Minimize SWOT

SWOT (Surface Water Ocean Topography) Mission

SWOT is a wide-swath altimeter mission concept - a proposal under study/definition in 2009 by NASA/JPL and CNES - for accurate future monitoring of local sea level changes at the land-sea interface. The SWOT mission has been recommended in 2007 by the NRC (National Research Council) decadal survey “Earth Science and Applications from Space: National Imperatives for the Next Decade and Beyond” for implementation by NASA. 1) 2) 3)

Note: The new name SWOT was adopted in February 2008, replacing the original name WATER HM (Water And Terrestrial Elevation Recovery) Hydrosphere Mapper. 4) 5)

The overall scientific objectives and goals of SWOT, in particular by the water resources and hydrologic community, are to contribute to a fundamental understanding of the Earth system by providing global measurements of continental surface water storage changes and discharge, which are critical for water and climate cycle models. 6) 7) 8) 9) 10) 11) 12) 13) 14) 15) 16) 17) 18) 19) 20)

The main mission goals of the demonstration mission are:

• The primary oceanographic objectives of the SWOT mission are to characterize the ocean mesoscale and sub-mesoscale circulation at spatial resolutions of 10 km and larger.

• The hydrologic science objectives of the SWOT mission are:

- To provide a global inventory of all terrestrial surface water bodies whose surface area exceeds 250 m2 (lakes, reservoirs, wetlands) and rivers whose width exceeds 100 m (requirement) (50 m goal)

- To measure the global storage change in terrestrial surface water bodies (for man-made reservoirs, total storage) at sub-monthly, seasonal, and annual time scales.

- To estimate the global change in river discharge at sub-monthly, seasonal, and annual time scales.


In 2006, WatER was an international (NASA, CNES, ESA) proposal and initiative (satellite mission in study phase) focused on the hydrologic processes related to the spatial and temporal variability in global terrestrial surface fresh water storage. Fresh water bodies cover at least 4% of Earth's terrestrial surface whereas tropical wetlands, particularly in the Amazon Basin, cover nearly 20% of their watershed. The vast storage capacity of wetlands, reservoirs, rivers, etc. impact the global water cycle.

The processes include the movement of water through a basin, across a continent and into the oceans; the hydrologic mass exchange that occurs between floodplains and channels; the changes in water storage on the continents; and the management of water resources. Climatic, sediment, biogeochemical, and temperature processes are inherently tied to hydrologic mass-balance and transport, thus they are included in our science goals to make for a more complete understanding of the terrestrial surface water branch of the global water cycle.

To identify the temporal and spatial variability in surface water storage requires measurements of volumetric change. Thus, the minimum requirements are the measurements of: 1) surface water area extent, 2) elevations of the water surface, h, of wetlands, rivers, lakes, reservoirs, etc., and 3) temporal changes in water levels, i.e. the derivatives in time and space (Δh/Δt, Δh/Δx). The requirements call for spatial resolutions of water surfaces in the range of 10-100 m at temporal resolutions of 1 week.

In the fall of 2012, SWOT passed two important milestones and has now entered "Phase A" in the NASA mission development life cycle. 21)

Some Background: A series of workshops and a symposium were held in Europe since 2003 [by a group of European (France, ESA, UK, etc.) and US scientists, in particular the NASA SWWG (Surface Water Working Group)] on the topic of defining a proposal for a satellite mission dedicated to terrestrial surface water.

- Workshop on Hydrology from Space, Toulouse, France, Sept. 29-Oct. 1, 2003

- Workshop at LEGOS (Laboratoire d'Études en Géophysique et Océanographie Spatiale), Toulouse, France, Nov. 15-16, 2004

- Surface Water Satellite Mission workshop at ESA/ESRIN, Frascaty, Italy March 7-8, 2005

- Symposium: 15 Years of Progress in Radar Altimetry, Venice, Italy, March 13-16, 2006

- Joint Meeting of Ocean Sciences and Surface Water Hydrology in Support of Wide-Swath Altimetry Measurements, Washington DC, Oct. 30-31, 2006

- OSTST (Ocean Surface Topography Science Team) meeting was held in Hobart, Australia on March 12-15, 2007.

The growing concern about our planet's fresh water resources, coupled with the economically driven decrease in groundbased gauge measurements, has focused attention on the possibility of using space-based data sets for remote measurements of river and lake heights. The most direct measurements of inland water heights are obtained from satellite altimeters, with long time series of such observations having been built up over the past decade.

Presently, altimeters are configured for oceanographic applications, thus lacking the spatial resolution that may be possible for rivers and wetlands. The conventional nadir-looking altimeters (of radar or lidar type) provide a very limited coverage (intersatellite distance of typically 150 km for the TOPEX/Poseidon - Jason-1 tandem), and a spatial resolution of ....... These conventional altimeter profiles are not suitable of supplying the measurements needed to address scientific and societal questions.

SWOT will repeatedly measure the spatially distributed water surface elevations (h) of wetlands, rivers, lakes, reservoirs, etc. Successive h measurements yield dh/dt, (t is time), hence a volumetric change in water stored or lost. Individual images of h yield dh/dx (x is distance), hence surface water slope, which is necessary for estimating streamflow. 22)


Figure 1: An overview of global altimeter missions, March 2012 (image credit: CNES) 23)



Mission architecture:

SWOT is a swath-based SAR altimetry mission designed to acquire elevations of water surfaces at spatial and temporal scales necessary for answering key water cycle and water management questions of global importance. SAR altimetry is the only method capable of producing images of high resolution water surface elevation measurements [i.e., provision of h, Δh/Δx (slope), and Δh/Δt (changes in water level over time)].

The SWOT mission architecture is pictured in Figure 2 and consists of a space segment comprising a Flight System composed of the spacecraft bus and science payload and a ground segment that includes the ground station network, spacecraft and payload operations centers, data processing systems, and data archiving systems. The Flight System collects data from its science payload and relays it via an X-band downlink of 800 Mbit/s to a global network of CNES-supplied ground stations. The large daily volume of ~7 Tbit requires ~ 20 downlinks/day. The spacecraft engineering and housekeeping telemetry, with its much more modest volume, is downlinked via S-band twice a day to the ground network. The spacecraft and science instrument commanding is done via S-band through the same ground station network. Once received, the science data are relayed to the JPL and CNES POCs (Payload Operation Centers) for processing, distribution to science and other users, and archiving. 24)


Figure 2: Overview of the mission architecture (image credit: NASA)

Key mission drivers: A number of top level mission requirements are key drivers to the mission concept design. The are the orbit, the ocean height accuracy, and the hydrology surface water spatial resolution. A non-sun-synchronous highly inclined orbit of 78º inclination was selected to minimize tidal aliasing of the ocean SSH measurements and to ensure coverage of major water bodies on land. The associated large variation in solar angle relative to the spacecraft drives the power subsystem design, resulting in large solar arrays (area ~35 m2) and increased battery sizing. The ocean height accuracy drives the interferometer baseline length, the antenna/boom stability and the roll knowledge drift requirement to < 50 marsec/2.5 minutes. The surface water spatial resolution of 50 m impacts the onboard data handling and data downlink requirements due to the large associated data volume (+ 7 TBit/day) and the raw data rate of KaRIn of 360 Mbit/s.


Measurement concept:

The SWOT measurement concept is illustrated in Figure 3. The SWOT spacecraft measures satellite and ocean range through its nadir altimeter, corrected for the effects of columnar water water through its microwave radiometer. These measurements are coupled with those made in two swaths by the KaRIn instrument. Ground based laser ranging systems and DORIS beacons, plus the spaceborne GPS (Global Positioning System) provide POD (Precision Orbit Determination) for calculating SSH (Sea Surface Height). For hydrology-related height and slope measurements for water bodies and rivers, a similar approach is taken, although the nadir altimeter measurements are not required due to less stringent height accuracy requirements. SWOT will provide measurements with a spatial resolution of 1 km for the ocean (after on-board processing), and 50 m for land water, both with centimetric height accuracy , ~ 3 cm for ocean and 10 cm for land (Ref. 24).


Figure 3: The SWOT measurement concept (image credit: NASA)

While conventional altimetry relies on the power and the specific shape of the leading edge of the return waveform, which is only available for the nadir point, the interferometric technique relies on the measurement of the relative delay between the signals measured by two antennas separated by a known distance (hereafter termed “baseline”, Figure 4), together with the system ranging information, to derive the height for every imaged pixel in the scene. 25)


Figure 4: KaRIn interferometer baseline (image credit: NASA/JPL, CNES)

For a given point on the ground, a triangle is thus formed by the baseline B, and the range distance to the two antennas, which can be used to geolocate in the plane of the observation. The range difference between the two antennas is determined by the relative phase difference between the two signals (Figure 5).


Figure 5: Interferometric measurement concept (image credit: NASA/JPL, CNES)

The importance of the cross-track pointing angle, including the roll knowledge (Θ), in the measurement is evident. For that reason, the SWOT flight system includes a precision gyro in the KaRIn payload module. In addition, its antenna/boom must be very stable and disturbances from spacecraft mechanisms must be minimized. The KaRIn antenna baseline (B) is specified to be 10 m.

The difference between two sides (Δ r) is obtained from the phase difference (Θ) between the two radar channels. One can determine the height measurement from the two equations stated in Figure 5.

KaRIn operates in the so- called “Non Ping Pong mode”: nominally, the radar transmits out of one antenna and receives on both, thus creating an interferometric pair of each swath (Figure 6) The isolation between the two swaths is accomplished by means of offset feed reflectarray antennas which produce beams of orthogonal polarizations for each swath.

The intrinsic range resolution is 75 cm, and the ground cross-track range resolution varies from about 70 m in the near swath to about 10 m in the far swath.

Several sources of errors limit the accuracy of the final height:

• Random errors, most notably the measurement noise of the interferometric phase difference. The random error contribution depends on several factors, most remarkably the system SNR (Signal-to-Noise Ratio), the length of the interferometric baseline, and the processing algorithm.

• Spacecraft bus and instrument systematic errors, such as unknown roll, baseline, range and phase drift errors. Lack of knowledge in the spacecraft roll angle, changes in the baseline due to thermal contraction or expansion, system timing errors, and phase errors introduced by the antennas or the electronics will induce height errors.

• Orbit and electromagnetic propagation (or media) errors, such as tropospheric and ionospheric propagation delays. While KaRIn will not directly measure tropospheric and ionospheric corrections, the SWOT altimeter/radiometer suite will be used to perform each range correction at nadir. The POD suite of instruments will be used to correct orbit errors.

• Wave-related errors, such and sea-state (also termed “electromagnetic”, EM) bias and SWH (Significant Wave Height) errors. The spatial variability of the wave and wind fields will introduce height biases.


Figure 6: Illustration of the Non Ping Pong mode (image credit: NASA/JPL, CNES)



Sensor complement: (KaRIn)

KaRIn (Ka-band Radar Interferometer)

SWOT's main instrument is KaRIn, a bistatic SAR system in Ka-band. The interferometric altimeter is a near-nadir viewing, 100 km wide-swath interferometric SAR (consisting of two separated 50 km swaths). The instrument concept uses two SAR antennas at opposite ends of a 10 m boom coupled to a nadir SAR to measure the highly reflective water surface. Interferometric processing of the returned pulses yield single-look 5 m azimuth and 10 m to 70 m range resolution, with an elevation accuracy of about ±50 cm. Polynomial based averaging increases the height accuracy to about ±3 cm. The entire globe is covered twice every 16 days. 26) 27) 28) 29) 30) 31) 32) 33) 34)

The KaRIn measurement concept has a rich heritage based on:

1) The many highly successful ocean observing radar altimeters (ERS-1, TOPEX/Poseidon, ERS-2, Jason-1, Envisat, Jason-2, etc.)

2) The SRTM (Shuttle Radar Topography Mission) - the 11-day mission took place in the period Feb. 11-22, 2000. Obviously, this short Shuttle mission could not provide multi-temporal observations over long periods of time. The mission objective was to obtain single-pass interferometric SAR imagery in C-band and X-band for DEM generation. SRTM used incidence angles of 30º - 60º. Although C-band yields some returns from the water surface, X-band produces returns everywhere. SRTM is the only mission to produce image-based elevation measurements of water surfaces. - Changing to Ka-band and 1º - 3º incidence for SWOT, should provide returns over all water surfaces.

3) The development effort of WSOA (Wide Swath Ocean Altimeter) by NASA/JPL (however, the WSOA option for ocean monitoring was dropped from the Jason-2/OSTM spacecraft in the spring of 2005 because of concerns about programmatic risk to the core Jason-2/OSTM mission and due to cost overruns). WSOA would have provided high-resolution measurements of SSH (Sea Surface Height) on approximately a 10 km grid across a 200 km swath centered on the satellite ground track.

The KaRIn instrument covers near-nadir swaths (0.6-4.1º incidence angle) on both sides of the satellite track. There are relatively few reports on backscattering from natural surfaces in Ka-band, especially in near-nadir, and they are generally limited with respect to the surface types taken into account, and the number and range of associated parameters (local incidence angle, soil humidity and roughness, water salinity, wave height, etc.).

Interferometric near-nadir Ka-band acquisitions were realized during an airborne campaign in the Camargue area in Southern France in 2011. To the knowledge of the project, these are the very first interferometric acquisitions realized in this particular configuration, including the incidence range of KaRIn on SWOT (0.6-4.1º). Several scene types were covered, including ocean (Mediterranean), a coastal area (Piemanson), a lagoon (Vaccares) and a hydrology site (the Rhône river south of Arles). Extensive ground truth were collected. 35) 36) 37) 38) 39)



Figure 7: Overview of the SWOT SSH spectral requirements (image credit: NASA) 40)

Legend to Figure 7: SSH error spectrum (red curve) as a function of spatial frequency. Shown, for reference is the SSH spectrum for a reference Jason pass (pass 132) (jagged line). Also shown as the solid black line is the expected spectral continuation. The intersection of the spectral signal with the noise floor at 15 km determines the resolving capabilities for the SWOT instrument. As can be seen, instrument noise dominates the Jason signal for wavelengths smaller than ~100 km.


Integrated measurement approach:

SWOT utilizes an integrated measurement approach, which includes the KaRIn system to observe in two off-nadir swaths, each of 50 km. KaRIn produces ocean and surface water heights and -co-registered weather imagery and elevations of 50 m and 1 km resolutions for hydrology and ocean communities, respectively. KaRIn includes an experimental nadir channel, either as a NNI (Near-Nadir Interferometer), or as a KNA (Ka-band Nadir Altimeter). The NNI is baselined. Both provide complimentary measurements to KaRIn and to support calibration and validation. The CNES-supplied Jason-heritage nadir altimeter specifically addresses SSH for long spatial wavelengths. The Jason-heritage microwave radiometer corrects the nadir altimeter range measurements for wet tropospheric delay and the GPS and DORIS receivers, with the LRA(Laser Retroreflector Assembly), provide precision orbit determination. The integrated measurement approach is illustrated in Figure 8 (Ref. 24).


Figure 8: SWOT integrated measurement approach (NASA, CNES)

KaRIn instrument: KaRIn is the primary instrument used to measure the swath of ocean and fresh water elevations. The instrument concept and core technologies for KaRIn were originally developed from NASA's ESD (Exploration Systems Development) efforts in the 2000's to develop the WSOA (Wide Swath Ocean Altimeter), a Ku-band centimeter-level precision concept for ocean observing that was developed to a substantial level of maturity, but deferred due to budgetary constraints. It demonstrated through hardware prototypes the ability to build very stable mechanical structures, phase stability, and ocean onboard processing directly relevant to the SWOT KaRIn instrument (Ref. 24).

The KaRIN instrument is expected to have a mass of ~294 kg, an orbital average power of ~ 810 W, and an average data rate of ~ 271 Mbit/s over land and ~ 3 Mbit/s over the ocean with onboard data processing. The overall size is: 3.0 m x 2.8 m x 2.8 m in stowed configuration, and 5.0 m x 10.6 m x 1.5 m in deployed configuration. KaRIn will use two graphine composite deployment masts attached to a central metering structure which also incorporates the antenna feeds. At the tip of each mast is a reflectarray support truss structure with two deployable wings. The configuration also takes advantage of the large transmit power (~1.5 kW) from the swath antennas to add receive channels pointing slightly off-nadir to eliminate the interference nadir gap to ±4 km and implement a synthetic aperture nadir altimeter, the NNI (Near Nadir Altimeter). The instrument detail, deployable reflectarray antenna, and the science mode of operations are illustrated in Figures 9, 10, and 6, respectively.


Figure 9: KaRIn instrument detail (image credit: NASA/JPL, CNES)


Figure 10: KaRIn deployable reflectarray (image credit: NASA/JPL, CNES)

Center frequency

35.75 GHz

Tx bandwidth, Tx pulse width

200 MHz, 4.5 µs

PRF (Pulse Repetition Frequency)

2 x 4420 Hz (average)

Peak transmit power (EOL)

1500 W

Physical baseline length

10 m

Antenna size

5 m x 0.25 m

Boresight look angle


Polarization, right swath


Polarization, left swath


Table 1: KaRIn instrument science mode operations parameters

Instrument technology readiness: The SWOT instruments, aside from KaRIn, are based on mature technologies derived from the Jason series altimetry missions and other projects. The dual-frequency nadir altimeter is based on an evolution of the Jason Poseidon-3 instrument and/or a design based on the SIRAL (SAR/Interferometric Radar Altimeter) flown on the CryoSat-2 mission of ESA (European Space Agency). Similarly, the three frequency microwave radiometer is of Jason series heritage. The GPSP and DORIS POD receivers are from existing product lines at Broad Reach Engineering and TAS (Thales Alenia Space). The LRA is a build to point copy of those used on the Jason series of spacecraft. The KaRIn instrument contains several technology development items. These are the RFU, the HPA (High Power Amplifier), the KaRIn digital electronics subsystem, and the reflectarray antenna. Their TRLs (Technology Readiness Levels) currently (2012) range from 3 to 5. All of these instrument areas will reach TRL 6 by the KaRIn PDR (Preliminary Design Review), scheduled for mid 2015, following a detailed and rigorous technology development plan. Fall-backs, using existing mature technologies, have been identified. Otherwise, 80% of the components within the instrument assembly require no new technology (Ref. 24).




The SWOT flight system is the spaceborne element of the mission. It is composed of the spacecraft bus, supplied by CNES, and two payload modules, the nadir payload module and the KaRIn payload module. The spacecraft bus provides basic services to the payload modules and includes C&DH (Command and Data Handling) subsystem, the EPS (Electrical Power Subsystem), ADCS (Attitude Determination and Control) subsystem, TCS (Thermal Control Subsystem), and the RF communication subsystem. The 35 m2 area twin solar arrays are oversized to minimize disturbances from array articulation. The arrays are fixed along the velocity vector also to minimize dynamic disturbances.

Other features of the spacecraft bus are batteries with 320 Ah capacity to support 2 kW observatory average power requirements, a SSR (Solid State Recorder) of 2.3 Tbit capacity, and a propulsion subsystem with a propellant tank capacity to meet the French Law on orbital debris mitigation.

The spacecraft bus uses high heritage technologies and generic standards developed through the CNES ISIS program. The nadir payload module accommodates all the science instruments aside from KaRIn [microwave radiometer, nadir altimeter, DORIS,GPSP(GPS Payload receiver), and LRA], and the X-band communication subsystem for the high rate downlink of the science data, including KaRIn's. The nadir payload module faces nadir and is mounted to the KaRIn payload module, which in turn is mounted to the spacecraft bus. The KaRIn payload module accommodates the KaRIn instrument, including the reflector antennas, the RF feeds and electronics, antenna booms, and a precision gyro to measure the roll parameters.

The nadir and KaRIn payload modules will be integrated and tested in parallel prior to environmental testing at JPL and subsequent shipment to France for integration with the spacecraft bus. This approach maximizes schedule efficiency and results in a fully qualified and integrated Nadir/KaRIn payload module assembly. The flight system configuration is illustrated in Figure 11 (Ref. 24).


Figure 11: The flight system configurations (image credit: CNES, NASA/JPL)

Spacecraft launch mass

1700 kg

Spacecraft power

2 kW total power demand

Solar panel size

35 m2


150 kg battery mass (320 Ah capacity)

Mass memory size

2.3 TB SSR capacity

KaRIn data rate

360 Mbit/s high rate between KaRIn and the SSR


130 liter propellant tank

Spacecraft envelope

5m total observatory height and 23 m span

Mission life

3 years (5 years goal)

Table 2: SWOT spacecraft characteristics


Launch: A launch of the SWOT spacecraft is planned for the 2020 using a NASA medium-class launch vehicle.

Orbit: During the six month commissioning/calibration period, SWOT will be flown in an 858 km altitude, 78º inclination, 1 day fast repeat orbit. Following its completion, the SWOT orbit will then be raised to an altitude of 873 km, inclination = 78º, with a repeat cycle = 22 days (Ref. 24).


Figure 12: SWOT spacecraft concept: current design (image credit: NASA/JPL, CNES)


Figure 13: Artist's rendition of the deployed SWOT spacecraft (mage credit: NASA/JPL)



Ground segment:

The ground segment architecture integrates all of the functions required to completely support mission operations. These elements provide various services: mission planning, sequence generation, station scheduling, spacecraft analysis, orbit determination, trajectory analysis and planning, maneuver design, instruments analysis, time correlation, data capture and distribution, science data gap reporting, generation of products for science support, as illustrated in Figure 15.

Spacecraft communication services will be provided by CNES Network Operation Center. SWOT will benefit from the CNES new multimission capabilities of ISIS (Initiative for Space Innovative Standards) for Spacecraft Command and Control, currently under development for future CNES missions.

JPL and CNES will provide engineering monitoring and commands for operating their respective instruments. Science data will be transmitted via X-band, while engineering telemetry and uplink data will be communicated via S-band, to the CNES provided Ground Station Network. There will be one pass per orbit of Inuvik/ Kiruna & Aussaguel Stations including Kiruna / Aussaguel overlapping plus one pass per day on HBK (Hartebeesthoek), South Africa. Each pass is relatively short in duration, less than 10 minutes. The spacecraft will downlink raw science data at a rate of 620 Mbit/s . Once the science data is downlinked to the ground, it is delivered to the SDS (Science Data System) at JPL and CNES.

Amongst the many key challenges to the SDS is the large data volume with an average production volume of 7 Tbit/day acquired by the Payload, and the consequent huge volume of data products produced (on the order of 23 PB for 3 years of operation). JPL and CNES have reached an initial agreement to jointly develop and operate the science data system using common data processing flow and interfaces, but each institution will develop their own unique data production and distribution system.


Figure 14: Overall Ground System architecture, including links to spacecraft (image credit: CNES, NASA/JPL)



Tracking Stations

- CNES S?band stations: Downlink for spacecraft engineering. Uplink commanding
- X-band stations (620 Mbit/s net data rate): Downlink for science and associated engineering data

Front End Networks

- Networks to/from CNES S-band stations to CNES (contractor) spacecraft operations center
- Networks from CNES X-band stations to X-band network center
- Network from CNES to/from JPL for S-band engineering data, payload commands
- Network from CNES X-band Data Center to JPL and CNES operation centers

Spacecraft Control Center (SCC, CNES spacecraft contractor)

Real time monitoring of spacecraft and payload via S-band housekeeping telemetry

Payload Operations Centers (POC)

- JPL: NRT (Near Real Time) health monitoring of KaRIn, GPS, Radiometer
- CNES: NRT health monitoring of Jason Altimeter Suite

Science Processing Centers

- JPL: Processing of KaRIn and associated data, POD
- CNES: Processing of Jason Suite, POD

Data Archiving and Distribution Centers

- JPL: NASA-specified archive center (PO.DAAC)
- CNES: Aviso

Project Data Distribution Networks

- JPL?CNES link
- Science Processing Centers to Archiving/Distribution Centers

Table 3: Proposed SWOT Ground System Elements


Figure 15: SWOT ground data system architecture (image credit: CNES, NASA/JPL)

The SWOT science data products will include ocean, hydrology, and enhanced hydrology higher level products in addition to level 1 products. These data products will be processed in a coordinated fashion by the NASA and CNES SDSs (Science Data processing Centers) and distributed to the NASA PO.DACC (Physical Oceanography Data Active Archive Center) and the CNES AVISO (Archivage, Validation et Interprétation des données des Satellites Océanographiques) systems for distribution to scientific and other users.

Data product


Initial data delivery to PO.DAAC*

Level 1

KaRIn, altimeter and radiometer sensor and ancillary data

Commissioning + 7 mos.

Level 2 Ocean

Maps of sea surface height, slope, height uncertainty, and backscatter

Commissioning + 7 mos.

Level 2 Hydrology

Surface water height, slope with uncertainties, water classification masks

Commissioning + 7 mos.

Level 2 enhanced hydrology

Global river discharge estimates**, floodplain height map (annual update) ***

Commissioning + 12 mos.

* The terminology “Commissioning+ x mos.” is understood to mean x-months after the completion of the Commissioning Phase
** River discharge has no performance requirements, but performance will be characterized as part of the validation process
*** Floodplain map made from multi-temporal water elevations

Table 4: Overview of SWOT data products

The SWOT NASA mission will study the global oceans at unprecedented temporal and spatial scales and provide unique insight into global terrestrial surface waters, including lake level height and river discharge volume. It is an international partnership involving the French space agency, CNES, and CSA (Canadian Space Agency). CSA is supporting the development of a sophisticated EIK (Enhanced Interaction Klystron) that will be at the heart of the interferometric radar instrument, KaRIn, on the SWOT mission.

An airborne version of SWOT, called AirSWOT, has been developed at NASA/JPL to provide calibration and validation for the mission when on orbit as well as to support science and technology during mission development. The first AirSWOT science flights will start in 2013. 41)


2) Ernesto Rodríguez, “Surface Water and Ocean Topography Mission (SWOT), Science Requirements Document,” NASA/JPL, March 19, 2009, URL:

3) Lee-Lueng Fu, Douglas Alsdorf, Ernesto Rodriguez, Rosemary Morrow, Nelly Mognard, Juliette Lambin, Parag Vaze, Thierry Lafon, “The SWOT (Surface Water and Ocean Topography) Mission: Spaceborne Radar Interferometry for Oceanographic and Hydrological Applications,” Proceedings of OceanObs'09, Venice, Italy, Sept. 21-25, 2009, URL:


5) “WatER and ITC: The Proposed Water Elevation Recovery satellite mission,”Symposium: 15 Years of Progress in Radar Altimetry, March 13-18, 2006, URL:

6) V. Enjolras, E. Rodriguez, P. Bates, S. Niemeyer, Ad De Roo, N. Mognard, A. Cazenave, “The WatER Mission in Europe: how can it help science?” Symposium: 15 Years of Progress in Radar Altimetry, Venice, Italy, March 13-16, 2006, URL:

7) V. Enjolras, P. Vincent, J.-C. Souyris, E. Rodriguez, L. Phillippou, A. Cazenave, “Performances Study of Interferometric Radar Altimeters: From the Instrument to the Global Mission Definition,” Symposium: 15 Years of Progress in Radar Altimetry, Venice, Italy, March 13-16, 2006, URL:

8) A. Alsdorf, D. Lettenmaier, C. Vörösmarty, “The Need for Global, Satellite-based Observations of Terrestrial Surface Waters,” EOS Transactions of AGU, Vol. 84, No. 29, 22 July 2003, pp. 269-280, URL:

9) Lee-Lueng Fu, Wide-Swath Ocean Altimeter Science Working Group, “Wide-Swath Altimetric Measurement of Ocean Surface Topography,” JPL Publication 03-002, Feb. 2003, URL:

10) N. Mognard, D. Alsdorf, E. Rodriguez, “WatER: The proposed Water Elevation Recovery satellite mission,” Symposium: 15 Years of Progress in Radar Altimetry, Venice, Italy, March 13-16, 2006

11) E. Caubet, N. Steunou, M. Meerman, E. Thouvenot, P. Vincent, “Phase B and breadboard results of the Ka-band altimeter for future micro-satellite altimetry missions,” Proceedings of IGARSS 2003, Toulouse, France, July 21-25, 2003

12) R. J. J. Dost, B. H. P. Maathuis, Z. Su, “ITC and WatER: The Proposed Water Elevation Recovery satellite mission,” Symposium: 15 Years of Progress in Radar Altimetry, Venice, Italy, March 13-18, 2006

13) N. Mognard, D. Alsdorf, E. Rodriguez, “WatER: The proposed Water Elevation Recovery satellite mission,” Symposium: 15 Years of Progress in Radar Altimetry, Venice, Italy, March 13-18, 2006

14) V. Enjolras, E. Rodriguez, “An Assessment of the Ka band Interferometric Radar Altimeter for Monitoring Rivers and Lakes with the WatER Mission,” Proceedings of IGARSS 2007 (International Geoscience and Remote Sensing Symposium), Barcelona, Spain, July 23-27, 2007

15) E. Rodríguez, “SWOT Technology and Expected Performance,” SWOT Hydrology Workshop September 15-17, 2008, The Ohio State University, Columbus Ohio, USA, URL:

16) Lee-Lueng Fu, Douglas Alsdorf, Erensto Rodriguez, Rosemary Morrow, Nelly Mognard, Juliette Lambin, Parag Vaze, Thierry Lafon, “The SWOT (Surface Water and Ocean Topography) Mission: Spaceborne Radar Interferometry for Oceanographic and Hydrological Applications,” March, 2009, URL:

17) Michael Durand, Lee-Lueng Fu, Dennis P. Lettenmaier, Douglas, E. Alsdorf, Ernesto Rodriguez, Daniel Esteban-Fernandez, “The Surface Water and Ocean Topography Mission: Observing Terrestrial Surface Water and Oceanic Submesoscale Eddies,” Proceedings of the IEEE, Vol. 98, No. 5, May 2010, Special Issue: Satellite Remote Sensing: Monitoring Water, Carbon & Global Climate Change, URL:


19) SWOT Hydrology Workshop, Sept. 15-17, 2008, OSU (Ohio State University), Columbus Ohio, Sponsored by NASA, CNES, JPL, and OSU’s Climate, Water, and Carbon Program, URL:

20) Lee-Lueng Fu, Douglas Alsdorf, Rosemary Morrow, Ernesto Rodriguez, Nelly Mognard, “SWOT: The Surface Water and Ocean Topography Mission - Wide-Swath Altimetric Measurement of Water Elevation on Earth,” JPL Publication 12-05, Feb. 2012, URL:

21) “SWOT mission enters Phase A,” NASA/JPL, Nov. 20.2012, URL:

22) Ernesto Rodríguez, “Surface Water and Ocean Topography Mission (SWOT) - Science Requirements Document,” Initial Release, March 19, 2009, URL:

23) Juliette Lambin, “CNES Interest in ocean currents monitoring,” March 7, 2012, URL:

24) Steven P. Neeck, Eric J. Lindstrom, Parag V. Vaze, Lee-Lueng Fu, “Surface Water and Ocean Topography (SWOT) Mission,” Proceedings of SPIE Remote Sensing 2012, 'Sensors, Systems, and Next-Generation Satellites,' Edinburgh, Scotland, UK, Vols. 8531-8539, Sept. 24-27, 2012

25) Thierry Lafon , Vincent Albouys , Parag Vaze, Brian Pollard, “The SWOT Mission Concept Description,” Proceedings of the 1st Workshop on Ka-band Earth Observation Radar, ESA/ESTEC, Noordwijk, The Netherlands, Oct. 8-9, 2012

26) A. Mallet, Eric Rodriguez, Roger Fjortoft, Thierry Lafon, Parag Vaze, “Surface Water and Ocean Topography Measurement Principle,” Proceedings of the 2nd Workshop on Advanced RF Sensors and Remote Sensing Instruments 2009, Noordwijk, The Netherlands, Nov. 17-18, 2009

27) Nelly Mognard, Sylvain Biancamaria, Doug Alsdorf, Aaron Boone, Stéphane Calmant, Anny Cazenave, Jean-François Crétaux, Philippe Maisongrande , and the SWOT Participants, “SWOT: The Surface Water and Ocean Topography Satellite Mission,” Earth Observation and Water Cycle Science - Towards a Water Cycle Multi-mission Observation Strategy, ESA/ESRIN, Frascati, Italy, Nov. 18-20, 2009

28) Daniel Esteban-Fernandez, Lee-Lueng Fu, Ernesto Rodriguez, Shannon Brown, Richard Hodges, “Ka-band SAR Interferometry Studies for the SWOT Mission,” Proceedings of IGARSS (IEEE International Geoscience and Remote Sensing Symposium) 2010, Honolulu, HI, USA, July 25-30, 2010

29) Parag Vaze, Vincent Albuys, Daniel Esteban-Fernandez, Thierry Lafon, Juliette Lambin, Alain Mallet, Ernesto Rodriguez, “The Surface Water and Ocean Mission: Building a Mission Concept zo Study the World's Oceans and Fresh Water,” Proceedings of the SPIE Remote Sensing Conference, Toulouse, France, Vol. 7826, Sept. 20-23, 2010, paper: 7826-35, 'Sensors, Systems, and Next-Generation Satellites XIV,' edited by Roland Meynart, Steven P. Neeck, Haruhisa Shimoda, doi: 10.1117/12.868439

30) Ernesto Rodriguez, Daniel Esteban-Fernandez, “The Surface Water and Ocean Topography Mission (SWOT): The Ka-band Radar Interferometer (KaRIn) for water level measurements at all scales,” Proceedings of the SPIE Remote Sensing Conference, Toulouse, France, Vol. 7826, Sept. 20-23, 2010, paper: 7826-36, 'Sensors, Systems, and Next-Generation Satellites XIV,' edited by Roland Meynart, Steven P. Neeck, Haruhisa Shimoda, doi: 10.1117/12.868525

31) D. Esteban-Fernandez, Ernesto Rodriguez, Lee-Lueng Fu, Douglas Alsdorf, Parag Vaze, “The Surface Water and Ocean Topography Mission: Centimetric Spaceborne Radar Interferometry,” Proceedings of the SPIE Remote Sensing Conference, Toulouse, France, Vol. 7826, Sept. 20-23, 2010, paper: 7826-37, Sensors, Systems, and Next-Generation Satellites XIV, edited by Roland Meynart, Steven P. Neeck, Haruhisa Shimoda, doi: 10.1117/12.868535

32) Jean-Claude Souyris, “Upcoming altimeter measurements: explaining Ka-band, SAR mode, interferometric SAR,” 2010 OSTST (Ocean Surface Topography Science Team) meeting, Lisbon, Portugal, Oct. 18-20, 2010, URL:

33) A. Mallet, B. Mametsa, R. Fjortoft, J. C. Souyris,V. Albouys, T. Lafon, “KaRIn/SWOT Performance analysis tool- Application to near nadir swath extension,” 2010 OSTST (Ocean Surface Topography Science Team) meeting, Lisbon, Portugal, Oct. 18-20, 2010, URL:

34) Ernesto Rodriguez, “The Surface Water and Ocean Topography (SWOT) Mission,” 2010 OSTST (Ocean Surface Topography Science Team) meeting, Lisbon, Portugal, Oct. 18-20, 2010, URL:

35) Roger Fjortoft, Jean-Claude Lalaurie, Nadine Pourthié, Jean-Claude Souyris, Jean-François Nouvel, Joseph Martinot-Lagarde , Hélene Oriot , Pierre Borderies, “Near-nadir Ka-band Interferometric Acquisitions and Backscattering Measurements in Preparation of the SWOT Mission,” Proceedings of the 1st Workshop on Ka-band Earth Observation Radar, ESA/ESTEC, Noordwijk, The Netherlands, Oct. 8-9, 2012

36) J. F. Nouvel, H. Oriot, J. Martinot-Lagarde, “Ka-band Radar backscattering measurements over water surfaces,” Proceedings of the 1st Workshop on Ka-band Earth Observation Radar, ESA/ESTEC, Noordwijk, The Netherlands, Oct. 8-9, 2012

37) Doug Alsdorf, Nelly Mognard, Jean-Francois Cretaux, Stephane Calmant, Dennis Lettenmaier, Ernesto Rodriguez, “Recent Hydrologic Developments in the SWOT Mission,” AGU Fall Meeting, 2012, URL:

38) Douglas Alsdorf, Nelly Mognard, Ernesto Rodriguez, “Transforming Surface Water Hydrology through SWOT Altimetry,” Proceedings of the Symposium '20 years of Progress in Radar Altimetry', Venice, Italy, Sept. 24-29, 2012, (ESA SP-710, Feb. 2013)

39) Lee-Lueng Fu, Douglas Alsdorf, Ernesto Rodriguez, Rosemary Morrow, Nelly Mognard, Parag Vaze, Thierry Lafon, “The Proposed Surface Water and Ocean Topography (SWOT) Mission,” Proceedings of the Symposium '20 years of Progress in Radar Altimetry', Venice, Italy, Sept. 24-29, 2012, (ESA SP-710, Feb. 2013)

40) Ernesto Rodríguez, “Surface Water and Ocean Topography Mission (SWOT), Science Requirements Document,” Second Release (V1.1), January 26, 2012, NASA/JPL, URL:

41) Becky Oskin, “Water-Mapping Mission Takes Flight,” NBCNews, March 7, 2013, URL:

The information compiled and edited in this article was provided by Herbert J. Kramer from his documentation of: ”Observation of the Earth and Its Environment: Survey of Missions and Sensors” (Springer Verlag) as well as many other sources after the publication of the 4th edition in 2002. - Comments and corrections to this article are always welcome for further updates.