Global internet access does seem like a worthy enterprise yet the rise of satellite megaconstellations there is a danger of the night sky becoming ruined. Astronomers the world over are keeping an eye on the impact these satellites are having on the night sky. Until recently the concerns have been relating to the reflection of visible light against the sky hindering night time observations. A recent study shows that the second-generation Starlink satellites leak 32 times the radio signal than the previous models. Are their presence putting at risk the radio sky now too?
The starlink satellites are the brainchild of SpaceX to provide high-speed broadband internet to every corner of the planet. The constellation of satellites consists of thousands of small satellites measuring just 2.8 metre in length. They form a network that can transmit data quickly around the planet offering high speed internet which is far more reliable than traditional satellite systems. The goal is to provide high speed connectivity to places where fibre or traditional infrastructure is difficult or too costly. As it expands though there will be more and more satellites in orbit.
An artist’s conception shows Starlink satellites in orbit. Credit: SpaceXIt’s not just SpaceX that is causing the problem though. Since 2019 other companies have been getting in on the act with organisations like OneWeb too having launched hundreds of thousands of satellites. The plan is for organisations like these to launch in excess of 100,000 satellites. If the rise in megaconstellations like these rise then the emissions (visible, radio or otherwise) could very easily make astronomical observations from the surface of Earth difficult if not impossible.
During the last year, observations with the Low Frequency Array (LOFAR) revealed that the Starlink satellites were emitting radio waves. Astronomers were concerned that the unintentional waves could have a negative impact on radio observations. As SpaceX expand their network with a second generation of satellites, their ‘V2-mini’ modules the risks seem to be increasing. New LOFAR observations have shown that the new satellites are producing up to 32 times more radio emissions than the earlier satellites! Anyone observing the universe in radio waves at the time of their passing is likely to receive a blinding radio signal that would ruin any observations.
The LOFAR ‘superterp’, part of the core of the extended telescope located in the Netherlands. Credit: LOFAR/ASTRONPutting the radio emissions into context, the new satellites are emitting radio waves 10 million times brighter than that detected by the faintest astronomical object detected by LOFAR so far! The discovery highlights the need for control and regulations around satellites and their emissions, intended or otherwise. Left unchecked then the future of astronomical observations will be highly compromised.
ASTRON operates LOFAR which is one of the most sensitive low frequency telescopes in the world. It’s only possible because it operates from the Netherlands which is one of the most densely populated countries in Europe. Despite the high population density, the national organisations of Netherlands co-operate and consult with ASTRON to safeguard the future of radio astronomy. We just need other organisations like SpaceX and OneWeb to jump on board to ensure our view of the universe isn’t lost for ever.
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When you look at the Moon, you don’t see any water on its surface. That doesn’t mean there isn’t any. In fact, there’s a lot of “wetness” on the Moon, but it’s in places and forms we can’t see. Understanding where all those resources are is the subject of a study based on NASA’s Moon Mineralogy Mapper (M3) data taken from aboard the Chandrayaan-1 spacecraft.
The analysis performed by a team led by Planetary Science Institute senior scientist Roger Clark shows that there are many sources of water and a group of chemicals called “hydroxyls” (OH). Water lies hidden in ice deposits in shaded areas, and inside enriched rocks.
Image showing the distribution of surface ice (which could supply water) at the Moon’s south pole (left) and north pole (right), detected by NASA’s Moon Mineralogy Mapper instrument. Credits: NASAHydroxyls are interesting. They form as solar protons interact with electrons on the Moon’s surface. That creates hydrogen atoms which hook up with oxygen atoms found in silicates and other oxygen-bearing molecules in the lunar regolith. Together, the hydrogen and oxygen make hydroxyl molecules, which are a component of water. While it would take some work, mining those “raw materials” for water on the Moon could be a huge boost for future crewed missions, according to Clark.
“Future astronauts may be able to find water even near the equator by exploiting these water-rich areas. Previously, it was thought that only the polar region, and in particular, the deeply shadowed craters at the poles were where water could be found in abundance,” said Clark. “Knowing where water is located not only helps to understand lunar geologic history but also where astronauts may find water in the future.”
How They Identified Lunar Water SourcesSearching out sources of lunar water requires special instruments. This is where the Chandrayaan mission and NASA’s mineralogy mapper data came in handy. Clark and his team zeroed in on a set of data taken by the lander’s imaging spectrometer from 2008-2009. This infrared spectroscopy data contains the spectral fingerprints of both water and hydroxyl in sunlight reflected from the Moon’s surface. The M3 instrument dissected the light into 85 different visible and infrared “colors”. That’s how they were able to spot the distinctive hints of water and hydroxyls across much of the Moon.
The team also looked at the location and geologic contexts of water and hydroxyl distribution. They also had to take into account the “lifetime” of these resources on the Moon. Interestingly, water gets slowly destroyed over time. Hydroxyl, however, lasts much longer. So, for example, if a crater smacks into the lunar surface, the “wet” rocks it “digs up” will lose that content over time through the action of the solar wind. The result is a diffuse layer or “aura” of hydroxyls that remain behind. In other places, solar wind protons that collide with the surface contribute to a thin layer or “patina” of hydroxyls on the surface. The hydroxyls last much longer and exist on the Moon up to millions of years.
“Putting all the evidence together, we see a lunar surface with complex geology with significant water in the sub-surface and a surface layer of hydroxyl. Both cratering and volcanic activity bring water-rich materials to the surface, and both are observed in the lunar data,” Clark said.
Near-infrared image of the Moon’s surface by NASA’s Moon Mineralogy Mapper on the Indian Space Research Organization’s Chandrayaan-1 mission. The mapper helped identify water- and hydroxyl-rich areas on the lunar surface. Image credit: ISRO/NASA/JPL-Caltech/Brown Univ./USGS Using Precious Lunar ResourcesLunar rocks may well help supply water to future visitors to the Moon. There are two kinds of rocks there. The dark mare rocks are mainly basaltic (like Hawaiian lava). The other type is the anorthosite rock. It exists in various places, including the lunar highlands. The anorthosites are relatively “wet” while the basalts remain very dry. The two rock types also contain hydroxyls bonded to different minerals.
The water-rich anorthosites should be a target for harvesting by lunar astronauts. To get a good supply, you have to heat the rocks and soils. The result of that process could be a long-lasting water supply. You could also get it by using methods to create chemical reactions that liberate hydroxyl and combine four hydroxyls to create oxygen and water.
Of course, a more immediate source lies at the poles. That’s where ice lies hidden inside shaded crater walls or under the surface, preserved for millions of years. That source is likely more easily harvested, but you still have to transport the water to other lunar regions. The downsides of getting water from rocks are the expense and the energy required to heat them for extraction. NASA and other agencies (such as the Chinese space agency) are looking at all the methods of producing supplies for upcoming missions. Studying the locations of ice deposits and hydroxyls is just one part of a larger “search for water” that will benefit future lunar bases.
For More InformationSources of Water and Hydroxyl are Widespread on the Moon
The Global Distribution of Water and Hydroxyl on the Moon as Seen by the Moon Mineralogy Mapper (M3)
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NASA’s Juno spacecraft was sent to Jupiter to study the gas giant. But its mission was extended, giving it an opportunity to study the unique moon Io. Io is the most volcanically active body in the Solar System, with over 400 active volcanoes.
Researchers have taken advantage of Juno’s flybys of Io to study how tidal heating affects the moon.
In recent months, Juno performed several flybys of Io, culminating in one that brought the spacecraft to within 1500 km of the surface. This gave Juno unprecedented close-up views of the volcanic moon. One of its instruments, the Jovian Infrared Auroral Mapper (JIRAM), is an infrared spectrometer, and its data is at the heart of new research into Io’s volcanic activity and how tidal heating drives it.
The new research letter, “JIRAM Observations of Volcanic Flux on Io: Distribution and Comparison to Tidal Heat Flow Models,” was published in the journal Geophysical Research Letters. Madeline Pettine, a doctoral student in astronomy at Cornell University, is the lead author.
Though Io is dead, the tidal heating that keeps it warm could contribute to habitability elsewhere.
“Studying the inhospitable landscape of Io’s volcanoes actually inspires science to look for life,” said lead author Pettine.
“It’s easier to study tidal heating on a volcanic world rather than peering through a kilometers-thick ice shell that’s keeping the heat covered up.”
Madeline Pettine, Cornell UniversityIo is one of the four Galilean moons. The other three, Callisto, Ganymede, and Europa, are all suspected of having liquid oceans under frozen layers of surface ice. If these oceans truly exist, they could potentially support life. Jupiter’s tidal heating provides the heat to keep those oceans warm. Io is valuable scientifically because we can witness the effects of tidal heating on its surface.
Juno isn’t the only spacecraft to have visited Jupiter’s moon Io. This global view of Io was obtained during the tenth orbit of Jupiter by NASA’s Galileo spacecraft. It’s a false colour image that highlights differences on Io’s surface. Image Credit: NASA“Tidal heating plays an important role in the heating and orbital evolution of celestial bodies,” said co-author Alex Hayes, the Jennifer and Albert Sohn Professor of Astronomy in the College of Arts and Sciences at Cornell. “It provides the warmth necessary to form and sustain subsurface oceans in the moons around giant planets like Jupiter and Saturn.”
Io’s volcanoes aren’t distributed evenly on its surface. The majority of them are in the equatorial region. However, in this work, the researchers found that the volcanoes on Io’s poles may act to regulate the moon’s interior temperature.
“I’m trying to match the pattern of volcanoes on Io and the heat flow that they’re producing with the heat flow we expected from theoretical models,” said Pettine.
Jupiter is the most massive planet in the Solar System and its gravitational pull is second only to the Sun’s. Jupiter’s powerful gravity does more than dictate Io’s orbit. It warps the moon and forces it to deform, generating heat.
This simple schematic shows how a planet can create tidal heating on an orbiting moon. The stretching and heating are most extreme when the moon is at its pericenter, the closest distance to the planet. Image Credit: Caltech.“The gravity from Jupiter is incredibly strong,” Pettine said. “Considering the gravitational interactions with the large planet’s other moons, Io ends up getting bullied, constantly stretched and scrunched up. With that tidal deformation, it creates a lot of internal heat within the moon.”
Io has no ocean, so the heat melts rock, creating a likely magma ocean inside the moon. That magma works its way up through the surface, erupting as volcanoes and lava flows. The gases from the magma colour the surface of the moon in reds, yellows, and browns.
To understand what’s happening inside Io, Pettine and her colleagues worked with a mathematical equation called spherical harmonic decomposition. This equation allows scientists to analyze data from a spherical surface and break it down, revealing patterns and important features.
Previous research shows that most of Io’s volcanic activity is in its equatorial region, although some volcanoes have been detected on its poles. In this work, it revealed systems of bright volcanoes at high latitudes.
“Our observations confirm previously detected systems of bright volcanoes at high latitudes,” the authors write. “While our map agrees with previous studies that suggest that low?to mid?latitude areas see the highest areas of volcanic activity, our map suggests that the poles of Io are comparably active to the equator.”
This figure’s perspective shows the sub-Jovian, north-polar view of Io in the left column and the anti-Jovian, south-polar view of Io in the right column. The topmost row shows the coverage map achieved for JIRAM during this study. The second row is a global map of volcanic flux. The hot spot in the north polar region is clear. Image Credit: Pettine et al. 2024.Pettine and her co-researchers compared their global heat flux maps with three different models that attempt to explain what’s going under Io’s surface: the Deep Mantle model, the Asthenospheric model, and the Global Magma model.
The Deep Mantle Model says that tidal heating keeps a large portion of the mantle in a molten state. The Asthenospheric Model says that less of the mantle is molten and that only the asthenosphere is in a molten state due to tidal heating. This is more similar to Earth. The Global Magma Ocean model is a more extreme interpretation of the data and says that a greater portion of Io’s interior is molten, perhaps extending from just below the surface to greater depths.
This figure shows what Io’s surface heat flux should look like for three different interior models. Image Credit: Pettine et al. 2024.The researchers also created a complete global map of heat flux produced by volcanic hot spots. “Viewing this flux on both a linear and a logarithmic scale better illustrates individual volcanic behaviour and global heat flow variations, particularly the lowest-flux regions,” the authors write.
“Our study finds that both poles are comparably active and that the observed flux distribution is inconsistent with an asthenospheric heating model, although the south pole is viewed too infrequently to establish reliable trends,” the authors explain.
These global volcanic flux maps show the average flux in milliwatts per square meter. The top is on a linear scale, while the bottom is on a logarithmic colour scale. The coloured bars and the line plots beside each map show the average flux projected horizontally (to the right of each map) and the average flux projected vertically (below each map) to show trends in flux by latitude and longitude. Image Credit: Pettine et al. 2024.The researchers say that their heat flux maps don’t favour any of the models. “Using spherical decomposition, we find that the distribution of flux is much more uniform than in-line with any of the models,” they write.
For now, a more complete understanding of Io’s tidal heating and volcanic activity is elusive. Juno’s JIRAM observations are just a snapshot of the moon. Over longer time periods, the heat maps will look different and may support different models and conclusions.
“I’m not solving tidal heating with this one paper,” said Pettine. “However, if you think about icy moons in the outer solar system, other moons like Jupiter’s Europa, or Saturn’s Titan and Enceladus, they’re the places that if we’re going to find life in the solar system, it will be one of those places.”
A better understanding of tidal heating will do more than explain aspects of our own Solar System. It may help us understand habitable zones in other solar systems and how exomoons might be heated by giant exoplanets.
Artist’s illustration of a large exomoon orbiting a large exoplanet. While we have no way of observing exomoons, that day will come soon enough. A better understanding of tidal heating will help us understand what we will see. Image Credit: NASA/ESA/L. HustakThat’s why, although Jupiter’s icy moons are prime targets for exploration, with two missions heading to study Europa, Ganymede, and Callisto, we need to keep a scientific eye on Io.
“We need to know how the heat is being generated,” Pettine said. “It’s easier to study tidal heating on a volcanic world rather than peering through a kilometers-thick ice shell that’s keeping the heat covered up.”
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For the second time in its 179-year history, Scientific American, which has become increasingly lame in its science reporting but increasingly “progressive” in its politics (see all my posts about this rag here), has decided to endorse a political candidate. I consider this endorsement—or any ensorsement—an abrogation of institutional neutrality that should go with science journals and magazines. I am opposed to science magazines making political or ideological statements in general. Of course Sci Am endorsed Harris, but I’d be just as opposed if they had endorsed Trump.) My main objections to an endorsement per se are fourfold:
Blame editor Laura Helmuth, who has taken the magazine to its present depths and must have approved this endorsement.
But let someone more articulate than I give his critique: writer Tom Nichols writing in The Atlantic. I’ve also put a link Scientific American’s long endorsement below. Click to read, or find the Atlantic piece archived here.
Like me, Nichols considers Trump a scientific ignoramus and someone whose actions, during the pandemic, almost certainly injured people:
I understand the frustration that probably led to this decision. Donald Trump is the most willfully ignorant man ever to hold the presidency. He does not understand even basic concepts of … well, almost anything. (Yesterday, he explained to a woman in Michigan that he would lower food prices by limiting food imports—in other words, by reducing the supply of food. Trump went to the Wharton School, where I assume “supply and demand” was part of the first-year curriculum.) He is insensate to anything that conflicts with his needs or beliefs, and briefing him on any topic is virtually impossible.
When a scientific crisis—a pandemic—struck, Trump was worse than useless. He approved the government program to work with private industry to create vaccines, but he also flogged nutty theories about an unproven drug therapy and later undermined public confidence in the vaccines he’d helped bring to fruition. His stubborn stupidity literally cost American lives.
It makes sense, then, that a magazine of science would feel the need to inform its readers about the dangers of such a man returning to public office. To be honest, almost any sensible magazine about anything probably wants to endorse his opponent, because of Trump’s baleful effects on just about every corner of American life. (Cat Fancy magazine-—now called Catster-—should be especially eager to write up a jeremiad about Trump and his running mate, J. D. Vance. But I digress.)
Catster??! Was Cat Fancy considered politically incorrect, perhaps implying that people were having sex with cats? But I digress, too. For after noting the above, Nichols still disagrees with Helmuth’s decision to endorse Harris.
Strange as it seems to say it, a magazine devoted to science should not take sides in a political contest. For one thing, it doesn’t need to endorse anyone: The readers of a magazine such as Scientific American are likely people who have a pretty good grasp of a variety of concepts, including causation, the scientific method, peer review, and probability. It’s something of an insult to these readers to explain to them that Trump has no idea what any of those words mean. They likely know this already.
And here are the reasons Nichols opposes political endorsements in general. The bold headings are mine.
They won’t sway the readers. Nichols has already said that the readers are too savvy to be influenced by the magazine. Indeed, I felt patronized when I read the endorsement, even though I agree in the main with the article’s opinions about Trump. And, Nichols says, Trump voters have pretty much made up their minds and won’t be swayed by what this magazine says:
Now, I am aware that the science and engineering community has plenty of Trump voters in it. (I know some of them.) But one of the most distinctive qualities of Trump supporters is that they are not swayed by the appeals of intellectuals. They’re voting for reasons of their own, and they are not waiting for the editors of Scientific American to brainiac-splain why Trump is bad for knowledge.
Well, there are people on the fence, and perhaps they might be influenced, right? Perhaps. But one of the biggest arguments about science magazines taking ideological stands is that they reduce the public’s trust in both the magazine and science. This is pretty well known from the Nature study cited next:
Political stands of magazines reduce public trust in science.
In fact, we have at least some evidence that scientists taking sides in politics can backfire. In 2021, a researcher asked a group that included both Biden and Trump supporters to look at two versions of the prestigious journal Nature—one with merely an informative page about the magazine, the other carrying an endorsement of Biden. Here is the utterly unsurprising result:
The endorsement message caused large reductions in stated trust in Nature among Trump supporters. This distrust lowered the demand for COVID-related information provided by Nature, as evidenced by substantially reduced requests for Nature articles on vaccine efficacy when offered. The endorsement also reduced Trump supporters’ trust in scientists in general. The estimated effects on Biden supporters’ trust in Nature and scientists were positive, small and mostly statistically insignificant.
In other words, readers who supported Biden shrugged; Trump supporters decided that Nature was taking sides and was therefore an unreliable source of scientific information.
To me this is the most important issue, and is why I keep my political views out of lectures on science, like when I’m defending evolution. I could go on and on in such lectures about how Republicans oppose evolution far more than do Democrats, and thus the audience should vote Democratic, but that would accomplish nothing save reduce my credibility about evolution. “Coyne must be pushing this issue because he’s a Democrat,” they’d say.
The Scientific American editorial ventured into fields that had little or nothing to do with science, and also dealt with debatable issues that can’t be “scientifically” settled.
But even if Scientific American’s editors felt that the threat to science and knowledge was so dire that they had to endorse a candidate, they did it the worst way possible. They could have made a case for electing Harris as a matter of science acting in self-defense, because Trump, who chafes at any version of science that does not serve him, plans to destroy the relationship between expertise and government by obliterating the independence of the government’s scientific institutions. This is an obvious danger, especially when Trump is consorting with kooks such as Laura Loomer and has floated bringing Robert F. Kennedy Jr.’s crackpot circus into the government.
Instead, the magazine gave a standard-issue left-liberal endorsement that focused on health care, reproductive rights, gun safety, climate policy, technology policy, and the economy. Although science and data play their role in debates around such issues, most of the policy choices they present are not specifically scientific questions: In the end, almost all political questions are about values—and how voters think about risks and rewards. Science cannot answer those questions; it can only tell us about the likely consequences of our choices.
. . . . Also unhelpful is that some of the endorsement seemed to be drawn from the Harris campaign’s talking points, such as this section:
Economically, the renewable-energy projects she supports will create new jobs in rural America. Her platform also increases tax deductions for new small businesses from $5,000 to $50,000, making it easier for them to turn a profit. Trump, a convicted felon who was also found liable of sexual abuse in a civil trial, offers a return to his dark fantasies and demagoguery …An endorsement based on Harris’s tax proposals—which again, are policy choices—belongs in a newspaper or financial journal. It’s not a matter of science, any more than her views on abortions or guns or anything else are.
This implies that it might be okay if the magazine endorsed Harris because her election is better for science than the election of Trump. That might well be true, but we can’t be sure (after all, both candidates are making promises they can’t keep). More important, even if the endorsement were based on the proposed effect on science in the U.S., it’s still based on politics and ideology (Scientific American is hardly politically neutral!), and is outside the ambit of what the magazine should be about. Readers may disagree, of course, and feel free to do so in the comments. But I’d feel the same way not only if they endorsed Trump, but also if a journal like Nature of Evolution endorsed any presidential candidates.
Here’s Nichols’s conclusion:
I realize that my objections seem like I’m asking scientists to be morally neutral androids who have no feelings on important issues. Many decent people want to express their objections to Trump in the public square, regardless of their profession, and scientists are not required to be some cloistered monastic order. But policy choices are matters of judgment and belong in the realm of politics and democratic choice. If the point of a publication such as Scientific American is to increase respect for science and knowledge as part of creating a better society, then the magazine’s highly politicized endorsement of Harris does not serve that cause.
But have a look at Sci Am’s endorsement below (click on the headline or find it archived here):
The topics covered in the endorsement are healthcare (a debatable issues on what kind to provide), reproductive rights, gun safety, environment and climate, and technology. Except for the undoubtable presence of anthropogenic climate change, which is a scientific reality that Trump has denied, all of these issues involve political differences. Now I agree with Helmuth Scientific American and Harris on nearly all these issues, and, indeed, I go further than most in my permissive views on abortion (I favor unrestricted abortion up to term). But I know that many regard abortion as murder, and how up to what point in gestation we should permit abortion is simply not a scientific issue. Gun issues, too, are a debatable proposition, and, of course, if you’re going to bring up issues that bear on science, then Title IX and gender ideology, in which I think the Trump administrator has done better than Biden, should make an appearance (they don’t).
Further, the op-ed gives credit to Harris for things that the Biden administration actually did, referring to the accomplishments of the “Biden-Harris” administration, as if they were one person and as if Harris had a major role. As Harris has emphasized repeatedly, “I am not Joe Biden.”
But this is all pilpul. The main point is that, in my view, science magazines should stay out of politics. If they want to publish articles about global warming, or the effect of gun laws on human lives, that’s fine, but let the readers absorb the scientific information and make their own judgments. To tell them how to vote is both patronizing and a slippery slope that could lead to the politicization of all science journals and magazines. (In fact, that’s already happening; have a look at the Lancet or Nature.)
Although most potentially habitable worlds orbit red dwarf stars, we know larger and brighter stars can harbor life. One yellow dwarf star, for example is known to have a planet teaming with life, perhaps even intelligent life. But how large and bright can a star be and still have an inhabited world? That is the question addressed in a recent article in the Astrophysical Journal.
Stable main-sequence stars such as the Sun are categorized by color or spectral type, with each type assigned a letter designation. For historical reasons the categories aren’t alphabetical. Red dwarf stars, the coolest stars with the smallest mass, are M type. Then with each brighter, bluer, and more massive category is K, G, F, A, B, and finally O. The Sun falls into the G category as a yellow star. Each spectral type is then broken into smaller sections, numbered 0 – 9. The Sun is G2 star because it is at the warmer end of G-type stars.
As you go up the scale, the potentially habitable zone shifts farther from the star but also gets larger. That makes it more likely for a planet to be in the zone. But larger stars also have shorter lives, which might not give life enough time to evolve on a world. Then there are other factors that can be harmful for life. The largest stars emit a tremendous amount of ionizing radiation, which could strip planets of their atmospheres, or sterilize the surface of a planet. Because of this, the largest stars of the B and O types aren’t likely to harbor life.
How habitable zones differ by spectral type. Credit: NASA, ESA and Z. Levy (STScI)But what about F-type stars? They are a bit brighter than the Sun and more white than yellow in color. They are also stable for around 4 billion years, which is long enough for life to evolve and thrive. And they also emit more ultraviolet radiation, which may have helped life arise on Earth. What are the odds of a habitable F-type planet?
To answer this question, the team went through the database of known exoplanets. About 80 F-type main-sequence stars are known to have at least one planet. Of those, 18 systems have exoplanets that spend at least part of their orbit in the habitable zone of the star. And in one case, the exoplanet 38 Virginis b, the planet is always in the habitable zone. Statistically around 5% – 20% of F-type stars have potential for life.
What’s interesting about 38 Virginis b is that it is a gas giant about 4 times more massive than Jupiter, so it isn’t likely to be habitable. But it could have Earth-sized moons, similar to the Galilean moons of Jupiter. A world orbiting a Jovian planet could be a perfect home for life.
F-type stars only comprise 3% of main-sequence stars in the Milky Way, and it’s possible that their excess UV light could rule out habitable worlds. But alien astronomers might make similar arguments about G-type stars like the Sun. As this study shows, we shouldn’t rule out the Sun’s brighter cousins in the search for living worlds.
Reference: Patel, Shaan D., Manfred Cuntz, and Nevin N. Weinberg. “Statistics and Habitability of F-type Star–Planet Systems.” The Astrophysical Journal Supplement Series 274.1 (2024): 20.
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