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Friday, August 11, 2017

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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NASA/JPL Edu
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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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NASA's Jet Propulsion Laboratory
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Pasadena, CA 91109

Wednesday, August 9, 2017

JPL News - Day in Review

 

DAY IN REVIEW
Cassini to Begin Final Five Orbits Around Saturn
NASA's Cassini spacecraft is about to embark on a set of ultra-close passes through Saturn's upper atmosphere with its final five orbits around the planet.
› Read the full story
Watch Martian Clouds Scoot, Thanks to NASA's Curiosity
Wispy, early-season clouds resembling Earth's ice-crystal cirrus clouds move across the Martian sky in some new image sequences from NASA's Curiosity Mars rover.
› Read the full story

 

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NASA Jet Propulsion Laboratory
NASA's Jet Propulsion Laboratory
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Pasadena, CA 91109

Monday, August 7, 2017

JPL News - Day in Review

 

DAY IN REVIEW
NASA JPL latest news release
Can Poor Air Quality Mask Global Warming's Effects?

During the 20th century, the average temperature of the continental United States rose by almost 1 degree Fahrenheit (0.5 degree Celsius) -- everywhere, that is, except in the Southeast. There, until the 1980s, the temperature actually decreased slightly. Climate scientists dubbed this peculiar phenomenon the "warming hole," and it was the cause of much speculation. But beginning in the 1990s, temperatures in the Southeast began to warm again, and in the early years of the 21st century this warming has accelerated.

A new study published in the journal Remote Sensing presents evidence that a significant improvement in air quality in the region may have contributed to the disappearance of the warming hole after about 1990 -- and that other polluted regions outside the United States, such as China and India, may experience the same phenomenon.

One major factor in poor air quality is airborne aerosols -- tiny particles of dust, soot from wood burning, coal and oil combustion, or sulfates created by precursor gases emitted from factories and car exhaust, to name a few sources. Aerosols can decrease temperature by dimming sunlight at Earth's surface and by increasing the amount and lifetimes of clouds, which reflect sunlight back into space.

After the warming hole mysteriously disappeared, various studies proposed possible causes: changes in cloud cover, precipitation or in the amount of aerosols produced by air pollution. In 2006, the U.S. Environmental Protection Agency (EPA) began implementing a more stringent cap on the concentration of aerosol particles smaller than about 1/10,000th of an inch (2.5 micrometers) in diameter. To comply with the regulation, many U.S. power utilities and industrial companies began reducing their use of coal and installing filters to reduce emissions.

A similar change to temperature trends occurred in Europe in the 1980s after new regulations improved air quality there. Because reduced aerosol particle concentrations allow more sunlight to reach Earth's surface, the scientists hypothesized that the improvements in U.S. air quality could also be responsible for the temperature change over the Southeast.

To test this hypothesis, a team led by Mika Tosca, a researcher at NASA's Jet Propulsion Laboratory in Pasadena, California (who is now with the School of the Art Institute of Chicago), used three surface temperature data sets. The data sets were compiled by the University of Delaware, the University of California (UC) at Berkeley, and the Global Historical Climatology Network (which compiles surface temperature and precipitation data). They also used aerosol data from two satellite instruments: the Multi-angle Imaging SpectroRadiometer (MISR) instrument on NASA's Terra satellite, launched in 1999, and the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) on the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) satellite, a joint mission between NASA and the French space agency, CNES, launched in 2006.

The data show that between 2000 and 2015, while summertime temperatures in the Southeast United States increased by roughly 1.5 degrees Fahrenheit (0.75 degree Celsius), significantly faster than the increase in the continental United States during the 20th century, the amount of summertime aerosols decreased overall by about 20 percent, with a much steeper decline after 2007. The timing of this decline coincided with the implementation of the new EPA standards.

To help determine how much of the temperature change was caused by the changes in aerosols, Tosca and colleagues used a model that simulates how the sun's energy travels through Earth's atmosphere, using the MISR and CALIOP satellite data as inputs. The increase in sunlight shown in the model results matches well with daily measurements taken at a National Oceanic and Atmospheric Administration (NOAA) solar radiation monitoring station in Goodwin Creek, Mississippi, suggesting that the decrease in aerosols is a plausible explanation for most of the disappearance of the warming hole.

Tosca acknowledges that linkages between aerosols and clouds could also play a role. The next step would be to run a more sophisticated climate model that takes into account clouds and the aerosols' effects on them. The team would also like to apply this kind of analysis to other areas with high air pollution levels, such as China and India. They hypothesize that these areas might have "warming holes" of their own -- regions where the effects of climate change are being muted by the high concentrations of aerosols in the atmosphere. If these areas reduce air pollution in the future, they might experience a sudden temperature jump as well.

"Overall, the goal is to more accurately predict what will happen to our planet," Tosca said. "This type of observation-based research gives us better models, better models give us better forecasts, and better forecasts enable better policy."

The study is titled "Attributing Accelerated Summertime Warming in the Southeast United States to Recent Reductions in Aerosol Burden: Indications from Vertically-Resolved Observations." Other institutions participating in the study included the Joint Center for Earth Systems Technology, a cooperative agreement between NASA's Goddard Space Flight Center in Greenbelt, Maryland, and the University of Maryland, Baltimore County; the Naval Research Laboratory in Monterey, California; and the University of North Dakota in Grand Forks. MISR was built and is managed by JPL, and CALIOP is jointly administered by NASA and the French space agency, Centre National d'Etudes Spatiales.

 

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Friday, August 4, 2017

JPL News - Day in Review

 

DAY IN REVIEW
NASA JPL latest news release
New Clues to Universe's Structure Revealed

What is our universe made of, and has its composition changed over time? Scientists have new insights about these fundamental questions, thanks to an international collaboration of more than 400 scientists called the Dark Energy Survey (DES). Three scientists from NASA's Jet Propulsion Laboratory in Pasadena, California, are part of this group that is helping to further our understanding of the structure of the universe.

The advances in astrophysics from DES are crucial to preparations for two upcoming space missions that will probe similar questions about the nature of the universe: ESA's Euclid mission (which has significant NASA participation) and NASA's Wide-Field Infrared Survey Telescope mission, both expected to launch in the 2020s.

"With this study, we are showcasing what's going to be possible with these much more complex observatories," said Andres Plazas Malagon, a postdoctoral researcher at JPL, who helped characterize DES's Dark Energy Camera detectors and who is also involved in detector studies for WFIRST.

Leading models of the universe suggest it is mostly composed of entities we cannot see: dark matter and dark energy. Dark matter acts like invisible glue, holding galaxies and galaxy clusters together gravitationally, while dark energy is thought to be responsible for the accelerated expansion of the universe. Some of our best predictions for how much dark matter and dark energy are in the universe come from the European Space Agency's Planck satellite, which looks at the light from about 400,000 years after the Big Bang.

Now, the Dark Energy Survey has examined the composition of the recent universe. Remarkably, the new results are close to forecasts made from Planck measurements of the distant past, allowing scientists to understand more about how the universe has evolved over approximately 14 billion years. The findings were revealed in a presentation at the American Physical Society Division of Particles and Fields meeting at the U.S. Department of Energy's Fermi National Accelerator Laboratory in Batavia, Illinois.

"The Planck results have been the landmark constraints in cosmology. It is truly amazing that you have a model that describes the universe at 400,000 years old, and now we have a similarly precise measurement of the universe at 13 billion years [old] that agrees with the model," said JPL's Tim Eifler, who led the Dark Energy Survey analysis team to develop the science software for the interpretation of the results.

Scientists find that about 70 percent of the energy in the universe is contained in dark energy. About 25 percent is composed of the mysterious dark matter, with normal matter making up the remainder. All of this agrees with precise measurements made to date. So far, DES has found no evidence that the amount of dark energy has changed over time -- a finding that is consistent with Albert Einstein's idea of a "cosmological constant."

The results are especially important to the scientific community because they mark the first time that observations from the more recent universe -- the "adult" universe -- by a technique called gravitational lensing and galaxy clustering, have yielded results as precise as those from the cosmic microwave background radiation -- light from the "infant" universe.

"This is the crossover point where gravitational lensing and galaxy clustering measurements and surveys will be the primary driver of what we know about dark energy in the universe," said Eric Huff, a JPL researcher who invented a new method of extracting the weak lensing signal, enhancing the precision of the DES galaxy shape catalogs.

The results come from the first-year data set of the Dark Energy Survey, which uses a 570-megapixel camera mounted on the 4-meter Blanco telescope at the National Optical Astronomy Observatory's Cerro Tololo Inter-American Observatory in Chile. Its data are processed at the National Center for Supercomputing Applications at the University of Illinois at Urbana-Champaign.

To measure dark matter, scientists first created maps of galaxy positions. Then, they precisely measured the shapes of 26 million galaxies to directly map patterns of dark matter over billions of light years, using gravitational lensing and galaxy clustering.

The DES team developed new ways to detect the tiny lensing distortions of galaxy images. In the process, they created the largest guide to spotting dark matter in the cosmos ever drawn. The new dark matter map is 10 times the size of the one DES released in 2015 and continues to grow.

The DES collaboration will publish on a data set five times larger over the next two years.

"There is a feeling of true discovery in the collaboration. For the first time, we have the data and tools in hand to see whether Einstein's cosmological constant prevails. We are all excited to explore the physical nature of dark energy," Eifler said. "In particular we want to see if there are hints in the data that suggest modifying the laws of gravity on the largest scales in the universe."

Read more at:

http://news.fnal.gov/2017/08/dark-energy-survey-reveals-accurate-measurement-dark-matter-structure-universe/

 

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NASA Jet Propulsion Laboratory
NASA's Jet Propulsion Laboratory
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Pasadena, CA 91109

Wednesday, August 2, 2017

JPL News - Day in Review

 

DAY IN REVIEW
Hubble Detects Exoplanet with Glowing Water Atmosphere
Scientists have discovered the strongest evidence to date for a stratosphere on a planet outside our solar system.
› Read the full story
What's Up in the August Skies?
What's Up for August? The total solar eclipse on Aug. 21, 2017, will traces a narrow path across the nation, though most of the U.S. will see a partial eclipse.
› Watch the video
Two Voyagers Taught Us How to Listen to Space
Over the mission's 40 years, NASA's Voyager spacecraft have paved the way for modern deep space communications.
› Read the full story
Five Years Ago and 154 Million Miles Away: Touchdown!
NASA's Curiosity Mars rover, which landed near Mount Sharp five years ago this week, is examining clues on that mountain about long-ago lakes on Mars.
› Read the full story

 

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Tuesday, August 1, 2017

How are you?

Hi! How are you?
My name is Anastasia (or shortly Nastya), and I�d love to know your name.
Do you visit this site oftentimes? I was hoping to talk to you in chat once but you left all of a sudden. Could you write me your address or send me a letter some day?
I believe we have a lot in common and talking to you will be much pleasure for me.

My email sentiliur@gmx.com

Looking forward to getting your letter,
Anastasia

How are you?

Hi! How are you?
My name is Anastasia (or shortly Nastya), and I�d love to know your name.
Do you visit this site oftentimes? I was hoping to talk to you in chat once but you left all of a sudden. Could you write me your address or send me a letter some day?
I believe we have a lot in common and talking to you will be much pleasure for me.

My email sartnomasil@gmx.com

Looking forward to getting your letter,
Anastasia