Lesson 3 of 6 · Jason
Jason: preserve a sea-level record across spacecraft
8 minute lesson · 3 checks along the way
Your goal for this lessonExplain how successive Jason missions extend an ocean-height record and why overlap measurements matter.
In this lesson 3 sections · 3 checks
Using archive links & definitions
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Continue a long observing record
The Jason series followed the French-American TOPEX/Poseidon mission in observing ocean-surface height. Jason-1 launched in 2001; Jason-2 followed in 2008 and Jason-3 in 2016. Their scientific value includes both individual observations and continuity across changing spacecraft. A trend that spans decades needs careful connections between instruments rather than a simple sequence of launch anniversaries.
measures the satellite-to-surface range. Combining that range with a well-determined orbit allows researchers to estimate sea-surface height relative to a reference. Ocean topography reflects processes including circulation, tides and changes in stored heat and water. A local observation is not automatically the same quantity as a global mean, which requires broader sampling and processing.
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Compare instruments during an overlap
Successive missions can observe nearly the same conditions during a tandem phase. In 2016, Jason-3 followed Jason-2 about two minutes apart in their reference orbit. Those paired observations helped teams compare measurements while limiting the effects of a changing ocean. The purpose was to establish how the new observations relate to the existing record.
Imagine two instruments observing a fictional stable target during an overlap. One repeatedly reports a height 2 centimeters above the other. That difference is evidence to investigate calibration, orbit and processing biases; it is not proof that the ocean suddenly rose when the satellite name changed. The correction must be supported across suitable observations, rather than chosen to force a preferred climate trend.
Jason-1 leaves the launch pad aboard a Delta II in December 2001. Its measurements would extend the earlier TOPEX/Poseidon record. Launch establishes the mission’s flight history; cross-calibration establishes how its data connect to other altimeters.
Look closely
Which evidence connects successive sea-level measurements?
See what to notice
Overlap observations, orbit solutions and documented calibration connect the records; launch imagery does not establish their relative measurement offsets.
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Separate weather-scale changes from a long trend
A single location can rise or fall as currents, winds and tides change. To investigate long-term mean sea level, researchers apply appropriate corrections, preserve a consistent reference and combine observations over time and space. Short-lived regional variability and a multi-decade global trend answer different questions. Both can be real without having the same sign on a particular day.
Jason-1 was decommissioned in 2013, but its calibrated observations remain part of the historical record. Mission completion does not make archived data scientifically useless. Keeping instrument documentation, processing versions and overlap evidence allows later researchers to re-evaluate the series. The enduring achievement is a defensible measurement record that survives replacement of the equipment used to build it.
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Explore further · Optional
Go to the source
Explore the evidence behind this lesson. These optional readings and videos open in a new tab.
- Read: JPL: Jason-1 mission historyThe history establishes Jason-1’s 2001 launch and 2013 decommissioning. Its old projected Jason-3 launch date is superseded by the actual 2016 record.
- Read: NASA: Jason-3 launch and observing lineageCompare the explanation and its assumptions with the worked example in this lesson.
- Read: NASA: Jason-3 and Jason-2 cross-calibrationA dated February 2016 account of the tandem observing phase, not a claim about present-day orbit assignments.