The purpose of this blog is the creation of an open, international, independent and free forum, where every UFO-researcher can publish the results of his/her research. The languagues, used for this blog, are Dutch, English and French.You can find the articles of a collegue by selecting his category. Each author stays resposable for the continue of his articles. As blogmaster I have the right to refuse an addition or an article, when it attacks other collegues or UFO-groupes.
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Deze blog is opgedragen aan mijn overleden echtgenote Lucienne.
In 2012 verloor ze haar moedige strijd tegen kanker!
In 2011 startte ik deze blog, omdat ik niet mocht stoppen met mijn UFO-onderzoek.
BEDANKT!!!
Een interessant adres?
UFO'S of UAP'S, ASTRONOMIE, RUIMTEVAART, ARCHEOLOGIE, OUDHEIDKUNDE, SF-SNUFJES EN ANDERE ESOTERISCHE WETENSCHAPPEN - DE ALLERLAATSTE NIEUWTJES
UFO's of UAP'S in België en de rest van de wereld Ontdek de Fascinerende Wereld van UFO's en UAP's: Jouw Bron voor Onthullende Informatie!
Ben jij ook gefascineerd door het onbekende? Wil je meer weten over UFO's en UAP's, niet alleen in België, maar over de hele wereld? Dan ben je op de juiste plek!
België: Het Kloppend Hart van UFO-onderzoek
In België is BUFON (Belgisch UFO-Netwerk) dé autoriteit op het gebied van UFO-onderzoek. Voor betrouwbare en objectieve informatie over deze intrigerende fenomenen, bezoek je zeker onze Facebook-pagina en deze blog. Maar dat is nog niet alles! Ontdek ook het Belgisch UFO-meldpunt en Caelestia, twee organisaties die diepgaand onderzoek verrichten, al zijn ze soms kritisch of sceptisch.
Nederland: Een Schat aan Informatie
Voor onze Nederlandse buren is er de schitterende website www.ufowijzer.nl, beheerd door Paul Harmans. Deze site biedt een schat aan informatie en artikelen die je niet wilt missen!
Internationaal: MUFON - De Wereldwijde Autoriteit
Neem ook een kijkje bij MUFON (Mutual UFO Network Inc.), een gerenommeerde Amerikaanse UFO-vereniging met afdelingen in de VS en wereldwijd. MUFON is toegewijd aan de wetenschappelijke en analytische studie van het UFO-fenomeen, en hun maandelijkse tijdschrift, The MUFON UFO-Journal, is een must-read voor elke UFO-enthousiasteling. Bezoek hun website op www.mufon.com voor meer informatie.
Samenwerking en Toekomstvisie
Sinds 1 februari 2020 is Pieter niet alleen ex-president van BUFON, maar ook de voormalige nationale directeur van MUFON in Vlaanderen en Nederland. Dit creëert een sterke samenwerking met de Franse MUFON Reseau MUFON/EUROP, wat ons in staat stelt om nog meer waardevolle inzichten te delen.
Let op: Nepprofielen en Nieuwe Groeperingen
Pas op voor een nieuwe groepering die zich ook BUFON noemt, maar geen enkele connectie heeft met onze gevestigde organisatie. Hoewel zij de naam geregistreerd hebben, kunnen ze het rijke verleden en de expertise van onze groep niet evenaren. We wensen hen veel succes, maar we blijven de autoriteit in UFO-onderzoek!
Blijf Op De Hoogte!
Wil jij de laatste nieuwtjes over UFO's, ruimtevaart, archeologie, en meer? Volg ons dan en duik samen met ons in de fascinerende wereld van het onbekende! Sluit je aan bij de gemeenschap van nieuwsgierige geesten die net als jij verlangen naar antwoorden en avonturen in de sterren!
Heb je vragen of wil je meer weten? Aarzel dan niet om contact met ons op te nemen! Samen ontrafelen we het mysterie van de lucht en daarbuiten.
17-02-2025
Fast facts: What is the Habitable Zone?
Fast facts: What is the Habitable Zone?
The definition of “habitable zone” is the distance from a star at which liquid water could exist on orbiting planets’ surfaces. Habitable zones are also known as Goldilocks’ zones, where conditions might be just right – neither too hot nor too cold – for life.
There's a helpful concept we use to help understand what distance from a given star you might expect to find planets with liquid water on their surface – liquid water being essential for life as we know it. It's called the habitable zone. Every star has a habitable zone, but where that zone lies is different for stars of different sizes and brightness. NASA/JPL-Caltech
When searching for possibly habitable exoplanets, it helps to start with worlds similar to our own. But what does “similar” mean? Many rocky planets have been detected in Earth’s size-range: a point in favor of possible life. Based on what we’ve observed in our own solar system, large, gaseous worlds like Jupiter seem far less likely to offer habitable conditions. But most of these Earth-sized worlds have been detected orbiting red-dwarf stars; Earth-sized planets in wide orbits around Sun-like stars are much harder to detect.
And, of course, when talking about habitable exoplanets, we’re really talking about their stars, the dominant force in any planetary system. Habitable zones potentially capable of hosting life-bearing planets are wider for hotter stars. Smaller, dimmer red dwarfs, the most common type in our Milky Way galaxy, have much tighter habitable zones as in the TRAPPIST-1 system. Planets in a red dwarf's comparatively narrow habitable zone, which is very close to the star, are exposed to extreme levels of X-ray and ultraviolet (UV) radiation, which can be up to hundreds of thousands of times more intense than what Earth receives from the Sun.
This infographic compares the characteristics of three classes of stars in our galaxy: Sunlike stars are classified as G stars; stars less massive and cooler than our Sun are K dwarfs; and even fainter and cooler stars are the reddish M dwarfs.
NASA, ESA and Z. Levy (STScI)
Where Are We Looking for Life, and Why?
An old joke offers an answer: Asked why, on a dark night, he was looking for his missing car keys beneath a street lamp, the man answered, "because the light's better." Life on other planets might be like nothing on Earth – it could be life as we don't know it. But it makes sense, at least at first, to search for something more familiar. Life as we know it should be easier to find. And "the light's better" in the habitable zone, or the area around a star where planetary surface temperatures could allow the pooling of water.
Other similarities to Earth come into sharper focus in the search for life. Many rocky planets have been detected in Earth’s size-range: a point in favor of possible life. Based on what we’ve observed in our own solar system, large, gaseous worlds like Jupiter seem far less likely to offer habitable conditions. But most of these Earth-sized worlds have been detected orbiting red-dwarf stars; Earth-sized planets in wide orbits around Sun-like stars are much harder to detect. Yet these red-dwarfs have a potentially deadly habit, especially in their younger years: Powerful flares tend to erupt with some frequency from their surfaces. These could sterilize closely orbiting planets where life had only begun to get a toehold. That’s a strike against possible life.
Because our Sun has nurtured life on Earth for nearly 4 billion years, conventional wisdom would suggest that stars like it would be prime candidates in the search for other potentially habitable worlds. G-type yellow stars like our Sun, however, are shorter-lived and less common in our galaxy.
The artist's conception shows a hypothetical planet with two moons orbiting in the habitable zone of a red dwarf star. More about stars ›
Stars slightly cooler and less luminous than our Sun — called orange dwarfs — are considered by some scientists as potentially better for advanced life. They can burn steadily for tens of billions of years. This opens up a vast timescape for biological evolution to pursue an infinity of experiments for yielding robust life forms. And, for every star like our Sun there are three times as many orange dwarfs in the Milky Way.
K dwarfs, are the true "Goldilocks stars," said Edward Guinan of Villanova University, Villanova, Pennsylvania. "K-dwarf stars are in the 'sweet spot,' with properties intermediate between the rarer, more luminous, but shorter-lived solar-type stars (G stars) and the more numerous red dwarf stars (M stars). The K stars, especially the warmer ones, have the best of all worlds. If you are looking for planets with habitability, the abundance of K stars pump up your chances of finding life."
Exoplanet temperature, size, star type: the galaxy offers up a menu of worlds that echo aspects of our own, yet at the same time are vastly different.
Traditional picture of the habitable zone – not too hot, not too cold.
NASA
Habitable Zone of our Solar System | Goldilocks Zone
An artist’s impression of the white dwarf star WD1054–226 orbited by clouds of planetary debris and a major planet in the habitable zone. Credit Mark A. Garlick / markgarlick.com Licence type Attribution (CC BY 4.0)
The Habitable Zone is a central concept in our explorations for life outside the Earth. Is it time to abandon it?
The Habitable Zone is defined as the region around a star where liquid water can exist on the surface of a planet. At first glance, that seems like a good starting place to hunt for alien life in other systems. After all, there’s only one kind of life known in the universe (ours) and it exists in the Habitable Zone of the Sun.
But researchers have long noted that the Habitable Zone concept is far too restrictive. Besides the examples of the icy moons in our own solar system, life itself is able to alter the chemistry of a planet, shifting its ability to retain or remove heat, meaning that the un-habitable regions of a distant system might be more clement than we thought.
Even if we restrict ourselves to the basic biochemistry that makes Earthly life possible, we have many more options than we naively thought. Hycean worlds, planets thought to be englobed by water surrounded by thick hydrogen atmospheres, once thought to be too toxic for any kind of life, might be even more suitable than terrestrial worlds.
What about tidally-locked planets around red dwarf stars, like our nearest neighbor Proxima b and the intriguing system of TRAPPIST-1? Conditions on those planets might be hellish, with one side facing the incessant glare of its star and the other locked in permanent night. Neither of those extremes seem suitable for life as we know it. But even those worlds can support temperate atmospheres if the conditions are just right. A delicate balancing act for sure, but a balancing act that every life-bearing planet must walk.
Our galaxy contains billions of dead stars, the white dwarves and neutron stars. We know of planets in those systems. Indeed, the first exoplanets were discovered around a pulsar. Sometimes those dead stars retain planets from their former lives; other times the planets assemble anew from the stellar wreckage. In either case, the stars, though dead, are still warm, providing a source of energy for any life that might find a home there. And considering the sheer longevity of those stars the incredibly long history of our galaxy, life has had many chances to appear – and sustain itself – in systems that are now dead.
Who needs planets, anyway? Methanogens could take advantage of the exotic, cold chemistry of molecular clouds, feasting on chemicals processed by millennia of distant high-energy starlight. It might even be possible for life to sustain itself in a free-floating biological system, with the gravity of its own mass holding on to an atmosphere. It’s a wild concept, but all the foundational functions of a free-floating habitat – scaffolding, energy capture and storge, semi-permeable membranes – are found on terrestrial life.
We should absolutely continue our current searches – after all, they’re not groundless. But before we invest in the next generation of super-telescopes, we should pause and reconsider our options. We should invest in research that pushes the edges of what life means and where it can exist, and we should explore pathways to identifying and observing those potential habitats. Only after we have extended research along these lines can we decide on a best-case strategy.
In other words, we should replace a goal, that of finding life like our own, with a vision of finding life wherever we can. Nature has surprised us many times in the past, and we shouldn’t let our biases and assumptions get in the way of our path of discovery.
The definition of “habitable zone” is the distance from a star at which liquid water could exist on orbiting planets’ surfaces. Habitable zones are also known as Goldilocks’ zones, where conditions might be just right – neither too hot nor too cold – for life.
There's a helpful concept we use to help understand what distance from a given star you might expect to find planets with liquid water on their surface – liquid water being essential for life as we know it. It's called the habitable zone. Every star has a habitable zone, but where that zone lies is different for stars of different sizes and brightness. NASA/JPL-Caltech
Spring-loaded Robot Could Explore the Asteroid Belt Almost Indefinitely
The asteroid belt beckons – it contains enough resources for humans to expand into the entire rest of the solar system and has no biosphere to speak of. Essentially, it is a giant mine just waiting to be exploited. So, a student team from the University of Texas at Austin has devised a plan to exploit it as part of the Revolutionary Aerospace System Concepts – Academic Linkage (RASC-AL), a competition sponsored by NASA to encourage undergraduate and graduate students to develop innovative ideas to solve some of space exploration’s challenges. UT Austin’s submission to the competition last year, known as the Autonomous Exploration Through Extraterrestrial Regions (AETHER) project, certainly fits that bill.
AETHER was submitted to the AI-Powered Self-Replicating Probes sub-section of RASC-AL 2024, which solicited ideas that would advance John von Neumann’s idea of a self-replicating space probe. AETHER addresses those challenges in two distinct ways.
First, it combines a spring-loaded landing system and a metal-burning rocket engine to hop between different asteroids in the belt. To fuel its rocket, it uses a system to harvest water and metal (specifically aluminum) from the surface of the asteroid it’s currently on, splits it into its components, and then dumps them into a fuel tank that can be used to power its next trip to a different asteroid. All of this is powered by a Kilowatt Reactor Using Stirling TechnoloY (KRUSTY) nuclear reactor that has been undergoing NASA and DoE testing for over a decade.
Fraser discusses the concept of von Neumann probes.
The springs in AETHER’s legs have a two-fold purpose. First, they allow for a soft landing on the surface of the gravitationally weak asteroid and can transfer some of the energy created by that landing into stored energy, which can be used to launch the system from its landing place later. It also has a set of wheels to navigate around the asteroid’s surface. When it’s time to jump off again, it replants its legs and springs back into space – with a little help from its rocket engine.
The rocket engine designed as part of AETHER can burn metal, such as aluminum, that the craft harvests from the asteroid to use as fuel. It is the primary system designed to take the craft from asteroid to asteroid, and it is meant to be a high-delta-v option for doing so quickly.
AETHER also tries to mimic a von Neumann probe by using a machine-learning algorithm to improve its resource-harvesting efforts. It would take data from various sensors, including synthetic aperture radar and a spectrometer, and estimate where the best spot would be to land to refuel. While collecting that additional fuel material, it would communicate back with Earth via a high-speed optical communication link, allowing an Earth-based server to update the machine learning parameters and improve the algorithm’s outcome for the next hop.
Fraser’s interest with self-replicating robots goes back a long way – here’s his explanation on HeroX about the concept. Credit – HeroX YouTuBe Channel
The original mission design for AETHER has it stopping at two specific asteroids before moving on to as-yet-unnamed ones. The first, which is probably no surprise, is Psyche, the big metallic asteroid that is about to be visited by its own dedicated probe. Data from that probe will help inform the first iteration of AETHER’s learning algorithm, and the input the sensors provide from its visit will update it before its next step – Themis. That asteroid, though smaller, is expected to contain a large amount of water ice, which is a necessary component for AETHER’s rocket engines.
After visiting the first two asteroids, the mission moves on to places unknown, as completing those steps would be considered a success. But given the longevity of the KRUSTY reactor and the craft’s ability to refill its own fuel tank, it is possible, or even likely, that AETHER would consider operating well past its rendezvous with Themis.
The UT Austin team was comprised entirely of undergraduate students, though it’s unclear what year of study they were in. But, given their experience with the 2024 version of RASC-AL, they would seem well-placed to submit a project proposal for the recently announced 2025 version. If they do, hopefully, their idea will be just as innovative as AETHER’s.
When astronomers detected the first known interstellar object, ‘Oumuamua, in 2017, it sparked a host of new studies trying to understand the origin and trajectory of the galactic sojourner.
‘Oumuamua’s unique properties – unlike anything orbiting our sun – had scientists pondering how such an object could have formed. Now, a pair of researchers, Xi-Ling Zheng and Ji-Lin Zhou, are using numerical simulations to test out possible solar system configurations that could result in ‘Oumuamua-like objects. Their findings show that solar systems with a single giant planet have the necessary orbital mechanics at work to create such an object – but that other explanations may still be required.
They began their study by working backward from the known properties of ‘Oumuamua.
When it was visible to Earth’s telescopes for just a few months in 2017, it showed an intensely variable brightness, changing from bright to dim every four hours. Astronomers interpreted this variability as an elongated, cigar-shaped object tumbling through space.
Two other things made ‘Oumuamua unique. First, it appeared to have a dry, rocky surface, akin to the asteroids known in our solar system. But it also changed its orbit in a way that could not purely be explained by the laws of gravity – something else made it change direction.
Redirections like this are sometimes seen in icy comets. As they approach the Sun, off-gassing released from the heated ice acts like a thruster, changing the comet’s trajectory.
An artist’s depiction of the interstellar comet ‘Oumuamua, as it warmed up in its approach to the sun and outgassed hydrogen (white mist), which slightly altered its orbit. (Image credit: NASA, ESA and Joseph Olmsted and Frank Summers of STScI)
Somehow, ‘Oumuamua displayed a mix of both comet-like and asteroid-like properties.
One plausible explanation, proposed in 2020, is that ‘Oumuamua-like objects are formed by tidal fragmentation. That’s when a ‘volatile-rich’ parent body (like a large comet) passes too close to its star at high speeds, shattering it into long, thin shards. The heating process in these extreme interactions causes the formation of an elongated rocky shell, but preserves an interior of subsurface ice. This unique combination, not seen in our own solar system, would explain ‘Oumuamua’s orbital maneuvers despite its rocky composition.
It also explains why we don’t tend to see them in our solar system, because “ejected planetesimals experienced tidal fragmentation at more than twice the rate of surviving planetesimals (3.1% versus 1.4%),” the authors write. In other words, if the orbital forces are strong enough for tidal fragmentation to happen, it also means they’re strong enough to kick the object out of the system entirely.
Interstellar space may therefore be full of dagger-shaped shards of rock and ice (an exaggeration, but a fun quote for dinner parties nonetheless).
The white dwarf Sirius B compared to Earth. Credit: ESA and NASA
The simplest star system that could cause this type of tidal fragmentation are those home to white dwarfs. These are the extremely dense, dead cores of old exploded stars. A white dwarf, encircled by a belt of distant comet-like objects, similar to the Sun’s Oort cloud, could spawn ‘Oumuamua clones with regular frequency.
But the process is enhanced in systems that host Jupiter-sized planets.
The exception is ‘Hot Jupiters’ that orbit close to their star. These are less likely to interact with objects subject to tidal fragmentation.
But Jupiter-sized planets distant from their host star are very effective at producing ‘Oumuamua clones, especially if they have eccentric orbits. But even here, it’s not a perfect match for the origin of ‘Oumuamua, because these interactions tend to produce shards that are not as elongated, and at a rate lower than what is expected for ‘Oumuamua-type objects.
The authors conclude that the planetary systems most likely to have spawned ‘Oumuamua are those with many planets, which are more “efficient at producing interstellar objects,” the authors say, though they propose a few other possibilities too.
So while there is now a strong, plausible explanation for the process that birthed ‘Oumuamua, the type of solar system that produced it is still very much an open question.
Scientists have been left baffled after discovering something vast and radioactive lurking in the depths of the Pacific Ocean.
While it might sound like the start of the next Godzilla movie, researchers say this 'blip' is a very real phenomenon.
An international team of scientists has found unexpectedly high levels of the rare radioactive isotope beryllium-10 in samples from the Pacific seabed.
And they believe it could have been caused by a blast of radiation from space more than 10 million years ago.
After forming, this isotope falls to the ground in the rain and settles to the bottom of the seabed at a fairly constant rate.
However, when the researchers looked at samples of the seabed from 10 million years ago, they found that the levels of beryllium-10 were almost twice what they had expected.
Study author Dr Dominik Koll, from Helmholtz-Zentrum Dresden-Rossendorf, Germany, says: 'We had stumbled upon a previously undiscovered anomaly.'
Scientists have been baffled to find something vast and radioactive lurking beneath the Pacific Ocean. Although it sounds like the plot of the next Godzilla movie, the researchers say this anomaly is very real
Researchers discovered an unexpectedly high amount of the rare radioactive isotope beryllium-10 from samples taken from the bottom of the Pacific Ocean. This compound is formed when cosmic rays hit oxygen and nitrogen in the atmosphere and falls to the ground in rain before sinking to the seabed
In their study, published in Nature Communications, the researchers looked at the accumulation of Beryllium-10 in the seabed deep below the Pacific Ocean.
These unique samples were collected from several miles beneath the water and are made up of a mixture of iron and manganese called a ferromanganese crust.
Using a highly sensitive method called Accelerator Mass Spectrometry, the researchers were surprised to find an unexpected spike in beryllium-10 levels occurring about 10 million years ago.
To ensure this wasn't a fluke, Dr Koll and his colleagues looked at samples taken from elsewhere in the Pacific, but these samples all showed the same anomalous blip.
The researchers argue that there are two possible ways to explain this strange phenomenon: one earthly, and one extraterrestrial.
Dr Koll says: 'This could have caused beryllium-10 to be unevenly distributed across the Earth for a period of time due to the altered ocean currents.'
'As a result, beryllium-10 could have become particularly concentrated in the Pacific Ocean.'
The levels of beryllium-10 should have been fairly consistant though time, but researchers found a significant spike in its abundance about 10 million years ago (illstrated)
These samples (pictured left) came from a region of the northeast Pacific (shaded yellow) that currently sits by major ocean currents (red and blue lines). The researchers suggest that massive changes to thes currents 10 million years ago could have built up more beryllium-10
What is beryllium-10?
Beryllium-10 is an isotope of beryllium which contains 10 neutrons in its nucleus.
This makes the atom unstable and radioactive, so it slowly decays into boron over millions of years.
Beryllium-10 has a half-life - the time needed for half of its atoms to decay - of 1.4 million years.
This means it can be used to date objects from more than 10 million years ago.
In the more out-of-this-world theory, something might have happened in space which exposed the Earth to a sudden burst of radiation.
This could have been triggered by the after-effects of a near-Earth supernova, which would have bathed the planet in intense radiation.
Alternatively, the planet might have briefly lost its protective solar shield, known as the heliosphere, after passing through a dense interstellar cloud.
In either case, this would mean that beryllium-10 should be unusually common 10 million ago in oceans all around the world.
Dr Koll says: 'Only new measurements can indicate whether the beryllium anomaly was caused by changes in ocean currents or has astrophysical reason.
'That is why we plan to analyze more samples in the future and hope that other research groups will do the same.'
Discovering that this anomaly is present all around the world could be extremely valuable for scientists looking into the distant past.
Even though radioactive isotope dating is generally accurate, researchers still need common reference points in order to compare different sets of samples.
Alternatively, the beryllium-10 could have been formed by the radioactive blast of supernova such as the one which left behind the Crab Nebula (pictured). This intense radiation would have led to more beryllium-10 forming all over the world
Dr Koll says: 'For periods spanning millions of years, such cosmogenic time markers do not yet exist.
'However, this beryllium anomaly has the potential to serve as such a marker.'
So, if this spike could be found all around the world, it would let researchers compare completely different archives by synching up to the same unexpected spike 10 million years ago.
Carbon dating, also referred to as radiocarbon dating or carbon-14 dating, is a method that is used to determine the age of an object.
Carbon-14 is a carbon isotope that is commonly used by archaeologists and historians to date ancient bones and artefacts.
The rate of decay of carbon-14 is constant and easily measured, making it ideal for providing age estimates for anything over 300 years old.
It can only be used on objects containing organic material - that was once 'alive' and therefore contained carbon.
The element carbon apears in nature in a few slightly different varieties, depending on the amount of neutrons in its nucleus.
Called isotopes, these different types of carbon all behave differently.
Most of the stable, naturally occurring carbon on Earth is carbon 12 - it accounts for 99 per cent of the element on our planet.
While carbon-14 is a radioactive version of carbon.
Carbon-14 occurs naturally in the atmosphere as part of carbon dioxide, and animals absorb it when they breathe.
Animals stop taking it in when they die, and a finite amount of the chemical is stored in the body.
Radioactive substances all have a half-life, the length of time it takes for a material to lose half of its radioactivity.
Carbon-14 has a long half-life, 5,370 years to be exact.
This long half-life can be used to find out how old objects are by measuring how much radioactivity is left in a specimen.
Due to the long half-life, archaeologists have been able to date items up to 50,000 years old.
Radiocarbon dating was first invented in the 1940s by an American physical chemist called Willard Libby. He won the 1960 Nobel Prize in Chemistry for his discovery.
NASA & Japan just launched two moon landers on a single SpaceX Falcon 9! These private-built landers carry critical scientific payloads for future lunar exploration. But there’s a twist—the Japanese lander has some unusual cargo!
NASA And Japan Moon Landing Update
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A Bola Robot Could Provide Stable Jumping Capability on Low-Gravity Bodies
New research on locomotion techniques that could be used in space exploration is constantly coming out. A lab from UCLA known as the Robotics and Mechanisms Laboratory (RoMeLa) is presenting a paper at the upcoming IEEE Aerospace Conference in March that details a unique system. The Space and Planetary Limbed Intelligent Tether Technology Exploration Robot (SPLITTER) consists of two miniaturized jumping robots tethered together.
Such a system might sound like a recipe for chaos and bring back memories of ladder ball games where no amount of control seems to make the tether go where you want it to. But, according to the paper, that system is actually quite stable, even in airless environments.
Mechanically, their system consists of two four-legged robots designed for jumping and tied together at their tops by a tether. Jumping is much more effective than “roving” on the surface of an asteroid because of all the jagged obstacles that need to be avoided. It is also more effective than flying since there is no atmosphere to push against in many space environments. Jumping robots, however, have been around for a while, but the real secret sauce is in the controls the RoMeLa team has developed.
Video describing some of the underlying tech of the SPLITTER robot. Credit – Alvin Zhu YouTube Channel
The concept they used is called inertial morphing. In the case of SPLITTER, the robots “adjust inertia with changes in limb configurations and tether length,” according to lead author Yusuke Tanaka in an interview with TechXplore. The researchers turned to a technique called Model Predictive Control (MPC) to determine how each variable needs to be adjusted.
MPC is used in various industries and comes as advertised, with a model (i.e., a mathematical representation of the robots) and a prediction, which reflects what the software estimates will happen to the model next. With the model’s current state and expected next state, a controller can change the variables that affect the model’s state. Those changes will result in a stable flying path, allowing SPLITTER to soar through the skies, even without air. It also uses a physical phenomenon known as the Tennis Racket Theorem, which describes how an object can flip rotation around its intermediate axis while rotating around it. Most famously, this was demonstrated on the ISS with a t-handle. It looks chaotic, but the mathematics behind the motion are well-understood.
Implementing it in a tethered robotic system is another matter altogether, though. While SPLITTER is flying, it looks a lot like a bola used in ladder ball, except instead of round spheres on each end, it’s a robot body with four legs splayed out in different directions. The orientation of how those legs are spread out and the length of the tether connecting the two ends are the variables the MPC controls to stabilize its flight. SPLITTER can operate without heavy attitude control hardware, like reaction wheels or thrusters.
Famous video of the Tennis Racket Effect on the ISS. Credit – Plasma Ben YouTube Channel
It also allows the system to perform other actions, like spelunking, where one robot is anchored firmly to the top of a cave system while the other rappels using the tether. Both robots only weigh about 10kg each on Earth, as well, which would make them even more agile on a world with smaller gravity like the Moon or an asteroid.
This isn’t the first robot system the RoMeLa lab designed for this purpose. They initially worked on a robot called the Spine-enhanced Climbing Autonomous Legged Exploration Robot) (SCALER), which had its limitations as they found the limbed climbing robot was too slow.
With SPLITTER, the research team thinks they have a better concept that can both traverse terrain faster and collect data that a robot tied to the ground would be unable to do. Unfortunately, for now, at least, SPLITTER is best described as a computer model, though some preliminary work has been done on the physics of MPC controlling a reaction wheel. Researchers at the lab intend to continue working on the concept, so maybe soon we’ll see a bola robot test jumping near Los Angeles.
Dramatically Decreasing the Time it Takes to Measure Asteroid Distances
Artist's impression of a Near-Earth Asteroid passing by Earth. Asteroids are out there and they pose a threat to Earth. A new method of determining their distance more quickly could help keep us safe. Image Credit: ESA
Dramatically Decreasing the Time it Takes to Measure Asteroid Distances
We all know that asteroids are out there, that some of them come dangerously close to Earth, and that they’ve struck Earth before with catastrophic consequences. The recent discovery of asteroid 2024 YR4reminds us of the persistent threat that asteroids present. There’s an organized effort to find dangerous space rocks and determine how far away they are and where their orbits will take them.
A team of scientists has developed a method that will help us more quickly determine an asteroid’s distance, a critical part of determining its orbit.
Our asteroid concern is centred on NEOs or Near-Earth Objects. These are asteroids whose closest approach to the Sun is less than 1.3 astronomical units (AU). (A small number of NEOs are comets.) There are more than 37,000 NEOs, and while potential impacts are rare, the results can be catastrophic. Considering what happened to the dinosaurs, there’s not much room for complacency or hubris.
Large asteroids in the Main Asteroid Belt (MAB) are easier to study. Their large sizes mean they produce a bigger signal when observed, and astronomers can more easily determine their orbits. However, the MAB holds many smaller asteroids around 100-200 meters. There could be hundreds of millions of them. They’re big enough to devastate entire cities if they strike Earth, and they’re more difficult to track. The first step in determining their orbits is determining their distances, which is challenging and takes time.
The Vera Rubin Observatory (VRO) should see its first light in July 2025. One of its scientific objectives is to find more small objects in the Solar System, including asteroids, by scanning the entire visible southern sky every few nights. If it moves and reflects light, the VRO has a good chance of spotting it. However, it won’t automatically determine the distance to asteroids.
The Vera Rubin Observatory is poised to begin observations in 2025. It could detect 130 Near Earth Objects each night. Image Credit: Rubin Observatory/NSF/AURA/B. Quint
“When asteroids are measured with short observation time windows, the dominant uncertainty in orbit construction is due to distance uncertainty to the NEO,” the authors of the new paper write. They claim their method can shorten the time it takes to determine an asteroid’s distance to one night of observations. It’s based on a technique called topocentric parallax.
Topocentric parallax is based on the rotation of the Earth. In a 2022 paper by some of the same researchers, the authors wrote that “Topocentric parallax comes from the diversity of the observatory positions with respect to the center of the Earth in an inertial reference frame. Observations from multiple observatories or a single observatory can measure parallax because the Earth rotates.”
In the two years since that paper, the researchers have refined their method. The research expands on previous algorithms and tests the technique using both synthetic data and real-world observations.
“In this paper, we further develop and evaluate this technique to recover distances in as quickly as a single night,” the authors write in the new paper. “We first test the technique on synthetic data of 19 different asteroids ranging from ~ 0.05 AU to ~ 2.4 AU.”
The figure below shows the results of the test with synthetic data. Each asteroid was observed six times in one night, and two different equations were employed to process the data.
This figure shows the measured and true distances to 19 asteroids as part of the method’s test. In this test, each asteroid was observed six times in one night. The top shows Measured distance (AU) versus True distance (AU) for all 19 asteroids considered in this analysis. Each panel is based on a separate equation that can be employed in the method. “We see the fit from Eq. 1 for the group of asteroids yielding precise distances with relatively good agreement with true distances,” the authors write. Image Credit: Fernandes et al. 2025.
The researchers also tested their method by taking 15 observations of each asteroid over five nights (3 per night). In this test, Equation 1 performed poorly, while Equation 2 performed well.
This scenario featured 15 observations taken over 5 nights, with three observations per night. Equation 1 produces poor distance agreement, while with Equation 2, the distance recovery improves. Image Credit: Fernandes et al. 2025.
Of course, the distance to the asteroid affected the accuracy of the measurements. The closer the object was, the more precise the measurement was. The paper notes that the method was able to recover distances “with uncertainties as low as the ~ 1.3% level for more nearby objects (about 0.3 AU or less) assuming typical astrometric uncertainties.”
After these tests with synthetic data, the team acquired their own single-night observations of two asteroids using a different algorithm. The real observations produced a less precise result, but it was still a meaningful improvement. The authors explain that they were able to recover distances “to the 3% level.”
So, what do all these tests, equations, and algorithms boil down to?
When we hear of an asteroid that could potentially strike Earth in a few years, people can wonder why the situation is so uncertain. Shouldn’t we know if an asteroid is heading straight for us? Trying to determine the orbit of these small rocks from tens of millions of km away is extremely difficult. An AU is almost 150 million km (93 million miles). 2024 YR, the latest asteroid of concern, is only 40 to 90 metres (130 to 300 ft) in diameter. Those numbers illustrate the problem.
If this method can improve the accuracy of our distance measurements and do it based on a single night of observations, that’s a big improvement.
The technique can be applied to data generated by the Vera Rubin Observatory and the Argus Array. According to the authors, “distances to NEOs on the scale of ~ 0.5 AU can be constrained to below the percent level within a single night.” As the study shows, the accuracy of those measurements from a single-site observatory depends heavily on the spacing between individual observations. If multiple observatories at different sites are used on the same night, the accuracy increases.
The Argus Array is a planned astronomical survey instrument that will be unique in its ability to observe the entire visible sky simultaneously. It will consist of 900 small telescopes, each with its own camera. It’s currently under construction, but its location isn’t being publicized. The researchers say their method can work with Argus’ data. Image Credit: Argus Array
Though larger asteroids, like the one that wiped out the dinosaurs, tend to remain stable in the main asteroid belt, smaller asteroids are more easily perturbed and can become part of the NEO population. An impact from a smaller asteroid might not spell the end of civilization, but it can still be extremely destructive.
Anything humanity can do to understand the asteroid threat is wise. Many asteroids have struck Earth in the past, and it’s only a matter of time before another one comes our way. If we can see it coming in advance, we can try to do something about it.
Four years ago, a green “ghost” appeared over a thunderstorm cloud in the Mediterranean Sea. To the delight of Spanish scientists, this ephemeral sighting finally offered a rare window into a little-known phenomenon playing out high in Earth’s skies.
When lightning strikes, it sometimes triggers the release of a violent optical emission at altitudes between 50 and 90 km above the thunderstorm cloud. These millisecond-long events, called transient luminous events (TLEs), are mysterious.
They can be shaped like jellyfish. These are known as sprites. Other TLE forms exist, boasting playful names like halos and elves. Just a few years ago, thrill seekers and citizen scientists discovered a new TLE, hovering above a sprite, called a ghost. While sprites appear red owing to the nitrogen in Earth’s atmosphere, and blue at more shallow altitudes due to higher atmospheric pressure, ghosts are green. They appear during and after the sprites, like fuzz on top of the jellyfish.
A green ghost, seen here, is a luminous glow that sometimes appears above a jellyfish sprite and lasts briefly after the sprite’s flash.
Thomas Ashcraft
This puzzling afterglow was the subject of a new paper published in the journal Nature Communications on Tuesday.
Finding a Good Ghost
Researcher María Passas Varo led a team to use a special instrument called the Granada Sprite Spectrograph and Polarimeter (GRASSP), located outside Barcelona, to make a clear ghost sighting.
She and other atmospheric researchers were intrigued when, in the early half of 2019, storm chaser Hank Schyma noticed something new: in the wake of a sprite over the skies of Oklahoma, there was a greenish afterglow. He called the emerald-colored splotch a ghost, short for Green emissions from excited Oxygen in Sprite Tops. The idea behind the name was that, since oxygen is associated with the verdant tones of auroras, that the gas creates the ghosts.
Passas Varo, a telecommunications engineer, spectroscopist, and surveyor of atmospheric electricity based at the Astrophysics Institute of Andalucía in Spain, searched relentlessly for a new ghost. But finding one that GRASSP could glean a lot of data from was hard.
“We have analyzed more than 2,000 spectra, one by one, with the naked eye. We only found one good spectrum of a ghost. So, it is a lot of work. It is tedious,” she tells Inverse.
A red sprite (circled) appears and just as quickly disappears. This triptych is part of a sequence from an April 2012 video taken onboard the International Space Station.
Then they finally found a science-worthy ghost, radiating from a thunderstorm cloud in the Mediterranean Sea on September 21, 2019. It was their best candidate for spectrographic analysis, in which the team peered into light from the ghost for clues about its composition.
They found a surprise. Oxygen was present, as they expected. But the team also found evidence of iron.
Iron is present in Earth’s upper atmosphere. It comes from the interplanetary dust particles that enter our atmosphere. But according to Passas Varo, it’s usually found at much higher altitudes.
Approximately one in every 100 sprites have ghosts. These events sometimes happen, but aren’t consistent. What makes a ghost appear could be a combination of different phenomena, and iron might provide a special clue.
A Need for Harmony
Cumulonimbus clouds are towers made of water droplets and ice crystals. These tiny particles journey along the updraft from the hot base of the cloud higher and higher until they reach the chilly top. Sometimes, they become larger molecules. If they bang against one another, they produce static electricity. These charged particles create lightning.
What goes down must be balanced in another form, and this need for harmony could be what causes the sprites and jets and all the other TLE oddities.
“When the lightning occurs, when the lightning strikes the ground, then an electric field appears above the cloud because you have to maintain, somehow, the balance of the electric field of the global electrical circuit,” Passas Varo tells Inverse. “Once you have this big discharge in the form of huge lightning downwards, then an electric field develops upwards. And this electric field develops a transient luminous event.”
One possible explanation for ghosts is that the sonic boom we know as thunder is, in one way or another, disrupting the iron from its usual altitude. Gravity waves on Earth, which are vertical, could also be playing a role in producing ghosts.
But what is clear is that a plethora of new observations are necessary. Passas Varo and the team have one good spectrum of a ghost but say it will take 99 more to get a clearer picture of what’s really happening.
David Rankin, an engineer with the NASA-funded Catalina Sky Survey Project, has sketched the 'risk corridor' according to the asteroid's current trajectory.
If 2024 YR4 really does hit Earth in 2032, it should fall somewhere in a narrow band stretching from northern South America across the Pacific to sub-Saharan Africa and into Asia.
Worryingly, this path extends over several densely populated regions including Chennai, India and Hainan Island, China.
Currently, NASA estimates that the asteroid has a one in 48, or 2.1 per cent, chance of colliding with the planet on December 22, 2032.
And with a diameter of up to 90 metres (300ft), or roughly the size of the Statue of Liberty, it could cause devastating damage to any populated area along the risk corridor.
If it were to strike, experts suggest it could unleash a blast equal to eight megatons of TNT - more than 500 times the size of the atomic bomb dropped on Hiroshima.
Scientists have predicted the exact path (shown in red) where the city-destroying asteroid 2024 YR4 could hit Earth. It should fall somewhere in a narrow band stretching from northern South America across the Pacific to sub-Saharan Africa and into Asia
The asteroid is currently the only large asteroid with an impact probability greater than one per cent and has been awarded the rare rating of three on the Torino Scale, a scale for measuring the danger posed by asteroids.
The 'God of Chaos' asteroid 99942 Apophis is the only other object in the history of astronomy to be given a rating of three or higher on this scale.
While the odds of 2024 YR4 hitting Earth are still slim, Dr Rankin was able to use data about its orbit to predict where it might hit.
In the scenario where the asteroid does indeed collide with Earth, the 'risk corridor' threatens countries including India, Pakistan, Bangladesh, Ethiopia, Sudan, Nigeria, Venezuela, Colombia, and Ecuador.
Where it lands will also determine just how powerful the impact is, with regions at the end of the corridor more likely to receive a glancing blow.
However, there currently isn't enough information to say where along this risk corridor the asteroid is most likely to hit.
Dr Rankin told Space.com: 'Size and are big players in possible damage, along with impact location.
NASA predicts that the asteroid 2024 YR4 currently has a one in 48, or 2.1 per cent, chance of hitting Earth on December 22, 2032 (stock image)
What do we know about 2024 YR4?
First detected: December 27, 2024
Estimated size: 40-90 metres (130-300 feet)
Speed relative to Earth: 29,000 miles per hour (46,800 kmph)
Date of closest pass: December 2, 2032
Probability of impact: 2.3 per cent (one in 43)
Destructive potential: A 'city killer' on a scale on the Tunguska asteroid, which detonated with a force equal to 15-30 megatons of TNT.
Where it could hit: 'Risk corridor' threatens countries including India, Pakistan, Bangladesh, Ethiopia, Sudan, Nigeria, Venezuela, Colombia, and Ecuador
'It's hard to constrain size and composition with the current orbital situation, as it's outbound. Typically, the best way to constrain size is with radar observations and those are not possible right now.'
It is currently estimated that the blast would be similar in size to the Tunguska asteroid which detonated in an air-burst explosion in 1908.
While this blast hit an unpopulated area, the shockwave still flattened an estimated 80 million trees over 830 square miles (2,150 square kilometres) - more than twice the land area of New York.
A blast this powerful would topple residential buildings and cause fatalities up to 12 miles (18.9 km) in any direction from the epicentre.
In the coming months, NASA and ESA hope to use Earth's most powerful telescopes to further refine their predictions about the asteroid's orbit.
This includes a rare emergency decision to grant an international team of scientists the use of the James Webb Space Telescope (JWST) to study 2024 YR4.
This team will use the JWST's infrared sensors to measure the heat radiating from the asteroid to make a better prediction of its size and orbit.
With an estimated size of up to 90 metres (300 ft), or roughly the size of the Statue of Liberty, 2024 YR4 could hit Earth with a blast equal to eight megatons of TNT (artist's impression)
Asteroid 2024 YR4 is about the same size as the Tunguska asteroid, which caused the largest impact event in recorded history when it shot through Earth's atmosphere in 1908, flattening 830 square miles (2,150 square km) of forest (pictured)
Scientists will also have a good opportunity to learn more about the asteroid when it makes its first close pass of Earth in March at a distance of around 5 million miles (8 million kilometres).
The world's space agencies currently predict that the impact probability will drop towards zero as they learn more, but an impact cannot currently be ruled out.
Dr Rankin's calculations suggest that there is a one in 333 chance that 2024 YR4 will collide with the lunar surface, creating a brilliant but otherwise harmless explosion that could be seen from Earth with the naked eye.
However, for the countries along this predicted risk corridor, these predictions raise the chilling possibility that they may face a devastating collision within the next eight years.
Currently, NASA would not be able to deflect an asteroid if it were heading for Earth but it could mitigate the impact and take measures that would protect lives and property.
This would include evacuating the impact area and moving key infrastructure.
Finding out about the orbit trajectory, size, shape, mass, composition and rotational dynamics would help experts determine the severity of a potential impact.
However, the key to mitigating damage is to find any potential threat as early as possible.
NASA and the European Space Agency completed a test which slammed a refrigerator-sized spacecraft into the asteroid Dimorphos.
The test is to see whether small satellites are capable of preventing asteroids from colliding with Earth.
The Double Asteroid Redirection Test (DART) used what is known as a kinetic impactor technique—striking the asteroid to shift its orbit.
The impact could change the speed of a threatening asteroid by a small fraction of its total velocity, but by doing so well before the predicted impact, this small nudge will add up over time to a big shift of the asteroid's path away from Earth.
This was the first-ever mission to demonstrate an asteroid deflection technique for planetary defence.
The results of the trial are expected to be confirmed by the Hera mission in December 2026.
Should Astronauts Add Jumping to their Workout Routine?
Italian astronaut Samantha Cristoforetti uses the Advanced Resistive Exercise Device aboard the International Space Station to simulate weightlifting in microgravity Credit:NASA / ESA
Should Astronauts Add Jumping to their Workout Routine?
It’s a familiar sight to see astronauts on board ISS on exercise equipment to minimise muscle and bone loss from weightlessness. A new study suggests that jumping workouts could help astronauts prevent cartilage damage during long missions to the Moon and Mars. They found that the knee cartilage in mice seems to grow stronger after jumping exercises, potentially counteracting the effects of low gravity on joint health. If effective in humans, this approach could be included in pre-flight routines or adapted for space missions.
In space, astronauts experience significant loss of bone and muscle mass due to microgravity. Without Earth’s gravitational pull, bones lose density, increasing fracture risk, while muscles, especially in the lower body and spine, weaken from reduced use. This deterioration can impair mobility when back on Earth and effect overall health. To combat this, astronauts follow rigorous exercise routines, including resistance and cardiovascular training, to maintain strength and bone integrity.
ESA astronaut Alexander Gerst gets a workout on the Advanced Resistive Exercise Device (ARED). Credit: NASA
The next obvious step as we reach out into the Solar System is the red planet Mars. Heading that far out into space will demand long periods of time in space since its a 9 month journey there. Permanent bases on the Moon too will test our physiology to its limits so managing the slow degradation is a big challenge to space agencies. A paper published by lead author Marco Chiaberge from the John Hopkins University has explored the knee joints of mice and how their cartilage grows thicker if they jump! They suggest astronauts should embed jumping activities into their exercise regiment.
Mars seen before, left, and during, right, a global dust storm in 2001. Credit: NASA/JPL/MSSS
Cartilage cushions the joints between bones and decreases friction allowing for pain free movement. Unlike many other tissues in the body, cartilage does not regenerate as quickly so it is important to protect it. Prolonged periods of inactivity, even from bed rest but especially long duration space flight can accelerate the degradation. It’s also been shown that radiation from space can accelerate the effect too.
To maintain a strong healthy body, astronauts spend a lot of time, up to 2 hours a day running on treadmills. This has previously shown to slow the breakdown of cartilage but the new study has shown that jumping based movements is particularly effective.
(Credit: Merlin74/Shutterstock)
The team of researchers found that, over a nine week program of reduced movement, mice experienced a 14% reduction in cartilage thickness in joints. Other mice performed jumping movements three times a week and their cartilage was found to be show a 26% increase compared to a control group of mice. Compared to the group that had restricted movement, the jumping mice had 110% thicker cartilage. The study also showed that jumping activities increased bone strength too with the jumping mice having a 15% higher density than the control.
JAXA (Japan Aerospace Exploration Agency) astronaut Satoshi Furukawa pedals on the upgraded CEVIS system.
NASA
An interesting piece of research but further work is needed to see whether jumping would herald in the same benefits to humans but the study is promising. If so, then jumping exercises are likely to be a part of pre-flight and inflight exercise programs for astronauts. It is likely that for this to be a reality in the micro-gravitational environment, astronauts will be attached to strong elasticated material to simulate the pull of gravity.
Curiosity’s Other Important Job: Studying Martian Clouds
NASA’s Curiosity Mars rover captured this feather-shaped iridescent cloud just after sunset on Jan. 27, 2023. Studying the colors in iridescent clouds tells scientists something about particle size within the clouds and how they grow over time. These clouds were captured as part of a seasonal imaging campaign to study noctilucent, or “night-shining” clouds. Image Credit: NASA/JPL-Caltech/MSSS
Curiosity’s Other Important Job: Studying Martian Clouds
MSL Curiosity is primarily a rockhound. It’s at Gale Crater, examining the rocks there and on Mt. Sharp, which sits in the middle of the crater and rises 5.5 km above the crater floor. But Curiosity is also a skywatcher, and its primary camera, Mastcam, was built with Martian clouds in mind.
When the sun set on Mars’ Gale Crater on January 17th, MSL Curiosity spent 16 minutes capturing images of the sky with Mastcam, the rover’s primary camera system. The images are part of an effort to understand noctilucent clouds, which are made of CO2 ice and only form over certain regions.
In the animation below, the 16 minutes of images have been sped up by about 480 times. “The white plumes falling out of the clouds are carbon dioxide ice that would evaporate closer to the Martian surface,” NASA says in a press release. “Appearing briefly at the bottom of the images are water-ice clouds travelling in the opposite direction roughly 31 miles (50 kilometres) above the rover.”
Earth has noctilucent clouds, too. They form in the upper atmosphere and are only visible during twilight when the atmosphere’s lower layers are in the shade and the upper atmosphere is sunlit. They form from water ice crystals between 76 to 85 km altitude and are the highest clouds in the atmosphere.
Mars’ noctilucent clouds are similar, but the main difference is that they contain carbon dioxide ice. They form at an altitude of around 60 to 80 km and are also classified as mesospheric clouds. On Mars, they occur in the Fall over the southern hemisphere. Only Mars’ high-altitude clouds containing carbon dioxide ice display iridescent colours.
This is the fourth year in succession that Curiosity has seen these noctilucent clouds. Its Mastcam instrument has different filters that let it see different wavelengths of light, and some of those filters are used to study the composition and particle size in clouds. It also has stereo vision, which helps scientists determine cloud height, shape, and the speed at which they’re moving. It can also observe the Sun through filters and determine how much sunlight the atmosphere is blocking. That tells scientists how much dust and ice is in the atmosphere and how it changes over time.
“I’ll always remember the first time I saw those iridescent clouds and was sure at first it was some color artifact,” he said in a press release. “Now it’s become so predictable that we can plan our shots in advance; the clouds show up at exactly the same time of year.”
These clouds form only in early Martian fall and only in the southern hemisphere. Their iridescence is from uniform particle size, which indicates that the clouds had a brief evolution in a uniform environment. When clouds are both noctilucent and iridescent, they’re called nacreous clouds. It’s interesting to note that these colours would be easily seen by an astronaut on the Martian surface.
This figure from the paper shows iridescent clouds in cylindrical projections. Each image was taken on a separate day. (d) is twice the resolution of the others. (e) shows a corona in the clouds caused by low variance in CO2 ice particle size. Image Credit: Lemmon et al. 2024.
One of the mysteries behind these clouds concerns their location. They’re only seen in Mars’ southern hemisphere, and the Perseverance rover, which is in the Jezero Crater in the northern hemisphere, has never seen them. It seems pretty clear that they only form in certain locations, but the reasons why are unknown.
Lemmon says that gravity waves, which are atmospheric phenomena separate from astrophysical gravitational waves, could be responsible. They cool the atmosphere and could give rise to clouds of frozen CO2. “Carbon dioxide was not expected to be condensing into ice here, so something is cooling it to the point that it could happen. But Martian gravity waves are not fully understood, and we’re not entirely sure what is causing twilight clouds to form in one place but not another,” Lemmon said.
Scientists need more data to better understand these clouds. Curiosity wasn’t the only one to see them; the InSight lander did, too. But they could only see for a few hundred kilometres around their landing sites and their data is incomplete. “Orbiters capable of sunset and twilight times could constrain the cloud altitude,” Lemmon and his co-authors write in their paper.
There are unanswered questions about these clouds. Scientists would like to understand how quickly particles in these clouds evolve. They’d also like to know what the nature of the corona-forming layer is. A larger data sample could help answer these questions, as could more time-lapse imagery.
American astronomers have christened this rocky exoplanet 'YZ Ceti b,' asserting that it's a prime candidate for an Earth-like magnetic field, which could be crucial in humanity's quest for alien life.
The discovery has been hailed as significant for identifying a planet likely to have a magnetic field and offering a future technique to discover more such planets.
Using a radio telescope, the scientists detected a recurring radio signal from exoplanet YZ Ceti b, located approximately 70.5 trillion miles from Earth.
They speculate that these waves could be produced by interactions between the exoplanet's magnetic field and its host star, a small red dwarf named YZ Ceti.
This finding is essential for pinpointing a planet likely to have a magnetic field and establishing a foundation to discover similar planets in the future.
The researchers further suggested that this could mean witnessing the Northern Lights phenomenon - a result of interactions between magnetic fields and solar weather - on distant planets and stars could be possible.
Magnetic fields are vital in preventing a planet's atmospheric erosion caused by stellar emissions over time.
Using a radio telescope, the scientists found exoplanet YZ Ceti b
Drs. Sebastian Pineda and Jackie Villadsen have recently identified a repetitive radio signal from YC Ceti, a red dwarf star located 12 light years away. For context, one light year is nearly 5.88 trillion miles.
The Karl G. Jansky Very Large Array, a prominent radio telescope managed by the National Radio Astronomy Observatory under the US National Science Foundation, was the instrument that allowed them to gain deeper insights into the magnetic dynamics between distant stars and their planets.
This groundbreaking work, outlined in Nature Astronomy, was also funded by the independent federal agency, the National Science Foundation (NSF).
Joe Pesce from NSF, who works as the program director for the National Radio Astronomy Observatory, hails these discoveries as key in the ongoing quest to find life on other worlds, emphasizing, "The search for potentially habitable or life-bearing worlds in other solar systems depends in part on being able to determine if rocky, Earth-like exoplanets actually have magnetic fields."
Recent research marks a significant advancement in exoplanet studies, indicating that some rocky planets beyond our solar system may have magnetic fields. This discovery was achieved through a novel technique that could help identify more of these intriguing worlds.
Dr. Pineda of the University of Colorado, located on America's west coast, expressed the team's elation at detecting planetary radio emissions similar to those Earth emits: "We saw the initial burst, and it looked beautiful," he said enthusiastically.
Moments of scientific triumph followed as Pineda recounted: "When we saw it again, it was very indicative that, OK - maybe we really have something here."
Dr. Pineda noted that a sturdy magnetic field can be pivotal for a planet's ability to retain its atmosphere.
From the other side of the country, Assistant Professor Villadsen of Bucknell University remarked on the distinctiveness of their findings: "I witnessed something that no one has observed before."
Prior detections of exoplanetary magnetic fields were mainly limited to gas giants resembling Jupiter. However, unearthing Earth-sized counterparts calls for different, refined methods.
Since magnetic fields are inherently intangible, detecting their presence around distant planets poses a significant astronomical challenge that Assistant Prof Villadsen and her team are committed to addressing.
She explained their strategy: "We're looking for planets that are really close to their stars and are a similar size to Earth."
"These planets are way too close to their stars to be somewhere you could live, but because they are so close the planet is kind of ploughing through a bunch of stuff coming off the star."
"If the planet has a magnetic field and it ploughs through enough star stuff, it will cause the star to emit bright radio waves."
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A star-planet system with a COHERENT radio signal from an AURORA
NASA Discovers New Substances on Mars: Implications for Future Exploration and Understanding of the Red Planet
Introduction
The quest to understand Mars has captivated scientists and enthusiasts alike for decades. With its striking similarities to Earth and its potential to harbor life, the Red Planet has been a focal point of exploration for NASA and other space agencies around the globe. Recent discoveries of new substances on Mars have opened up exciting avenues for research and exploration. This article delves into the significance of these findings, the methods used to uncover them, and what they mean for the future of Mars exploration.
The Historical Context of Mars Exploration
Mars, often referred to as the "Red Planet" due to its reddish appearance from iron oxide (rust) on its surface, has been a subject of human fascination for centuries. The first observations of Mars were made through telescopes in the 1600s, but it wasn't until the 20th century that space missions began to provide detailed information about its atmosphere, surface, and potential for life.
NASA's Viking missions in the 1970s were pivotal, providing the first close-up images and data about the Martian surface. Subsequent missions, including the Mars Pathfinder, Mars Exploration Rovers (Spirit and Opportunity), and the Mars Science Laboratory (Curiosity), have progressively advanced our understanding of the planet.
The Curiosity rover, which landed in Gale Crater in 2012, has been a key player in Mars exploration. It has analyzed various rocks and soil samples, providing evidence of past water flows and organic molecules, which are crucial for understanding the planet's potential for life.
NASA Finds Ancient Organic Material, Mysterious Methane on Mars - This low-angle self-portrait of NASA’s Curiosity Mars rover shows the vehicle at the site from which it reached down to drill into a rock target called “Buckskin” on lower Mount Sharp.
Credits: NASA/JPL-Caltech/MSSS
Recent Discoveries: New Substances on Mars
NASA's ongoing missions have recently reported the discovery of new substances on Mars, particularly through the Perseverance rover and the Ingenuity helicopter. Perseverance, which landed on Mars in February 2021, has been tasked with seeking signs of ancient life and collecting rock and soil samples for future return to Earth.
Organic Molecules and Their Significance
One of the most groundbreaking discoveries from Perseverance has been the identification of organic molecules in Martian rocks. Organic molecules are carbon-based compounds that are often associated with life. Their presence does not confirm life on Mars but suggests that the building blocks of life may exist on the planet.
NASA scientists have detected these molecules using the Scanning Habitable Environments with Raman & Luminescence for Organics & Chemicals (SHERLOC) instrument, which utilizes advanced spectroscopy techniques to analyze the composition of rock samples. This discovery has revived discussions about the potential for past microbial life on Mars.
NASA's Curiosity Rover Discovers Mysterious Crystals On Mars
Salts and Their Geological Implications
Another significant finding from Perseverance is the presence of various salts in the Martian soil. These salts, including perchlorates, are of particular interest because they can provide insights into the planet's past climate and potential for habitability. Salts can indicate the presence of liquid water in the past, as they often form in evaporative environments.
The discovery of salts raises questions about the history of water on Mars. Understanding the distribution and concentration of these salts can help scientists reconstruct the planet's climatic history and assess whether conditions were ever suitable for life.
Curiosity Mars Rover captured this on Martian sand on February 13, 2022
Unusual Rock Formations and Their Composition
Perseverance has also encountered unusual rock formations that suggest a complex geological history. These formations, characterized by unique textures and mineral compositions, may tell a story of past volcanic activity, sedimentation, and erosion.
Researchers are employing a variety of analytical techniques to understand the mineralogy of these rocks. The ChemCam instrument, which uses laser-induced breakdown spectroscopy, has been instrumental in identifying the elemental composition of Martian rocks, revealing a diverse geological landscape.
The Role of Ingenuity in Exploration
The Ingenuity helicopter, accompanying Perseverance, has demonstrated the feasibility of powered flight on another planet. Its successful flights have not only provided aerial perspectives of the Martian terrain but have also guided Perseverance to scientifically interesting locations.
Ingenuity's ability to scout the landscape has been invaluable in directing the rover to areas with promising geological features. This synergy between the two missions highlights the potential for innovative technologies in planetary exploration.
A photograph of a "Silver Mountain" rock sample collected by NASA's Perseverance Mars Rover as it explores the rim of Jezero Crater.
(Image credit: NASA/JPL-Caltech)
Implications for Future Mars Missions
The discoveries made by Perseverance and Ingenuity have profound implications for future Mars exploration. As NASA plans for the Artemis program and aims to return humans to the Moon, the lessons learned from Mars missions will inform the agency's approach to exploring other celestial bodies.
Sample Return Missions
One of the most ambitious goals of the current Mars exploration program is the return of samples to Earth. The Mars Sample Return mission, a collaboration between NASA and the European Space Agency (ESA), aims to bring back rock and soil samples collected by Perseverance. Analyzing these samples in terrestrial laboratories could yield insights that are currently beyond our reach with remote sensing and in-situ analysis.
Search for Life
The discoveries of organic molecules and salts have intensified the search for life on Mars. Future missions will likely focus on identifying biosignatures—chemical indicators of past or present biological activity. This search will involve more sophisticated instruments capable of detecting and analyzing potential life forms, including microbial life.
Human Exploration
As NASA prepares for the eventual human exploration of Mars, understanding the planet's geology, climate, and potential hazards will be crucial. The presence of resources, such as water in the form of ice or brines, will play a significant role in sustaining human life on Mars. Future missions will prioritize the identification and assessment of these resources.
Public Interest and International Collaboration
The discoveries on Mars have also sparked renewed public interest in space exploration. NASA's commitment to transparency and engagement with the public has fostered a sense of excitement and curiosity about the Red Planet. Educational outreach programs and interactive platforms have allowed people worldwide to participate in the journey of discovery.
Moreover, international collaboration in space exploration has become increasingly important. As countries like China, the United Arab Emirates, and India launch their Mars missions, the sharing of data and findings can enhance our collective understanding of the planet. Collaborative efforts can also help address the challenges of planetary exploration, including technology development and resource allocation.
Conclusion
The recent discoveries of new substances on Mars mark a significant milestone in our exploration of the Red Planet. The identification of organic molecules, salts, and unique geological formations has profound implications for our understanding of Mars' past and its potential to support life.
As NASA and other space agencies continue their missions, the integration of innovative technologies and international collaboration will be key to unlocking the mysteries of Mars. The quest for knowledge about our neighboring planet is not only a scientific endeavor but also an opportunity to inspire future generations to explore the cosmos.
In the coming years, as we await the return of samples from Mars and prepare for human exploration, the discoveries made today will shape our understanding of life beyond Earth and our place in the universe. The journey to Mars is just beginning, and the excitement of discovery continues to propel us forward into the unknown.
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An international team of astronomers has announced the discovery of a new dwarf planet in our Solar System, finding a distant object beyond Neptune that circles the Sun in a spectacularly wide orbit.
Dubbed 2015 RR245 by the International Astronomical Union while they come up with a better name, the dwarf planet is about 700 kilometres in diameter, and its elongated orbit sends it out some 120 times further from the Sun than Earth. So it's a pretty distant neighbour.
Astronomers are finding more of these dwarf planets in the Kuiper belt all the time, but even so RR245 stands out for its size and orbit. In fact, the scientists who found it – as part of the Outer Solar System Origins Survey (OSSOS) – say it's the largest OSSOS discovery to date, of more than 500 trans-Neptunian objects identified by the Survey.
"The icy worlds beyond Neptune trace how the giant planets formed and then moved out from the Sun. They let us piece together the history of our Solar System," said researcher Michele Bannister from the University of Victoria in British Columbia, Canada. "But almost all of these icy worlds are painfully small and faint: it's really exciting to find one that's large and bright enough that we can study it in detail."
RR245's huge orbit – which you can see in the image above – takes it about 700 years to circle the Sun, and the researchers say it's currently travelling in for its closest approach, which will see it get within 5 billion kilometres of the Sun sometime around 2096.
That's after spending hundreds of years at more than 12 billion kilometres from the Sun, although the team acknowledges there's still a lot to be confirmed about RR245's precise movements, as we've only been able to observe just a tiny fraction of its epic loop so far.
Scientists think there were once many more of these dwarf planets in our Solar System, but most were destroyed or ejected when the larger planets in our Solar System moved to their current positions. But now RR245 joins the ranks of other survivors from this period – such as Ceres, Pluto, Haumea, Makemake, and Eris, which have all been recognised as dwarf planets by the International Astronomical Union – amidst the tens of thousands of much smaller objects beyond Neptune.
The researchers first spotted the dwarf planet in February, when astronomer JJ Kavelaars from the National Research Council of Canada was sifting through OSSOS data recorded in September 2015.
"There it was on the screen," said Bannister, "this dot of light moving so slowly that it had to be at least twice as far as Neptune from the Sun."
The team suggests it's possible that RR245 may be one of the last large worlds detected beyond Neptune with today's telescopes, as the brightest dwarf planets have already been mapped – although the debut of the Large Synoptic Survey Telescope next decade could turn up new discoveries we haven't been able to detect so far.
"OSSOS was designed to map the orbital structure of the outer Solar System to decipher its history," said one of the researchers, Brett Gladman of the University of British Columbia in Canada. "While not designed to efficiently detect dwarf planets, we're delighted to have found one on such an interesting orbit."
But beyond helping us map the outer reaches of our Solar System, the discovery of these dwarf planets – and their unique geological composition – helps us understand more about the cosmic past in our corner of the galaxy.
"They are the closest thing to a time capsule that transports us to the birth of the Solar System," astrophysicist Pedro Lacerda from Queen's University Belfast in Northern Ireland, who wasn't involved with the discovery, told Ian Sample at The Guardian. "You can make an analogy with fossils, which tell us about creatures long gone."
Terrifying animation reveals the projected path of the 'city-destroying' asteroid heading towards Earth - as scientists warn the MOON could also be in the firing line
This is actually slightly less than previous estimates, which suggested there was a 2.3 per cent (one in 43) chance of impact.
Meanwhile, the scientist predicts there's a roughly 0.3 per cent (one in 333) chance of 2024 YR4 hitting the moon.
If the asteroid does hit Earth, the impact could release a blast of energy equivalent to 15 megatons of TNT - 100 times more powerful than the atomic bomb dropped on Hiroshima during World War II.
David Rankin, operations engineer for the University of Arizona's Catalina Sky Survey, calculated the route 2024 YR4 is most likely to take (white line). Showing the precise collision course which could lead to a deadly impact
A terrifying new simulation reveals the path of the city-killer asteroid 2024 YR4 which has a 2.1 per cent probability of colliding with Earth in 2032
(stock image)
The asteroid was first detected by the NASA-funded Asteroid Terrestrial-impact Last Alert System (ATLAS) station in December last year.
Although that probability has now slightly decreased, 2024 YR4 is still the only large asteroid with an impact probability greater than one per cent - making it by far Earth's biggest threat.
However, Dr Rankin's calculations present a chilling new possibility that the asteroid could collide with the moon instead.
In a post on BlueSky, Dr Rankin revealed that there was a roughly 0.3 per cent chance of 2024 YR4 hitting the moon.
Without any atmosphere to slow its approach, the asteroid would slam into the lunar surface at a staggering speed of 31,000 miles per hour (50,000 kilometres per hour).
The collision would unleash an explosion 343 times the size of the atomic bomb dropped on Hiroshima and carve out a crater up to 1.2 miles (2km) across.
Should it hit the moon, it is most likely to land in the region stretching south from the Mare Crisium, a large plain of solidified lava, to the crater Tycho.
Asteroid 2024 YR4 is about the same size as the Tunguska asteroid, which caused the largest impact event in recorded history when it shot through Earth's atmosphere in 1908, flattening 830 square miles (2,150 square km) of forest (pictured)
Analysis of 2024 YR4's orbit indicates that the asteroid will most likely pass by Earth on December 22, 2032. However, new calculations suggest that it could also collide with the moon
What do we know about 2024 YR4?
First detected: December 27, 2024
Estimated size: 40-90 metres (130-300 feet)
Speed relative to Earth: 29,000 miles per hour (46,800 kmph)
Date of closest pass: December 2, 2032
Probability of impact: 2.1 per cent (one in 48)
Destructive potential:A 'city killer' on a scale on the Tunguska asteroid, which detonated with a force equal to 15-30 megatons of TNT.
This could be concerning since this would place the impact on the side of the moon facing Earth, potentially exposing us to a shower of lunar shrapnel.
Thankfully, experts say that the Earth likely wouldn't be harmed by any impact which occurs on the moon.
Dr Rankin told New Scientist: 'There is the possibility this would eject some material back out that could hit the Earth, but I highly doubt it would cause any major threat.'
Unlike a large object such as 2024 YR4, these smaller pieces of debris should burn up harmlessly in the atmosphere creating nothing more than a particularly bright meteor shower.
In fact, some experts suggest that the collision between the asteroid and the moon could create a truly spectacular display.
Gareth Collins, a professor of planetary science at Imperial College London, told New Scientist: 'The impact flash of vaporised rock would be visible from Earth, even in the daytime.'
That means any keen stargazers on Earth could see the moment the asteroid detonates on the lunar surface with the naked eye.
However, it is currently seven times more likely to hit Earth rather than the moon.
Without any atmosphere to slow it down, the asteroid would hit the moon at 31,000 miles per hour (50,000 kilometres per hour), creating an explosion bright enough to see from Earth with the naked eye
These probabilities are likely to change in the future as scientists gather more information about the asteroid's orbit.
The current estimates for 2024 YR4's orbital path, speed, and size come from hundreds of images taken by powerful telescopes all around the world.
However, over such a short period of time, it is difficult to precisely predict where the asteroid will travel.
While astronomers hope that the probability of an impact will rapidly fall towards zero, a direct collision with Earth cannot be ruled out.
The JWST will record the heat emitted by the asteroid using its infrared sensors which will give a more accurate estimate for its size.
A team of ESA scientists will make one observation in March when the asteroid reaches its peak brightness and another in May as it travels away from Earth.
This will be the last chance to observe 2024 YR4 before it becomes too dim to see from Earth until it returns again in 2028.
The European Space Agency has been given emergency access to the James Webb Space Telescope (pictured) to measure the asteroid's size more accurately
Already, NASA has reached a hugely-important milestone with the DART asteroid deflection mission. In September 2022, the DART spacecraft was intentionally crashed into Dimorphos, an asteroid 6.8 million miles away. A similar method could be used to deflect asteroid 2024 YR4 before it reaches Earth
Those observations will be critical for determining whether the world's space agencies need to take action to divert its course.
In a post on X, Dr Robin George Andrews, a volcanologist and author based in London, points out that we 'have less than eight years to potentially deal with it'.
'You need 10 years or more to build, plan and execute an asteroid deflection mission,' he said.
Terrifying projected path of 'city-destroying' asteroid
Currently, NASA would not be able to deflect an asteroid if it were heading for Earth but it could mitigate the impact and take measures that would protect lives and property.
This would include evacuating the impact area and moving key infrastructure.
Finding out about the orbit trajectory, size, shape, mass, composition and rotational dynamics would help experts determine the severity of a potential impact.
However, the key to mitigating damage is to find any potential threat as early as possible.
NASA and the European Space Agency completed a test which slammed a refrigerator-sized spacecraft into the asteroid Dimorphos.
The test is to see whether small satellites are capable of preventing asteroids from colliding with Earth.
The Double Asteroid Redirection Test (DART) used what is known as a kinetic impactor technique—striking the asteroid to shift its orbit.
The impact could change the speed of a threatening asteroid by a small fraction of its total velocity, but by doing so well before the predicted impact, this small nudge will add up over time to a big shift of the asteroid's path away from Earth.
This was the first-ever mission to demonstrate an asteroid deflection technique for planetary defence.
The results of the trial are expected to be confirmed by the Hera mission in December 2026.
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NASA will send astronauts Butch Wilmore and Suni Williams home from the International Space Station early on a previously used SpaceX Dragon space capsule, not on a brand-new one, the agency announced.
A NASA astronaut testing equipment on a spacewalk outside the International Space Station.
(Image credit: NASA)
Stranded Starliner astronauts Butch Wilmore and Suni Williams finally have a return date to head back to Earth, and it's a few weeks earlier than previously expected.
NASA announced Tuesday (Feb. 11) that the two astronauts, who hitched a ride to the International Space Station (ISS) on a Boeing Starliner spacecraft last June, will head home on a SpaceX Dragon capsule that will leave Earth with the ISS Crew-10 on Wednesday, March 12. After a few days' handover period, Williams and Wilmore will leave the ISS with the rest of the Crew-9 mission, after having spent about 250 consecutive days in orbit.
NASA's Boeing Starliner astronauts Butch Wilmore and Sunita Williams will now return to Earth on a SpaceX Dragon capsule in February 2025.
(Image credit: NASA)
Williams and Wilmore were initially meant to spend about a week in space, but problems with the propulsion and helium systems on their Boeing Starliner led NASA to return the capsule to Earth empty after three months of troubleshooting couldn't resolve the issues. The capsule ended up landing safely in New Mexico on Sept. 7, 2024. However, a watchdog report just released by the Aerospace Safety Advisory Panel found that new thruster problems did appear during the descent. In October, The Wall Street Journal reported that Boeing is in the early stages of considering a sale of its space business, including Starliner.
In December 2024, NASA announced that Williams and Wilmore would return on a newly designed SpaceX Dragon capsule in late March 2025 at the earliest. But now, the astronauts and the rest of Crew-9 will come home on a previously flown Dragon capsule, the Endurance. This will allow the swap between Crew-9 and Crew-10 to happen sooner while SpaceX continues to finalize the interior and final integration of the new Dragon capsule, according to NASA.
Along with Wilmore and Williams, astronaut Nick Hague and Roscosmos cosmonaut Aleksandr Gorbunov will leave the ISS in March. They'll be replaced by NASA astronauts Anne McClain and Nichole Ayers, Japan Aerospace Exploration Agency astronaut Takuya Onishi, and Roscosmos cosmonaut Kirill Peskov. The precise day of the return will be determined by weather conditions near Florida, where Endurance will splash down.
Astronomers have long suspected that several moons in our Solar System, including those orbiting Jupiter, Saturn,Uranus, and Neptune, may conceal vast liquid oceans beneath their frozen crusts. Now, new research suggests that Uranus’s moon Ariel might be offering a rare glimpse into its hidden depths.
Cracks in Ariel’s Surface May Expose Its Interior
Deep chasms mark Ariel’s surface, and researchers believe these fractures could be transporting material from the moon’s interior to the surface. Among the substances detected is carbon dioxide ice, which suggests the possibility of chemical processes occurring below the crust. If these deposits originated from within Ariel, they may provide a unique window into the moon’s subsurface environment—without the need for complex drilling missions.
“If we’re right, these medial grooves are probably the best candidates for sourcing those carbon oxide deposits and uncovering more details about the moon’s interior,” says planetary geologist Chloe Beddingfield of Johns Hopkins University Applied Physics Laboratory.
Unlike other surface features, these chasms appear to be the only structures facilitating material movement from Ariel’s interior, making them particularly valuable for future study.
Scientists analyzing Ariel’s terrain have found striking similarities to a geological process observed on Earth known as spreading. This occurs along volcanic ridges where the seafloor slowly separates, allowing molten material to rise and form new crust.
On Ariel, a similar process could be unfolding as warmer material from the moon’s interior forces its way up, splitting the icy surface before filling the cracks. Researchers tested this theory by digitally aligning the two sides of Ariel’s chasms as if “zipping them back up,” and found a perfect match. The presence of parallel grooves along some chasm floors further supports the idea that material has been accumulating over time through repeated geological activity.
Could a Hidden Ocean Be Driving These Changes?
Another factor influencing Ariel’s surface could be gravitational interactions between Uranus and its moons. These interactions, known as orbital resonance, create internal heating that can melt ice and sustain liquid water beneath the crust.
Recent observations from the James Webb Space Telescope (JWST) provide compelling evidence that a hidden ocean may exist beneath Ariel’s surface. If so, this ocean might be responsible for the carbon dioxide deposits seen within the moon’s deep chasms. However, current data is insufficient to determine the exact size and depth of this possible ocean.
“The size of Ariel’s possible ocean and its depth beneath the surface can only be estimated, but it may be too isolated to interact with spreading centers,” Beddingfield explains.
Despite significant advancements in planetary exploration, much about Ariel remains unknown. While the Voyager 2 spacecraft provided valuable data during its 1986 flyby, it lacked the instruments needed to map the precise distribution of ices on the moon’s surface. Future missions with more advanced sensors will be crucial in determining whether Ariel is truly home to a hidden ocean—and what that might mean for our understanding of ocean worlds beyond Earth.
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While thousands of asteroids pass harmlessly through space, a select few have orbits that bring them dangerously close to Earth. These objects, classified as potentially hazardous asteroids (PHAs), are actively monitored by NASA, ESA, and other space agencies. Though the probability of impact remains low for most of them, even a small chance is enough to warrant continuous tracking. Here are the five most dangerous asteroids that could collide with Earth and are currently being monitored.
1. 2024 YR4
Potential Impact Date: December 22, 2032
Estimated Size: 40–90 meters
Impact Probability: 1 in 43 (2.3%)
Energy Release Upon Impact: Equivalent to 8 megatons of TNT
Discovered in late 2024, 2024 YR4 is currently the most concerning asteroid on record due to its high impact probability. The latest NASA observations indicate a 2.3% chance of collision in 2032—which translates to 1 in 43 odds.
If 2024 YR4 were to strike Earth, it could cause severe regional devastation, releasing an explosion about 500 times stronger than the Hiroshima bomb. The potential impact zone, known as the “risk corridor,” stretches across the Pacific Ocean, South America, the Atlantic, Africa, and parts of Asia.
Although further tracking will likely lower the impact probability, 2024 YR4 is a top priority for planetary defense experts.
Energy Release Upon Impact: Equivalent to 1.4 billion tons of TNT
Bennu is one of the most well-studied potentially hazardous asteroids, thanks to NASA’s OSIRIS-REx mission, which returned samples in 2023.
Although the impact probability is low, a collision would be catastrophic—releasing enough energy to cause continent-wide destruction and severe climate disruptions. NASA scientists continue to monitor Bennu to determine if future deflection strategies will be necessary.
3. 1950 DA
Potential Impact Date: March 16, 2880
Estimated Size:1,300 meters
Impact Probability: 1 in 34,500 (0.0029%)
Energy Release Upon Impact: Equivalent to 75 billion tons of TNT
1950 DA is a massive asteroid that, despite its low impact probability, remains a serious long-term threat. If it were to hit Earth, it would cause global devastation—triggering tsunamis, firestorms, and potentially a planet-wide climate crisis.
Although the impact risk is expected to decrease with further observations, planetary defense programs continue to monitor this colossal object.
4. 2023 VD3
Potential Impact Date: November 8, 2034
Estimated Size:11–24 meters
Impact Probability: 1 in 387 (0.26%)
Energy Release Upon Impact: Comparable to the Chelyabinsk meteor event
Although 2023 VD3 is much smaller than the other asteroids on this list, its relatively high impact probability makes it a major concern. With a 1 in 387 chance of impact in 2034, it has one of the highest statistical risks currently known.
While it wouldn’t cause a global disaster, an asteroid of this size could explode in the atmosphere, producing a shockwave strong enough to damage buildings and injure thousands—similar to the Chelyabinsk event in 2013, where a 20-meter asteroid caused widespread damage.
Further observations will determine whether 2023 VD3 will safely pass Earth or require further attention.
5. 1979 XB
Potential Impact Date: December 14, 2113
Estimated Size:400–900 meters
Impact Probability: 1 in 1.8 million (0.000055%)
Energy Release Upon Impact: Equivalent to 30 billion tons of TNT
First observed in 1979, 1979 XB is one of the largest asteroids on the risk list. Because of its size, a collision with Earth would have severe global consequences, similar to the asteroid that wiped out the dinosaurs.
However, 1979 XB is classified as a lost asteroid, meaning its exact orbit is uncertain. Scientists are working to relocate it and refine its trajectory to confirm whether it poses a real long-term risk.
Can We Stop an Asteroid Impact?
While none of these asteroids pose an imminent danger, scientists are working on planetary defense strategies to ensure Earth’s safety.
NASA’s DART Mission– Successfully altered an asteroid’s trajectory in 2022, proving that impact deflection is possible.
Upcoming Space Missions– Future missions will explore gravity tractors, nuclear deflection, and other techniques to steer dangerous asteroids away from Earth.
Advanced Tracking Systems – Telescopes like ATLAS, Pan-STARRS, and the Vera C. Rubin Observatory are improving our ability to detect threats decades in advance.
The likelihood of a catastrophic asteroid impact remains low, but continuous tracking is critical for ensuring early detection and possible deflection efforts.
Among all the asteroids being monitored, 2024 YR4 is the most immediate concern due to its relatively high impact probability in 2032. While ongoing observations will likely refine its trajectory, planetary defense experts are paying close attention—ensuring that if an asteroid ever truly threatens Earth, we’ll be ready.
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A Blown-Glass Structure Could House Astronauts on the Moon
Humanity will eventually need somewhere to live on the Moon. While aesthetics might not be the primary consideration when deciding what kind of habitat to build, it sure doesn’t hurt. The more pleasing the look of the habitat, the better, but ultimately, the functionality will determine whether or not it will be built. Dr. Martin Bermudez thinks he found a sweet synergy that was both functional and aesthetically pleasing with his design for a spherical lunar habitat made out of blown glass. NASA apparently agrees there’s potential there, as he recently received a NASA Institute for Advanced Concepts (NIAC) Phase I grant to flesh out the concept further.
Bermudez’s vision’s artistic design looks like something out of an Arthur C. Clarke novel: a glass sphere rising off the lunar surface that could potentially contain living and work areas for dozens of people. His firm, Skyeports, is founded on creating these blown glass structures in space.
The design has some challenges, as Dr. Bermudez discusses in an interview with Fraser. First is how to build this thing. It’s far too large to ship in any conventional lunar lander. However, there’s also no air on the Moon to use as the blown gas to create the spherical shape. Dr. Bermudez plans to utilize argon, which would initially be shipped up from Earth to fill the sphere. Argon has several advantages in that it’s a noble gas and not very reactive, so it’s unlikely to explode in the furnace while the glass is blown.
Video animation showing the blown glass concept. Credit – Skyeports YouTube Channel
Surprisingly, the lack of outside air pressure actually makes it easier to form a sphere than it would be on Earth since less pressure would be necessary to expand the sphere outwards. There are some nuances in the glass as well, with it being more like a glass lattice with embedded titanium or aluminum to make it stronger. Specific kinds of glass, such as borosilicate glass, could potentially add to the strength of the glass itself.
Most of the materials required to create such a structure could already be found on the lunar surface. Lunar regolith is full of the raw building materials required to make the structure work. Some of it has already been blasted into glass-like structures called agglutinates when micrometeoroids hit the lunar surface.
Those micrometeoroid impacts pose another risk to the glass sphere. Dr. Bermudez suggests having multiple layers of glass protecting the habitat, each with a layer of argon between them, like modern-day double-glazed windows. He suggests that spinning the outer layer might also provide some advantage, as will the spherical shape itself, as the impact force will dissipate better into the structure than it would on a flat surface.
Fraser interviews Dr. Martin Bermudez, the PI of the new NIAC project.
Dr. Bermudez’s dreams don’t stop at the Moon, though. He suggests such a glass-blown structure could be useful on Mars or asteroids, where the microgravity would make it even easier to create these structures. On Mars, such a habitat might be limited to the top of Olympus Mons, where the atmosphere is thinner, and there isn’t as much wind and dust that could erode away the outer layers.
Many use cases exist for a structure like this, though many technical challenges remain. NIAC is the place for novel ideas that could potentially impact space exploration, and this one certainly fits that bill. As Dr. Bermudez works through de-risking his design, we get closer than ever to a future of aesthetically pleasing habitats on the Moon and everywhere else in the solar system.
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Over mijzelf
Ik ben Pieter, en gebruik soms ook wel de schuilnaam Peter2011.
Ik ben een man en woon in Linter (België) en mijn beroep is Ik ben op rust..
Ik ben geboren op 18/10/1950 en ben nu dus 74 jaar jong.
Mijn hobby's zijn: Ufologie en andere esoterische onderwerpen.
Op deze blog vind je onder artikels, werk van mezelf. Mijn dank gaat ook naar André, Ingrid, Oliver, Paul, Vincent, Georges Filer en MUFON voor de bijdragen voor de verschillende categorieën...
Veel leesplezier en geef je mening over deze blog.