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SARAL

SARAL (Satellite with ARgos and ALtiKa) is a joint Indo-French satellite mission launched on February 25, 2013, by the from using the PSLV-C20 rocket, in collaboration with the , to conduct altimetric observations for oceanographic research. The mission operates in a at approximately 800 km altitude with a 35-day repeat cycle, enabling precise, repetitive global measurements of sea surface height, significant wave heights, and wind speeds essential for monitoring ocean circulation, topography, and surface elevation. The satellite's primary payload, AltiKa, is a Ka-band radar altimeter developed by that provides higher resolution data compared to previous C-band or Ku-band instruments, while the ARGOS-3 system, also from , facilitates the collection and location of environmental data from buoys, balloons, and other platforms worldwide. Built on ISRO's Indian Mini Satellite-2 (IMS-2) bus with a launch mass of 407 kg and a designed lifespan of five years, SARAL has exceeded expectations and remains operational as of 2025, contributing to applications in operational oceanography, climate modeling, and coastal management. Its data supports international efforts like the Global Ocean Observing System (GOOS) by improving understanding of phenomena such as El Niño, , and marine .

Background and development

Mission objectives

The 's primary objective is to deliver continuous, high-precision altimetric measurements of surface using the Ka-band AltiKa , enabling detailed studies of circulation, significant , speeds, and with enhanced compared to previous C-band systems. This focuses on advancing operational , including mesoscale variability (wavelengths of 50–500 km and periods of days to a year), coastal processes, and mean tracking. Secondary objectives include augmenting global through the system, which collects data from platforms worldwide for applications in , , and marine , while the receiver and array ensure precise to support altimetry accuracy. Specific aims encompass bridging the observational gap between the and missions by re-occupying their ground tracks, complementing Jason-2 data for improved mean monitoring, and contributing to marine and ecosystem studies. Technically, SARAL targets an along-track of 7–8 km for altimetry measurements, facilitated by the Ka-band's smaller , and operates in a to achieve coverage over more than 80% of Earth's ice-free oceans with a 35-day repeat cycle. This joint effort between and underscores collaborative goals.

International cooperation

The SARAL mission represents a key bilateral collaboration between the Indian Space Research Organisation () and the French Centre National d'Études Spatiales (), formalized through a (MOU) signed on February 23, 2007. This agreement outlined the joint development and operation of the satellite to advance ocean altimetry observations, leveraging complementary expertise from both agencies. Under the MOU, responsibilities were clearly divided to optimize resource allocation. provided the satellite platform using its bus based on the IMS-2 design, handled the launch via the (PSLV), and managed the Indian ground segment for satellite operations, telemetry, tracking, command, platform data processing, archiving, and distribution. , in turn, developed and supplied all payloads—including the ALtiKa , ARGOS-3 , , and Laser Retroreflector Array (LRA)—while overseeing the French ground segment for payload data processing, archiving, and international distribution, along with providing scientific expertise and shared . This partnership built on a longstanding history of Indo-French space cooperation, which dates back to the but gained momentum in the early through missions like , an Indo-French satellite launched in 2011 for tropical atmospheric studies. emerged as a dedicated, cost-effective altimetry initiative, proposed by in 2002 initially as part of Oceansat-3 but evolved into an independent by 2006 due to scheduling needs; it served as a critical gap-filler following the unexpected failure of the European Space Agency's mission in April 2012. Development commenced in 2007 shortly after the MOU, culminating in the satellite's launch on February 25, 2013, with a planned nominal of five years to ensure sustained for oceanographic .

Spacecraft and orbit

Design specifications

SARAL is a mini-satellite utilizing the Mini Satellite-2 (IMS-2) platform developed by the Space Research Organisation (), featuring a three-axis stabilization system for precise attitude control. The platform employs an honeycomb sandwich structure designed for satellites in the 400-450 kg class, providing modular integration for payloads with housekeeping functions such as propulsion, power management, and data handling. The has a launch mass of 407 , with a body configuration measuring approximately 1.62 m in length, 1.2 m in width, and 1.897 m in height, including deployable arrays for enhanced power generation. The power subsystem consists of two deployable panels that generate an average of 906 , supplemented by a 46.8 Ah pack to support operations during eclipse phases. Key subsystems include an attitude and orbit control system (AOCS) equipped with star trackers, gyroscopes, reaction wheels, and mono-propellant thrusters for maintaining three-axis stabilization and performing orbit adjustments. , tracking, and command functions are handled via S-band links, while payload data is transmitted at 32 Mbps using X-band for high-rate downlink. The platform's thermal control system and environmental hardening ensure reliability over a nominal 5-year mission life, withstanding launch vibrations up to the specifications of the PSLV vehicle and exposure to space radiation in . This design supports a configuration for consistent observational geometry.

Orbital parameters

The SARAL satellite operates in a sun-synchronous, near-circular, dawn-dusk orbit with a local time of ascending node (LTAN) at 6:00 AM, enabling consistent solar illumination conditions for its instruments during global ocean observations. This orbit type ensures repeatable ground tracks, facilitating long-term monitoring of sea surface height, waves, and winds. Key orbital parameters during the initial repetitive phase (February 2013 to July 2016) include a mean altitude of 800 , an inclination of 98.55°, an of 0.000165, and a nodal period of 100.59 minutes. The features a 35-day exact repeat cycle comprising 501 revolutions and 1002 passes, with a separation of 75 at the , providing complementary coverage to missions like Jason-2. This configuration supports approximately 14 orbits per day, achieving over 99.5% coverage of ocean surfaces.
ParameterValueDescription/Source
Altitude (mean)800 kmNominal repetitive phase
Inclination98.55°Sun-synchronous
Eccentricity0.000165Near-circular trajectory
Nodal Period100.59 minutesTime per
Repeat Cycle35 days (501 rev.)Exact repetition
Ground Track Spacing75 km ()Inter-track distance for coverage
Precision orbit determination is achieved using the onboard receiver and Laser Retroreflector Array (LRA), maintaining radial accuracy of approximately 1 cm , which is essential for altimetric measurements. Post-launch maneuvers circularized the initial orbit, with subsequent minor adjustments to control drift and ensure stability during the repetitive phase. In July 2016, following anomalies, the orbit entered a drifting phase with a 1 km altitude increase, preserving subcycles of 15–17 days but abandoning exact repetition.

Instruments

ALtiKa altimeter

The ALtiKa altimeter is a Ka-band radar altimeter developed by the French space agency CNES as the primary instrument for the SARAL mission, designed to provide high-resolution measurements of ocean surface topography. Operating at a center frequency of 35.75 GHz with a 500 MHz bandwidth, it features a 1 m diameter offset reflector antenna that enables precise nadir-pointing observations from an altitude of approximately 800 km. The instrument's design draws from the Poseidon series but advances to Ka-band to achieve finer spatial resolution compared to previous Ku-band systems. ALtiKa measures three key parameters: the range to the sea surface for height determination, (SWH) up to 10 m, and the backscatter coefficient (σ⁰) for estimating near-surface wind speeds. These measurements are derived from the returned of short pulses, with a of about 4 kHz, yielding a pulse-limited along-track of 7-8 km at 1 Hz sampling rate. The Ka-band operation inherently reduces ionospheric path delays—typically a major error source in lower-frequency altimeters—allowing reliance on external models like JPL's Global Ionosphere TEC maps for corrections rather than onboard dual-frequency altimetry. Overall sea surface height accuracy achieves an RMS of 3.4 cm, meeting mission goals for ocean circulation monitoring. For atmospheric corrections, ALtiKa incorporates an integrated dual-frequency operating at 23.8 GHz and 37 GHz to estimate and subtract wet tropospheric delays with an accuracy better than 1 cm. Ground-based absolute occurs at dedicated sites, such as Cape Senetosa in (41°34'N, 8°48'E), where radar transponders simulate echoes to verify range bias and instrument stability. A key innovation of the Ka-band design is its reduced beam of approximately 8 km diameter (at -6 dB), roughly half that of Ku-band altimeters (around 20 km), which minimizes volume errors and enhances over coastal zones, inland waters, and ice-covered regions. This smaller , combined with the higher frequency's to , supports improved profiling in areas where traditional altimeters struggle. The altimeter's precise ranging benefits from integration with the onboard receiver, which provides orbit determination accuracy on the order of 3 cm radially.

ARGOS system

The on SARAL represents the third generation of the data collection and location system, developed by the French space agency to receive and process signals from remote platforms worldwide. These platforms, equipped with transmitters known as platform transmitter terminals (PTTs), include ocean buoys, atmospheric balloons, and animal tags, and operate by sending short bursts of data via UHF signals at 401.65 MHz. The system's core capability lies in Doppler-based positioning, which measures frequency shifts in the incoming signals to determine platform locations with an accuracy of up to 150 in optimal conditions. It collects environmental parameters, such as and , bundled into messages of up to 256 bits each, enabling the relay of sensor data from dispersed platforms. Globally, the constellation, including SARAL, processes approximately 3 million messages per day (over 1 billion annually) from tens of thousands of active PTTs worldwide. Equipped with a UHF tuned to approximately MHz, the instrument features fully digital onboard processing to compute locations and extract in near during satellite passes. This is then downlinked via L-band to ground stations for integration into the broader network, ensuring rapid dissemination to users. The supports multiple channels, allowing simultaneous handling of signals from numerous PTTs within the satellite's . Relative to its predecessor, ARGOS-2, the ARGOS-3 version incorporates key enhancements, such as an uplink bit rate increased to 4.8 kbit/s from 400 bit/s, enabling faster data transmission, and improved anti-jamming resilience through a wider reception of 110 kHz and advanced digital filtering techniques. On SARAL, the ARGOS-3 system complements altimetry observations by relaying multi-parameter data from ocean platforms, supporting comprehensive environmental monitoring.

DORIS receiver

The (Doppler Orbitography and Radiopositioning Integrated by Satellite) receiver on SARAL, provided by the French space agency , is a dual-frequency instrument designed for precise . It tracks continuous uplink signals transmitted from approximately 60 globally distributed ground beacons at the uplink frequencies of 2.03625 GHz (S-band) and 401.25 MHz (UHF). The receiver measures Doppler frequency shifts in these signals to compute the satellite's and position, enabling high-precision . This functionality supports real-time via the onboard processor and contributes to post-processed with a radial accuracy of 2 cm RMS when combined with other tracking data. The system processes Doppler data from 7 to 15 passes per , correcting for ionospheric effects through dual-frequency observations. Key components include a multi-channel unit, an ultra-stable oscillator providing frequency stability better than 3 × 10^{-13} over 8 hours for accurate time-tagging, and a single mounted on the panel. The operates in dual-string cold for reliability, automatically switching chains if needed. In the SARAL mission, the receiver plays a critical role in mitigating range errors caused by orbital uncertainties, ensuring the accuracy of sea surface height measurements from the ALtiKa instrument. It is integrated into the international DORIS network managed by the International DORIS Service (IDS), which includes beacons operated by agencies in (e.g., ), the United States (e.g., ), , and other countries for worldwide coverage.

Laser retroreflector array

The (LRA) on the SARAL satellite is a passive developed by the agency and manufactured by Thales SESO, consisting of nine corner-cube made from Suprasil . Each has a clear of 30 mm and a height of 24 mm, arranged in a truncated conical configuration with one central cube and eight others distributed azimuthally around it. This array is mounted on the nadir-facing panel of the satellite to optimize visibility from ground stations. The LRA functions by reflecting laser pulses transmitted from ground-based (SLR) stations operated by the International Laser Ranging Service (ILRS) directly back to their origin, enabling precise two-way without requiring onboard power or electronics. These reflections allow for independent validation of the satellite's position with millimeter-level accuracy, complementing other systems. The retroreflectors are optimized for wavelengths in the visible (e.g., 532 nm) to near-infrared , with each featuring a offset of 1.5 arcseconds and a error below 40 nm to minimize signal distortion. The array's spans 150° in and a full 360° in , ensuring broad coverage for acquisitions. In operation, the LRA supports post-pass analysis of ranging data collected during satellite overflights of ILRS stations worldwide, including key facilities such as in and Wettzell in . This data is used to calibrate orbits derived from the receiver, achieving radial orbit accuracies better than 1 cm , and contributes to the maintenance of the International Terrestrial Reference Frame (ITRF) by providing geodetic ties between space and ground reference points. By enabling high-precision SLR observations, the LRA enhances the overall accuracy of SARAL's altimetric measurements.

Launch

Launch vehicle and site

The (PSLV) in its configuration, flight number C20, was the launch vehicle for the SARAL mission. This four-stage expendable rocket employs alternating solid and liquid propulsion: the first and third stages use solid motors, while the second stage is powered by a liquid-fueled Vikas engine, and the fourth stage uses a liquid bipropellant system. Measuring 44 meters in height with a lift-off mass of 320 tonnes, the PSLV-XL variant is optimized for sun-synchronous orbits and can deliver payloads of up to approximately 1,400 kg to a 600 km altitude, scaling to lower capacities at higher altitudes like 800 km. The launch occurred from the First Launch Pad at the SHAR (SDSC SHAR) in , , a coastal site on the selected for its equatorial proximity and safety over the ocean. On February 25, , at 12:31 UTC (18:01 local IST), PSLV-C20 lifted off successfully after a 59-hour , marking the 23rd flight of the PSLV series. The ascent sequence proceeded nominally, with the first stage () burning for 113 seconds to reach an altitude of about 67 km, followed by separation and ignition of the second stage (PS2) for orbital insertion burns. Stage 3 (PS3) and Stage 4 (PS4) firings refined the trajectory, culminating in the deployment of approximately 17-18 minutes after liftoff. The vehicle achieved precise injection into a sun-synchronous of 785 km × 820 km at 98.55° inclination, providing the with the necessary conditions for subsequent onboard maneuvers to circularize at ~810 km. This performance demonstrated the PSLV's reliability for multi-payload missions, including brief accommodation of secondary satellites.

Secondary payloads

The PSLV-C20 deployed SARAL as the primary , followed by six secondary payloads consisting of foreign micro- and mini-satellites with a combined launch mass of 259.5 . These satellites were released sequentially from the fourth stage of the approximately 18 to 22 minutes after liftoff, into sun-synchronous polar orbits at altitudes around 785 km, with slight adjustments to ensure orbital separation and collision avoidance. The payloads were selected for their alignment with the mission's orbital parameters, enabling low-cost rideshare opportunities for international partners focused on , space situational awareness, and technology demonstrations. The secondary payloads included two Canadian satellites for space surveillance: NEOSSat (74 kg), which carried a visible/near-infrared to detect and track near-Earth objects and resident space objects, and (148 kg), equipped with an optical sensor for monitoring man-made satellites and debris in as part of the Canadian Space Surveillance System. From , the mission carried UniBRITE (14 kg) and TUGSAT-1 (14 kg), both student-led projects. UniBRITE, part of the BRITE constellation, featured a wide-field for photometric observations of bright stars to study stellar variability and oscillations. TUGSAT-1 served as a demonstrator with a multispectral camera for imaging and tests of attitude control systems. The contributed STRaND-1 (3.5 kg), a 3U developed by the and Ltd. to demonstrate smartphone-based computing for onboard , radiation tolerance, and low-cost nanosatellite operations. Denmark's AAUSAT-3 (1 kg), a 1U built by students, included payloads for detecting gamma-ray bursts via scintillation detectors and testing (AIS) receivers for maritime vessel tracking in polar regions. These payloads primarily aimed at advancing low-cost and scientific research through university collaborations and international partnerships with . Several operated for several years or longer, providing valuable data for their missions; for instance, NEOSSat and remain operational as of 2025, contributing to ongoing efforts, while the BRITE contributions from UniBRITE and TUGSAT-1 supported long-term stellar studies. The rideshare also facilitated student training in satellite design and operations across participating institutions.

Operations

Mission timeline

The SARAL satellite was launched on February 25, 2013, aboard an PSLV-C20 rocket from the in , . Following launch, initial commissioning activities commenced immediately, with satellite subsystems activated on February 25–26, 2013, and all instruments achieving nominal performance by March 8, 2013. Orbit raising maneuvers were completed by March 13, 2013, establishing the at approximately 814 km altitude, after which the first measurement cycle began on March 14, 2013; full operational capability was reached shortly thereafter in early April 2013. The nominal mission phase spanned from 2013 to July 2016, aligning with the satellite's designed lifetime of three years for the AltiKa altimeter and five years for the system. During this period, SARAL operated in a repetitive 35-day cycle, providing continuous altimetric data collection with availability exceeding 95% over ocean surfaces and achieving greater than 99% global system uptime. In March 2015, technical anomalies with the reaction wheels were detected, prompting CNES and ISRO to initiate orbit relaxation measures to preserve satellite stability and extend operational life. This led to the transition to an extended drifting phase (SARAL-DP) starting July 4, 2016, where the orbit altitude was increased by about 1 km, eliminating the repetitive ground track in favor of subcycles of 15–17 days while maintaining altimeter functionality. The extended phase has continued beyond the original design life, with the satellite remaining operational as of November 2025, exceeding 12 years in orbit, and continuing to acquire data, including GDR cycle 196 in progress. End-of-life planning targets natural orbital decay for deorbiting around December 2025, ensuring compliance with space debris mitigation guidelines by avoiding long-term orbital remnants.

Data processing and distribution

The ground segment of the SARAL mission is managed collaboratively by the Indian Space Research Organisation (ISRO) and the French space agency CNES, with support from the European Organisation for the Exploitation of Meteorological Satellites (EUMETSAT). ISRO oversees satellite command and control, as well as data distribution to Indian users through its Meteorological and Oceanographic Satellite Data Archival Centre (MOSDAC). CNES operates the AltiKa Mission Center at its Toulouse Space Center for payload data reception, processing, and archiving, while EUMETSAT facilitates tracking via ground stations in Europe, including Svalbard, and handles near-real-time data relay. This dual-center approach ensures robust coverage and redundancy in data acquisition and initial processing. Data processing follows standardized altimetry pipelines, producing products at multiple levels to support various user needs. Level 1 products consist of data records in units, including unprocessed echoes and brightness temperatures from the ALTIKA . Level 2 geophysical data records (GDRs) derive key parameters such as sea surface height (SSH), (SWH), and wind speed, available in operational (OGDR, latency 3-5 hours), interim (IGDR, latency <1.5 days), and full (GDR, latency ~40 days) variants. Higher-level products at Level 3 and 4 include gridded multi-mission maps and along-track , generated through the SSALTO/DUACS system for merged altimetry datasets. These levels enable progression from to validated geophysical insights, with accuracies improving from 30 cm in OGDR to 3 cm in GDR. Core algorithms focus on handling the Ka-band specifics of ALTIKA to achieve high precision. Waveform retracking employs the maximum likelihood estimator (MLE4) for open-ocean returns and specialized Ice1, Ice2, or retrackers for polar regions, optimizing range estimation from the narrower Ka-band footprints. Essential corrections account for propagation delays and geophysical effects, including dry and wet tropospheric delays (from ECMWF models and onboard ), ionospheric delays (via JPL global maps), solid and ocean (using FES2014b and GOT4.10c models), and inverse barometer response to . Sea state bias corrections, based on non-parametric models, further refine SSH estimates, ensuring compatibility with Ku-band missions like . These methods enhance data quality for coastal and high-latitude applications. SARAL data products are distributed through multiple channels to ensure accessibility for operational and users. Near-real-time OGDRs are disseminated via EUMETCast, EUMETSAT's broadcast , reaching users within hours for applications like marine forecasting. Delayed-time IGDRs and GDRs are available via FTP servers at (ftp-access.aviso.altimetry.fr) and ISRO's MOSDAC, with long-term archives maintained at for global access and NASA's Distributed Active Archive Center (PO.DAAC) for U.S.-based users. Products are formatted in NetCDF-4 (compliant with CF-1.1 conventions) or BUFR for meteorological integration, facilitating seamless download and analysis. The mission adheres to international standards for data , aligning with Committee on Earth Observation Satellites (CEOS) guidelines and Global Climate Observing System (GCOS) requirements for essential climate variables like . This compliance, through standardized formats and processing chains, enables SARAL data to integrate with reference missions such as and Sentinel-6, supporting long-term ocean monitoring continuity.

Applications

Oceanographic monitoring

SARAL's AltiKa altimeter provides high-precision measurements of sea surface height (SSH), enabling detailed mapping of ocean dynamics with a root mean square accuracy of 3.4 cm, surpassing the mission's 4 cm requirement. This capability allows for effective tracking of mesoscale eddies and major currents, such as the , by capturing variability at scales of 40-50 km along the satellite's track. Additionally, SSH data from SARAL contribute to detecting signals associated with climate phenomena like El Niño and La Niña through anomalies in sea surface topography. The mission also delivers (SWH) measurements with accuracy for values up to 10 m and estimates ranging from 0.5 to 25 m/s, derived from backscatter analysis. These observations benefit from AltiKa's Ka-band operation, which yields a smaller of approximately 8 compared to prior Ku-band altimeters, enhancing resolution in coastal zones where previous missions faced limitations due to land contamination. Validation against buoys confirms reliable performance for SWH and wind in regions like the North . SARAL extends its utility to polar regions by monitoring and extent and freeboard, leveraging the altimeter's sensitivity to ice surface elevations during winter cycles. Over , it tracks inland levels in lakes and , with reduced interference from due to the instrument's finer and higher frequency, enabling observations in challenging terrains. Key findings from SARAL data include revelations of fine-scale fronts through enhanced along-track resolution, supporting model validation with continuous datasets from onward. Integration of SARAL's SSH and with float profiles improves estimates of the three-dimensional state, particularly for subsurface temperature and validation in assimilation models. This enhances understanding of vertical structure and circulation patterns.

Climate and

SARAL/AltiKa has significantly contributed to tracking global mean sea level (GMSL) rise by providing high-precision sea surface height (SSH) measurements as part of the altimetry constellation. Since its launch in 2013, the mission's data have been integrated into multi-mission records, enabling the observation of an average GMSL rise rate of approximately 3.3 ± 0.3 mm/year from 1993 to 2021, with recent acceleration to about 4.5 mm/year as of 2023–2025, to which SARAL's ongoing data continue to contribute despite its drifting orbit. These measurements, achieving an accuracy of 3.4 cm, support long-term records by filling temporal gaps left by predecessor missions like , ensuring over 99.5% ocean coverage for decadal trend analysis. In climate monitoring, SARAL's SSH anomaly data play a key role in assessing (OHC), a critical indicator of . By detecting SSH variations linked to , the mission aids in quantifying upper ocean warming trends that contribute substantially to , with altimetry-derived records supporting IPCC assessments of accelerated ocean heat uptake since the . For instance, SARAL's inclusion in homogeneous altimeter datasets has improved estimates of steric sea level changes, highlighting a rising trend of 0.64–0.97 mm/year in global steric components over recent decades. The ARGOS-3 instrument on SARAL facilitates through location and environmental data collection for tracking, particularly marine mammals such as and whales. These data reveal migration patterns and use, informing efforts amid climate-induced changes like shifting . Additionally, SARAL's altimetry supports and risk modeling by providing water level data for hydraulic simulations, such as those for the Tapi River in , where it calibrates flood wave propagation with high accuracy (R² = 0.98). This enhances predictive models for storm surges and inundation, as demonstrated by detections of up to 3 m surges during Cyclone Xaver in 2013. SARAL data also advance applications by aiding delineation and zone detection critical for fisheries. SSH anomalies, when integrated with and signatures, identify nutrient-rich regions (e.g., negative SSHa correlating with high at -0.73), supporting management and protection. The mission's extended operations, despite orbital drifts since , have bolstered 20-year climate records by maintaining continuity in the altimetry constellation, reducing uncertainties in global environmental trend assessments.

Mission status

In-orbit performance

SARAL has maintained robust in-orbit performance well beyond its nominal 5-year design life, achieving 12 years of operations by February 2025 with data products that continue to meet mission requirements. On February 25, 2025, SARAL completed 12 years in orbit, with its data products continuing to meet mission requirements. The satellite's overall reliability is evidenced by a global system availability of approximately 99.1% after nearly 10 years in orbit and greater than 99.5% ocean data coverage in recent assessments. No catastrophic subsystem failures have occurred, though minor degradations in attitude control components have necessitated operational adjustments. The ALtiKa altimeter instrument remains fully operational, exhibiting stable performance with no significant drifts or noise degradation throughout its mission phases, including the post-2016 drifting and post-2019 anomaly periods. Operating in the Ka-band, it delivers sea surface anomalies with an RMS accuracy of 3.4 cm, outperforming equivalent Ku-band systems in noise reduction and . The ARGOS-3 system operates at full capacity for collecting and relaying data from surface platforms, while the DORIS receiver and Laser Retroreflector Array (LRA) provide uninterrupted precise , supporting radial accuracies at the 1-2 cm level. Key anomalies include a failure in 2015, which prompted a controlled drifting phase starting in July 2016 to conserve and extend life, and a star sensor malfunction in February 2019 that temporarily degraded pointing but was compensated through ground-commanded maneuvers. These events resulted in short-term data gaps but did not compromise long-term instrument functionality, with recovery achieved within weeks. Telemetry data confirm thermal stability via the satellite's passive and control within design limits, featuring 3-axis stabilization and a drift rate of ±10^{-4} °/s (3σ). Performance metrics highlight the mission's enduring precision, with calibrated to -4.7 cm relative to Jason-2 standards and overall anomaly stability enabling reliable mesoscale monitoring. By November 2025, SARAL has downlinked extensive datasets at rates up to 32 Mbit/s via X-band, accumulating petabyte-scale volumes that support global altimetry archives.

Legacy and end-of-life

SARAL/AltiKa has established a significant scientific legacy through its provision of over 12 years of high-resolution Ka-band altimetry data, which has advanced radar altimetry techniques by demonstrating improved and reduced ionospheric effects compared to traditional Ku-band systems. This dataset has enhanced understanding of mesoscale variability, coastal dynamics, and inland , serving as a for subsequent missions. Notably, the mission's Ka-band innovations influenced the design of the Altimeter (SRAL) on ESA's satellites, providing validation data for their operational phases. The full SARAL dataset, encompassing near-real-time and geophysical data records, is preserved in archives maintained by through and by , ensuring long-term availability for reanalysis and climate studies. This has supported extensive research, resulting in numerous peer-reviewed publications that leverage the mission's precise sea surface height measurements for applications in circulation modeling and . As of late 2024, and agreed to extend operations until the end of 2025, marking the nominal end-of-life for the mission originally designed for five years. Post-mission, the satellite will enter a passivation phase with no further orbit maneuvers except for collision avoidance, aligning with international mitigation standards such as ISO 24113 to minimize orbital risks. Looking ahead, SARAL's extended dataset bridges the gap to missions like NASA's SWOT, launched in 2022, by offering complementary Ka-band observations that inform wide-swath altimetry calibration and highlight the value of Ka-band for future high-precision instruments. The mission exemplifies successful Indo-French collaboration under a 2007 , where provided the satellite platform and launch while contributed the AltiKa payload and data systems, delivering cost-effective global oceanographic benefits.

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