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Tuesday, November 24, 2015

JPL News - Day in Review

 

DAY IN REVIEW
Strange Star Likely Swarmed by Comets
New clues emerge in the mystery of a star with odd light patterns.
› Read the full story
Loss of Carbon in Martian Atmosphere Explained
A process involving ultraviolet light from the sun helps explain the ratio of heavier to lighter carbon in Mars' atmosphere and resolve a dilemma about "missing" carbon.
› Read the full story

 



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Monday, November 23, 2015

JPL News - Day in Review

 

DAY IN REVIEW
Earth Might Have Hairy Dark Matter
Dense filaments of dark matter particles, called "hairs," are sprouting from Earth, according to a new study based on computer simulations.
› Read the full story
NEOWISE Identifies Greenhouse Gases in Comets
Data from NASA's NEOWISE mission are giving new insights into comet dust, nucleus sizes, and production rates for difficult-to-observe gases like carbon dioxide and carbon monoxide.
› Read the full story

 



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Thursday, November 19, 2015

JPL News - Day in Review

 

DAY IN REVIEW
2015 and 1997 El Niños: Déjà vu, or Something New?
Forecasters say this year's El Niño looks just like the giant event of 1997-98. But when it comes to El Niños, there are no identical twins.
› Read the full story
Satellite Sensors Would Deliver Global Fire Coverage
Wildfires can wreak havoc on human health, property and communities, so it's imperative to detect them as early as possible.
› Read the full story

 



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Tuesday, November 17, 2015

December Educator Workshop - Lunar and Meteorite Sample Certification

 

 

Lunar and Meteorite Sample Certification

When: Saturday, Dec. 5, 9 a.m. to 1 p.m.

Where: NASA Jet Propulsion Laboratory, Von Karman Auditorium, Pasadena, California

Target Audience: Teachers for grades K-12

Overview: NASA makes actual samples from the historic Apollo missions available to lend to teachers. You must attend this certification process to bring the excitement of real lunar rocks and regolith samples to your students.

Call the Educator Resource Center at 818-393-5917 to reserve your spot.

This free workshop is offered through the NASA/JPL Educator Resource Center, which provides formal and informal educators with NASA resources and materials that support STEM learning.

Discover more upcoming educator workshops and events from NASA/JPL Education.

 

 



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Thursday, November 12, 2015

JPL News - Day in Review

 

DAY IN REVIEW
Seven Case Studies in Carbon and Climate
Every part of Earth's surface mosaic absorbs and releases carbon in a different way, with wild-card events complicating the picture.
› Read the full story
A Breathing Planet, Off Balance
As people burn fossil fuels and clear forests, only half of the carbon dioxide released stays in the atmosphere. Earth's vegetation ecosystems and oceans remove the other half.
› Read the full story
As Earth Warms, NASA Targets 'Other Half' of Carbon, Climate Equation
During a 9 am PST (noon EST) media teleconference today, NASA and university scientists will discuss new insights, tools and agency research into key carbon and climate change questions.
› Read the full story
In Greenland, Another Major Glacier Comes Undone
A new study by NASA and university researchers spells more trouble for Greenland's Ice Sheet and global sea levels.
› Read the full story

 



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Wednesday, November 11, 2015

JPL News - Day in Review

 

DAY IN REVIEW
Upgrade Helps NASA Study Mineral Veins on Mars
Diverse composition of mineral veins at the "Garden City" site investigated by NASA's Curiosity Mars rover suggests multiple episodes of groundwater activity.
› Read the full story
Secondhand Spacecraft Has Firsthand Asteroid Experience
NASA's NEOWISE mission has observed 158,000 asteroids and discovered more than 35,000 since December 2009.
› Read the full story

 



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Monday, November 9, 2015

JPL News - Day in Review

 

DAY IN REVIEW
NASA JPL latest news release
NASA Holds Media Briefing on Carbon's Role in Earth's Future Climate

NASA will host a media teleconference at 9 a.m. PST (noon EST) on Thursday, Nov. 12, to discuss the latest insights into how Earth is responding to rising levels of heat-trapping gases in the atmosphere, and what this means for our future climate.

Later this month, a United Nations climate meeting in Paris will focus on setting limits on future levels of human-produced carbon emissions. This NASA briefing will present new observations from the Orbiting Carbon Observatory-2 (OCO-2) mission, NASA's first satellite dedicated to measuring carbon dioxide, and preview field work planned in the North Atlantic and Alaska.

The panelists will be:

-- Michael Freilich, director of NASA's Earth Science Division at the agency's headquarters in Washington

-- Mike Behrenfeld, principal investigator for NASA's NAAMES field campaign, Oregon State University in Corvallis

-- George Hurtt, lead for NASA's Carbon Monitoring System, University of Maryland in College Park

-- Annmarie Eldering, deputy project scientist for NASA's OCO-2 mission at the agency's Jet Propulsion Laboratory in Pasadena, California

-- Lesley Ott, research scientist in the Global Modeling and Assimilation Office at NASA's Goddard Space Flight Center in Greenbelt, Maryland

Audio of the briefing will stream live at:

http://www.nasa.gov/newsaudio

and

http://www.ustream.tv/nasajpl2

The public may ask questions during the briefing on Twitter using the hashtag #askNASA.

Earth's land and ocean currently absorb about half of all carbon dioxide emissions from the burning of fossil fuels, but it's uncertain whether the planet can keep this up in the future. NASA's Earth science program works to improve our understanding of how carbon absorption and emission processes work in nature and how they could change in a warming world with increasing levels of carbon dioxide and methane emissions from human activities.

For more information about NASA's Earth science programs, visit:

http://www.nasa.gov/earth

 



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Friday, November 6, 2015

JPL News - Day in Review

 

DAY IN REVIEW
NASA JPL latest news release
NASA's RapidScat Celebrates One-Year Anniversary

Where do predictions for regional weather patterns come from? For one source, look to the ocean. About 70 percent of Earth's surface is covered in oceans, and changes in ocean winds are good predictors of many weather phenomena on small and large scales.

NASA's ISS-RapidScat instrument, which last month celebrated its one-year anniversary, helps make these ocean wind measurements to enhance weather forecasting and understanding of climate. The instrument was first activated on the International Space Station on Oct. 1, 2014.

"Especially with the recent hurricane season, our data have been appearing on weather websites around the world," said Glen Havens, project manager for the mission, based at NASA's Jet Propulsion Laboratory, Pasadena, California.

In its first year in action, the instrument has collected data on many severe storms, including typhoons and tropical cyclones. RapidScat has proven valuable for tracking the Southern Hemisphere's hurricane season and the Northern Hemisphere's winter storm season.

Most recently, RapidScat played a role in tracking Hurricane Patricia, which loomed over Mexico in October. Patricia was the strongest hurricane ever recorded in the Western Hemisphere, with maximum winds of 200 mph (320 kilometers per hour). When it first made landfall on the Pacific coast of Mexico on Oct. 23, it was a destructive Category 5 storm.

Worldwide, many meteorological agencies include RapidScat data in the ensemble of data sets used to create forecasts. The agencies include the U.S. Navy, the National Oceanographic and Atmospheric Administration (NOAA), and the European Organization for the Exploitation of Meteorological Satellites.

High wind warnings, to which RapidScat data contribute, are especially important for anyone involved in shipping and sailing. Wind information from RapidScat can also be useful for enthusiasts of water sports.

"People who go sailing, and sometimes even surfers, look at RapidScat data to find where big waves are," said Stacey Boland, project systems engineer for RapidScat at JPL.

RapidScat measures winds that are just above the ocean surface. The instrument is a Ku-band scatterometer that transmits pulses of microwave energy toward Earth. The surface of Earth reflects this signal, and RapidScat measures the strength of the pulse that comes back. Stronger return signals from the ocean indicate larger waves. The return signal also carries information about wind direction.

Most scatterometers are launched in sun-synchronous orbits, such that each time they fly over the same place on Earth, it's at the same local time. But because RapidScat is mounted on the space station, which is not in a sun-synchronous orbit, it sees different places at different local times. The instrument samples all local times of day over the course of about two months, allowing scientists to learn more about how winds vary over the course of a day for a given location.

Another unique aspect of the mission is that the instrument was constructed using hardware built in the 1990s. Engineers adapted hardware that was originally built to test QuikScat, which was launched in 1999 into a sun-synchronous orbit. They added a smaller reflector antenna and a new interface to the repurposed instrument to make it work on the space station.

Repurposing the QuikScat test hardware significantly reduced the cost of the mission compared to what it would have been if the instrument had been built from scratch. It also allowed for a relatively quick turnaround time for building the instrument: A mere two years from approval to launch.

The RapidScat team addressed challenges that come with using older technology, such as the radar receiver electronics. But the "plucky radar" system, as Havens calls it, continues collecting science data and sending it back to Earth.

"We immediately started getting high-quality data after the instrument began operating," said Howard Eisen of JPL, who served as project manager at the beginning of the mission.

The instrument resides on the Columbus module on the space station, and will stay there until at least early 2017.

For more information on RapidScat, visit:

http://winds.jpl.nasa.gov/missions/RapidScat/

http://www.nasa.gov/rapidscat

For more information about NASA's Earth science activities, visit:

http://www.nasa.gov/earth

 



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Wednesday, November 4, 2015

Last Call! November Educator Workshop - Climate Change

 

 

Climate Change

When: Saturday, Nov. 7, 10 a.m. to 12:30 p.m.

Where: NASA Jet Propulsion Laboratory, Von Karman Auditorium, Pasadena, California

Target Audience: Educators for grades 3-8 (all educators are welcome)

Overview: In this workshop teachers will get an overview of what we know about climate change and how we know it. Enjoy some simple chemistry, videos, games and student inventions. This is a great, standards-based way to teach and inspire students to think about our impact on our environment.

Call the Educator Resource Center at 818-393-5917 to reserve your spot.

This free workshop is offered through the NASA/JPL Educator Resource Center, which provides formal and informal educators with NASA resources and materials that support STEM learning.

Discover more upcoming educator workshops and events from NASA/JPL Education.

 

 



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Tuesday, November 3, 2015

JPL News - Day in Review

 

DAY IN REVIEW
Whopping Galaxy Cluster Spotted with Help of NASA Telescopes
A giant gathering of galaxies has been spotted 8.5 billion light-years away.
› Read the full story
Radar Images Provide New Details on Halloween Asteroid
The highest-resolution images of asteroid 2015 TB145 yield new information about surface features.
› Read the full story

 



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Monday, November 2, 2015

JPL News - Day in Review

 

DAY IN REVIEW
NASA JPL latest news release
NASA Finds New Way to Track Ocean Currents from Space

A team of NASA and university scientists has developed a new way to use satellite measurements to track changes in Atlantic Ocean currents, which are a driving force in global climate. The finding opens a path to better monitoring and understanding of how ocean circulation is changing and what the changes may mean for future climate.

In the Atlantic, currents at the ocean surface, such as the Gulf Stream, carry sun-warmed water from the tropics northeastward. As the water moves through colder regions, it sheds its heat. By the time it gets to Greenland, it's so cold and dense that it sinks a couple of miles down into the ocean depths. There it turns and flows back south. This open loop of shallow and deep currents is known to oceanographers as the Atlantic Meridional Overturning Circulation (AMOC) -- part of the "conveyor belt" of ocean currents circulating water, heat and nutrients around the globe and affecting climate.

Because the AMOC moves so much heat, any change in it is likely to be an important indicator of how our planet is responding to warming caused by increasing greenhouse gases. In the last decade, a few isolated measurements have suggested that the AMOC is slowing down and moving less water. Many researchers are expecting the current to weaken as a consequence of global warming, but natural variations may also be involved. To better understand what is going on, scientists would like to have consistent observations over time that cover the entire Atlantic.

"This [new] satellite approach allows us to improve projections of future changes and -- quite literally -- get to the bottom of what drives ocean current changes," said Felix Landerer of NASA's Jet Propulsion Laboratory, Pasadena, California, who led the research team.

Landerer and his colleagues used data from the twin satellites of NASA's Gravity Recovery and Climate Experiment (GRACE) mission. Launched in 2002, GRACE provides a monthly record of tiny changes in Earth's gravitational field, caused by changes in the amount of mass below the satellites. The mass of Earth's land surfaces doesn't change much over the course of a month; but the mass of water on or near Earth's surface does, for example, as ice sheets melt and water is pumped from underground aquifers. GRACE has proven invaluable in tracking these changes.

At the bottom of the atmosphere -- on Earth's surface -- changes in air pressure (a measure of the mass of the air) tell us about flowing air, or wind. At the bottom of the ocean, changes in pressure tell us about flowing water, or currents. Landerer and his team developed a way to isolate in the GRACE gravity data the signal of tiny pressure differences at the ocean bottom that are caused by changes in the deep ocean currents.

"We've wanted to observe this phenomenon with GRACE since we launched 13 years ago, but it took us this long to figure out how to squeeze the information out of the data stream," said Michael Watkins, director of the Center for Space Research at the University of Texas at Austin, former GRACE project scientist and a co-author of the study.

The squeezing process required some very advanced data processing, but not as many data points as one might think. "In principle, you'd think you'd have to measure every 10 yards or so across the ocean to know the whole flow," Landerer explained. "But in fact, if you can measure the farthest eastern and western points very accurately, that's all you need to know how much water is flowing north and south in the entire Atlantic at that section. That theory has long been known and is exploited in buoy networks, but this is the first time we've been able to do it successfully from space."

The new measurements agreed well with estimates from a network of ocean buoys that span the Atlantic Ocean near 26 degrees north latitude, operated by the Rapid Climate Change (RAPID) group at the U.K.'s National Oceanography Centre, Southampton. The agreement gives the researchers confidence that the technique can be expanded to provide estimates throughout the Atlantic. In fact, the GRACE measurements showed that a significant weakening in the overturning circulation, which the buoys recorded in the winter of 2009-10, extended several thousand miles north and south of the buoys' latitude.

Gerard McCarthy, a research scientist in the RAPID group who was not involved with the study, said, "The results highlight synergies between [direct measurements] like [those from] RAPID and remote sensing -- all the more important given the rapid and surprising changes occurring in the North Atlantic at the present time." Eric Lindstrom, NASA's Physical Oceanography Program manager at the agency's headquarters in Washington, pointed out, "It's awesome that GRACE can see variations of deep water transport, [but] this signal might never have been detected or verified without the RAPID array. We will continue to need both in situ and space-based systems to monitor the subtle but significant variations of the ocean circulation."

A paper in the journal Geophysical Research Letters describing the new technique and first results is available online in prepublication form:

http://onlinelibrary.wiley.com/doi/10.1002/2015GL065730/abstract?campaign=wolacceptedarticle

 



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