OSTM/Jason-2, or the Ocean Surface Topography Mission on the Jason-2 satellite, was an international Earth observation satellite mission that continued the sea surface height measurements begun in 1992 by the joint NASA/CNES TOPEX/Poseidon mission and followed by the NASA/CNES Jason-1 mission launched in 2001.
|Ocean Surface Topography Mission|
Artist's interpretation of the Jason-2 satellite
|Mission type||Earth orbiter|
|Operator||NASA, NOAA, CNES, EUMETSAT|
|Website||Ocean Surface Topography from Space|
|Mission duration||Design: 3 years |
Final: 11 years, 3 months and 11 days
|Manufacturer||Thales Alenia Space|
|Launch mass||510 kilograms (1,120 lb)|
|Start of mission|
|Launch date||June 20, 2008, 07:46:25 UTC|
|Rocket||Delta II 7320-10C D334|
|Launch site||Vandenberg SLC-2W|
|End of mission|
|Deactivated||October 1, 2019|
|Semi-major axis||7,715.0 kilometers (4,793.9 mi)|
|Perigee altitude||1,332 kilometers (828 mi)|
|Apogee altitude||1,343 kilometers (835 mi)|
|Argument of perigee||273,8057 degrees|
|Mean anomaly||280,076 degrees|
|Epoch||09 April 2016 21:16:10 UTC|
Like its two predecessors, OSTM/Jason-2 used high-precision ocean altimetry to measure the distance between the satellite and the ocean surface to within a few centimeters. These very accurate observations of variations in sea surface height—also known as ocean topography—provide information about global sea level, the speed and direction of ocean currents, and heat stored in the ocean.
Jason-2 was built by Thales Alenia Space using a Proteus platform, under a contract from CNES, as well as the main Jason-2 instrument, the Poseidon-3 altimeter (successor to the Poseidon and Poseidon 2 altimeter on-board TOPEX/Poseidon and Jason-1)
OSTM/Jason-2 was launched on June 20, 2008, at 07:46 UTC, from Space Launch Complex 2W at Vandenberg Air Force Base in California, by a Delta II 7320 rocket. The spacecraft separated from the rocket 55 minutes later.
It was placed in a 1,336 km (830 mi) circular, non-sun-synchronous orbit at an inclination of 66 degrees to Earth's equator, allowing it to monitor 95 percent of Earth's ice-free ocean every 10 days. Jason-1 was moved to the opposite side of Earth from Jason-2 and now flies over the same region of the ocean that Jason-2 flew over five days earlier. Jason-1's ground tracks fall midway between those of Jason-2, which are about 315 kilometers (196 mi) apart at the equator. This interleaved tandem mission provided twice the number of measurements of the ocean's surface, bringing smaller features such as ocean eddies into view. The tandem mission also helped pave the way for a future ocean altimeter mission that would collect much more detailed data with its single instrument than the two Jason satellites did together.
With OSTM/Jason-2, ocean altimetry made the transition from research into operational mode. Responsibility for collecting these measurements moved from the space agencies to the world's weather and climate forecasting agencies, which use them for short-range, seasonal, and long-range weather and climate forecasting.
Spaceborne radar altimeters have proven to be superb tools for mapping ocean-surface topography, the hills and valleys of the sea surface. These instruments send a microwave pulse to the ocean's surface and time how long it takes to return. A microwave radiometer corrects any delay that may be caused by water vapor in the atmosphere. Other corrections are also required to account for the influence of electrons in the ionosphere and the dry air mass of the atmosphere. Combining these data with the precise location of the spacecraft makes it possible to determine sea-surface height to within a few centimetres (about one inch). The strength and shape of the returning signal also provides information on wind speed and the height of ocean waves. These data are used in ocean models to calculate the speed and direction of ocean currents and the amount and location of heat stored in the ocean, which, in turn, reveals global climate variations.
Another payload aboard Jason-2 is the T2L2 (Time Transfer by Laser Link) instrument. T2L2 is used to synchronize atomic clocks at ground stations, and to calibrate the on-board clock of the Jason-2 DORIS instrument. On November 6, 2008, CNES reported the T2L2 instrument was working well.
OSTM/Jason-2 was a joint effort by four organizations. The mission participants were:
CNES provided the spacecraft, NASA and CNES jointly provided the payload instruments, and NASA's Launch Services Program at the Kennedy Space Center was responsible for the launch management and countdown operations. After completing the on-orbit commissioning of the spacecraft, CNES handed over operation and control of the spacecraft to NOAA in October 2008.
CNES processed, distributed, and archived the research-quality data products that became available in 2009. EUMETSAT processed and distributed operational data received by its ground station to users in Europe and archived that data. NOAA processed and distributed operational data received by its ground stations to non-European users and archived that data along with the CNES data products. NOAA and EUMETSAT both generated near-real-time data products and distributed them to users.
NASA evaluated the performance of the following instruments: the advanced microwave radiometer, the Global Positioning System payload, and the laser retroreflector assembly. NASA and CNES also validated scientific data products together. NASA's Jet Propulsion Laboratory in Pasadena, California, managed the mission for NASA's Science Mission Directorate in Washington.
The two previous altimetry missions, TOPEX/Poseidon and Jason-1, led to major advances in the science of physical oceanography and in climate studies. Their 15-year data record of ocean surface topography provided the first opportunity to observe and understand the global change of ocean circulation and sea level. Their results improved scientific understanding of the role of the ocean in climate change and improved weather and climate predictions. Data from these missions were used to improve ocean models, forecast hurricane intensity, and identify and track large ocean/atmosphere phenomena such as El Niño and La Niña. The data was also used in daily applications as diverse as routing ships, improving the safety and efficiency of offshore industry operations, managing fisheries and tracking marine mammals.
Some of the areas in which TOPEX/Poseidon and Jason-1 have made major contributions, and to which OSTM/Jason-2 continued to add, are:
The missions revealed the surprising variability of the ocean, how much it changes from season to season, year to year, decade to decade and on even longer time scales. They ended the traditional notion of a quasi-steady, large-scale pattern of global ocean circulation by proving that the ocean is changing rapidly on all scales, from huge features such as El Nino and La Nina, which can cover the entire equatorial Pacific, to tiny eddies swirling off the large Gulf Stream in the Atlantic.
Measurements by TOPEX/Poseidon and Jason-1 show that mean sea level has been rising by about three millimeters (.12 inches) a year since 1993. This is about twice the estimates from tide gauges for the previous century, indicating a possible recent acceleration in the rate of sea level rise.
The data record from these altimetry missions has given scientists important insights into how global sea level is affected by natural climate variability, as well as by human activities.
TOPEX/Poseidon and Jason-1 made clear the importance of planetary-scale waves, such as Rossby and Kelvin waves. Thousands of kilometers wide, these waves are driven by wind under the influence of Earth's rotation and are important mechanisms for transmitting climate signals across the large ocean basins. At high latitudes, they travel twice as fast as scientists believed previously, showing the ocean responds much more quickly to climate changes than was known before these missions.
The precise measurements of TOPEX/Poseidon's and Jason-1 have brought knowledge of ocean tides to an unprecedented level. The change of water level due to tidal motion in the deep ocean is known everywhere on the globe to within 2.5 centimeters (one inch). This new knowledge has revised notions about how tides dissipate. Instead of losing all their energy over shallow seas near the coasts, as previously believed, about one third of tidal energy is actually lost to the deep ocean. There, the energy is consumed by mixing water of different properties, a fundamental mechanism in the physics governing the general circulation of the ocean.
TOPEX/Poseidon and Jason-1 observations provided the first global data for improving the performance of the numerical ocean models that are a key component of climate prediction models.
Validated data products in support of improved weather, climate and ocean forecasts were distributed to the public within a few hours of observation. Beginning in 2009, other data products for climate research were made available a few days to a few weeks after observations were taken by the satellite.
Altimetry data have a wide variety of uses from basic scientific research on climate to ship routing. Applications include:
The OSTM/Jason-2 mission concluded on October 1, 2019, after NASA and its mission partners made the decision to decommission the spacecraft upon discovering significant recent deterioration of the spacecraft's power systems. Because Jason-2 is orbiting at an altitude of over 1,300 kilometers (810 mi), NASA estimates that it will remain in orbit for at least 500 to 1,000 years after decommissioning.
The fourth spacecraft to be part of the Ocean Surface Topography Mission is Jason-3. Like its predecessors, the primary instrument aboard Jason-3 is a radar altimeter. Additional instruments include:
Jason-3 launched from Vandenberg Air Force Base on board a SpaceX Falcon 9 v1.1 launch vehicle in 2016. The satellite was shipped to Vandenberg Air Force Base on June 18, 2015, and after delays due to a June 2015 Falcon 9 launch failure, the mission was launched January 17, 2016 at 10:42:18 AM PST.
The technologies and data-sets pioneered by Jason-1, OSTM/Jason-2, and Jason-3, will be continued through the Sentinel-6/Jason-CS satellites, planned for launch in 2020 and 2025.
Media related to Ocean Surface Topography Mission at Wikimedia Commons
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Jason-1 was a satellite oceanography mission to monitor global ocean circulation, study the ties between the ocean and the atmosphere, improve global climate forecasts and predictions, and monitor events such as El Niño and ocean eddies.Jason-3
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Founded in the 1930s, the JPL is currently owned by NASA and managed by the nearby California Institute of Technology (Caltech) for NASA. The laboratory's primary function is the construction and operation of planetary robotic spacecraft, though it also conducts Earth-orbit and astronomy missions. It is also responsible for operating NASA's Deep Space Network.
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Ocean surface topography or sea surface topography, also called ocean dynamic topography, are highs and lows on the ocean surface, similar to the hills and valleys of Earth's land surface depicted on a topographic map.
These variations are expressed in terms of average sea surface height (SSH) relative to the Earth's geoid.
The main purpose of measuring ocean surface topography is to understand the large-scale ocean circulation.
Orbital meteorological and remote sensing systems
Thuraya 3 | TecSAR | Ekspress AM-33 | Progress M-63 | STS-122 (Columbus) | Thor 5 | Kizuna | Jules Verne ATV | STS-123 (Kibō ELM-PS · Dextre · Spacelab MD002) | USA-200 | AMC-14 | USA-201 | DirecTV-11 | SAR-Lupe 4 | Soyuz TMA-12 | ICO G1 | C/NOFS | Vinasat-1 · Star One C2 | Tianlian I-01 | GIOVE-B | Cartosat-2A · TWSAT · CanX-2 · CUTE-1.7 + APD II · Delfi-C3 · AAUSAT-II · Compass-1 · SEEDS-2 · CanX-6 · Rubin-8 | Amos-3 | Progress M-64 | Galaxy 18 | Kosmos 2437 · Kosmos 2438 · Kosmos 2439 · Yubileiny | Feng Yun 3A | STS-124 (Kibō PM) | ChinaSat 9 | Fermi | Skynet 5C · Türksat 3A | Orbcomm FM29 · Orbcomm FM37 · Orbcomm FM38 · Orbcomm FM39 · Orbcomm FM40 · Orbcomm FM41 | OSTM/Jason-2 | Kosmos 2440 | Badr-6 · ProtoStar 1 | EchoStar XI | SAR-Lupe 5 | Kosmos 2441 | Trailblazer · NanoSail-D · PRESat · Explorers | Superbird-C2 · AMC-21 | Omid | Inmarsat-4 F3 | Tachys · Mati · Choma · Choros · Trochia | Huan Jing 1A · Huan Jing 1B | GeoEye-1 | Progress M-65 | Nimiq-4 | Galaxy 19 | Kosmos 2442 · Kosmos 2243 · Kosmos 2444 | Shenzhou 7 (Banxing-1) | Ratsat | THEOS | Soyuz TMA-13 | IBEX | Chandrayaan-1 (MIP) | Shijian 6E · Shijian 6F | COSMO-3 | Venesat-1 | Chuang Xin 1B · Shiyan Weixing 3 | Astra 1M | Kosmos 2445 | STS-126 (Leonardo MPLM · PSSC-1) | Progress M-01M | Yaogan 4 | Kosmos 2446 | Yaogan 5 | Hot Bird 9 · Eutelsat W2M | Feng Yun 2E | Kosmos 2447 · Kosmos 2448 · Kosmos 2449
Payloads are separated by bullets ( · ), launches by pipes ( | ). Manned flights are indicated in bold text. Uncatalogued launch failures are listed in italics. Payloads deployed from other spacecraft are denoted in brackets.