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Kornacki breaks down Trump approvals in exit polling

admin - Latest News - November 5, 2025
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NBC News’ Steve Kornacki breaks down exit polling on President Trump’s approval rating in Virginia, New Jersey, New York City and California.



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October 20, 2025
Oct. 20, 2025, 5:27 AM EDTBy Rohan NadkarniEntering Sunday, NFL teams had won 1,602 consecutive games when they were leading by 18 points in the final six minutes of a game.On Sunday, that streak was broken.The New York Giants had a historic collapse against the Denver Broncos, losing 33-32 in what was the wildest game of the NFL season so far.With rookie quarterback Jaxson Dart under center, the Giants appeared to be turning their season around, taking a 19-0 lead into the fourth quarter against the Broncos and their stingy defense. New York was stuck on 19 because of a missed extra point and a failed 2-point conversion, both of were factors in the roller-coaster final frame. The Broncos’ comeback began early in the fourth, when a tipped pass in the end zone fell into the hands of Troy Franklin for a touchdown. Denver completed a 2-point conversion to cut the lead to 19-8. Not to be outdone, the Giants followed up with a tip-drill touchdown of their own, as Theo Johnson caught a deflected pass on third-and-17 and ran with it for a 41-yard score on the ensuing possession.Johnson’s score spiked New York’s win probability. On the Broncos’ next drive, they faced third-and-12 from their own 47 with 7 minutes and 12 seconds to go. At that moment, the Giants’ win probability was 99.8%, according to ESPN. But a 9-yard pass and a defensive pass interference penalty on the next two plays gave Denver new life. Quarterback Bo Nix would lead the team down the field for another score, running for a touchdown with 5 minutes and 13 seconds to go. Denver converted another 2-pointer to make the score 26-16.On the Giants’ next drive, Dart made a backbreaking mistake.On third-and-5, he was picked off by Justin Strnad, who ran the ball back 21 yards to set up Denver’s offense inside the red zone.Four plays later, Nix threw another touchdown pass to cut the lead to 26-23.New York couldn’t answer the score, punting after only three plays and taking only a minute and 9 seconds off the clock in the process.Six plays. Sixty-eight yards and 51 seconds later, the Broncos had their first lead of the game. Nix completed a 31-yard pass on third-and-11 to keep the scoring drive alive, then ran for a touchdown three plays later to put Denver ahead.But the drama was far from finished.With 1 minute and 8 seconds to go, the Giants were staring down a fourth-and-19 from their own 26-yard line and the game on the line. Dart scrambled and found Wan’Dale Robinson for first down, with a roughing-the-passer penalty giving New York another 15 yards.After a pass interference penalty moved the Giants all the way to the 1-yard line, Dart called his own number for a score. Crucially, however, New York kicker Jude McAtamney missed his second extra point of the game, which meant the Giants led by only 2, 32-30, with 37 seconds to go. Still, with no timeouts left, the Broncos faced an uphill climb to get in position for another score.But their next drive started fortuitously, when Nix seemingly overthrew a receiver only for the ball to fall into the hands of an awaiting Marvin Mims for a 29-yard gain. As Denver lined up to spike the ball after the completion, a New York defender couldn’t get onside in time, giving the Broncos 5 more yards.After the penalty, Nix found Courtland Sutton for 22 yards, putting Denver firmly in field-goal range. The Broncos spiked the ball with 3 seconds left, bringing on Will Lutz for a 39-yard kick.The field goal easily sailed through the uprights, and Denver’s shocking comeback was complete.The Broncos’ 33 points in the fourth quarter were the most in NFL history by a team that had been shut out during the first three quarters, per ESPN. Denver went from having a 0.2% chance of winning to improving to 5-2, remaining in first place in the AFC West.The Giants, meanwhile, were robbed of winning two straight games for the first time this season. And instead of being 3-4 and potentially in the playoff hunt, New York exited Sunday tied for the second fewest wins in the NFC. Rohan NadkarniRohan Nadkarni is a sports reporter for NBC News. 
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Sept. 25, 2025, 5:12 PM EDTBy Evan BushWhen the Mendocino earthquake ruptured off the California coast in 2024, it shook houses off their foundations, sent a 3-inch tsunami racing toward shore and touched off a fascinating science experiment — in the server room of a local police station, of all places. More than two years before the quake, scientists installed a device called a “distributed acoustic sensing interrogator” at the Arcata Police Station near the coast. The device fires a laser through the fiber optic cables that provide the station with internet service and senses how some of that laser light quivers or bends as it returns to its source.Now, in a study published Thursday in the journal Science, researchers announced that they were able to use the data from the fiber optic cable to “image” the Mendocino earthquake — determining the magnitude, location and length of the rupture.The study shows how scientists can essentially turn fiber optic cables into seismometers that return detailed data about earthquakes at the speed of light. Outside scientists said this fast-developing technology could drastically improve earthquake early-warning systems, giving people more time to seek safety, and could be key to predicting catastrophic earthquakes in the future, if that’s possible.“This is the first study that’s imaging an earthquake rupture process from an earthquake that’s this large,” said James Atterholt, a research geophysicist at the United States Geological Survey, and the first author of the new study. “This shows that there’s potential to improve earthquake early warning alerts with telecom fibers.”The study suggests that researchers could piggyback their equipment to already vast networks of telecommunications cables — which are used by Google, Amazon and AT&T, for example — to gather data where seismometers are sparse. Seafloor seismic monitoring is particularly expensive, and this could offer a more affordable option. Emily Brodsky, a professor of earth sciences at the University of California, Santa Cruz, who was not involved in the research, said “earthquake early warning could be dramatically improved tomorrow” if scientists are able to broker widespread access to existing telecommunication networks.“There’s not a technical hurdle there. That’s what the Atterholt study demonstrates,” Brodsky said in an interview. And in the more distant future, the use of this technology with fiber optic cables could help researchers determine whether some of the most catastrophic earthquakes could be predicted in advance. Scientists have noticed intriguing patterns on underwater subduction zones in recent years before some of the biggest earthquakes, like the 2014 magnitude-8.1 earthquake in Chile and the 2011 Tohoku earthquake and tsunami in Japan, which touched off the Fukushima nuclear disaster. Both of these massive earthquakes were preceded by what are called “slow-slip” events, which release their energy slowly over weeks or months, but don’t cause perceptible shaking to humans. Scientists aren’t sure what to make of the pattern because there are only a few examples of it, and earthquakes of magnitude-8.0 and above are rare and sparsely documented with in-depth monitoring. If scientists were able to monitor seismic activity on telecommunications networks, they’d have a better chance of documenting these events closely and determining whether there’s clear evidence of a pattern that could predict future catastrophe. “What we want to know is whether faults slip slowly before they slip quickly” and produce a big quake, Brodsky said. “We keep seeing these hints from far away. And what we really need is instruments up close and personal on the fault.” Brodsky said it’s not clear whether these large subduction zone earthquakes are predictable, but the subject is the source of lots of scientific debate, which this new fiber optic technology could help settle. Researchers have been pursuing seismic monitoring through fiber optic cables for about a decade. Brodsky said this research demonstrates that the federal government, the scientific community and telecommunications providers ought to negotiate over access. “There are legitimate concerns. They’re worried about anybody sticking an instrument on an extremely valuable asset for them. They’re worried about damage to the cables or someone listening,” Brodsky said of the telecommunications companies. “However it’s pretty clear it’s also in the public safety interest to have that data, so that is a problem that needs to be solved at the regulatory level.” Atterholt said the fiber optic sensing technology would not supplant traditional seismometers, but would supplement what data already exists and would be less expensive than installing seismometers on the seafloor. Using the cables for seismic monitoring typically does not affect their core purpose of data transmission. Jiaxuan Li, an assistant professor of geophysics and seismology at the University of Houston, who was not involved in this research, said there are still technical hurdles to overcome to use distributed acoustic sensing (DAS) technology offshore. Right now, the technology can be used for distances up to about 90 miles. Li said similar technology is being used in Iceland to record how magma is moving in volcanoes. “We used DAS to perform early warnings for volcanic eruptions,” Li said. “It is operational now. The Iceland Meteorological Office is using this technology to issue an early warning.” The technology also helped reveal that the Mendocino quake was a rare “supershear” earthquake, when the fault’s fracture is happening faster than its seismic waves are traveling. It’s akin to a “fighter jet exceeding the speed of sound” and producing a sonic boom, Atterholt said. The new research unexpectedly revealed the pattern in Mendocino and could offer new clues to this phenomenon. “We haven’t really nailed down why some earthquakes go supershear and why some don’t,” Atterholt said. “It can alter how hazardous the earthquake is, though we don’t fully understand that relationship either.” Evan BushEvan Bush is a science reporter for NBC News.
November 11, 2025
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