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Thursday, August 17, 2017

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Get Ready for Monday's Total Solar Eclipse! Tips, Lessons & Activities from NASA/JPL Edu

NASA/JPL Education – Teachable Moment: Get Students Excited About Science With This Month's Total Solar Eclipse
 

Get Ready for Monday's Total Solar Eclipse

This Monday, Aug. 21, every state in the U.S. will have a chance to see one of the sky's most captivating shows, a solar eclipse. Some, in what's called the path of totality, will even get to see a total solar eclipse, where the moon completely covers the disk of the sun.

These lessons, activities and resources from NASA/JPL Edu will help you engage students in scientific observations and discovery before, during and after the eclipse. Plus find information on how solar eclipses work, how to safely view one in action and how to contribute to NASA science!

NASA/JPL Edu News – Teachable Moment – Eclipse 2017 Teachable Moment Blog – Learn all about the eclipse, how to watch it safely and how to make it a Teachable Moment for students.
Read more
NASA/JPL Edu Learn – Projects– How to Make a Pinhole Camera Project: How to Make a Pinhole Camera – Learn how to make your very own pinhole camera to safely see a solar eclipse in action!
Read more
NASA/JPL Edu Teach – Activities – Moon Phases Lesson: Moon Phases (Grades 1-6) – Students learn about the phases of the moon by acting them out.
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NASA/JPL Edu Teach – Activities – Measuring Solar Energy During an Eclipse NEW! Lesson: Measuring Solar Energy During an Eclipse (Grades 4-7) – Students use mobile devices to measure the impact a solar eclipse has on the energy received at Earth's surface.
Read more
NASA/JPL Edu Teach – Activities – Modeling the Earth-Moon System NEW! Lesson: Modeling the Earth-Moon System (Grades 6-8) – Students learn about scale models and distance by creating a classroom-size Earth-Moon system.
Read more
NASA/JPL Edu Teach – Activities – Epic Eclipse: A Pi in the Sky Math Challenge Lesson: Epic Eclipse: A Pi in the Sky Math Challenge (Grades 6-12) – In this lesson, students use the mathematical constant pi to approximate the area of land covered by the Moon's shadow during the eclipse.
Read more
NASA Eclipse 2017 Website NASA Eclipse 2017 Website – Find more eclipse info, including safety tips, maps and how to watch on NASA TV.
Read more

 

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JPL News - Day in Review

 

DAY IN REVIEW
NASA JPL latest news release
Scientists Improve Brown Dwarf Weather Forecasts

Dim objects called brown dwarfs, less massive than the Sun but more massive than Jupiter, have powerful winds and clouds -- specifically, hot patchy clouds made of iron droplets and silicate dust. Scientists recently realized these giant clouds can move and thicken or thin surprisingly rapidly, in less than an Earth day, but did not understand why.

Now, researchers have a new model for explaining how clouds move and change shape in brown dwarfs, using insights from NASA's Spitzer Space Telescope. Giant waves cause large-scale movement of particles in brown dwarfs' atmospheres, changing the thickness of the silicate clouds, researchers report in the journal Science. The study also suggests these clouds are organized in bands confined to different latitudes, traveling with different speeds in different bands.

"This is the first time we have seen atmospheric bands and waves in brown dwarfs," said lead author Daniel Apai, associate professor of astronomy and planetary sciences at the University of Arizona in Tucson.

Just as in Earth's ocean, different types of waves can form in planetary atmospheres. For example, in Earth's atmosphere, very long waves mix cold air from the polar regions to mid-latitudes, which often lead clouds to form or dissipate.

The distribution and motions of the clouds on brown dwarfs in this study are more similar to those seen on Jupiter, Saturn, Uranus and Neptune. Neptune has cloud structures that follow banded paths too, but its clouds are made of ice. Observations of Neptune from NASA's Kepler spacecraft, operating in its K2 mission, were important in this comparison between the planet and brown dwarfs.

"The atmospheric winds of brown dwarfs seem to be more like Jupiter's familiar regular pattern of belts and zones than the chaotic atmospheric boiling seen on the Sun and many other stars," said study co-author Mark Marley at NASA's Ames Research Center in California's Silicon Valley.

Brown dwarfs can be thought of as failed stars because they are too small to fuse chemical elements in their cores. They can also be thought of as "super planets" because they are more massive than Jupiter, yet have roughly the same diameter. Like gas giant planets, brown dwarfs are mostly made of hydrogen and helium, but they are often found apart from any planetary systems. In a 2014 study using Spitzer, scientists found that brown dwarfs commonly have atmospheric storms.

Due to their similarity to giant exoplanets, brown dwarfs are windows into planetary systems beyond our own. It is easier to study brown dwarfs than planets because they often do not have a bright host star that obscures them.

"It is likely the banded structure and large atmospheric waves we found in brown dwarfs will also be common in giant exoplanets," Apai said.

Using Spitzer, scientists monitored brightness changes in six brown dwarfs over more than a year, observing each of them rotate 32 times. As a brown dwarf rotates, its clouds move in and out of the hemisphere seen by the telescope, causing changes in the brightness of the brown dwarf. Scientists then analyzed these brightness variations to explore how silicate clouds are distributed in the brown dwarfs.

Researchers had been expecting these brown dwarfs to have elliptical storms resembling Jupiter's Great Red Spot, caused by high-pressure zones. The Great Red Spot has been present in Jupiter for hundreds of years and changes very slowly: Such "spots" could not explain the rapid changes in brightness that scientists saw while observing these brown dwarfs. The brightness levels of the brown dwarfs varied markedly just over the course of an Earth day.

To make sense of the ups and downs of brightness, scientists had to rethink their assumptions about what was going on in the brown dwarf atmospheres. The best model to explain the variations involves large waves, propagating through the atmosphere with different periods. These waves would make the cloud structures rotate with different speeds in different bands.

University of Arizona researcher Theodora Karalidi used a supercomputer and a new computer algorithm to create maps of how clouds travel on these brown dwarfs.

"When the peaks of the two waves are offset, over the course of the day there are two points of maximum brightness," Karalidi said. "When the waves are in sync, you get one large peak, making the brown dwarf twice as bright as with a single wave."

The results explain the puzzling behavior and brightness changes that researchers previously saw. The next step is to try to better understand what causes the waves that drive cloud behavior.

JPL manages the Spitzer Space Telescope mission for NASA's Science Mission Directorate, Washington. Science operations are conducted at the Spitzer Science Center at Caltech in Pasadena, California. Spacecraft operations are based at Lockheed Martin Space Systems Company, Littleton, Colorado. Data are archived at the Infrared Science Archive housed at the Infrared Processing and Analysis Center at Caltech. Caltech manages JPL for NASA. For more information about Spitzer, visit:

http://spitzer.caltech.edu

https://www.nasa.gov/spitzer

 

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Wednesday, August 16, 2017

JPL News - Day in Review

 

DAY IN REVIEW
NASA JPL latest news release
NASA-led Mission Studies Storm Intensification

A group of NASA and National Oceanic and Atmospheric Administration (NOAA) scientists, including scientists from NASA's Jet Propulsion Laboratory, Pasadena, California, are teaming up this month for an airborne mission focused on studying severe storm processes and intensification. The Hands-On Project Experience (HOPE) Eastern Pacific Origins and Characteristics of Hurricanes (EPOCH) field campaign will use NASA's Global Hawk autonomous aircraft to study storms in the Northern Hemisphere to learn more about how storms intensify as they brew out over the ocean.

The scope of the mission initially focused only on the East Pacific region, but was expanded to both the Gulf and Atlantic regions to give the science team broader opportunities for data collection.

"Our key point of interest is still the Eastern Pacific, but if the team saw something developing off the East Coast that may have high impact to coastal communities, we would definitely recalibrate to send the aircraft to that area," said Amber Emory, NASA's principal investigator.

Having a better understanding of storm intensification is an important goal of HOPE EPOCH. The data will help improve models that predict storm impact to coastal regions, where property damage and threat to human life can be high.

NASA has led the campaign through integration of the HOPE EPOCH science payload onto the Global Hawk platform and maintained operational oversight for the six planned mission flights. NOAA's role will be to incorporate data from dropsondes -- devices dropped from aircraft to measure storm conditions -- into NOAA National Weather Service operational models to improve storm track and intensity forecasts that will be provided to the public. NOAA first used the Global Hawk to study Hurricane Gaston in 2016.

With the Global Hawk flying at altitudes of 60,000 feet (18,300 meters), the team will conduct six 24-hour-long flights, three of which are being supported and funded through a partnership with NOAA's Unmanned Aircraft Systems program.

NASA's autonomous Global Hawk is operated from NASA's Armstrong Flight Research Center at Edwards Air Force Base in California and was developed for the U.S. Air Force by Northrop Grumman. It is ideally suited for high-altitude, long-duration Earth science flights.

The ability of the Global Hawk to autonomously fly long distances, remain aloft for extended periods of time and carry large payloads brings a new capability to the science community for measuring, monitoring and observing remote locations of Earth not feasible or practical with piloted aircraft or space satellites.

The science payload consists of a variety of instruments that will measure different aspects of storm systems, including wind velocity, pressure, temperature, humidity, cloud moisture content and the overall structure of the storm system.

Many of the science instruments have flown previously on the Global Hawk, including the High-Altitude MMIC Sounding Radiometer (HAMSR), a microwave sounder instrument that takes vertical profiles of temperature and humidity; and the Airborne Vertical Atmospheric Profiling System (AVAPS) dropsondes, which are released from the aircraft to profile temperature, humidity, pressure, wind speed and direction.

New to the science payload is the ER-2 X-band Doppler Radar (EXRAD) instrument that observes vertical velocity of a storm system. EXRAD has one conically scanning beam as well as one nadir beam, which looks down directly underneath the aircraft. EXRAD now allows researchers to get direct retrievals of vertical velocities directly underneath the plane.

The EXRAD instrument is managed and operated by NASA's Goddard Space Flight Center in Greenbelt, Maryland; and the HAMSR instrument is managed by JPL. The National Center for Atmospheric Research developed the AVAPS dropsonde system, and the NOAA team will manage and operate the system for the HOPE EPOCH mission.

Besides the scientific value that the HOPE EPOCH mission brings, the campaign also provides a unique opportunity for early-career scientists and project managers to gain professional development.

HOPE is a cooperative workforce development program sponsored by the Academy of Program/Project & Engineering Leadership (APPEL) program and NASA's Science Mission Directorate. The HOPE Training Program provides an opportunity for a team of early-entry NASA employees to propose, design, develop, build and launch a suborbital flight project over the course of 18 months. This opportunity enables participants to gain the knowledge and skills necessary to manage NASA's future flight projects.

Emory started as a NASA Pathways Intern in 2009. The HOPE EPOCH mission is particularly exciting for her, as some of her first science projects at NASA began with the Global Hawk program.

The NASA Global Hawk had its first flights during the 2010 Genesis and Rapid Intensification Processes (GRIP) campaign. Incidentally, the first EPOCH science flight targeted Tropical Storm Franklin as it emerged from the Yucatan peninsula into the Gulf of Campeche along a track almost identical to that of Hurricane Karl in 2010, which was targeted during GRIP and where Emory played an important role.

"It's exciting to work with people who are so committed to making the mission successful," Emory said. "Every mission has its own set of challenges, but when people come to the table with new ideas on how to solve those challenges, it makes for a very rewarding experience and we end up learning a lot from one another."

 

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Monday, August 14, 2017

JPL News - Day in Review

 

DAY IN REVIEW
NASA JPL latest news release
Study Finds Drought Recoveries Taking Longer

As global temperatures continue to rise, droughts are expected to become more frequent and severe in many regions during this century. A new study with NASA participation finds that land ecosystems took progressively longer to recover from droughts in the 20th century, and incomplete drought recovery may become the new normal in some areas, possibly leading to tree death and increased emissions of greenhouse gases.

In results published Aug. 10 in the journal Nature, a research team led by Christopher Schwalm of Woods Hole Research Center, Falmouth, Massachusetts, and including a scientist from NASA's Jet Propulsion Laboratory, Pasadena, California, measured recovery time following droughts in various regions of the world. They used projections from climate models verified by observations from the Moderate Resolution Imaging Spectroradiometer (MODIS) instrument on NASA's Terra satellite and ground measurements. The researchers found that drought recovery was taking longer in all land areas. In two particularly vulnerable regions -- the tropics and northern high latitudes -- recovery took ever longer than in other regions.

Schwalm noted that in model projections that assumed no new restrictions on greenhouse gas emissions (the so-called business-as-usual scenario), "Time between drought events will likely become shorter than the time needed for land ecosystems to recover from them."

"Using the vantage point of space, we can see all of Earth's forests and other ecosystems getting hit repeatedly and increasingly by droughts," said study co-author Josh Fisher of JPL. "Some of these ecosystems recover, but, with increasing frequency, others do not. Data from our 'eyes' in space allow us to verify our simulations of past and current climate, which, in turn, helps us reduce uncertainties in projections of future climate."

The scientists argue that recovery time is a crucial metric for assessing the resilience of ecosystems, shaping the odds of crossing a tipping point after which trees begin to die. Shorter times between droughts, combined with longer drought recovery times, may lead to widespread tree death, decreasing the ability of land areas to absorb atmospheric carbon.

The research is funded by the National Science Foundation and NASA. Other participating institutions include Northern Arizona University, Flagstaff; the University of Utah, Salt Lake City; Carnegie Institution for Science, Stanford, California; the University of New Mexico, Albuquerque; the U.S. Forest Service, Ogden, Utah; Arable Labs Inc., Princeton, New Jersey; the National Snow and Ice Data Center, Boulder, Colorado; Oak Ridge National Laboratory, Oak Ridge, Tennessee; the University of Maine, Orono; Pacific Northwest National Laboratory, Richland, Washington; the University of Illinois, Urbana; the University of Nevada, Reno; and Auburn University, Auburn, Alabama.

 

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Friday, August 11, 2017

JPL News - Day in Review

 

DAY IN REVIEW
TRAPPIST-1 is Older Than Our Solar System
If we want to know more about whether life could survive on a planet outside our solar system, it's important to know the age of its star.
› Read the full story
Cassini Prepares to Say Goodbye to a True Titan
The giant, hazy moon Titan has been essential to Cassini's mission, from the spacecraft's 2004 arrival at Saturn to the very end.
› Read the full story
NASA Announces Television Coverage for Aug. 21 Solar Eclipse
NASA TV will carry the Aug. 21 solar eclipse live from unique vantage points on the ground, from aircraft and from spacecraft, including the International Space Station.
› Read the full story

 

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Pasadena, CA 91109

New Teachable Moment from NASA/JPL Edu – Eclipse 2017

NASA/JPL Education – Teachable Moment: Get Students Excited About Science With This Month's Total Solar Eclipse
 

Get Students Excited About Science With This Month's Total Solar Eclipse

This month marks the first time in 38 years that one of nature's most awe-inspiring sights, a total solar eclipse, will be visible from the continental United States. Every state in the US will have a chance to see at least a partial eclipse and 14 will have a chance to see the eclipse in totality – with the moon completely covering the disk of the sun.

It's a great opportunity to look at the sky and engage students in scientific observations and discovery.

Find out how a solar eclipse works, how to safely view one in action (remember to never look directly at the sun without certified eclipse glasses or a solar filter), and see how you can contribute to NASA science during the eclipse.

It's all in the latest Teachable Moment from NASA/JPL Education:


Check it out
 

And explore these standards-aligned math and science lessons all about the eclipse:

  • Epic Eclipse – Students use the mathematical constant pi to approximate the area of land covered by the moon's shadow during the eclipse.
  • Pinhole Camera – Learn how to make your very own pinhole camera to safely see a solar eclipse in action from anywhere the eclipse is visible, partial or full!
  • Moon Phases - Students learn about the phases of the Moon by acting them out. In 30 minutes, they will act out one complete, 30-day, moon cycle.
  • NASA GLOBE Observer – Students can become citizen scientists and collect data for NASA's GLOBE Program using this app available for iOS and Android devices (eclipse update available starting August 18, 2017).

 

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IMG_7474.PDF

Thursday, August 10, 2017

JPL News - Day in Review

 

DAY IN REVIEW
NASA JPL latest news release
25 Years of Global Sea Level Data, and Counting

Today marks the 25th anniversary of the launch of a revolutionary ocean research vessel -- a space "ship." As the NASA/CNES Topex-Poseidon satellite ascended into orbit, it ushered in a new era of oceanography with the first highly accurate, global measurements of sea levels. That mission and its three successors, all named Jason, have continuously mapped global ocean currents and tides; opened our eyes to the global reach of El Niño and other climate events; created a quarter-century-long, extraordinarily precise record of global and regional sea level rise; and enabled improved forecasts of extreme weather events such as hurricanes, floods and droughts.

A new slideshow celebrates this important data set -- a fundamental measurement for the study of the oceans and climate -- and the longstanding U.S.-French collaboration that brought it about.

Topex-Poseidon

Topex launch

Topex-Poseidon launch, 1992. Credit: CNES
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In 1992, when Topex-Poseidon launched, no one foresaw that its record of precision ocean height measurements would continue through three decades and four spacecraft. In fact, many oceanographers at the time weren't convinced that Topex-Poseidon's sensors would be accurate enough to reveal the signal of sea level rise out of the noise of waves, tides and other changes. But the radar altimeter and radiometer measurement system outperformed expectations from the start. In 25 years of continuous operation, Topex-Poseidon and its successors have recorded 2.8 inches (7 centimeters) of global average sea level rise.

Our planet's oceans are too vast and complex to be fully measured by any single satellite, or even by any single nation. Topex-Poseidon and its successor Jason satellite missions are shining examples of the power of a sustained, long-term international partnership, led by the U.S. and French space agencies, NASA and CNES. For nearly three decades, NASA and CNES scientists and engineers have pooled their expertise, talents and insights to design and construct an integrated spaceborne measurement system far more powerful than the sum of its parts. NASA and CNES have worked together, applying advanced technology to collect measurements of remarkable precision and accuracy, and then making those measurements freely and openly available. With this effort, they have provided humanity with unprecedented views of the global oceans, how they change on time scales of days to decades, and how the oceans influence -- and respond to -- weather and climate.

"For more than a generation, NASA and CNES scientists and engineers have collaborated to make exquisitely accurate measurements of the ocean surface from space, providing insights into the workings and interactions of our planet's two great fluid systems, the oceans and the atmosphere," said Michael Freilich, director of NASA's Earth Science Division in Washington.

Ocean Currents

The Topex-Poseidon mission was the first to monitor the changing patterns of major ocean surface currents in a comprehensive way. Ocean current locations are revealed by large-scale hills and valleys on the ocean surface, which can vary by more than 6 feet (2 meters) in height. The peaks and dips defining the ocean's topography are caused by variations in water temperature and pressure. Large-scale currents like the Gulf Stream tend to flow along contours of constant ocean height, following the sides of the hills and valleys. The steepness of a slope indicates the speed of the current. Unlike terrain on land, however, the liquid "landscape" shifts with changes in winds, temperature and other factors, causing shifts in the locations and speeds of the currents. The only way to monitor these changes over the entire surface of Earth's ocean is to make precise measurements of the height of the ocean surface from orbiting satellites.

Measuring the ocean shape over nearly the entire globe every 10 days, Topex-Poseidon gave the first quantitative view of how ocean currents change with the seasons. Topex/Poseidon and the Jason-1, Jason-2 and Jason-3 missions have provided unique insights into how ocean circulation affects climate by moving heat from place to place on our planet.

Heat Storage in the Ocean

ocean heat

NOAA's annual assessment of the heat in the upper ocean (2015 shown), a measure of global warming, draws on Topex series data. Credit: NOAA
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More than 90 percent of the heat from global warming is stored in the ocean, which means oceans are key players in global climate. Heat causes ocean water to expand, adding to sea level rise. Measuring both long-term sea level trends and the shape of the ocean surface related to currents, Topex-Poseidon and the Jason series provide two basic ingredients for understanding the ocean's role in global climate variations.

"As human-caused global warming drives sea levels higher and higher, we are literally contributing to the reshaping of the surface of our planet," said Josh Willis, NASA project scientist for Jason-3 at NASA's Jet Propulsion Laboratory in Pasadena, California. "The precision altimetric satellite missions tell us how much and how fast."

El Niño, La Niña, and More

97 99 ENSO

Among Topex-Poseidon's early achievements was recording the full extent of a record El Niño in 1997 and the succeeding La Niña in 1999. Darker colors are sea levels lower than normal, lighter and white colors are higher than normal. Credit: NASA/JPL-Caltech
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For decades, scientists could not predict how El Niño and other year-to-year ocean variations changed regional weather. That was partly because, using only ships and buoys, they couldn't observe the genesis and growth of these changes far out in the equatorial Pacific. Topex-Poseidon and the Jason satellites have given the first frequent, global views of the full extent and life cycles of El Niño and La Niña events. Lee-Lueng Fu of JPL -- project scientist for the first two ocean altimetry missions -- pointed out, "Topex-Poseidon allowed us to follow their evolution and showed that these events weren't limited to just the tropics. It also gave us evidence of even longer-lasting ocean variations." One of these is the Pacific Decadal Oscillation, similar to El Niño and La Niña in character but with phases lasting up to several decades.

In the last 25 years, with the help of altimetry data, scientists have pinpointed many global connections between these multi-year ocean variations and weather consequences such as drought and flooding throughout the globe. While these events have by no means yielded all their secrets, they are better understood and better forecast than before global spaceborne observations began.

Tides on the Open Ocean

Global Tides

A numerical model of daily global tides using sea level data from Topex-Poseidon. Credit: ESR
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Before satellite measurements, deep-ocean tide measurements were difficult to make, expensive and sparse. Topex-Poseidon made the first global maps of tides, which changed scientists' understanding of how tides dissipate. The data show that a third of tidal energy dissipates in the open ocean, playing important and previously unknown roles in mixing water within the ocean.

Jason-1

Topex-Poseidon had a three-year prime mission, but long before that time was up, oceanographers and other Earth scientists recognized the value of continuing its measurements as long as possible. Fu explained, "Sea surface height is a fundamental measure of the Earth system, so it was a no-brainer that scientists would want to have this kind of information indefinitely." With strong community support, Jason-1 was constructed by NASA and CNES and launched in December 2001. For three years, Topex-Poseidon and Jason-1 flew in coordinated orbits that allowed scientists to cross-calibrate their measurements and then combine the data sets to observe the global oceans more frequently. Each succeeding mission has also overlapped its predecessor, ensuring a consistent data record.

So far, each of the ocean altimetry missions has proven to be long-lived. Topex-Poseidon was eventually decommissioned in 2005 after 13 years in orbit. Jason-1 survived almost 12 years, until July 2013. Nine-year-old Jason-2 and Jason-3 (launched in January 2016) are still in operation.

Jason-2

Lee Fu_and Josh Willis

Lee Fu (left) was the project scientists for Topex Poseidon and Jason-1 and -2. Josh Willis is the current project scientist for Jason-2 and -3. Credit: NASA/JPL-Caltech
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With the launch of Jason-2 in June 2008, the focus of spaceborne ocean altimetry transitioned from research objectives to data applications providing tangible benefits to society. Mission operations moved from the research agencies NASA and CNES to the U.S. National Oceanic and Atmospheric Administration (NOAA) and the European Organisation for the Exploitation of Meteorological Satellites (EUMETSAT); indeed, satellite altimeter measurements are used routinely in NOAA's El Niño forecasts. NASA and CNES continue to provide science teams, instrument design, and science-focused, specialized data management.

Forecasting

Forecasting

Jason-1 data contributed to this forecast of Hurricane Rita's track across the Gulf of Mexico in 2005. The storm track appears as a black line. Jason-1 observed a tongue of very warm water (red) in the gulf, 13-23 inches ( 35-60 centimeters) higher than surrounding water. Ocean heat can strengthen hurricane intensity. Credit: NASA/JPL-Caltech/University of Colorado
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On smaller space and time scales, satellite altimetry measurements provide information directly useful for marine storm prediction. Hurricanes are fueled by heat stored in the ocean below, and since the upper ocean expands and contracts as it heats and cools, sea level height is a marker for water temperature and heat content. So it is hardly surprising that ocean altimetry data are routinely used in forecasting hurricane strength.

In 2014, an unexpected forecasting use for altimetry data became operational. Bangladesh, whose 46-year history has encompassed death-dealing river floods, uses Jason-2 measurements of river levels in its flood forecasting and warning system. Within the first year using these data, Bangladesh's system enabled the most accurate, long-lead flood warnings ever given for that nation.

Navigation

Navy navigation

The U.S. Navy uses the ocean altimetry satellites' data to aid surface and underwater navigation. Credit: U.S. Navy
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Civilian sailors and the U.S. Navy use the series' near-real-time data on currents, eddies, winds and waves to aid surface and underwater navigation. Information on eddy currents in the Gulf of Mexico has been used by marine operators to schedule offshore drilling operations, with significant cost savings.

Jason-3

When Jason-3 launched in 2016, NASA project scientist Willis commented, "This mission has big shoes to fill. Its predecessors have built one of the clearest records we have of our changing climate." Jason-3 has performed flawlessly in continuing the global record of precise sea-surface topography measurements and is now halfway through its prime mission.

A New Role for Jason-2

NOAA sea floor map

Jason-2's new, lower orbit will allow scientists -- such as Walter H. Smith (NOAA) and David Sandwell (Scripps Institution of Oceanography), who produced this map -- to improve their understanding of features on the global seafloor. Credit: NOAA
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This year, Jason-2's onboard systems began to show signs of space radiation damage. The mission management decided to lower the satellite out of its shared orbit with Jason-3. At the urging of the science community, the satellite was lowered by 17 miles (27 kilometers), where it will collect data along a series of ground tracks only 5 miles (8 kilometers) apart, with a one-year repeat cycle.

Besides protecting Jason-3, the new orbit will allow Jason-2 to produce an improved, high-resolution estimate of Earth's average sea surface height. Because ocean topography is partly determined by the contours on the ocean bottom, the estimate is expected to enable scientists to improve maps of the seafloor, resolving currently unknown details of underwater features such as seamounts. These maps will permit advances in ocean modeling, tsunami wave forecasting and naval operations support.

Into the Future

Sentinel 6

Illustration of the upcoming Sentinel-6 mission. Credit: ESA
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The next ocean altimetry mission, expected to launch in 2020, is called Jason Continuity of Service (Jason-CS) on the Sentinel-6 mission. As the long name implies, it will carry on the proud Jason legacy, but with a new partner: the European Space Agency. EUMETSAT will lead the mission, and NASA's role will remain similar to its role in Jason-3.

Satellites have already revolutionized oceanography, and soon they will do the same for hydrology -- the study of water on land. The French/U.S. Surface Water and Ocean Topography (SWOT) mission will be at the forefront, carrying an innovative interferometer dubbed KaRin that marks a break with today's technologies.

Fu notes that these changes show the value the world scientific community places on the ocean altimetry program. "The measurement is so important, and the technology is fully demonstrated," he said. "In the long haul, ocean altimetry is an international commitment."

 

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