by the (ESA) to investigate the Jovian system, with a primary focus on characterizing Jupiter's three large ocean-bearing moons—, , and Callisto—as planetary bodies and potential habitats for life, while also exploring the planet's complex environment and its role as an archetype for gas giants. Launched on 14 April 2023 aboard an rocket from Europe's in , , JUICE is the first large-class mission in ESA's 2015–2025 program and involves contributions from (including the ultraviolet spectrometer instrument and hardware for other payloads) and (components for several instruments). The spacecraft, with a wet mass of approximately 6,000 kg and equipped with 10 scientific instruments plus the PRIDE radio experiment, relies on expansive arrays spanning about 85 m² for power generation during its eight-year cruise to . JUICE's mission objectives encompass detailed and in-situ measurements to assess the moons' subsurface oceans, icy surfaces, and geological evolution; to probe Jupiter's atmosphere, , and interaction with its satellites; and to evaluate the broader system as an analog for extrasolar planetary systems. The instruments include optical imagers like , spectrometers such as MAJIS and SWI, a laser altimeter (), radar (), (J-MAG), particle detectors (PEP), and radio/wave analyzers (RPWI), enabling comprehensive multispectral and particle observations. Following launch, JUICE's trajectory involves multiple gravity-assist maneuvers: a lunar-Earth flyby in August 2024, a flyby in August 2025, an flyby in September 2026, and a final flyby in 2029, before arriving at in July 2031 for a four-year phase. Upon arrival, the spacecraft will conduct about 35 close flybys of the icy moons, including multiple encounters with and Callisto, before entering orbit around in December 2034—the first spacecraft to orbit a moon other than 's—for dedicated close-up study until at least September 2035. As of November 2025, is en route to following its successful flyby in late August 2025, during which an onboard anomaly was resolved, and the instrument was confirmed operational; the mission is also scheduled to perform opportunistic observations of the interstellar comet 3I/ATLAS later in November 2025 using its cameras, spectrometers, and particle sensors. This mission complements NASA's , launched in October 2024, by providing overlapping data on the Jovian icy worlds to advance understanding of in our solar system.

Background and Development

Scientific Motivation

, as the largest planet in the Solar System and an for s, plays a pivotal role in understanding planetary formation processes and the emergence of habitable environments. Its massive gravitational influence shaped the early Solar System by influencing the distribution of material during accretion, and its , , , and Callisto—represent diverse outcomes of satellite formation around a , with the three outer moons emerging as prime examples of potential worlds. Exploration of these icy moons began with the and 2 flybys in 1979, which revealed highly reflective, icy surfaces on , , and Callisto, hinting at volatile-rich compositions but leaving key questions about their interiors unresolved, such as the presence of liquid water and internal dynamics. The Galileo mission, orbiting Jupiter from 1995 to 2003, provided transformative evidence for subsurface oceans beneath their icy crusts. For , Galileo's detected an induced signature consistent with a conductive, saline layer approximately 100 km beneath the surface, implying a global ocean of saltwater sustained by from orbital resonances with and . On , the largest moon in the Solar System, Galileo observations revealed both an intrinsic magnetic —unique among icy bodies—and an induced , supporting the existence of a subsurface ocean sandwiched between layers of ice and rock, with inferred from the . Callisto, the outermost moon, showed weaker but suggestive evidence of a deep, salty subsurface ocean through induced magnetic perturbations during Galileo flybys, potentially decoupled from the surface by a thick ice layer. These oceans are primarily energized by , where gravitational interactions with and mutual resonances among the moons generate internal friction, providing a source for geochemical processes. The Jovian system's unique magnetic interactions, including Jupiter's intense influencing moon-ionosphere coupling and auroral activity, further shape these environments, raising profound implications for by enabling possible chemical disequilibria and nutrient transport in the oceans. However, Voyager and Galileo data left critical gaps, such as the precise ocean depths, ice shell thicknesses, and the extent of water-rock interactions, motivating deeper investigation into whether these worlds could harbor or preserve biosignatures from the Solar System's formative epochs.

Mission Selection

The JUpiter ICy moons Explorer () emerged from the reformulation of the earlier Europa Jupiter System (EJSM/Laplace), a joint ESA-NASA proposal initially selected as a candidate large-class (L-class) under ESA's 2015-2025 program in 2009. Following NASA's decision to prioritize a separate Europa-focused , ESA initiated a reformulation study in 2011 to adapt the concept into a single European-led spacecraft targeting the Jovian system, particularly , , and Callisto. This reformulated JUICE proposal was developed by an international science team led by ESA, drawing on expertise from European institutions and early input from partners including and the Japanese Aerospace Exploration Agency (). In the competitive selection process for the L1 mission slot within , competed against two other mature concepts: the Advanced Telescope for High Energy Astrophysics () and the New (NGO, later evolved into ). Phase A studies for the original Laplace concept, conducted from 2008 to 2011, provided foundational assessments of scientific objectives, feasibility, and cost, informing the reformulation during its dedicated assessment phase (Phase 0/A) completed in early 2012. ESA's Programme Committee () approved as the L1 mission on 17 April 2012, with the selection publicly announced on 2 May 2012, recognizing its alignment with themes on and system formation. The mission received an initial budget allocation of approximately €830 million for development and operations, enabling progression from selection to launch preparation over the subsequent decade. Key post-selection milestones included payload instrument selection in 2013, formal adoption by the ESA Member States in November 2014, and entry into the implementation phase (Phase B/C/D) in 2015, culminating in launch on an rocket from , , on 14 April 2023. International partnerships solidified during this period, with providing the ultraviolet spectrometer (UVS) and science instruments, contributing the particle environment package subsystem, and additional support from the Canadian Space Agency () and for specific instruments.

Engineering and Collaboration

Following its selection as part of ESA's programme in 2012, the (JUICE) mission entered a detailed phase led by the (ESA), with selected as the prime contractor in July 2015 under a €350 million contract to handle , development, integration, testing, and launch preparations. This effort involved a global collaboration of 83 companies and 18 institutions from 23 countries, encompassing over 2,000 personnel who contributed to the spacecraft's assembly and scientific payload. Key international contributions included NASA's provision of the Ultraviolet Imaging Spectrograph (UVS) instrument, developed by the and delivered in 2021, along with subsystems for two ESA-led instruments: the Radar for Icy Moons Exploration () and the Particle Environment Package (PEP). The Japan Aerospace Exploration Agency () supplied hardware components for four instruments—Ganymede Laser Altimeter (), Submillimetre Wave Instrument (SWI), Radio and Plasma Wave Investigation (RPWI), and PEP—facilitating enhanced and surface studies during the mission. ESA's core project team, based at the agency's ESTEC facility in the , oversaw overall integration, mission operations planning, and coordination among partners, ensuring alignment with scientific objectives for Jupiter's and icy moons. Engineering challenges centered on preparing the for Jupiter's intense environment, where charged particles in the planet's can damage electronics; solutions involved radiation-hardened components, such as shielded processors and redundant systems, tested to withstand doses up to 300 krad over the mission lifetime. Additionally, deployment mechanisms for antennas and booms faced ground-test hurdles, which were resolved through design modifications and iterative testing to ensure reliable in-space extension. These efforts were part of broader risk mitigation for the harsh outer Solar System conditions, including low solar intensity requiring large solar arrays. The development culminated in rigorous testing phases at Airbus facilities in , , where the fully assembled spacecraft underwent vibration tests in early 2022 to simulate launch stresses from the rocket, followed by thermal vacuum tests from mid-2022 through year-end to replicate space's temperature extremes (-180°C to +120°C) and vacuum conditions, confirming operational integrity before shipment to the launch site in . These phases validated the spacecraft's resilience, paving the way for its successful launch on April 14, 2023.

Spacecraft Design

Overall Configuration

The Jupiter Icy Moons Explorer () features a compact, cuboidal architecture optimized for the demanding journey to and its moons, with a stowed configuration measuring approximately 4.1 m in height and 2.9 m in width, excluding deployed appendages. The total launch mass is 6,100 kg, which includes 3,650 kg of propellant for propulsion maneuvers, enabling the spacecraft to perform multiple assists and orbital insertions over its 8-year and phases. This design emphasizes structural integrity and thermal management in the deep-space environment, drawing on heritage from previous ESA missions while incorporating enhancements for Jupiter's and low solar flux. JUICE employs a modular comprising a central service module for core subsystems, a payload platform accommodating scientific instruments, and two large wings spanning 85 m² in total area to generate power in the dim at Jupiter's distance from . The wings, each consisting of five panels measuring about 2.5 m by 3.5 m, deploy to a tip-to-tip width of roughly 27 m, providing an average of 850 W of electrical power at end-of-mission while allowing for yaw steering to maximize efficiency during nominal operations. This configuration supports the spacecraft's 3-axis stabilization, with the service module housing propulsion tanks, batteries, and avionics below the platform to facilitate integration and testing of the 10-instrument suite. To withstand Jupiter's intense radiation belts, JUICE incorporates specialized shielding, including layers of for spot protection of critical electronics and overall vaults that limit total ionizing dose to under 50 krad over the mission lifetime. These measures, combined with radiation-hardened components and trajectory planning to avoid the innermost belts, ensure operational reliability for the sensitive instruments and data systems. Following launch aboard an rocket in April 2023, the deployment sequence commences in , beginning with the extension of the two solar wings over several days to their full span, followed by the unfurling of instrument-specific appendages such as the 10.6 m boom, 16 m antenna, and 3 m booms. The 2.5 m High Gain Antenna and medium-gain antennas are then deployed to establish communication links, with all mechanisms verified through ground simulations to mitigate risks in the vacuum of . This phased rollout transitions the spacecraft from its compact launch posture to a fully operational configuration ready for the interplanetary cruise.

Power and Propulsion Systems

The power system of the Jupiter Icy Moons Explorer () is designed to provide reliable for its eight-year journey to and subsequent operations in the low-solar-intensity , where sunlight is approximately 25 times weaker than at . The primary consists of two deployable solar array wings, each comprising five panels for a total area of 85 m² equipped with (GaAs) solar cells numbering 23,560. These arrays generate about 850 of electrical at , sufficient to support the 's subsystems, instruments, and needs during nominal operations. To ensure continuity during periodic eclipses behind or its moons, which can last up to 4.8 hours, JUICE incorporates five modules acting as a rechargeable bank. These batteries store energy from the solar arrays during illuminated periods and deliver during shadow transits, maintaining full functionality for critical tasks such as and adjustments. The overall power budget is managed through a power conditioning and distribution unit that regulates voltage and prioritizes loads, enabling efficient allocation across the mission phases. The subsystem employs a chemical bi-propellant to achieve the high delta-v requirements of approximately 2,700 m/s for interplanetary , insertions, and moon flybys. The main engine, a 425 N bipropellant using monomethyl hydrazine (MMH) fuel and (MON) oxidizer, handles major trajectory corrections and the Ganymede insertion. Complementing this are smaller (RCS) —eight 22 N and twelve 10 N units—also bipropellant, for precise attitude control, wheel off-loading, and fine orbital adjustments. The total load of 3,650 kg of MMH/ supports these operations without relying on electric , prioritizing high-thrust impulses over for the mission's demanding gravitational maneuvers. This configuration contributes to the spacecraft's overall wet of about 6,000 kg, balancing capability with structural constraints.

Communication and Data Handling

The JUICE spacecraft's communication system relies on a fixed 2.5-meter diameter high-gain (HGA) to transmit , scientific , and perform radio science experiments, while also serving as a sunshield during certain maneuvers. This operates in X-band and Ka-band frequencies for both uplink commands and downlink , enabling a transfer rate exceeding 2 gigabits per day to ground stations under optimal conditions. A steerable medium-gain provides backup capability for routine operations and safe-mode communications. At Jupiter's distance, where signal is significant due to the vast separation of over 600 million kilometers, the effective downlink rate is projected to average around 43 kilobits per second, sufficient for returning key observations while prioritizing high-value . The onboard data handling subsystem centers on a robust central software that manages command execution, generation, and autonomous fault recovery, supported by radiation-hardened processors designed for the intense Jovian environment. Dual-redundant solid-state mass memory provides 1.25 terabits of storage capacity, equivalent to about 156 gigabytes, allowing accumulation of several days' worth of science data during non-contact periods caused by communication blackouts or high-priority observations. Data flows through a network connecting the 10 instruments to this memory, ensuring efficient prioritization and packaging of payloads before transmission. To bridge the gap between the instruments' high-volume output—potentially reaching several gigabits per second during simultaneous , , and operations—and the constrained downlink bandwidth, advanced data algorithms are integrated into the payload processing units. These algorithms, including lossless and lossy techniques tailored to specific data types like hyperspectral images and particle measurements, reduce file sizes by factors of 2 to 10 while preserving scientific fidelity, thereby optimizing storage and transmission efficiency. Mission operations are coordinated from ESA's (ESOC) in , , which handles spacecraft commanding, trajectory monitoring, and data reception via the agency's deep-space antenna network. In cases of network overload or enhanced tracking needs, NASA's Deep Space Network (DSN) antennas in , , and provide supplementary support under international cross-support agreements, ensuring uninterrupted links throughout the eight-year journey.

Launch and Cruise Phase

Launch Details

The Jupiter Icy Moons Explorer () mission lifted off on April 14, 2023, from Europe's Spaceport at the in , , aboard an ECA rocket designated as flight VA260. The launch occurred at 12:14 UTC, successfully injecting the into a hyperbolic escape trajectory relative to . The upper stage delivered to an escape with a () of approximately 121 km²/s², equivalent to a hyperbolic excess of about 11 km/s, enabling the start of its eight-year cruise to the system. Ion propulsion was activated the following day on April 15 to begin low-thrust adjustments, supporting the mission's gravity-assist . Post-launch activities commenced immediately after separation, with acquisition confirmed via ESA's New Norcia about 50 minutes after liftoff. The 's large solar arrays, spanning 27 meters in length and providing approximately 850 watts of at Jupiter's , were successfully deployed roughly one hour after launch, verifying full electrical functionality. Over the ensuing days, the initial checkout phase proceeded nominally, including the extension of the 10.6-meter boom on April 21 to position sensors away from interference. All critical systems, including , , and , were validated as operational during this period. The 2023 launch window for JUICE spanned April 5 to 25, a 21-day interval dictated by planetary alignments necessary for the mission's double Venus-Earth-Earth gravity-assist to optimize and arrival timing at in July 2031. Backup opportunities within 2023 were limited to the remaining days of this window, with subsequent periods available in 2024 if delays occurred.

Gravity Assist Maneuvers

The Jupiter Icy Moons Explorer (JUICE) mission employs a series of gravity assist maneuvers, also known as slingshot trajectories, to efficiently alter its path and velocity toward Jupiter without significant fuel expenditure. These maneuvers leverage the gravitational pull of planets to "steal" orbital momentum, enabling the spacecraft to reach the outer Solar System after launch from Earth. The sequence is designed to minimize the delta-V requirements on the spacecraft's propulsion system, which relies on bipropellant chemical thrusters for major corrections and radio-frequency ion thrusters for fine adjustments, providing a total capability of approximately 2.7 km/s across the mission. The interplanetary cruise phase begins with a double flyby of the Earth-Moon system on August 19–20, 2024, marking the first-ever lunar-Earth . JUICE approached the Moon from the night side at an altitude of about 750 km, using its gravity to slightly redirect the trajectory, followed by an Earth flyby at 6,840 km altitude over and the . This maneuver reduced the spacecraft's heliocentric velocity by 4.8 km/s relative to , setting it on course for while allowing instrument calibration and opportunities. The next maneuver was a Venus flyby on August 31, 2025, at a periapsis altitude of 5,088 km above the planet's surface. This increased JUICE's velocity, redirecting it back toward for subsequent encounters while testing the spacecraft's thermal protection against the intense solar proximity—Venus was at about 0.72 AU from . The flyby was executed flawlessly after resolving a pre-encounter communications , confirming the trajectory adjustment with no deviation. Future maneuvers include a second Earth flyby in September 2026, planned at an altitude of around 3,700 km to further boost outbound velocity, and a third flyby in 2029 at approximately 150,000 km to fine-tune the final approach. These assists, combined with mid-course corrections totaling about 1.6 km/s from the propulsion system, ensure arrival at on July 14, 2031, with sufficient margins for the science phase. Navigation for these maneuvers relies on precise ground-based tracking via ESA's network of deep-space antennas, which monitor JUICE's position to within meters using ranging and Doppler measurements. Real-time adjustments to aim points are computed during each flyby, as demonstrated in the lunar-Earth event where optical and onboard cameras refined the path to achieve the targeted velocity change. This precision is critical, as even small errors in flyby geometry could propagate to miss the window. Risk mitigations include contingency planning for solar conjunction periods, where the Sun-Earth-spacecraft alignment disrupts communications for up to two weeks; during the approach in mid-2025, teams prepared for potential blackouts by uploading autonomous commands and prioritizing thermal management to withstand solar fluxes up to 6 times Earth's levels. Redundant systems and pre-flyby simulations ensured resilience, with no mission impacts observed.

In-Flight Operations and Status

Following the successful gravity-assist flyby on August 31, 2025, at a closest approach of approximately 5,088 km above the planet's surface, the Jupiter Icy Moons Explorer () spacecraft confirmed its trajectory remains on course for subsequent maneuvers, with initial post-encounter data indicating nominal performance of key systems. In early November 2025, JUICE commenced planned observations of the interstellar comet 3I/ATLAS, conducting remote sensing campaigns from November 2 to 25 at a minimum distance of 0.428 AU, utilizing its JANUS camera, MAJIS near-infrared spectrometer, and other instruments to capture images, spectral data, and particle measurements for calibration and opportunistic science. The mission has encountered and resolved several anomalies during cruise. Shortly after launch in April 2023, the 16-meter Radar for Icy Moons Exploration (RIME) antenna experienced a deployment issue due to a stuck pin, which engineering teams addressed through targeted maneuvers and diagnostics, achieving full extension on May 12, 2023. More recently, in August 2025 ahead of the flyby, a software caused a temporary loss of contact, placing the in a ; this was swiftly resolved by uploading a patch, restoring full operations without impact to the timeline. Routine health and performance monitoring as of November 2025 reports all propulsion systems, including the 12 thrusters, functioning at 100% efficiency, with no degradation observed during trajectory corrections or attitude adjustments. Cruise-phase activities include ongoing instrument calibrations leveraging flybys and stellar fields, with preparations for early remote observations of the system, such as distant imaging campaigns using the and UVS instruments, scheduled to begin in 2029 following the final Earth .

Science Mission at Jupiter

Arrival and Orbital Phases

The JUICE spacecraft is scheduled to arrive at the Jupiter system in July 2031 after an eight-year cruise phase involving multiple gravity assists. Upon approach, the mission's Jupiter orbit insertion (JOI) will occur on 20 July 2031, primarily utilizing the spacecraft's chemical bi-propellant propulsion system for a major burn of approximately 900 m/s delta-V at perijove, augmented by a close flyby to achieve capture without excessive propellant use. This maneuver will place JUICE into an initial highly elliptical capture extending to about 11 million kilometers from , equivalent to roughly 150 Jupiter radii, allowing for preliminary of the planet and its over an extended period of several months. Following , the spacecraft will employ its radio-frequency thrusters (RIT-22) for gradual orbit reduction, providing a low-thrust delta-V of around 200 m/s distributed over months to from the large capture to a more manageable elliptical path with an apoapsis of approximately 250,000 km and periapsis near 4,000 km. This phase, lasting about 500 days in the initial wide before full reduction, enables efficient energy management while minimizing radiation exposure during early operations. Over the subsequent 35 elliptical around , spanning roughly 3.5 years in the system, will conduct broad surveys of the Jovian environment, including magnetospheric mapping and distant moon observations. To phase into targeted moon encounters, the mission will leverage resonant orbits with and Callisto, such as 38:1 and 8:1 resonances, combined with precise gravity assists to adjust inclination and periapsis without large expenditures. These resonant strategies facilitate a smooth progression from planet-centered orbits to moon-centric tours, optimizing science return across the satellites over the mission's nominal duration. The nominal mission will conclude in September 2035 with a controlled deorbit and impact on 's surface to prevent unintended contamination of other moons.

Moon Flyby Sequence

The Jupiter Icy Moons Explorer () mission's Jovian tour features a sequence of 35 flybys across , Callisto, and to gather data on their surfaces, compositions, and environments while adjusting the spacecraft's trajectory for subsequent phases. These flybys total two for , 21 for Callisto, and 12 for , enabling repeated observations without entering prolonged high-radiation zones near . The sequence begins shortly after Jupiter orbit insertion in July 2031 with a Ganymede flyby on 31 July 2031 to aid capture, followed by additional Ganymede and Callisto encounters. The two targeted Europa flybys will occur on 2 July and 16 July 2032 during a dedicated one-month phase focused on this moon's non-ice materials and subsurface ocean indicators. These flybys approach at altitudes of approximately 400 km, allowing high-resolution imaging at better than 50 m/pixel over regions of interest, such as middle latitudes in both hemispheres, and sampling of potential plume particles in the wake. Callisto flybys commence on 21 June 2032 and continue through 2034, totaling 21 encounters primarily used for gravity assists to tweak the orbit inclination up to 30 degrees and enable polar views of Jupiter; initial passes occur at 1,000–2,000 km altitudes, with later ones reduced to over 200 km for regional-scale mapping at 400 m/pixel and selected high-resolution targets under 100 m/pixel. Ganymede flybys occur throughout the Jupiter tour, with 12 encounters at altitudes ranging from 20,000 to 45,000 km initially, narrowing to closer approaches including some at around 400 km for detailed surface and measurements. These passes reduce the spacecraft's velocity for orbit insertion while capturing global imaging at 500–1,000 km resolutions and in-situ particle data to characterize 's induced and subsurface structure. The sequence integrates high-resolution during illuminated approaches and fields/particles for wake sampling across all moons, prioritizing during the ~2-hour closest approach windows. Mission planners have incorporated contingencies for potential failures, such as radiation-induced anomalies or errors, including flyby targeting strategies with re-phasing maneuvers and adjustments within 4.9–5.5 km/s tolerances to avoid hazards like collisions (risk below 10^{-4}). If primary sequences are compromised, alternative Callisto or assists can substitute for trajectory corrections, with data downlink prioritized via file selection to manage the ~150 Gbit volume per Europa flyby. These measures ensure robust execution of the tour leading into orbit insertion in late October 2034.

Ganymede Orbit Insertion

The Ganymede Orbit Insertion (GOI) marks the culmination of the () mission, representing the first dedicated orbital mission around a moon beyond . Scheduled for 31 2034, the insertion will be achieved through a braking maneuver utilizing approximately 185 m/s of delta-V, transitioning the from a transfer trajectory into an initial highly elliptical around with a period of about 12 hours. This orbit, inclined at roughly 86 degrees to Ganymede's equator, will enable polar coverage and set the stage for a comprehensive nine-month orbital ending in September 2035. Following insertion, the mission will execute a series of orbital adjustments to progressively lower the pericenter and circularize the , optimizing scientific returns while conserving . The sequence begins with an elliptical lasting about 30 days, followed by a high-altitude at 5,000 km for 90 days to conduct broad surveys with reduced . Subsequent elliptical transfers will lead to a medium-altitude at 500 km altitude for approximately 102 days, providing detailed global mapping. If sufficient fuel remains, the will be further decayed to a low-altitude at 200 km for 30 days to acquire high-resolution data on surface features and subsurface structures, culminating in a controlled impact on to prevent uncontrolled reentry and potential contamination. This decay strategy balances scientific priorities with the mission's limited of around 2,700 m/s total capability. The orbital phase will enable unprecedented continuous monitoring of the moon's subsurface ocean and its induced , leveraging JUICE's suite of instruments for in-depth characterization. By maintaining prolonged proximity, the spacecraft will use magnetometers and radio experiments to detect electromagnetic signatures of the conductive ocean layer beneath the ice shell, revealing its depth, , and interaction with Jupiter's . This sustained observation will also track variations in the induced over multiple rotations, providing insights into ocean dynamics and 's unique intrinsic —the only known instance of a moon generating its own . Operational challenges during the Ganymede orbit stem primarily from the intense radiation environment within 's , which poses risks to electronics and instruments despite 's relatively outer position. is designed with radiation-hardened components and shielding vaults capable of withstanding up to 300 krad total dose, but the cumulative exposure—estimated at several gigarads for exposed elements—will necessitate periodic instrument safe modes or shutdowns during high-flux periods near pericenter to protect sensitive detectors like those in the imaging and particle instruments. Additionally, constraints from the arrays, delivering about 850 at , and limited data downlink rates of 1.4 Gb/day will require meticulous scheduling to prioritize ocean and observations amid these hazards.

Scientific Objectives

Jupiter System Characterization

The Jupiter Icy Moons Explorer (JUICE) mission seeks to characterize the Jupiter system as an archetype for environments, emphasizing the planet's atmosphere, , and overarching dynamics to understand their influence on the surrounding moons. This involves multi-wavelength observations spanning , visible, , and radio spectra to probe atmospheric phenomena such as auroras, which reveal coupling between the , , and interactions. Similarly, monitoring of storms and circulation patterns will provide insights into meteorological processes and from the cloud tops to the , enabling models of long-term variability over the mission's extended orbital phases. These efforts aim to quantify how Jupiter's dynamic environment shapes planet-moon interactions, including the deposition of material from the planet onto the icy satellites. A key aspect of the characterization involves detailed study of Jupiter's , utilizing long-baseline magnetometry to map three-dimensional field variations and flows within the magnetodisc. This will elucidate the 's response to forcing and internal sources, including contributions from the moons' exospheres and Io's volcanic activity, which influences loading and affects distant satellites like . Observations of belts will assess their structure, intensity, and temporal evolution, highlighting their role in surface alteration and hazards for the icy moons. By integrating these measurements, JUICE will model the magnetospheric circulation and its feedback loops with the planetary atmosphere, providing a comprehensive view of processes. Exosphere analysis forms another pillar, focusing on the tenuous atmospheres of the to trace links between Io's intense and material transport across the system, such as sulfur and oxygen ions impacting Europa's surface. This characterization extends to gravitational and tidal interactions, examining long-term orbital evolution and resonant dynamics among the moons that stabilize their configurations. Through comparative planetology, the mission will evaluate how 's atmospheric circulation, magnetic field strength, and radiation environment modulate the habitability potential of the icy moons by influencing surface processes and external inputs. Instruments like MAJIS (Moons and Jupiter Imaging Spectrometer) and the J-MAG will support these objectives by providing contextual data on system-scale phenomena.

Icy Moon Habitability

The mission evaluates the potential of Jupiter's —Europa, , and Callisto—by characterizing subsurface liquid reservoirs, internal energy sources, and surface-subsurface material exchange, key ingredients for as we know it. These assessments draw on the moons' shared traits as ocean worlds, where global subsurface may interact with interiors and icy surfaces, fostering conditions for chemical disequilibria and nutrient cycling. By integrating , in-situ analysis, and geophysical modeling, addresses whether these environments could support microbial , prioritizing the stability and composition of their water layers over geological timescales. A primary focus is ocean detection through radar sounding of the ice shells, using the RIME (Radar for Icy Moon Exploration) instrument to penetrate the subsurface and map stratigraphy. RIME operates at 9 MHz to probe depths of up to approximately 9 km on Europa, Ganymede, and Callisto, enabling detection of ice-ocean interfaces and constraints on shell thickness. Current models estimate ice shell thicknesses ranging from 10 to 100 km across these moons, with thinner shells on Europa (around 10-30 km) and thicker ones on Ganymede and Callisto, implying substantial water volumes potentially exceeding Earth's oceans in total. These observations will refine water volume estimates by identifying salinity and conductivity signatures, confirming ocean presence and extent essential for habitability. JUICE also investigates energy budgets to determine if internal heat sustains liquid states and drives geochemical processes. Tidal dissipation models, informed by JUICE's and radio , predict heating rates of 10^{12} to 10^{14} W in Europa's rocky and , arising from orbital resonances that flex the moon's interior. This heat flux, combined with radiogenic contributions, could maintain in the ocean and ice shell, cycling nutrients and organics; similar but lower-energy effects apply to and Callisto, where JUICE will quantify dissipation via orbital dynamics and surface deformation measurements. These energy estimates establish the moons' capacity for long-term by powering potential hydrothermal vents at ocean floors. Surface composition mapping further probes by identifying chemical building blocks exchanged with subsurface . Instruments like MAJIS (Moons and Jupiter Spectrometer) will spectrally map non-ice materials, including salts (e.g., sodium chlorides and sulfates), organics, and potential precursors across the moons' terrains. On , targets plume deposits— and particles vented from the —for in-situ analysis of dissolved , revealing ocean chemistry and organic inventory. These mappings highlight endogenic activity linking surface and , with hydrated salts indicating recent and organics suggesting prebiotic synthesis pathways. Callisto's stands out due to its orbital position beyond Jupiter's intense belts, experiencing low fluxes that preserve ancient crustal layers and potential interfaces. This stability minimizes surface alteration, allowing to probe a fossilized record of early evolution through RIME sounding and compositional analysis, contrasting with the dynamically active environments of inner moons. Low here implies reliance on radiogenic sources for maintenance, offering insights into quiescent habitable zones.

Ganymede Magnetic Field

possesses the Solar System's only known intrinsic generated by a , arising from action within its metallic . The Jupiter Icy Moons Explorer () mission will characterize this field during dedicated orbital phases around , utilizing the J-MAG to map its structure and strength with high precision. This intrinsic field, with an equatorial surface strength of approximately 720 nT, interacts dynamically with Jupiter's dominant magnetosphere, creating a complex dual-layer magnetic environment. A key aspect of JUICE's investigation involves the induced magnetic field generated by Ganymede's subsurface saltwater , which acts as a conductor interacting with the rapidly varying Jovian . As Jupiter's rotates relative to , it induces electric currents in the ocean via Faraday's law of , producing secondary magnetic fields that oppose and modify the primary ones. JUICE's surveys during close orbits will resolve these induced signatures, enabling models to constrain the ocean's electrical conductivity, estimated at around 1 S/m, which corresponds to a level supporting potential . These measurements will also elucidate the dynamo mechanism powering Ganymede's intrinsic , likely driven by convective motions in a liquid iron-rich core beneath the rocky mantle. By separating the core-generated from induced components, JUICE data will refine models of the moon's internal structure, including core size and composition, providing insights into the generation process that sustains the 720 nT against external perturbations.

Instrument Payload

Remote Sensing Instruments

The instruments aboard the Icy Moons Explorer () form a sophisticated suite for observing the surfaces, subsurfaces, atmospheres, and exospheres of and its —Europa, , and Callisto—without physical contact. These tools, including cameras, spectrometers, a sounder, an spectrograph, a altimeter, and a submillimeter wave instrument, enable high-resolution , compositional , profiling, and detection of buried structures such as potential subsurface oceans. By capturing data across to submillimeter wavelengths and radio frequencies, they support investigations into geological processes, indicators, and atmospheric dynamics. The (Jovis, Amorum ac Natorum Undique Scrutator) camera system serves as the primary optical imager, delivering panchromatic and multispectral images to study global morphology, local geologic features, and processes on the icy moons, as well as Jupiter's cloud layers, rings, and small moons like . Operating in the visible to near-infrared range of 350–1050 , it employs a 25 cm aperture with a of 1.72° × 1.29° and a detector equipped with 13 narrow-band filters to detect elements such as , salts, and rock-forming minerals. Resolutions reach up to 2.4 m/pixel during orbit for high-resolution targets, 400 m/pixel for global mapping of , and approximately 10 km/pixel at , enabling and digital terrain models in synergy with other instruments. Led by Pasquale Palumbo of the University of , will acquire around 2500 full-resolution images covering about 1% of 's surface to reveal cratering history, tectonic structures, and evidence of cryovolcanism. The MAJIS (Moons and Jupiter Imaging Spectrometer) is a hyperspectral imager designed to characterize the composition of surfaces, including , organics, salts, and minerals, while profiling 's atmospheric constituents, cloud features, and aurorae. It covers a broad spectral range from 0.4 to 5.7 μm across visible, near-, and channels, with 1280 spectral bands and resolutions of 3.66–6.51 nm, achieving spatial resolutions down to 25 m/ on and up to 100 km/ for 's global views via a 3.4° in push-broom or modes. With a high exceeding 100, MAJIS will produce approximately 90 spectral cubes to map non- components and track tropospheric dynamics, supporting assessments of moon through detection of hydrated salts and organic residues. François Poulet of the Institut d'Astrophysique Spatiale oversees this instrument, which operates without yaw steering for nadir-pointed observations. The RIME (Radar for Icy Moon Exploration) radar sounder probes the subsurface structures of the icy moons to depths of up to 9 km, aiming to identify ice-water interfaces, warm ice pockets, and evidence of global oceans beneath Ganymede, Europa, and Callisto. Operating at a center frequency of 9 MHz (with bandwidth up to 3 MHz and range 9–26 MHz), it uses a 16 m nadir-looking dipole antenna deployed on the spacecraft's anti-Jovian side, providing vertical resolutions of 50 m in high-resolution mode or 140 m in low-resolution mode, and horizontal resolutions from 0.3 to 10 km. During Ganymede's 500 km orbit and moon flybys, RIME penetrates icy crusts to map dielectric properties and layering, integrating with surface data from JANUS and altimetry for contextual analysis of ocean salinity and thickness. Principal investigator Lorenzo Bruzzone of the University of Trento leads this effort, which will generate detailed stratigraphic profiles to inform models of moon interiors and geological evolution. Provided by , the UVS (Ultraviolet Spectrograph) investigates the composition, structure, and dynamics of exospheres, tenuous atmospheres, and aurorae on the icy moons and , including searches for plumes and magnetospheric interactions. Sensitive to far-ultraviolet wavelengths of 55–210 with spectral resolutions below 0.6 , it features a of 0.1° × 7.3° for imaging and a narrower 0.2° × 0.2° slit for occultations, enabling spatial resolutions of about 0.5 km/pixel on . UVS performs stellar and solar occultations, limb scans, and semi-continuous ground-track scanning for up to 16 hours per day, offering 1–2 orders of magnitude higher sensitivity than prior Galileo instruments to detect trace gases like atomic oxygen and . Weighing 18 kg and consuming 7.5 W, this compact device, led by principal investigator Randy Gladstone of , will cover up to 73.5% of moon surfaces in focused observations to reveal processes and plume activity. The Laser Altimeter () maps topography and derives ice shell thicknesses to support geophysical investigations of the icy moons' surfaces and interiors. Operating at a 1064 nm with a Nd:YAG laser emitting 17 mJ pulses at 30 Hz (up to 50 Hz), it achieves a ~40-50 m spot size and 0.1 m vertical resolution at 200 km altitude. German-led by the (DLR), GALA uses a 25 cm to time-of-flight measure surface elevations, enabling response analysis tied to subsurface conductivity from magnetic data. The Submillimeter Wave Instrument (SWI) is a spectrometer for remote observations of atmospheric trace gases and exospheres on and the icy moons. Operating in two bands—530–625 GHz and 1080–1275 GHz—SWI achieves a of up to 10^7, allowing identification of such as H₂O, , and PH₃ at volume mixing ratios as low as 10^{-9}. Its acousto-optical spectrometer backend processes signals in real time, with a 2.5 MHz instantaneous per , enabling mapping of vertical profiles and during flybys. SWI's includes cooled receivers (down to 80 ) for low noise, making it suitable for faint emissions from moon exospheres and potential plumes.

Fields and Particles Instruments

The Fields and Particles Instruments on the Icy Moons Explorer () mission form a critical suite for probing the dynamic electromagnetic environment of and its icy moons, including interactions, composition, and wave phenomena that influence moon habitability. These instruments enable in-situ measurements during orbital phases around the planet and dedicated moon encounters, providing data on how 's couples with Ganymede's internal dynamo, as referenced in the mission's objectives. The JUICE Magnetometer (J-MAG) measures three-dimensional magnetic field vectors to characterize Jupiter's global magnetosphere, its variability, and interactions with Ganymede's induced field during orbit insertion. It consists of two fluxgate magnetometers—one inboard and one outboard—plus a scalar magnetometer (MAGSCA) for absolute field strength, all mounted on a 10.6-meter deployable boom to minimize spacecraft interference. This configuration achieves high-precision vector measurements across a wide dynamic range, supporting detection of subsurface ocean signatures through magnetic anomalies on icy moons. Led by Imperial College London with international collaboration, J-MAG operates continuously to map field topologies essential for understanding plasma-moon interactions. The Particle Environment Package (PEP) investigates the and populations in Jupiter's and their exchanges with the icy moons' atmospheres and surfaces. This NASA-contributed suite includes six sensors: the Jovian Plasma Dynamics and analyzer (JDC) for low-energy ions, Jovian Energetic Electrons (JoEE) and Ions (JENI) for high-energy particles, Jovian Electrons and Ions analyzer (JEI) for mid-range electrons and ions, Neutral and Ion Mass spectrometer (NIM), and Jovian Neutral Analyzer (JNA) for energetic neutrals. PEP covers energy ranges from below 0.001 to over 1 MeV for electrons and ions, with mass resolution exceeding 1000 and full 4π angular coverage, enabling analysis of pick-up ions and moon-sourced particles. Swedish-led with co-leadership, it quantifies particle fluxes to reveal and charge exchange processes at moon interfaces. The Radio and Plasma Wave Investigation (RPWI) detects electromagnetic waves and plasma densities to study radio emissions from Jupiter's aurorae and decametric radiation, as well as Langmuir waves in the magnetosphere. It features four Langmuir probes for electric field and density measurements, a search coil magnetometer (SCM) for magnetic fluctuations, and radio antennas including three dipoles on the 10.6-meter boom, supported by receivers such as GANDALF (low-frequency), MIME (medium), FRODO (DC fields), and JENRAGE (high-frequency imaging). RPWI spans frequencies from DC to 45 MHz, with radio spectrum coverage from 80 kHz to 45 MHz at up to 100 Msamples/second, allowing triangulation of emission sources and plasma wave-particle interactions. Swedish-led, it complements particle data by identifying wave-driven acceleration regions near the moons.

In-Situ Analyzers

The in-situ analyzers on the mission enable direct characterization of the chemical composition of exospheres, plumes, and surface-ejected materials from Jupiter's icy moons, providing critical data on and geological processes. These instruments focus on close-range sampling during flybys and orbits, distinguishing them from techniques by their ability to analyze and ionized at the spacecraft's or through onboard radio measurements. The primary suite for particle measurements is the Particle Environment Package (PEP), which includes sensors optimized for the tenuous environments around , , and Callisto, complemented by geophysical radio instruments. The Neutral Gas and Ion Spectrometer (), a component of PEP, is a time-of-flight (TOF) mass spectrometer designed to measure the chemical, , and isotopic of neutral gases and ionospheric ions in the exospheres of the icy moons. It features an ion mirror for enhanced and operates across a (m/z) range of 1 to 650 amu, achieving a mass of at least 500 () to distinguish key like , oxygen, and hydrocarbons derived from surface , , or . employs two ionization modes: an for direct sampling of high-speed neutrals during flybys (with a 300° azimuthal ) and a closed source for thermalized (covering 10/3 π steradians), enabling sensitivity down to densities of 10^4–10^6 particles per cm³. Electron impact at 70 is used, with radiation-hardened components ensuring operation in Jupiter's intense environment; the instrument's dynamic range spans nearly six orders of magnitude, supporting isotopic ratio measurements essential for tracing volatile origins and processes. The 3GM (Gravity & Geophysics of Jupiter and Galilean Moons) instrument uses the spacecraft's radio system for Doppler and range measurements to characterize the gravity fields, internal structures, and tidal responses of and its moons, aiding detection of subsurface . It comprises a Ka-band (KaT), ultrastable oscillator (USO), and high-accuracy (HAA), enabling precision tracking of mass distribution and atmospheric/ionospheric properties during flybys and orbits. Led by an international team, 3GM will provide data on moon densities and ocean depths, integrating with other instruments for habitability assessments. The Planetary Radio Interferometer and Doppler Experiment () enhances positioning and science return using ground-based (VLBI) on JUICE's radio signals for high-precision Doppler shifts and lateral position measurements. It supports gravity experiments, ephemerides improvement, and plasma density mapping without dedicated onboard hardware, relying on the spacecraft's telecommunication system. Coordinated by ESA's Deep Space Antenna Network, PRIDE will refine moon orbits and contribute to joint analyses with NASA's . While dedicated dust impact analyzers like a time-of-flight elemental composition sensor were proposed in early mission concepts (e.g., for surface-derived grains), the final JUICE payload relies on PEP's energetic particle sensors, such as the Jovian Energetic Neutrals and Ions (), to indirectly sample dust-related ions and neutrals from impacts and , with insights derived from spectra up to 1 MeV/. Infrared observations for auroral heating and surface mineralogy, such as those provided by the mission's JIRAM, are complemented on by the Moons and Jupiter Imaging Spectrometer (MAJIS), which extends spectral coverage into the near-IR for close-range detection of ices and non-ice materials during low-altitude passes.

References

  1. [1]
    ESA - Juice factsheet - European Space Agency
    Name: Juice (Jupiter Icy Moons Explorer). Mission objectives: Juice will characterise Jupiter's ocean-bearing icy moons – Ganymede, Europa and Callisto – as ...<|control11|><|separator|>
  2. [2]
    ESA - Juice - European Space Agency
    ESA's Jupiter Icy Moons Explorer, Juice, will make detailed observations of the giant gas planet and its three large ocean-bearing moons.Where is Juice now? · Juice factsheet · Facts about Jupiter · The moons of Jupiter
  3. [3]
    The science: Juice's key objectives at Jupiter - ESA
    Juice's main goal is to characterise Jupiter's moons as both celestial bodies and possible habitats for life (either past or present). The system contains a ...
  4. [4]
    Jupiter Facts - NASA Science
    Data from the Galileo spacecraft indicate that Jupiter's ring system may be formed by dust kicked up as interplanetary meteoroids smash into the giant planet's ...
  5. [5]
    A history of Jupiter exploration: the journey to Juice - ESA
    Galileo found that Europa has a global ocean of liquid water beneath its icy surface, and suggested that Ganymede and Callisto may have subsurface water, too.
  6. [6]
    Jupiter's Moon Callisto May Hide Salty Ocean
    Oct 21, 1998 · This premise was inspired by Galileo data indicating electrical currents flowing near Europa's surface cause changes in Europa's magnetic field.Missing: salinity | Show results with:salinity
  7. [7]
    [PDF] JUICE/Laplace Reformulation Review - ESA Science & Technology
    Dec 18, 2011 · The EJSM/Laplace was selected as a Large-class candidate mission in the Cosmic Vision 2015-25 programme and underwent an assessment study ...
  8. [8]
    NASA and JPL Contribute to European Jupiter Mission
    Feb 21, 2013 · NASA has selected key contributions to a 2022 European Space Agency mission to study Jupiter and three of its largest moons.Missing: Phase 2008-2011 2011 budget
  9. [9]
    [PDF] ESA/SPC(2012)12
    Apr 17, 2012 · The SPC is invited to approve the selection of the JUICE mission as the “L1” mission in the. Cosmic Vision plan, with a foreseen launch date of ...<|control11|><|separator|>
  10. [10]
    [PDF] EJSM-Laplace - ESA Science & Technology
    Feb 1, 2011 · Should EJSM-Laplace be down-selected in June 2011, JGO would move into the next study phase,. Phase A/B1 mission definition phase, during ...
  11. [11]
    Esa selects 1bn-euro Juice probe to Jupiter - BBC News
    May 2, 2012 · The European Space Agency (Esa) is to mount a billion-euro mission to Jupiter and its icy moons. The probe, called Juice, has just been approved.
  12. [12]
    JUICE mission gets green light for next stage of development
    Nov 28, 2014 · Chosen by ESA in May 2012 to be the first large mission within the Cosmic Vision Programme, JUICE is planned to be launched in 2022 and to reach ...<|control11|><|separator|>
  13. [13]
    ESA's Juice lifts off on quest to discover secrets of Jupiter's icy moons
    Apr 14, 2023 · Juice is a mission under ESA leadership with contributions from NASA, JAXA and the Israel Space Agency. It is the first Large-class mission in ...
  14. [14]
    Airbus Defence and Space Signs €350M Contract to Develop and ...
    Dec 9, 2015 · The world's second largest space company, have signed a €350M contract to develop and build ESA's JUICE (JUpiter ICy moons Explorer) spacecraft.Missing: engineering NASA UVS J- JAXA UVI
  15. [15]
    Juice: an ESA-led global collaboration - European Space Agency
    Some key numbers include: 18 institutions; 23 countries; 83 companies; 116 industry contracts; >2000 people; ~1.6 billion euros (mission cost). Juice will make ...
  16. [16]
    First ultraviolet data collected by ESA's JUICE mission
    Jul 5, 2023 · The JUICE mission, with SwRI's UVS, will study Jupiter and its moons, including Ganymede, and will record UV light to reveal their composition.Missing: contractor international J- JAXA
  17. [17]
    The JUICE Mission: Japan joins ESA to head to the icy moons
    Apr 11, 2023 · The JUpiter ICy moon Explorer (JUICE) is set to embark on an eight year journey to the icy moons of our Solar System's largest planet.Missing: partners | Show results with:partners
  18. [18]
    Juice's first year in space: “it's real now” - ESA
    Apr 12, 2024 · One year since the launch of ESA's Jupiter Icy Moons Explorer (Juice), we catch up with core team members Claire Vallat, Giuseppe Sarri, ...
  19. [19]
    Jupiter's radiation belts – and how to survive them - ESA
    Apr 6, 2023 · The problem for Juice mission planners is that heading to Jupiter's icy moons means passing through the radiation belts as well. Europa is the ...
  20. [20]
    JUICE (Jupiter Icy Moons Explorer) - eoPortal
    Feb 10, 2025 · JUICE is the first large-class mission in ESA's Cosmic Vision 2015-2025 program. JUICE will spend at least three years making detailed ...<|control11|><|separator|>
  21. [21]
    [PDF] The JUICE Mission to Jupiter and its Icy Moons - eucass
    The spacecraft environmental test campaign will be concluded in Airbus Toulouse over the last six months of 2022, with propulsion tests, a complement of thermal ...
  22. [22]
    ESA - Juice spacecraft specs - European Space Agency
    ESA's Jupiter Icy Moons Explorer (Juice) is currently heading to Jupiter to explore the planet, its wider space environment, and its moons.
  23. [23]
    [PDF] JUICE Red Book - ESA Science & Technology
    The JUICE (JUpiter ICy moon Explorer) mission, selected by ESA in May 2012 to be the first large mission within the Cosmic Vision Program 2015–2025, will ...
  24. [24]
    Payload and Spacecraft - JUICE - ESA Cosmos
    The payload consists of 10 state-of-the-art instruments plus one experiment that uses the spacecraft telecommunication system with ground-based instruments.
  25. [25]
    JUICE Astrobiology Mission Update
    Jan 25, 2025 · The data rate is currently around 86 kbit/s and in a couple of weeks will be at 43 kbit/s – the same rate Juice will have at Jupiter.
  26. [26]
    JUICE interplanetary operations design : drivers and challenges
    This paper provides an overview of JUICE mission and its scientific goals. It describes the spacecraft journey from. Earth to Jupiter: a seven year ...
  27. [27]
    [PDF] Common DPU and Basic Software for JUICE Instruments
    Feb 25, 2019 · On-Board Computer. (OBC). Processor Module. (CSW). OBC Mass. Memory ... While in JUICE the common DPU and Basic SW were introduced after.
  28. [28]
    The JUICE spacecraft - Deutsches Zentrum für Luft- und Raumfahrt
    In addition to ESA, NASA and the Japanese space agency JAXA have also contributed to the mission. ESA is providing funding for the satellite platform, the ...
  29. [29]
    Ariane 5 rocket launches Europe's first mission to Jupiter
    Apr 13, 2023 · JUICE separation confirmed. The European Space Agency's first mission to Jupiter is flying free of the Ariane 5 rocket after reaching a top ...Missing: VA261 | Show results with:VA261
  30. [30]
    Ariane 5 was mission-optimized for the launch of JUICE
    Apr 21, 2023 · To set the probe off on its interplanetary cruise, Ariane 5 had to accelerate JUICE to Earth-escape velocity (11 km/s). This meant ...
  31. [31]
    Designing the JUICE Trajectory | Space Science Reviews
    Sep 2, 2024 · It should be noted that the JUICE mission proposal, as selected for phase A, included a 30-day long orbital phase around Ganymede at an altitude ...Missing: milestones | Show results with:milestones
  32. [32]
    Juice's first taste of science from space - ESA
    Apr 26, 2023 · The Juice magnetometer boom (J-MAG) was deployed on 21 April, when Juice was about 1.7 million km from Earth. Data collected by J-MAG captured ...Missing: post | Show results with:post
  33. [33]
    Juice's Daring Maneuver: Setting Course for a Historic Earth-Moon ...
    Nov 21, 2023 · Today's burn also gave the teams the opportunity to make sure Juice's main engine is working correctly. It was first tested shortly after launch ...
  34. [34]
    Juice rerouted to Venus in world's first lunar-Earth flyby - ESA
    Aug 21, 2024 · ESA's Jupiter Icy Moons Explorer (Juice) has successfully completed a world-first lunar-Earth flyby, using the gravity of Earth to send it Venus-bound.Missing: altitude | Show results with:altitude
  35. [35]
    After a Boost from Earth and the Moon, Juice is On its Way to Venus ...
    Aug 26, 2024 · The spacecraft took a shortcut by travelling close to Earth and the Moon and using their gravity to gain momentum and change trajectory.
  36. [36]
    Juice team resolves anomaly on approach to Venus - ESA
    Aug 25, 2025 · The spacecraft is currently much closer to the Sun and must point its large, high-gain antenna towards the Sun to act as a heat shield. The ...
  37. [37]
    Juice's Venus flyby a Success - Swedish Space Corporation
    Sep 5, 2025 · Juice is now on course using a carefully planned series of four gravity-assist flybys at Earth and Venus to gradually reach the speed needed to ...Missing: sequence | Show results with:sequence
  38. [38]
    The journey – from Earth to Jupiter in a roundabout way
    After its launch, the probe will first pass by Earth once more in August 2024 and gain momentum with the first ever extremely close flyby of the Moon and Earth.Missing: arrays | Show results with:arrays<|control11|><|separator|>
  39. [39]
    JUICE | Missions - NASA Astrobiology
    JUICE (JUpiter ICy moons Explorer) is an ESA mission to explore Jupiter and its icy moons, Ganymede, Callisto, and Europa, and help understand habitable worlds.
  40. [40]
    Juice's lunar-Earth flyby: all you need to know - ESA
    Jul 15, 2024 · The first-ever lunar-Earth flyby, and the first-ever double gravity assist manoeuvre. It will change Juice's speed and direction to alter ...Missing: sequence | Show results with:sequence
  41. [41]
    [PDF] This paper presents the Lunar Earth Gravity Assist (LEGA ... - STAR
    May 30, 2025 · This paper presents the Lunar Earth Gravity Assist (LEGA) navigation strategy defined for the JUICE mission at the European Space Operations ...Missing: precision | Show results with:precision
  42. [42]
    Mission Calendar - JUICE - ESA Cosmos
    This page details the key dates for the Flight Activities in the Juice mission. These informations are coming from the JUICE Mission Calendar (Report 1.6).Missing: November | Show results with:November
  43. [43]
    Europe regains contact with JUICE Jupiter probe ahead of ... - Space
    Aug 26, 2025 · The probe will steal a small fraction of Venus' orbital momentum, helping propel it toward its next planetary flyby in September 2026, when ...
  44. [44]
    JUICE mission to Jupiter completes Venus flyby - EarthSky
    Bottom line: The JUICE mission successfully performed a gravity assist around Venus on August 31, 2025, helping it pick up speed for its long journey to Jupiter ...
  45. [45]
    Comet 3I/ATLAS – frequently asked questions - ESA
    Juice will attempt observations in November 2025 using several instruments, including cameras, spectrometers and a particle sensor. Coordination with NASA's ...
  46. [46]
    Jupiter-Bound Mission To Study Interstellar Comet 3I/ATLAS From ...
    Oct 31, 2025 · “JUICE will observe 3I/ATLAS between 2 and 25 November. We will be using five instruments: the camera, the near-infrared imaging instrument ...
  47. [47]
    Interstellar object 3I/ATLAS is leaving the solar system - EarthSky
    Oct 30, 2025 · Between November 2 and 25, ESA's Jupiter Icy Moons Explorer (JUICE) will be observing the comet with various instruments. As JUICE looks ...
  48. [48]
    Solving the RIME deployment mystery - ESA
    Jul 6, 2023 · When the RIME antenna on ESA's Juice mission failed to deploy a few days after launch, the engineering teams faced the mighty challenge to understand the fault ...Missing: radiation hardening
  49. [49]
    Europe's JUICE Jupiter probe has an antenna glitch in deep space
    Apr 28, 2023 · NASA's Galileo mission never was able to deploy its high-gain antenna properly ahead of visiting Jupiter and its icy moons between 1995 and 2003 ...Missing: pre- | Show results with:pre-
  50. [50]
    Juice spacecraft overcomes antenna issue ready for Jupiter
    in this case, an ...Missing: pre- | Show results with:pre-
  51. [51]
    Juice team resolves anomaly on approach to Venus - Phys.org
    Aug 25, 2025 · Juice will use the gravity of Venus this week to bend its orbit around the sun and gain speed relative to Earth without using fuel. The Venus ...
  52. [52]
    ESA engineers trace anomaly in silent spacecraft to code bug
    Aug 26, 2025 · If there had been a major failure, Juice might have gone into survival mode and entered a slow spin, sweeping its antenna across the Earth once ...Missing: high- deployment
  53. [53]
    JUICE: Earth and Moon through MAJIS eyes - CNES
    Sep 13, 2024 · During its Moon and Earth flyby on 19 and 20 August 2024, JUICE pointed its optical instruments at Earth and the Moon to gather useful data for calibrating ...
  54. [54]
    Calibration of the Moons And Jupiter Imaging Spectrometer (MAJIS)
    Jul 3, 2024 · The JUpiter ICy moons Explorer (JUICE) mission, launched on April 14, 2023, is the first large mission within the Cosmic Vision Program ...Missing: distant | Show results with:distant
  55. [55]
    [PDF] JUpiter ICy Moon » with EP - Electric Rocket Propulsion Society
    The Jupiter Orbit Insertion is a short time-high ∆v need that is out of the range of current capability of TRL5 EP because of the low electrical power ...
  56. [56]
    Mission analysis for the JUICE mission - ResearchGate
    Aug 9, 2025 · The goal of the JUICE mission analysis consisted in implementing these mission elements within a tight mass and radiation budget. A shift in ...<|control11|><|separator|>
  57. [57]
    [PDF] The JUICE Spacecraft and its Instrumentation, Overviews ans ...
    May 14, 2024 · Science Exploration Phase. Page 15. 15. Mission timeline. The main Juice mission milestones are listed below. Dates are approximate and more ...Missing: key | Show results with:key
  58. [58]
    The moons of Jupiter: What will Juice discover? - ESA
    It will end its mission by colliding with Ganymede's surface in 2035. Europa. Juice will complete two flybys of Europa in July 2032, approaching the moon at a ...Missing: controlled | Show results with:controlled
  59. [59]
    trajectory-assessment
    There will be 12 Ganymede flybys, the closest approach altitute of 3 of them ... JUICE will suffer 65 eclipses by Jupiter, the longest one will extend ...<|control11|><|separator|>
  60. [60]
    Overview - JUICE - ESA Cosmos
    The mission was launched on 14 April 2023 and will arrive at Jupiter in July 2031, it will spend at least four years making detailed observations.
  61. [61]
    Mission Scenario and Operations - ESA Science & Technology
    Nov 10, 2021 · During the tour, gravity assists with Callisto and Ganymede will shape the trajectory. Two targeted Europa flybys are included focusing on ...
  62. [62]
    [PDF] JUICE JUPITER ICY MOONS EXPLORER Science Management Plan
    High delta-V capability (2700 m/s). Radiation ... Specifically this will include the overall responsibility for: • Checkout of JUICE in the cruise phase;.Missing: total ion
  63. [63]
    The JUICE Radiation Environment Monitor, RADEM
    May 6, 2025 · To prepare for this hard environment, the JUICE mission has applied extra precautions such as more shielding to all spacecraft subsystems and ...
  64. [64]
    Science Objectives - JUICE - ESA Cosmos
    The focus of JUICE is to characterise the conditions that may have led to the emergence of habitable environments among the Jovian icy satellites.Missing: characterization | Show results with:characterization
  65. [65]
    [PDF] Exploring the emergence of habitable worlds around gas giants
    The JUICE (JUpiter ICy moon Explorer) concept results from the reformulation of the EJSM- Laplace mission into a European-led mission.
  66. [66]
  67. [67]
    JUICE's instruments - ESA Science & Technology
    May 16, 2023 · RIME, the Radar for Icy Moon Exploration, is an ice-penetrating radar to study the subsurface structure of the icy moons down to a depth of ...Missing: REASON | Show results with:REASON
  68. [68]
    Radar attenuation in Europa's ice shell: Obstacles and opportunities ...
    Jan 18, 2017 · For the JUICE mission, the RIME instrument (Radar for Icy Moons Exploration) has been chosen to study the subsurface structure of the Galilean ...
  69. [69]
    Europa Up Close - NASA Science
    Scientists are unsure of the thickness of Europa's outer icy shell, with many estimates ranging from approximately 10 to 15 miles (15 to 25 kilometers) thick.
  70. [70]
    Implications for Internal Ocean Thickness and Surface Heat Flow
    Ice-shell thickness and ocean depth are calculated for steady state models of tidal dissipation in Europa's ice shell using the present-day values of the ...
  71. [71]
    [PDF] Tidal Heating: Lessons from Io and the Jovian System
    Europa Clipper and JUpiter ICy moons Explorer (JUICE) will provide in-depth studies of Europa and Ganymede in the 2030s. The easily observed heat flow of Io, ...
  72. [72]
    Targets - JUICE - ESA Cosmos
    As was the case with Ganymede, the Galileo mission provided strong evidence for the existence of subsurface ocean lying beneath Europa's crust. This liquid ...Missing: salinity | Show results with:salinity
  73. [73]
    Characterization of the Surfaces and Near-Surface Atmospheres of ...
    Aug 8, 2024 · The mapping of the surface composition of the icy Galilean moons at different spatial scales, with particular emphasis on the detection and ...
  74. [74]
    JUICE's secondary target: Callisto - ESA Science & Technology
    Because of its remote location, orbiting beyond Jupiter's main radiation belts, Callisto sees lower radiation levels and less influence from the Jovian ...Missing: habitability preserved
  75. [75]
    Geophysical Characterization of the Interiors of Ganymede, Callisto ...
    Jul 11, 2024 · In this review article, we describe how JUICE will investigate the interior of the three icy Galilean moons, Ganymede, Callisto and Europa.
  76. [76]
    Science Objectives
    The focus of JUICE is to characterise the conditions that may have led to the emergence of habitable environments among the Jovian icy satellites, with special ...Missing: characterization | Show results with:characterization
  77. [77]
    Dynamics of Ganymede's magnetopause: Intermittent reconnection ...
    Dec 2, 2010 · The intrinsic magnetic field of Ganymede, whose equatorial surface strength (∼720 nT) is ∼7 times larger than the ambient Jovian field ...
  78. [78]
    Discovery of Ganymede's magnetic field by the Galileo spacecraft
    Dec 12, 1996 · Here we report the discovery during these encounters of an internal magnetic field associated with Ganymede (the only other solid bodies in the ...Missing: intrinsic | Show results with:intrinsic
  79. [79]
    JUICE's primary target: Ganymede - ESA Science & Technology
    Finding out more about Ganymede's liquid layer, including its composition and conductivity, is a main objective of JUICE since the ocean might be habitable. The ...
  80. [80]
    Magnetic Induction Responses of Jupiter's Ocean Moons Including ...
    Dec 25, 2020 · Ganymede is a special case because of its intrinsic magnetic field with surface field strength of 720 nT at the equator and approximately ...<|control11|><|separator|>
  81. [81]
    The search for a subsurface ocean in Ganymede with Hubble Space ...
    Feb 3, 2015 · We present a new approach to search for a subsurface ocean within Ganymede through observations and modeling of the dynamics of its auroral ...Abstract · Introduction · Models of the Magnetic Field... · Results and DiscussionMissing: dual- | Show results with:dual-
  82. [82]
    JANUS camera system - Deutsches Zentrum für Luft- und Raumfahrt
    The JANUS camera system is the 'eye' of the JUICE mission. It will primarily provide high-resolution multispectral images of Jupiter's large moons.<|separator|>
  83. [83]
    DLR – The scientific instruments
    Magnetometer J-MAG (JUICE Magnetometer) J-MAG will be used to investigate Jupiter's internal magnetic field and its interaction with the magnetosphere.Missing: UVI | Show results with:UVI
  84. [84]
    The MAJIS imaging spectrometer
    The MAJIS instrument consists of three main hardware units: the optical head, the main electronics unit and a wiring harness connecting the electronically ...Missing: specifications | Show results with:specifications
  85. [85]
    SwRI delivers ultraviolet instrument for ESA's Jupiter mission
    Feb 25, 2020 · UVS will be one of 10 science instruments and 11 investigations for the JUICE mission. The mission has overarching goals of investigating ...
  86. [86]
    ESA Science & Technology - Science Payload
    May 16, 2023 · The table below lists the JUICE experiments, their primary science contribution and key characteristics. An optical camera to study global, ...Missing: total data rate Gbps
  87. [87]
    ESA - Juice magnetometer fit to take data - European Space Agency
    May 16, 2023 · The J-MAG instrument will be crucial for Juice's mission to characterise the oceans expected to be found beneath the outer icy crusts of three ...
  88. [88]
    MAGBOOM successfully attached to JUICE - Airbus
    Mar 16, 2021 · Once deployed its total length is 10.6 metres. The 6.2 ton JUICE spacecraft will set off in 2022 on its near 600 million-kilometers-long journey ...
  89. [89]
    Space Particle Instrument Prepped and Primed for Jovian Journey
    Jupiter Energetic Neutrals and Ions (JENI) and Jovian Energetic Electrons (JoEE) — is ...<|control11|><|separator|>
  90. [90]
    PEP (Particle Environmental Package) - MPS
    PEP (Particle Environment Package) is a particle spectrometer to measure neutral and charged particles in the Jupiter system.
  91. [91]
    JUICE – Swedish Institute of Space Physics
    Dec 17, 2019 · PEP, the Particle Environment Package, will study the interaction between space and Jupiter's icy moons. The instrument with its various sensors ...
  92. [92]
    ESA - Celebrating RPWI deployment - European Space Agency
    Details ... The last step involved swinging out and locking into place of the probes and antennas that make up Juice's Radio & Plasma Wave Investigation (RPWI).
  93. [93]
    Calibration of the JUICE RWI Antennas by Numerical Simulation
    Oct 25, 2021 · The three dipole antennas are perpendicular to each other, and the tip-to-tip length of each dipole is 2.5 m. The antennas were built from ...
  94. [94]
    The Radio & Plasma Wave Investigation (RPWI) instrument on the ...
    May 26, 2023 · The suite of RPWI sensors complement each other and have overlapping frequency ranges, from DC up to 45 MHz. Together the sensors are capable ...
  95. [95]
    The Ganymede Laser Altimeter (GALA) for the Jupiter Icy Moons ...
    Mar 1, 2022 · The Ganymede Laser Altimeter (GALA) is an instrument onboard JUICE, whose main scientific goals are to understand ice tectonics based on topographic data.Missing: shutdown | Show results with:shutdown
  96. [96]
    The GALA altimeter
    GALA is a 'laser altimeter' – an instrument that measures the heights and depths of a planetary landscape via the transit time of laser pulses.
  97. [97]
    [PDF] Description of the Mass Spectrometer for the Jupiter Icy Moons ...
    Jun 10, 2021 · The Neutral gas and Ion Mass spectrometer (NIM) is part of the ... We demonstrated a mass range of 642 u and a mass resolution of m/Δm ...
  98. [98]
    NIM - Particle Environment Package (PEP) - Universität Bern
    The NIM instrument is a highly sensitive mass spectrometer for neutral atmospheric gas and ionospheric ions specifically developed for the tenuous gases of ...
  99. [99]
    SWI (Submillimetre Wave Instrument) - MPS
    The Submillimetre Wave Instrument (SWI) will investigate the Galilean moons of the giant planet Jupiter, the chemistry, meteorology, and structure of Jupiter's ...
  100. [100]
    [PDF] PARTICLE ENVIRONMENT PACKAGE (PEP) FOR THE ESA JUICE ...
    PEP sensors overview: The PEP sensors are (1) an ion mass analyzer, (2) an electron spectrometer, (3) a low energy ENA imager, (4) a high energy ENA and.
  101. [101]
    (PDF) SUDA: A Dust Mass Spectrometer for Surface Mapping for the ...
    Feb 11, 2016 · We present the SUDA (Surface Dust Analyzer) instrument that will provide detailed answers to the main goals of ESA's JUICE mission about ...