ACEAP 2019: Cerro Pachón and Cerro Tololo

Looking along a road toward a large telescope dome, with a second dome to the right.

The Gemini Observatory consists of twin 8.1-meter diameter optical/infrared telescopes located in Hawai’i and Chile. Here is Gemini South – located on the summit of Cerro Pachón in Chile – with the Large Synoptic Survey Telescope (LSST) to the right. Image via R. Pettengill (NRAO/AUI/NSF).

About an hour’s flight north of Santiago near the city of Vicuña, in the Equi Valle, lie some of the world’s best sites for observatories: Cerro Pachón and Cerro Tololo. Vicuña, in the Elqui Valley, calls itself the world capitol of astronomy, with many tourist and research observatories nearby. The ACEAP (Astronomy in Chile Educator Ambassador Program) cadre was treated to a night of stargazing at the lovely Alpha Aldea and learned about the many educational programs that they support.

The 2019 ACEAP expedition was given full access to both locations and spent two nights with the astronomers there.

Cerro Pachón is the newer facility including the 4 meter SOAR (Southern Astrophysical Research) telescope, 10 m Gemini South, and under construction the 8.4 m LSST (Large Synoptic Survey Telescope). The Gemini telescope is the southern skies twin to the Gemini on Mauna Kea in Hawaii. Both SOAR and Gemini use adaptive optics correcting for atmospheric turbulence with sodium laser guide stars.

Nearby, Cerro Tololo hosts most of the U.S. National Science Foundation and National Optical Astronomy Observatory facilities. Cerro Tololo is ground zero for astronomical collaboration between the U.S. and Chile.

Group photo in front of large telescope, inside a large dome.

Cerro Tololo Inter-American Observatory (CTIO) is a complex of astronomical telescopes and instruments located approximately 50 miles (80 km) to the east of La Serena, Chile, at an altitude of 7,200 feet (2,200 meters). Here is the CTIO 1.5-meter telescope with ACEAP 2019. Image via K Flores/ C Johns (NRAO/AUI/NSF).

Professor Federico Rutllant of the University of Chile collaborated with AURA (Association of Universities for Research in Astronomy) to identify a site for a large Chilean American telescope in 1959 with the 1.5-meter telescope completed in 1965. The 4-meter telescope completed in 1976 named for Puerto Rican astronomer Victor Blanco is now the CTIO’s largest.

Large telescope with astronomy group in front, holding up a lighted sign reading ACEAP 2019.

Astronomy in Chile Educator Ambassador Program (ACEAP 2019) in front of the Blanco telescope on Cerro Tololo. Image via L. Sparks (NRAO/AUI/NSF).

The profound darkness and silence of these sites at night is broken only by the deep hum of the telescopes dancing with the stars. We were treated to spectacular views of the Milky Way and the Magellanic Clouds.

Daytime at the observatories were filled with talks and questions. Our meals at the cafeteria (casino to Chileans) were good with spectacular vistas.

Spectacular view of mountains and valleys in the Chilean Andes.

The view from the Cerro Tololo casino (cafeteria), via R. Pettengill (NRAO/AUI/NSF).

We are headed next to San Pedro de Atacama and up to the ALMA radio telescope at 16,500-feet elevation.

Bottom line: Robert Pettengill reports from the busy ACEAP (Astronomy in Chile Educator Ambassador Program) trip to Chile in July and August 2019. Read his first dispatch here: Astronomy educators to rendezvous in Chile



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Looking along a road toward a large telescope dome, with a second dome to the right.

The Gemini Observatory consists of twin 8.1-meter diameter optical/infrared telescopes located in Hawai’i and Chile. Here is Gemini South – located on the summit of Cerro Pachón in Chile – with the Large Synoptic Survey Telescope (LSST) to the right. Image via R. Pettengill (NRAO/AUI/NSF).

About an hour’s flight north of Santiago near the city of Vicuña, in the Equi Valle, lie some of the world’s best sites for observatories: Cerro Pachón and Cerro Tololo. Vicuña, in the Elqui Valley, calls itself the world capitol of astronomy, with many tourist and research observatories nearby. The ACEAP (Astronomy in Chile Educator Ambassador Program) cadre was treated to a night of stargazing at the lovely Alpha Aldea and learned about the many educational programs that they support.

The 2019 ACEAP expedition was given full access to both locations and spent two nights with the astronomers there.

Cerro Pachón is the newer facility including the 4 meter SOAR (Southern Astrophysical Research) telescope, 10 m Gemini South, and under construction the 8.4 m LSST (Large Synoptic Survey Telescope). The Gemini telescope is the southern skies twin to the Gemini on Mauna Kea in Hawaii. Both SOAR and Gemini use adaptive optics correcting for atmospheric turbulence with sodium laser guide stars.

Nearby, Cerro Tololo hosts most of the U.S. National Science Foundation and National Optical Astronomy Observatory facilities. Cerro Tololo is ground zero for astronomical collaboration between the U.S. and Chile.

Group photo in front of large telescope, inside a large dome.

Cerro Tololo Inter-American Observatory (CTIO) is a complex of astronomical telescopes and instruments located approximately 50 miles (80 km) to the east of La Serena, Chile, at an altitude of 7,200 feet (2,200 meters). Here is the CTIO 1.5-meter telescope with ACEAP 2019. Image via K Flores/ C Johns (NRAO/AUI/NSF).

Professor Federico Rutllant of the University of Chile collaborated with AURA (Association of Universities for Research in Astronomy) to identify a site for a large Chilean American telescope in 1959 with the 1.5-meter telescope completed in 1965. The 4-meter telescope completed in 1976 named for Puerto Rican astronomer Victor Blanco is now the CTIO’s largest.

Large telescope with astronomy group in front, holding up a lighted sign reading ACEAP 2019.

Astronomy in Chile Educator Ambassador Program (ACEAP 2019) in front of the Blanco telescope on Cerro Tololo. Image via L. Sparks (NRAO/AUI/NSF).

The profound darkness and silence of these sites at night is broken only by the deep hum of the telescopes dancing with the stars. We were treated to spectacular views of the Milky Way and the Magellanic Clouds.

Daytime at the observatories were filled with talks and questions. Our meals at the cafeteria (casino to Chileans) were good with spectacular vistas.

Spectacular view of mountains and valleys in the Chilean Andes.

The view from the Cerro Tololo casino (cafeteria), via R. Pettengill (NRAO/AUI/NSF).

We are headed next to San Pedro de Atacama and up to the ALMA radio telescope at 16,500-feet elevation.

Bottom line: Robert Pettengill reports from the busy ACEAP (Astronomy in Chile Educator Ambassador Program) trip to Chile in July and August 2019. Read his first dispatch here: Astronomy educators to rendezvous in Chile



from EarthSky https://ift.tt/2OC4wrd

A new species of duck-billed dinosaur

Head of duck-billed dinosaur with bulbous red crest on its nose.

Meet Aquilarhinus palimentus, a new species of hadrosaurid – a duck-billed dinosaur – discovered in Texas. Image via ICRA Art/Taylor & Francis Group.

New species of dinosaurs – well, their fossils – continue to be discovered by scientists. Now, an unusual species of duck-billed dinosaur, a hadrosaurid, has been found, which lived 80 million years ago in southwestern Texas. The skull is the most complete yet discovered of a duck-billed dinosaur from Big Bend National Park.

The finding was announced by Albert Prieto-Márquez at the Catalan Institute of Palaeontology in Barcelona, and the peer-reviewed results were published in the Journal of Systematic Palaeontology on July 12, 2019.

The exquisite skull specimen reveals a a new genus and species of duck-billed dinosaur, and has been named Aquilarhinus palimentus. Its aquiline nose, curved like an eagle’s beak, and wide lower jaw, shaped like two trowels laid side by side, give it a unique appearance among the duck-billed dinosaurs. Prieto-Márquez explained the significance of the finding:

This new animal is one of the more primitive hadrosaurids known and can therefore help us to understand how and why the ornamentation on their heads evolved, as well as where the group initially evolved and migrated from. Its existence adds another piece of evidence to the growing hypothesis, still up in the air, that the group began in the southeastern area of the US.

Four-legged dinosaur with raised head, open mouth, long stiff striped tail.

A complete view of Aquilarhinus palimentus as it might have looked when still alive. Image via ICRA Art/Taylor & Francis Group.

The facial and cranial construction of the dinosaur suggests that it fed itself by shoveling loose, wet sediment to scoop up loosely-rooted aquatic plants from the tidal marshes of an ancient delta. It is one of the oldest and most primitive hadrosaurids found to date.

The skull and other bones had first been found in the 1980s by Tom Lehman at Texas Tech University, in rock layers on Rattlesnake Mountain in Big Bend National Park. However, some of them were stuck together, making analysis difficult. The arched nasal crest and unique jaw were discovered by research in the 1990s. At first, the bones were thought to belong to a hadrosaurid called Gryposaurus, but the more recent analysis showed that they were more primitive.

Aquilarhinus palimentus did not fit in with the main group of hadrosaurids, called Saurolophidae. The fact that it is more primitive is evidence that there were a greater number of lineages than previously thought. Bony cranial crests were common on the heads of hadrosaurids, and came in a variety of shapes and sizes. Some of these were solid, while others were hollow. The bony crest of Aquilarhinus palimentus, however, was simpler in structure, shaped simply like a humped nose. This crest was solid, providing evidence that all such crests evolved from a common ancestor, a hadrosaurid with a simple humped nose.

Oblong brown fossil with spoon-like feature at left end.

A fossilized mandible of Aquilarhinus palimentus, with unusual upturned end. Image via Albert Prieto-Marquez/The University of Texas at Austin/Taylor & Francis Group.

Fossil location on Rattlesnake Mountain with vertical chart of rock formations on left side of drawing.

The location of the Aquilarhinus palimentus skull and other bones on Rattlesnake Mountain in Big Bend National Park, Texas. Image via Albert Prieto-Márquez/Journal of Systematic Palaeontology.

Hadrosaurids were the most common herbivorous – plant-eating – dinosaurs in the late Mesozoic Era. While there were some differences among species, these duck-billed dinosaurs generally look similar, where the front of the jaws would meet in a U-shape to support a cupped beak. Aquilarhinus palimentus is the first known species of this dinosaur to show significant differences in facial and cranial structure. Unlike other hadrosaurids, the lower jaws of Aquilarhinus palimentus met in a weird W-shape, which created a wide, flattened scoop. This would have been ideal for eating the loose aquatic plants in the marshes. As well as in North America, hadrosaurids were also common in Asia and Europe. Fossil evidence suggests that they had camel-like feet and stiff tails, and spent most of their time on land, but close to bodies of water. The cranial crests on some hadrosaurids are thought to most likely have served as resonating chambers, allowing them to make deep, loud sounds.

Bottom line: Scientists have discovered a previously unknown species of a duck-billed dinosaur that used to roam in what is now southwestern Texas. The skull is the most complete hadrosaurid skull ever found so far.

Source: An unusual ‘shovel-billed’ dinosaur with trophic specializations from the early Campanian of Trans-Pecos Texas, and the ancestral hadrosaurian crest

Via Taylor & Francis Group



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Head of duck-billed dinosaur with bulbous red crest on its nose.

Meet Aquilarhinus palimentus, a new species of hadrosaurid – a duck-billed dinosaur – discovered in Texas. Image via ICRA Art/Taylor & Francis Group.

New species of dinosaurs – well, their fossils – continue to be discovered by scientists. Now, an unusual species of duck-billed dinosaur, a hadrosaurid, has been found, which lived 80 million years ago in southwestern Texas. The skull is the most complete yet discovered of a duck-billed dinosaur from Big Bend National Park.

The finding was announced by Albert Prieto-Márquez at the Catalan Institute of Palaeontology in Barcelona, and the peer-reviewed results were published in the Journal of Systematic Palaeontology on July 12, 2019.

The exquisite skull specimen reveals a a new genus and species of duck-billed dinosaur, and has been named Aquilarhinus palimentus. Its aquiline nose, curved like an eagle’s beak, and wide lower jaw, shaped like two trowels laid side by side, give it a unique appearance among the duck-billed dinosaurs. Prieto-Márquez explained the significance of the finding:

This new animal is one of the more primitive hadrosaurids known and can therefore help us to understand how and why the ornamentation on their heads evolved, as well as where the group initially evolved and migrated from. Its existence adds another piece of evidence to the growing hypothesis, still up in the air, that the group began in the southeastern area of the US.

Four-legged dinosaur with raised head, open mouth, long stiff striped tail.

A complete view of Aquilarhinus palimentus as it might have looked when still alive. Image via ICRA Art/Taylor & Francis Group.

The facial and cranial construction of the dinosaur suggests that it fed itself by shoveling loose, wet sediment to scoop up loosely-rooted aquatic plants from the tidal marshes of an ancient delta. It is one of the oldest and most primitive hadrosaurids found to date.

The skull and other bones had first been found in the 1980s by Tom Lehman at Texas Tech University, in rock layers on Rattlesnake Mountain in Big Bend National Park. However, some of them were stuck together, making analysis difficult. The arched nasal crest and unique jaw were discovered by research in the 1990s. At first, the bones were thought to belong to a hadrosaurid called Gryposaurus, but the more recent analysis showed that they were more primitive.

Aquilarhinus palimentus did not fit in with the main group of hadrosaurids, called Saurolophidae. The fact that it is more primitive is evidence that there were a greater number of lineages than previously thought. Bony cranial crests were common on the heads of hadrosaurids, and came in a variety of shapes and sizes. Some of these were solid, while others were hollow. The bony crest of Aquilarhinus palimentus, however, was simpler in structure, shaped simply like a humped nose. This crest was solid, providing evidence that all such crests evolved from a common ancestor, a hadrosaurid with a simple humped nose.

Oblong brown fossil with spoon-like feature at left end.

A fossilized mandible of Aquilarhinus palimentus, with unusual upturned end. Image via Albert Prieto-Marquez/The University of Texas at Austin/Taylor & Francis Group.

Fossil location on Rattlesnake Mountain with vertical chart of rock formations on left side of drawing.

The location of the Aquilarhinus palimentus skull and other bones on Rattlesnake Mountain in Big Bend National Park, Texas. Image via Albert Prieto-Márquez/Journal of Systematic Palaeontology.

Hadrosaurids were the most common herbivorous – plant-eating – dinosaurs in the late Mesozoic Era. While there were some differences among species, these duck-billed dinosaurs generally look similar, where the front of the jaws would meet in a U-shape to support a cupped beak. Aquilarhinus palimentus is the first known species of this dinosaur to show significant differences in facial and cranial structure. Unlike other hadrosaurids, the lower jaws of Aquilarhinus palimentus met in a weird W-shape, which created a wide, flattened scoop. This would have been ideal for eating the loose aquatic plants in the marshes. As well as in North America, hadrosaurids were also common in Asia and Europe. Fossil evidence suggests that they had camel-like feet and stiff tails, and spent most of their time on land, but close to bodies of water. The cranial crests on some hadrosaurids are thought to most likely have served as resonating chambers, allowing them to make deep, loud sounds.

Bottom line: Scientists have discovered a previously unknown species of a duck-billed dinosaur that used to roam in what is now southwestern Texas. The skull is the most complete hadrosaurid skull ever found so far.

Source: An unusual ‘shovel-billed’ dinosaur with trophic specializations from the early Campanian of Trans-Pecos Texas, and the ancestral hadrosaurian crest

Via Taylor & Francis Group



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What does a marsquake feel like?

Fifty years after Apollo 11 astronauts deployed the first seismometer on the surface of the moon, data from NASA InSight’s seismic experiment has given researchers the opportunity to compare marsquakes to moon and earthquakes.

Southern California got all shook up after a set of recent earthquakes. But Earth isn’t the only place that experiences quakes: Both the moon and Mars have them as well.

The Apollo 11 mission took the first seismometer to the moon in 1969. In late 2018, NASA’s InSight lander brought the first seismometer to Mars. The seismometer, called the Seismic Experiment for Interior Structure (SEIS), detected its first marsquake on April 6, 2019. Scientists at ETH Zurich in Switzerland compared moonquakes detected by Apollo-era seismometers, with two quakes recently detected by SEIS on Mars, and quakes recorded here on Earth.

Quakes look and feel different depending on the material their seismic waves pass through. While seismic waves that travel through the Earth typically persist between tens of seconds to a few minutes, moonquakes can last up to an hour or more. The extent of the seismic signal is due to distance and to differences in geological structures.In a new video (above), the researchers demonstrate this by using data from the Apollo-era seismometers on the moon, two of the first quakes detected on Mars by SEIS and quakes recorded here on Earth. By running data from these worlds through a quake simulator, or shake room, scientists can experience for themselves how different the earthquakes can be.

Arc-shaped waves from a point source travel through planet to break upon the surface far away.

This artist’s concept is a simulation of what seismic waves from a marsquake might look like as they move through different layers of the Martian interior. Image via NASA/JPL-Caltech/ETH Zurich/Van Driel.

Bottom line: New video compares marsquakes, moonquakes, and earthquakes.

Via NASA



from EarthSky https://ift.tt/2YlHXLJ

Fifty years after Apollo 11 astronauts deployed the first seismometer on the surface of the moon, data from NASA InSight’s seismic experiment has given researchers the opportunity to compare marsquakes to moon and earthquakes.

Southern California got all shook up after a set of recent earthquakes. But Earth isn’t the only place that experiences quakes: Both the moon and Mars have them as well.

The Apollo 11 mission took the first seismometer to the moon in 1969. In late 2018, NASA’s InSight lander brought the first seismometer to Mars. The seismometer, called the Seismic Experiment for Interior Structure (SEIS), detected its first marsquake on April 6, 2019. Scientists at ETH Zurich in Switzerland compared moonquakes detected by Apollo-era seismometers, with two quakes recently detected by SEIS on Mars, and quakes recorded here on Earth.

Quakes look and feel different depending on the material their seismic waves pass through. While seismic waves that travel through the Earth typically persist between tens of seconds to a few minutes, moonquakes can last up to an hour or more. The extent of the seismic signal is due to distance and to differences in geological structures.In a new video (above), the researchers demonstrate this by using data from the Apollo-era seismometers on the moon, two of the first quakes detected on Mars by SEIS and quakes recorded here on Earth. By running data from these worlds through a quake simulator, or shake room, scientists can experience for themselves how different the earthquakes can be.

Arc-shaped waves from a point source travel through planet to break upon the surface far away.

This artist’s concept is a simulation of what seismic waves from a marsquake might look like as they move through different layers of the Martian interior. Image via NASA/JPL-Caltech/ETH Zurich/Van Driel.

Bottom line: New video compares marsquakes, moonquakes, and earthquakes.

Via NASA



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Rare reflection rainbow over Michigan

There are primary and secondary rainbows in the sky here (the 2 outside bows; note their colors are reversed). The 3rd bow (the inner one) is called a reflection rainbow. Beverly Ulfig caught this rare rainbow with an iPhone 6.

Beverly Ulfig captured this rainbow photo at Sands Park on Manistee Lake in Kalkaska, Michigan, on July 23, 2018. She wrote:

The entire day had a feel of rain off and on. It did rain at approximately 5:30 p.m. for about 10 minutes. But it remained somewhat cloudy. The sun appeared about 7 p.m., and then we were treated to this special occurrence.

What Beverly caught is a rare type of rainbow, called a reflection rainbow. You sometimes see one over water, as in the photo above. At the great website Atmospheric Optics, Les Cowley explains:

Sunlight reflected off the water and traveling upwards makes the reflection bow. To raindrops, the reflected light appears to come from a second sun the same angular distance below the water as the real sun is above it.

Les has a lot more to say about reflection rainbows, which you can read here.

Thank you, Beverly and Les!

Bottom line: July 23, 2018, photo of a rare reflection rainbow, captured in Michigan.



from EarthSky https://ift.tt/2YAfmxn

There are primary and secondary rainbows in the sky here (the 2 outside bows; note their colors are reversed). The 3rd bow (the inner one) is called a reflection rainbow. Beverly Ulfig caught this rare rainbow with an iPhone 6.

Beverly Ulfig captured this rainbow photo at Sands Park on Manistee Lake in Kalkaska, Michigan, on July 23, 2018. She wrote:

The entire day had a feel of rain off and on. It did rain at approximately 5:30 p.m. for about 10 minutes. But it remained somewhat cloudy. The sun appeared about 7 p.m., and then we were treated to this special occurrence.

What Beverly caught is a rare type of rainbow, called a reflection rainbow. You sometimes see one over water, as in the photo above. At the great website Atmospheric Optics, Les Cowley explains:

Sunlight reflected off the water and traveling upwards makes the reflection bow. To raindrops, the reflected light appears to come from a second sun the same angular distance below the water as the real sun is above it.

Les has a lot more to say about reflection rainbows, which you can read here.

Thank you, Beverly and Les!

Bottom line: July 23, 2018, photo of a rare reflection rainbow, captured in Michigan.



from EarthSky https://ift.tt/2YAfmxn

Protection from mosquitos key to avoid West Nile virus

"In Georgia, West Nile virus is primarily spread by the southern house mosquito Culex quinquefasciatus," says Gonzalo Vazquez-Prokopec, associate professor in Emory's Department of Environmental Sciences. (CDC/James Gathany)

August to September is the peak of the West Nile virus (WNV) season and Atlanta area health officials have reported finding mosquitoes testing positive for the pathogen, including from 11 locations across DeKalb County. No human cases, however, have been reported.

WNV is most commonly spread to people by the bite of an infected mosquito. Most people who become infected do not feel sick, but about one in five develop a fever and other symptoms. And about one out of 150 people infected develop a serious, sometimes fatal, illness, according to the CDC.

Gonzalo Vazquez-Prokopec, associate professor in Emory University's Department of Environmental Sciences, is an expert in mosquito-borne diseases. His lab has studied the urban ecology of metro Atlanta and the Culex mosquito — a vector for WNV and other human pathogens.

Vazquez-Prokopec is currently in the field in Brazil, but we caught up with him via email for a brief Q and A.

What should people know about the particular type of mosquito that spreads WNV?

In Georgia, West Nile virus is primarily spread by the southern house mosquito Culex quinquefasciatus. This light-brown colored species bites at dusk and dawn, and is found in high numbers in and around houses and in open areas, such as parks.

Is it normal to detect WNV in so many Atlanta-area mosquitoes this time of year? 

Yes, the infection rates in mosquitoes, gathered from different mosquito traps, are following trends that we’ve seen in previous years. What we do not see is human cases — so far this year none have been reported for Georgia.

Is Atlanta normally at higher or average risk for human cases of WNV? 

Human infection with WNV is low in Georgia compared to some states in the Northeast or Midwest. This is remarkably different from what we see in mosquitoes and birds which, in Atlanta, have equally high WNV levels compared to the Northeast and Midwest. What seems to be different is the rate of spillover of the virus, or transfer from the wildlife cycle to humans, which definitely appears to be suppressed in the Southeastern United States.

How can people best protect themselves? 

Reducing human exposure to Culex mosquitoes is key to maintaining the low rates of human infection. It’s best to follow the recommendations on the CDC web site to use insect repellent and wear long-sleeved shirts and long pants when outside to protect yourself from mosquito bites, and to remove any standing water around your home. Dekalb County has a great checklist on its web site to help locate potential mosquito breeding sites around your yard.

Related:
Cardinals may reduce West Nile virus spillover in Atlanta
Sewage raises West Nile virus risk

from eScienceCommons https://ift.tt/2YC2qLF
"In Georgia, West Nile virus is primarily spread by the southern house mosquito Culex quinquefasciatus," says Gonzalo Vazquez-Prokopec, associate professor in Emory's Department of Environmental Sciences. (CDC/James Gathany)

August to September is the peak of the West Nile virus (WNV) season and Atlanta area health officials have reported finding mosquitoes testing positive for the pathogen, including from 11 locations across DeKalb County. No human cases, however, have been reported.

WNV is most commonly spread to people by the bite of an infected mosquito. Most people who become infected do not feel sick, but about one in five develop a fever and other symptoms. And about one out of 150 people infected develop a serious, sometimes fatal, illness, according to the CDC.

Gonzalo Vazquez-Prokopec, associate professor in Emory University's Department of Environmental Sciences, is an expert in mosquito-borne diseases. His lab has studied the urban ecology of metro Atlanta and the Culex mosquito — a vector for WNV and other human pathogens.

Vazquez-Prokopec is currently in the field in Brazil, but we caught up with him via email for a brief Q and A.

What should people know about the particular type of mosquito that spreads WNV?

In Georgia, West Nile virus is primarily spread by the southern house mosquito Culex quinquefasciatus. This light-brown colored species bites at dusk and dawn, and is found in high numbers in and around houses and in open areas, such as parks.

Is it normal to detect WNV in so many Atlanta-area mosquitoes this time of year? 

Yes, the infection rates in mosquitoes, gathered from different mosquito traps, are following trends that we’ve seen in previous years. What we do not see is human cases — so far this year none have been reported for Georgia.

Is Atlanta normally at higher or average risk for human cases of WNV? 

Human infection with WNV is low in Georgia compared to some states in the Northeast or Midwest. This is remarkably different from what we see in mosquitoes and birds which, in Atlanta, have equally high WNV levels compared to the Northeast and Midwest. What seems to be different is the rate of spillover of the virus, or transfer from the wildlife cycle to humans, which definitely appears to be suppressed in the Southeastern United States.

How can people best protect themselves? 

Reducing human exposure to Culex mosquitoes is key to maintaining the low rates of human infection. It’s best to follow the recommendations on the CDC web site to use insect repellent and wear long-sleeved shirts and long pants when outside to protect yourself from mosquito bites, and to remove any standing water around your home. Dekalb County has a great checklist on its web site to help locate potential mosquito breeding sites around your yard.

Related:
Cardinals may reduce West Nile virus spillover in Atlanta
Sewage raises West Nile virus risk

from eScienceCommons https://ift.tt/2YC2qLF

ESA and ESO confirm asteroid will miss Earth in September

Diagram showing orbits of Earth, inner planets, and asteroid 2006 QV89.

Viewed on this scale, from above the solar system, it looks as if the paths of Earth and asteroid 2006 QV89 intersect. Yet this asteroid’s pass on September 9, 2019 shouldn’t be a particularly close one. Image via NASA’s Center for Near Earth Object Studies.

We’re still getting emails from people asking about asteroid 2006 QV89, a space rock that’ll pass closest to Earth on September 9, 2019. Since June, there’ve been numerous online articles (for example, here and here), some focusing the minuscule chance this asteroid might strike Earth in September. We’re here to focus on the much, much, much greater chance this asteroid will not strike us. In fact, asteroid 2006 QV89 is currently classified by astronomers as NO HAZARD. It is not expected to hit Earth. In July, for example, in what astronomers said is “the first known case of ruling out an asteroid impact through a ‘non-detection’,” the European Space Agency (ESA) and the European Southern Observatory (ESO) concluded that this asteroid is not on a collision course with Earth in 2019 – and the chance of any future impact is also extremely remote. More about the ESA/ESO non-detection below.

Before we get into ESA and ESO’s non-detection and no-collision conclusion, though, let’s ask … what does NASA say? As of June 2019, calculations made by NASA/JPL with the available data suggest the space rock will not even have a particularly close approach to Earth in September 2019. According to NASA’s Center for Near Earth Object Studies, 2006 QV89 will likely pass so far from our planet that there is a 99.989 percent chance the space rock will miss the Earth in September 2019.

Why the uproar about asteroid 2006 QV89 in the first place? The reason stems in part from the fact that this asteroid does appear on a “risk objects list” from the ESA, as do many other objects. In the case of asteroid 2006 QV89, it’s important to note that the asteroid has a Torino Scale of 0, which indicates its no hazard status. You can note that for yourself on the chart below, from ESA. Like many asteroids, 2006 QV89 is on a “risk” list, but ESA currently classifies it as a non-priority risk.

ESA chart showing various orbital parameters for 2006 QV89.

This chart from the European Space Agency – published in June 2019 – shows the September 2019 distance of asteroid 2006 QV89 as 4,263,660 miles (6,861,695 km), or some 17 times the moon’s distance. The object is in astronomers’ “risk” category, but it’s not on their “priority” list.

Many asteroids temporarily appear in a risk list due to uncertainties in their orbits. These sorts of uncertainties typically occur when an object has been recently discovered by observatories, and seen only during a few nights after the discovery, afterwards becaming too faint to observe. As an asteroid is re-observed – and astronomers’ asteroid-orbit modeling programs recognize it as an asteroid previously detected – the incoming new observations let astronomers better refine its orbit. The Catalina Sky Survey in Arizona discovered 2006 QV89 on August 29, 2006. At that time, it had a very short (10-day) observation arc. The Arecibo Observatory made radar observations of this asteroid on September 6, 2006. Then, as it sped on, it was lost from view again and has not been detected since 2006.

And that brings us to ESA and ESO’s recent non-detection of the asteroid. ESA said on July 16, 2019:

While we do not know 2006 QV89’s trajectory exactly, we do know where it would appear in the sky if it were on a collision course with our planet. Therefore, we can simply observe this small area of the sky to check that the asteroid is indeed, hopefully, not there.

This way, we have the chance to indirectly exclude any risk of an impact, even without actually seeing the asteroid.

This is precisely what ESA and the European Southern Observatory (ESO) did on July 4 and 5, 2019, as part of the ongoing collaboration between the two organizations to observe high-risk asteroids using ESO’s Very Large Telescope (VLT).

Teams obtained very ‘deep’ images of a small area in the sky, where the asteroid would have been located if it were on track to impact Earth in September.

Nothing was seen.

The image below shows the region of the sky where asteroid 2006 QV89 would have been seen, only if it were on a collision course with Earth in 2019.

A blank image, with 3 red crosses on it.

The segment shown by the three red crosses in this VLT image shows where asteroid 2006 QV89 would have appeared had it been on a collision course with Earth in September 2019. The image has been processed to remove background star contamination, so the object would have appeared as a single bright round source inside the segment. ESA said, “Even if the asteroid were smaller than expected, at only a few meters across, it would have been seen in the image. Any smaller than this and the VLT could not have spotted it, but it would also be considered harmless as anything this size would burn up in Earth’s atmosphere.” Image via ESA.

From their brief observations of it – and from their knowledge of asteroids in general, which has grown dramatically in recent decades – astronomers can estimate that 2006 QV89 is about 98-131 feet (30-40 meters) in diameter, or about the length of an American football field. It’s classified as an Apollo type asteroid, which are Earth-crossing asteroids, of which some 20,000 are known as of January 2019.

Writing at Science20, Robert Walker had a good explanation for the status on asteroid 2006 QV89. He wrote on June 7, 2019:

Short summary for the panicking: Expected to miss and currently classified NO HAZARD. Tiny, most likely for an asteroid of that size is ‘Splosh in Pacific’. Likely many thousands of years before any such asteroid hits an urban area.

It is just a random asteroid, there are many in the table every year with dates that they ‘could’ hit, but they are classified as no hazard because they are all expected to miss. The press just picks up one of those many asteroids at random from time to time. Every year many asteroids are removed from the table that had dates of possible impacts that year. It is just one of numerous NO HAZARD asteroids currently in the table.

Some time in the next century or two then we can expect one of those many asteroids to hit, but if they are being tracked we would have at least 10 years warning to evacuate any city. The most likely thing is that the next asteroid to hit just sploshes harmlessly in the ocean. Hitting a city is extremely unlikely and most likely have to wait many thousands of years for that. An impact close enough to a city to warn residents to watch out for flying glass like Chelyabinsk is more likely and could happen, but not nearly as likely as a harmless splosh in the ocean.

This is an example of a ‘sensationalist press chose a random asteroid’ story. NASA didn’t warn us about it, and nor did ESA. It is expected to miss and is currrently classified as no hazard.

In short … don’t worry about ateroid 2006 QV89. It’s not going to hit us.

So how about seeing it as it passes? According to ESA, asteroid 2006 QV89 will show a maximum brightness or magnitude of +21.9 in September 2019, which means the space rock will appear extremely faint. It’ll be so faint that it will not even be visible with most telescopes, except for a few huge, observatory-type instruments.

Diagram of spacecraft's trajectory toward small space rock in orbit around slightly larger one.

NASA plans to try to deflect a space rock from its path around September 2022. This schematic of the DART mission shows the impact on the moonlet of asteroid Didymos. Post-impact observations from Earth-based optical telescopes and planetary radar would, in turn, measure the change in the moonlet’s orbit about the parent body. Image via NASA/Johns Hopkins Applied Physics Lab.

Astronomers and other scientists are practicing with every close pass of an asteroid, in order to better prepare for a real scenario of any dangerous close approach on the future. What’s more, NASA is going to practice deflecting an asteroid from its path. The Double Asteroid Redirection Test (DART mission) is a planned space probe that will demonstrate the effects of crashing an impactor spacecraft into an asteroid moon for planetary defense purposes. It will launch in June 2021 and will try to impact a 525-foot (160-meter) moonlet in the binary asteroid Didymos. The intentional impact should occur sometime in September 2022. Read more about DART.

Eventually, it’s likely we will learn to deflect an incoming asteroid. Right now, though, if scientists were to detect an incoming asteroid, the best defense we have is to determine the impact area as precisely as possible, and then to evacuate the area. An excellent exercise occurred on November 13, 2015. A small object – which then was determined to be space debris – was detected with a trajectory that would intercept Earth. A team of scientists was able to determine it would enter Earth’s atmosphere over the ocean near Sri Lanka, and a “no fly”and “no fishing” zone was issued.

So there you have it. As we’ve said many times before, and as is still true, as of now, there’s no known dangerous asteroid that poses any imminent risk of Earth impact. Could an asteroid strike Earth? Of course. That’s why astronomers continue to be watchful.

Bottom line: Asteroid 2006 QV89 has been unfairly hyped as posing a threat to Earth in September 2019. In fact, it’s one of many asteroids on astronomers’ risk list, but it’s not classified as a priority risk. It’s classified as “no hazard.” In July, the European Space Agency and the European Southern Observatory concluded that this asteroid is not on a collision course this year – and the chance of any future impact is extremely remote.



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Diagram showing orbits of Earth, inner planets, and asteroid 2006 QV89.

Viewed on this scale, from above the solar system, it looks as if the paths of Earth and asteroid 2006 QV89 intersect. Yet this asteroid’s pass on September 9, 2019 shouldn’t be a particularly close one. Image via NASA’s Center for Near Earth Object Studies.

We’re still getting emails from people asking about asteroid 2006 QV89, a space rock that’ll pass closest to Earth on September 9, 2019. Since June, there’ve been numerous online articles (for example, here and here), some focusing the minuscule chance this asteroid might strike Earth in September. We’re here to focus on the much, much, much greater chance this asteroid will not strike us. In fact, asteroid 2006 QV89 is currently classified by astronomers as NO HAZARD. It is not expected to hit Earth. In July, for example, in what astronomers said is “the first known case of ruling out an asteroid impact through a ‘non-detection’,” the European Space Agency (ESA) and the European Southern Observatory (ESO) concluded that this asteroid is not on a collision course with Earth in 2019 – and the chance of any future impact is also extremely remote. More about the ESA/ESO non-detection below.

Before we get into ESA and ESO’s non-detection and no-collision conclusion, though, let’s ask … what does NASA say? As of June 2019, calculations made by NASA/JPL with the available data suggest the space rock will not even have a particularly close approach to Earth in September 2019. According to NASA’s Center for Near Earth Object Studies, 2006 QV89 will likely pass so far from our planet that there is a 99.989 percent chance the space rock will miss the Earth in September 2019.

Why the uproar about asteroid 2006 QV89 in the first place? The reason stems in part from the fact that this asteroid does appear on a “risk objects list” from the ESA, as do many other objects. In the case of asteroid 2006 QV89, it’s important to note that the asteroid has a Torino Scale of 0, which indicates its no hazard status. You can note that for yourself on the chart below, from ESA. Like many asteroids, 2006 QV89 is on a “risk” list, but ESA currently classifies it as a non-priority risk.

ESA chart showing various orbital parameters for 2006 QV89.

This chart from the European Space Agency – published in June 2019 – shows the September 2019 distance of asteroid 2006 QV89 as 4,263,660 miles (6,861,695 km), or some 17 times the moon’s distance. The object is in astronomers’ “risk” category, but it’s not on their “priority” list.

Many asteroids temporarily appear in a risk list due to uncertainties in their orbits. These sorts of uncertainties typically occur when an object has been recently discovered by observatories, and seen only during a few nights after the discovery, afterwards becaming too faint to observe. As an asteroid is re-observed – and astronomers’ asteroid-orbit modeling programs recognize it as an asteroid previously detected – the incoming new observations let astronomers better refine its orbit. The Catalina Sky Survey in Arizona discovered 2006 QV89 on August 29, 2006. At that time, it had a very short (10-day) observation arc. The Arecibo Observatory made radar observations of this asteroid on September 6, 2006. Then, as it sped on, it was lost from view again and has not been detected since 2006.

And that brings us to ESA and ESO’s recent non-detection of the asteroid. ESA said on July 16, 2019:

While we do not know 2006 QV89’s trajectory exactly, we do know where it would appear in the sky if it were on a collision course with our planet. Therefore, we can simply observe this small area of the sky to check that the asteroid is indeed, hopefully, not there.

This way, we have the chance to indirectly exclude any risk of an impact, even without actually seeing the asteroid.

This is precisely what ESA and the European Southern Observatory (ESO) did on July 4 and 5, 2019, as part of the ongoing collaboration between the two organizations to observe high-risk asteroids using ESO’s Very Large Telescope (VLT).

Teams obtained very ‘deep’ images of a small area in the sky, where the asteroid would have been located if it were on track to impact Earth in September.

Nothing was seen.

The image below shows the region of the sky where asteroid 2006 QV89 would have been seen, only if it were on a collision course with Earth in 2019.

A blank image, with 3 red crosses on it.

The segment shown by the three red crosses in this VLT image shows where asteroid 2006 QV89 would have appeared had it been on a collision course with Earth in September 2019. The image has been processed to remove background star contamination, so the object would have appeared as a single bright round source inside the segment. ESA said, “Even if the asteroid were smaller than expected, at only a few meters across, it would have been seen in the image. Any smaller than this and the VLT could not have spotted it, but it would also be considered harmless as anything this size would burn up in Earth’s atmosphere.” Image via ESA.

From their brief observations of it – and from their knowledge of asteroids in general, which has grown dramatically in recent decades – astronomers can estimate that 2006 QV89 is about 98-131 feet (30-40 meters) in diameter, or about the length of an American football field. It’s classified as an Apollo type asteroid, which are Earth-crossing asteroids, of which some 20,000 are known as of January 2019.

Writing at Science20, Robert Walker had a good explanation for the status on asteroid 2006 QV89. He wrote on June 7, 2019:

Short summary for the panicking: Expected to miss and currently classified NO HAZARD. Tiny, most likely for an asteroid of that size is ‘Splosh in Pacific’. Likely many thousands of years before any such asteroid hits an urban area.

It is just a random asteroid, there are many in the table every year with dates that they ‘could’ hit, but they are classified as no hazard because they are all expected to miss. The press just picks up one of those many asteroids at random from time to time. Every year many asteroids are removed from the table that had dates of possible impacts that year. It is just one of numerous NO HAZARD asteroids currently in the table.

Some time in the next century or two then we can expect one of those many asteroids to hit, but if they are being tracked we would have at least 10 years warning to evacuate any city. The most likely thing is that the next asteroid to hit just sploshes harmlessly in the ocean. Hitting a city is extremely unlikely and most likely have to wait many thousands of years for that. An impact close enough to a city to warn residents to watch out for flying glass like Chelyabinsk is more likely and could happen, but not nearly as likely as a harmless splosh in the ocean.

This is an example of a ‘sensationalist press chose a random asteroid’ story. NASA didn’t warn us about it, and nor did ESA. It is expected to miss and is currrently classified as no hazard.

In short … don’t worry about ateroid 2006 QV89. It’s not going to hit us.

So how about seeing it as it passes? According to ESA, asteroid 2006 QV89 will show a maximum brightness or magnitude of +21.9 in September 2019, which means the space rock will appear extremely faint. It’ll be so faint that it will not even be visible with most telescopes, except for a few huge, observatory-type instruments.

Diagram of spacecraft's trajectory toward small space rock in orbit around slightly larger one.

NASA plans to try to deflect a space rock from its path around September 2022. This schematic of the DART mission shows the impact on the moonlet of asteroid Didymos. Post-impact observations from Earth-based optical telescopes and planetary radar would, in turn, measure the change in the moonlet’s orbit about the parent body. Image via NASA/Johns Hopkins Applied Physics Lab.

Astronomers and other scientists are practicing with every close pass of an asteroid, in order to better prepare for a real scenario of any dangerous close approach on the future. What’s more, NASA is going to practice deflecting an asteroid from its path. The Double Asteroid Redirection Test (DART mission) is a planned space probe that will demonstrate the effects of crashing an impactor spacecraft into an asteroid moon for planetary defense purposes. It will launch in June 2021 and will try to impact a 525-foot (160-meter) moonlet in the binary asteroid Didymos. The intentional impact should occur sometime in September 2022. Read more about DART.

Eventually, it’s likely we will learn to deflect an incoming asteroid. Right now, though, if scientists were to detect an incoming asteroid, the best defense we have is to determine the impact area as precisely as possible, and then to evacuate the area. An excellent exercise occurred on November 13, 2015. A small object – which then was determined to be space debris – was detected with a trajectory that would intercept Earth. A team of scientists was able to determine it would enter Earth’s atmosphere over the ocean near Sri Lanka, and a “no fly”and “no fishing” zone was issued.

So there you have it. As we’ve said many times before, and as is still true, as of now, there’s no known dangerous asteroid that poses any imminent risk of Earth impact. Could an asteroid strike Earth? Of course. That’s why astronomers continue to be watchful.

Bottom line: Asteroid 2006 QV89 has been unfairly hyped as posing a threat to Earth in September 2019. In fact, it’s one of many asteroids on astronomers’ risk list, but it’s not classified as a priority risk. It’s classified as “no hazard.” In July, the European Space Agency and the European Southern Observatory concluded that this asteroid is not on a collision course this year – and the chance of any future impact is extremely remote.



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Spot the young moon in early August

Most of us in the world’s Eastern Hemisphere – and even a good deal of the world’s Western Hemisphere – won’t spot this month’s young moon until August 2, 2019. Then – as the chart above shows – day by day, the moon will be a waxing crescent in the west after sunset, showing more of its day side in our sky and staying out longer each evening after sunset.

As for moon sightings on August 1 … some in western North America or islands in the Pacific might catch the exceedingly thin crescent very shortly after sunset. For example, as seen from Seattle, Washington, the young moon will be only about 1.7 percent illuminated as it sets some 48 minutes after the sun on August 1.

Seeing the moon on August 1 will be a challenge. You’ll need an unobstructed horizon in the direction of sunset. Start looking for the moon before it gets completely dark. You might also want to bring along your binoculars to help you to tease out the whisker-thin moon from the bright haze of evening twilight.

After all, the new moon happens on August 1, 2019, at 03:12 UTC; translate UTC to your time. At that instant of new moon, according to astronomers’ definitions, the old moon becomes a young moon again, as the moon transitions out of the morning sky and into evening sky.

The simulated image below – via the U.S. Naval Observatory – shows a young moon as seen from Seattle, Washington, on August 1.

Read more: What’s the youngest moon you can see?

Visit the Sunrise Sunset Calendars site to find out when the sun and moon set in your sky, remembering to check the moonrise and moonset box. The setting times presume a level horizon.

Almost black moon with very thin crescent line on right side.

Simulated image of the young moon on August 1, 2019, as seen from Seattle, Washington.

Very narrow irregular yellow crescent shimmering above trees on horizon.

Young moon refracted by the atmosphere as it nears the horizon – October 20, 2017 – by Mike Cohea.

Day by day, as the moon in its orbit moves farther away from the sun in our sky, the moon will be higher up at sunset and will stay out longer after dark. Moreover, the waxing moon’s illuminated side will continue to grow. Thus on August 3, 4 and 5, the moon will be easily visible to all, a lovely sight in the western twilight sky.

On all of these evenings – August 1 to 5, 2019 – watch for the soft glow of earthshine on the dark side of the crescent moon. Earthshine is twice-reflected sunlight. Consider that – when we see the moon as a thin sliver in our sky – people standing on the moon’s near side would be gazing at a nearly full Earth. A bright Earth lights up the nighttime side of the moon in much the same way that a bright moon lights up the nighttime terrain here on Earth. And that bright glow – sunlight that has bounced off Earth and is now bouncing off the moon’s dark side – is earthshine. Watch for it in the evenings ahead.

View of almost-full Earth from moon with East Asia and Australia on left, dark crescent on right.

Simulation of the nearly full Earth, as seen from the moon, as the sun sets over North America exactly 3 days after new moon (August 3, 2019, at 8:12 p.m. PDT – or August 4, at 3:12 UTC). This almost-full waning gibbous Earth will be casting its light on the dark side of a slender crescent moon seen in Earth’s sky. Thus, from Earth, the moon’s darkened portion will shine with the soft glow of earthshine. Image via Fourmilab’s EarthView.

On a waxing moon, the lunar terminator – the line between dark and light on the moon’s disk – shows you where sunrise is on the moon. It’s along the terminator that you have your best three-dimensional views of the lunar terrain through binoculars or the telescope. Because the lunar glare can be overpowering at night, it might be to your advantage to view the sights along the terminator in a daytime or twilight sky, as the moon waxes in phase this week.

Bottom line: Watch for the young moon as it first appears in the western evening sky in early August 2019.



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Most of us in the world’s Eastern Hemisphere – and even a good deal of the world’s Western Hemisphere – won’t spot this month’s young moon until August 2, 2019. Then – as the chart above shows – day by day, the moon will be a waxing crescent in the west after sunset, showing more of its day side in our sky and staying out longer each evening after sunset.

As for moon sightings on August 1 … some in western North America or islands in the Pacific might catch the exceedingly thin crescent very shortly after sunset. For example, as seen from Seattle, Washington, the young moon will be only about 1.7 percent illuminated as it sets some 48 minutes after the sun on August 1.

Seeing the moon on August 1 will be a challenge. You’ll need an unobstructed horizon in the direction of sunset. Start looking for the moon before it gets completely dark. You might also want to bring along your binoculars to help you to tease out the whisker-thin moon from the bright haze of evening twilight.

After all, the new moon happens on August 1, 2019, at 03:12 UTC; translate UTC to your time. At that instant of new moon, according to astronomers’ definitions, the old moon becomes a young moon again, as the moon transitions out of the morning sky and into evening sky.

The simulated image below – via the U.S. Naval Observatory – shows a young moon as seen from Seattle, Washington, on August 1.

Read more: What’s the youngest moon you can see?

Visit the Sunrise Sunset Calendars site to find out when the sun and moon set in your sky, remembering to check the moonrise and moonset box. The setting times presume a level horizon.

Almost black moon with very thin crescent line on right side.

Simulated image of the young moon on August 1, 2019, as seen from Seattle, Washington.

Very narrow irregular yellow crescent shimmering above trees on horizon.

Young moon refracted by the atmosphere as it nears the horizon – October 20, 2017 – by Mike Cohea.

Day by day, as the moon in its orbit moves farther away from the sun in our sky, the moon will be higher up at sunset and will stay out longer after dark. Moreover, the waxing moon’s illuminated side will continue to grow. Thus on August 3, 4 and 5, the moon will be easily visible to all, a lovely sight in the western twilight sky.

On all of these evenings – August 1 to 5, 2019 – watch for the soft glow of earthshine on the dark side of the crescent moon. Earthshine is twice-reflected sunlight. Consider that – when we see the moon as a thin sliver in our sky – people standing on the moon’s near side would be gazing at a nearly full Earth. A bright Earth lights up the nighttime side of the moon in much the same way that a bright moon lights up the nighttime terrain here on Earth. And that bright glow – sunlight that has bounced off Earth and is now bouncing off the moon’s dark side – is earthshine. Watch for it in the evenings ahead.

View of almost-full Earth from moon with East Asia and Australia on left, dark crescent on right.

Simulation of the nearly full Earth, as seen from the moon, as the sun sets over North America exactly 3 days after new moon (August 3, 2019, at 8:12 p.m. PDT – or August 4, at 3:12 UTC). This almost-full waning gibbous Earth will be casting its light on the dark side of a slender crescent moon seen in Earth’s sky. Thus, from Earth, the moon’s darkened portion will shine with the soft glow of earthshine. Image via Fourmilab’s EarthView.

On a waxing moon, the lunar terminator – the line between dark and light on the moon’s disk – shows you where sunrise is on the moon. It’s along the terminator that you have your best three-dimensional views of the lunar terrain through binoculars or the telescope. Because the lunar glare can be overpowering at night, it might be to your advantage to view the sights along the terminator in a daytime or twilight sky, as the moon waxes in phase this week.

Bottom line: Watch for the young moon as it first appears in the western evening sky in early August 2019.



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