New research shows that several Titan rivers do not flow into a delta

The Earth’s coastline is an attractive place where liquids are mixed and materials are shaped into clear terrain, such as the River Delta. Similar active coastlines exist in Titan, the moon of Saturn, where liquid hydrocarbons (methane and ethane) replace water. However, studies of Titan’s coastline, particularly the River Delta, are challenging due to the limited imaging data and the unknown nature of its materials. To overcome these challenges, Brown University planetary scientists, MIT, the MIT-Whoi joint program of oceanography, Woods Hole Marine Facilities, Cornell University, have developed a new model that simulates the Earth’s coastline as if it were found in NASA’s Cassini spacecraft. They discovered that they could detect large terrain in Titan with the correct contrast. They then returned to Titan and remap the coastline. Surprisingly, they discovered that unlike on Earth, where many large rivers house the delta of rivers, many of the Titan rivers do not end in the delta. They also discovered submerged features of Titan on the seabed, suggesting changes in sea level and active currents below sea level.

This composite image shows an infrared view of Titan. In this image, blue represents the wavelength centered at 1.3 microns, green represents 2.0 microns, and red represents 5.0 microns. Views at visible wavelengths show only the hazy atmosphere of Titan. The near-infrared wavelength of this image allows Cassini’s vision to penetrate the haze and reveal the surface of the moon. The view focuses primarily on the terrain in the hemisphere facing Saturn in Titan. Image credit: NASA/JPL-Caltech/Space Science Institute.

“We’ve seen a lot of effort into this world,” said Dr. Sam Burch, a researcher at Brown University.

“But the absence of delta raises many new questions.”

“We take it for granted that we get a delta if we have rivers and sediments.”

“But Titan is odd. It’s a playground for studying the processes we thought we understood.”

Titan is the largest of Saturn’s 274 confirmed moons. Its thick nitrogen and methane atmosphere creates many earth-like climate and weather features.

Titan has clouds, wind, rain, rivers, lakes and oceans. However, instead of water, Titan’s liquids contain methane and ethane. Methane is a liquid at Titan’s chilly surface temperatures.

Scientists learned about Titan’s liquid body when Cassini’s spaceship flew in 2006. Peering into the thick atmosphere of Titan with Cassini’s synthetic aperture radar (SAR), the spacecraft revealed a large body of liquid and a large flat area with a large flat area.

However, what is largely missing from Cassini’s SAR images was the delta, even at the mouth of the large river.

However, it was not clear whether Delta was really absent or not shown in Cassini’s SAR data.

That is a question Dr. Burch and his colleagues tried to answer in their new research.

The problem with Cassini’s SAR data is that shallow liquid methane is largely transparent in every image.

Therefore, while images of the SAR allowed us to see wide ocean and river channels, it is difficult to create coastal features with confidence, as it is difficult to see where the coast ends and where the seabed begins.

For this study, the authors developed a numerical model to simulate what Cassini’s SAR sees whether they are viewing a landscape that scientists understand well: Earth.

In the model, Earth’s rivers and ocean waters were replaced by Titan methane liquids with different radar absorption properties compared to water.

“We basically created a synthetic SAR image of the Earth that assumes the properties of Titan’s liquids instead of the Earth,” Dr. Burch said.

“If you see the SAR images of the landscape, we know so well that we can go back to Titan and get a little better at what we’re looking at.”

Researchers have found that synthetic SAR images of the Earth clearly solved large deltas and many other large coastal landscapes.

“If you have the size of a delta at the mouth of the Mississippi River, you should be able to see it,” Dr. Burch said.

“If we have a big barrier island or similar coastal landscape that we see along the US Gulf Coast, we should be able to see them.”

But as scientists shook the Titan images in light of new analysis, they were almost empty.

The rest of the moon’s river was completely delta free, except for two possible deltas near Titan’s Antarctic.

They found that only about 1.3% of the large rivers of Titan that end on the coastline have the delta. In contrast, on Earth, almost every river of similar size has a delta.

“It’s not entirely clear why Titans generally lack delta,” Dr. Burch said.

“The fluid properties of the Titan river should allow sediment to be carried and deposited.”

“Because the sea level in Titan is rising so rapidly, the delta can crush the landscape faster than it accumulates in a single location.”

“The winds and currents along the Titan coast can also play a similarly large role in preventing delta formation.”

And the only delta of mystery posed by new research is not missing.

A new analysis of Cassini SAR data on the Titan coast reveals holes of unknown origin deep within the lake and ocean.

Researchers also found deep waterways on the ocean floor, which appear to have been carved by the river flow, but it is not clear how they got there.

“All of these surprises require more research to fully understand,” Dr. Burch said.

“This is not really what we expected. But Titan does this well for us, and I think it’s an attractive place to study.”

study It was published in Journal of Journal Geophysics: Planets.

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SPD Birch et al. 2025. Detectability of coastal topography on Titan using Cassini radar. jgr planet 130 (3): e2024je008737; doi: 10.1029/2024je008737

Source: www.sci.news

The ebb and flow of celebrity video greeting app Cameo: A tale of hello and goodbye | Technology

IAs is often the case, this incident began with drama in a WhatsApp group. In 2021, a loose coalition of my friends and acquaintances, in order to survive repeated lockdowns, started playing a much maligned online game called “Excuse.” Betrayal and backstabbing are all part of the game.


Except this time people went too far, someone got so upset that he left the group, and to get him back, my friends came up with a dubious plan: they got Nigel Farage, of all people, to make a sarcastic apology video, urging his comrades to rejoin the group.

This was easy to do, thanks to Cameo, which Farage had recently signed up for. For around £100, Farage had 24 hours to record a 60-second video clip and distribute it through the app. The ploy worked, and peace was restored within the friend group, thanks to Cameo and Farage’s rather bewildered recitation of a series of inside jokes that he completely failed to understand.

It’s one of the many uses for Cameo, a service that lets anyone request custom videos for friends from celebrities and influencers and have them delivered within 24 hours. The site became an unexpected hit during the COVID-19 lockdown, helping it attract investment that put it at a $1 billion valuation in 2021.


The front page of the Cameo website, featuring some of the celebrities registered with the site. Photo: Cameo

But since then, things have been tough. The video is still being made, and it’s still… Eclectic. A number of celebrities and influencers (more on that later) are on board, but they seem to be struggling to pay the relatively small bills.

last month, Business Insider Reported Cameo reaches settlement with 30 U.S. states. The company was found to have violated the Federal Trade Commission’s rules regarding celebrity endorsements.

Cameo was fined $600,000, a modest sum for a billion-dollar company in theory, but court filings attested that it couldn’t afford that amount and instead settled for $100,000 (split among 30 states). So what went wrong?

Day to day, the site operates much the same as before, offering custom videos to those seeking them from a range of actors, comedians and influencers, including British names like actor Miriam Margolyes (£134 a video), former footballer John Terry (£197), singer Gareth Gates (£47) and presenter and environmental activist Ben Fogle (£71).

In the US, NSync’s Lance Bass (235 pounds) and Dean Norris (235 pounds), who played DEA agent Hank Schrader, Breaking Bad (193 pounds), and former supporters of the U.S. version. Office Kevin Malone, aka Brian Baumgartner (154 pounds), or “Drunk Meredith” Kate Flannery (150 pounds).

While each has its own fanbase, sometimes with cult followings, Cameo has struggled to attract or retain A-list celebrities and influencers with top-tier followings, in part because using the app poses significant risks to a celebrity’s reputation: Some have used the app for more nefarious purposes, such as scripting videos to trick celebrities into making racist or other insults.

Last year, the “Russian group” A series of videos was commissioned and stitched together. Video recordings from Cameo and similar services made it appear as if various prominent U.S. figures were calling Ukrainian President Volodymyr Zelensky a corrupt drug addict, creating the illusion that they were helping to stage an intervention.

The disinformation campaign also included cameos from actor Elijah Wood and convicted rapist boxer Mike Tyson, though both have since withdrawn their cameos, and both Norris and Flannery are still active on the site.

Cameo takes 30% of creators’ fees for handling sales, transaction fees, and hosting and submitting the videos. Larger creators appear to have decided to forgo this potential revenue stream because it would require making lots of individual videos that never get published, or because of the risks. But smaller creators say it’s a convenient, hassle-free source of funding with few downsides.

Source: www.theguardian.com

Astronomers Analyze Gas Flow in Uncommonly Bright Infrared Galaxy

Ultraluminous infrared galaxies are the rarest and most extreme star-forming systems and are found only in the distant universe.

Radiative distribution of stars, cold gas, and ionized gas in the unusual HyLIRG Einstein ring PJ0116-24. Image courtesy of Liu others., doi:10.1038/s41550-024-02296-7.

“Ultraluminous Infrared Galaxies (HyLIRGs) are incredibly luminous galaxies illuminated by extremely rapid star formation within their interiors,” said Dr Daizhong Liu from the Max Planck Institute for Extraterrestrial Physics and his colleagues.

“Previous studies had suggested that such extreme galaxies must have arisen through galactic mergers.”

“The collisions of these galaxies are thought to create regions of dense gas that trigger rapid star formation.”

“However, isolated galaxies could also become HyLIRGs through internal processes alone if star-forming gas flows rapidly toward the galaxy's center.”

In the new study, the astronomers focused on a gravitationally lensed HyLIRG galaxy known as PJ0116-24.

“PJ0116-24 is so distant that it took its light about 10 billion years to reach Earth,” the researchers said.

“By chance, the foreground galaxy acts as a gravitational lens, bending and magnifying the light from the background galaxy, PJ0116-24, and directing it towards the Einstein ring.”

“This precise configuration of space allows us to magnify very distant objects and see them with a level of detail that is very difficult to achieve any other way.

The researchers used ESO's Very Large Telescope (VLT) and the Atacama Large Millimeter/submillimeter Array (ALMA) to study the motion of gas within PJ0116-24.

“ALMA tracks the cold gas which appears blue here, while the VLT with its new High Resolution Imaging Spectrograph (ERIS) tracks the warm gas which appears red,” the researchers say.

“Thanks to these detailed observations, we now know that the gas in this extreme galaxy rotates in an organized manner, rather than the chaotic state expected after a galaxy collision. A stunning result!”

“This convincingly shows that a merger is not necessarily required for a galaxy to become a HyLIRG.”

Team paper Published in the journal Natural Astronomy.

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D. Liu othersA detailed study of a rare, ultra-luminous rotating disk in a 10 billion year old Einstein ring. Nat AstronPublished online July 15, 2024; doi: 10.1038/s41550-024-02296-7

Source: www.sci.news

The huge magma flow in Iceland set a new speed record

On February 8th, lava erupted near Grindavik, Iceland.

Iceland Civil Defense/Handout/Anadolu, via Getty Images

Prior to the recent volcanic eruption in Iceland, the influx of magma into the 15-kilometre-long fissure occurred at the highest rate of its kind ever observed anywhere in the world.

“Higher eruption rates can occur in very large eruptions,” he says.
Freistein Sigmundson at the University of Iceland in Reykjavik. “But I don't know of any higher estimates for magma flowing into cracks in the surface.”

Sigmundsson is part of a team that is monitoring recent volcanic activity beneath Iceland's Reykjanes Peninsula using ground-based sensors and satellites. It started when magma built up several kilometers beneath the Svartsengi region, the site of a geothermal power plant that supplies hot water to the tourist attraction Blue Lagoon Spa.

On November 10, 2023, a giant fissure several kilometers deep and 15 kilometers long formed nearby. When the magma opened, some of the accumulated magma flowed into it at a speed of 7,400 cubic meters per second, according to the researchers' calculations.

This is about 100 times faster than the magma flow that occurred during the 2021, 2022 and 2023 eruptions in the nearby Fagradalsfjall region, Sigmundsson said.

The magma inside the crack is at most 8 meters wide, so it can be visualized like a piece of paper, he says. This crack formed because Iceland is located on the boundary where the tectonic plates are moving apart.

On December 18, a so-called fissure eruption began along part of this terrain and lasted for three days. Another lava wave that lasted two days began on January 14, with some of the lava reaching the evacuated town of Grindavik.

Sigmundsson said the lava flow destroyed only a few buildings, but cracks in the ground caused extensive damage to roads and pipes, and created underground cavities.

On February 8, another eruption began a short distance from Grindavik. Lava from here flowed across pipes carrying hot water from the Svartsengi geothermal power plant. This means heating is cut off in some neighborhoods, and most buildings in Iceland rely on geothermal water for heating.

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Source: www.newscientist.com

Incredible flow of natural gas beneath permafrost

Scientists have discovered that methane trapped beneath Svalbard’s permafrost could escape and put it at risk of a warming cycle. Frequent methane accumulations found in well exploration highlight the potential for increased global warming as permafrost thaws. Credit: SciTechDaily.com

Scientists say large amounts of methane may be trapped beneath the permafrost and could escape if it thaws.

Research in Svalbard has shown that methane is moving beneath the permafrost. Lowland regions have ice-rich permafrost, which acts as an effective gas seal, while highland regions with less ice appear to be more permeable. If permafrost thaws too much, greenhouse gas emissions could leak and temperatures could rise further.

Millions of cubic meters of methane are trapped beneath Svalbard’s permafrost. And scientists now know that methane can escape by moving beneath the cold seal of permafrost. A large-scale escape could create a warming cycle that would cause methane emissions to skyrocket. Global warming will thaw permafrost, releasing more gases; warming will thaw more permafrost, releasing more gases. These mobile methane deposits may exist elsewhere in the Arctic, as Svalbard’s geological and glacial history is very similar to other parts of the Arctic region.

“Methane is a powerful greenhouse gas,” said the study’s lead author, Dr. Thomas Birshall of the Svalbard University Center. Frontiers of Earth Science. “Although leakage from beneath the permafrost is currently very low, factors such as retreating glaciers and thawing of the permafrost could ‘uncover’ the problem in the future.”

Refrigerated

Permafrost, ground that remains below freezing Celsius It has been prevalent in Svalbard for over two years. However, it is not uniform or continuous. The western part of Svalbard is warmer due to ocean currents, so the permafrost can be thinner and more patchy. Permafrost in highlands is drier and more permeable, whereas permafrost in lowlands is saturated with ice. The rocks below are often a source of fossil fuels and emit methane, which is locked away by permafrost. However, even where permafrost exists continuously, gas can escape depending on the geographical features.

The bottom of permafrost is difficult to study because it is inaccessible. But over the years, many wells have been sunk into permafrost by companies looking for fossil fuels. Researchers used historical data from commercial and research wells to map permafrost across Svalbard and identify permafrost gas accumulations.

“My boss, Kim, and I looked at a lot of historical well data in Svalbard,” Birchall said. “Kim noticed one recurring theme, and that was the accumulation of gas at the bottom of the permafrost.”

Discover methane accumulation

Initial temperature measurements are often compromised by heating the drilling mud to prevent freezing of the wellbore. But by observing trends in temperature measurements and monitoring boreholes over time, scientists were able to identify permafrost. They also looked at ice formation within the wellbore, changes in drill chips produced during drilling of the wellbore, and changes in background gas measurements.

Well monitors confirmed the flow of gas into the wellbore, indicating that gas was accumulating beneath the permafrost, and abnormal pressure measurements indicated that the icy permafrost was acting as a seal. I did. In other cases, the permafrost and underlying geology are suitable for trapping gas, and even if the rock is a known source of hydrocarbons, it may not be present and the gas produced This suggests that they were already on the move.

Unexpectedly frequent discoveries

Scientists stressed that gas buildup is much more common than expected. Of his 18 hydrocarbon exploration wells drilled in Svalbard, eight showed evidence of permafrost, and half of them showed gas accumulation.

“All wells that encounter gas accumulation have done so by chance. In contrast, hydrocarbon exploration wells that specifically target accumulation in more typical environments have a success rate of well over 50%. It was below,” Birchall said. “This seems to be a common occurrence. One anecdotal example comes from a recently drilled well near the airport in Longyearbyen.Drillers heard bubbling coming from the well. So I decided to take a look, equipped with a rudimentary alarm designed to detect explosive levels of methane. As soon as I held the alarm over the well, it went off.”

Impact on climate change

Experts have shown that the active layer of permafrost – the top 1-2 meters that thaws and refreezes seasonally – is expanding as the climate warms. However, little, if any, is known about how deeper permafrost is changing. Understanding this depends on understanding fluid flow beneath permafrost. As permanently frozen permafrost becomes thinner and more splotchy, this methane can move and escape more easily, accelerating global warming and potentially exacerbating the climate crisis.

References: “Natural gas trapped in permafrost in Svalbard, Norway” by Thomas Birchall, Marte Jochman, Peter Bethlem, Kim Senger, Andrew Hodson and Snorre Olaussen, October 30, 2023. Frontiers of Earth Science.
DOI: 10.3389/feart.2023.1277027

Source: scitechdaily.com

Overcome the lava flow and rebuild from the ashes

Above: Photo taken from an astronaut aboard the International Space Station on February 13, 2016 (before the eruption). Below: Photo taken from astronauts aboard the International Space Station on August 18, 2023.

Two years after the Cumbre Vieja eruption in the Canary Islands, some roads have been rebuilt.

astronaut on board international space station (ISS) took these photos of La Palma Island while in orbit over the North Atlantic Ocean. La Palma is part of Spain’s Canary Islands, approximately 480 kilometers (300 miles) off the coasts of Morocco and Western Sahara. The island is basalt shield volcano This volcano consists of two volcanic centers. One is the old collapsed Caldera de Taburiente and the other is the young and active Cumbre Vieja.

From September to December 2021, eruption Lava flows, lava fountains, and volcanic ash clouds occurred on the southwest flank of Cumbre Vieja. The mission lasted about 85 days and gave astronauts on the space station the opportunity to take photos of plumes and glowing lava flows at night.

In total, the lava flow and ash covered more than 12 square kilometers (5 square miles) of La Palma and extended 5 kilometers (3 miles) from the fissure to the coastline.Ash and lava damaged Over 3,000 buildings and some banana plantations, caused yellowing of pine forests.

These photos were taken in February 2016 (top) and August 2023 (bottom) and show the landscape several years before and after the eruption. In the two years since the eruption, some roads have been rebuilt and are visible as thin, brightly colored lines cutting through the lava flow. This road will reconnect the town of Los Llanos de Aridane with Puerto Naos and other nearby communities. In this photo, the eruption crack is clearly visible as a brighter, linear feature halfway down the side of the volcano.

Although not noticeable in the spatial resolution of these images, sparse trees and shrubs continue to grow within the deposited volcanic ash. canary islands pine (Pinus canariensis).This fire resistance serotinic Coniferous trees, endemic to the Canary Islands, use the heat from fires to melt the resin surrounding their pine cones and produce viable seeds.

Astronaut photo ISS069-E-62382 was acquired on August 18, 2023 with a Nikon D5 digital camera using a focal length of 400 millimeters. Astronaut photo ISS046-E-40929 was acquired on February 13, 2016 with a Nikon D4 digital camera using a focal length of 400 millimeters. Images provided by the ISS Crew Earth Observation Facility and the Johnson Space Center Earth Science and Remote Sensing Unit. The images were taken by Expedition 69 crew members and Expedition 46 crew members. Images have been cropped and enhanced to improve contrast and lens artifacts have been removed. The International Space Station Program supports this laboratory as part of the ISS National Laboratory, allowing astronauts to take the most valuable photographs of Earth to scientists and the public, and to make those images available on the Internet. We support it so that it can be used freely. Caption by Cadan Cummings, Jacobs, JETS II Contract NASA-JSC.

Source: scitechdaily.com