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Science

Gulf Coast Prepared To Develop A Heart For Carbon Storage – Watt Up With That?

University of Texas at Austin

Research news

PICTURE: The energy infrastructure along the Gulf Coast offers opportunities to capture and transport CO2 for storage. View More Credit: Carol M. Highsmith / Library of Congress.

According to a study led by the University of Texas at Austin, the conditions are in place for a new carbon storage economy along the Gulf Coast, with the region offering ample opportunities to capture and store carbon and with recent state and federal incentives adding a push to get started.

Carbon Capture and Storage, or CCS, is a technology that keeps CO2 out of the atmosphere by capturing emissions and storing them deep underground. It can help fight climate change by lowering industrial emissions now while developing renewable energy sources, said Tip Meckel, a senior researcher at the Gulf Coast Carbon Center, a research group at the UT Bureau of Economic Geology, has been using CCS for the past 20 years Years.

“This is a viable way to reduce emissions in the short term,” said Meckel. “It is feasible and has a reasonable economic structure that can support, maintain and create jobs.”

The study, published in Greenhouse Gases: Science and Technology, provides a comprehensive overview of policy incentives for CCS and how Texas and Louisiana’s high industrial density and unique offshore geology make the region a particularly good place for building a carbon storage economy.

The issues covered in the paper are particularly relevant given the recent moves Texas has taken to put carbon storage under a regulatory framework similar to that of oil and gas. In June, Governor Greg Abbott signed Law HB 1284, which gave the Texas Railroad Commission the same regulatory powers over CO2 injection wells as it did over oil and gas wells. In May, the Texas General Land Office announced that it would accept lease proposals for carbon storage on state land off the coast of Jefferson County. Any royalties or income related to storage goes to the Texas Permanent School Fund, as is the case with oil and gas activities.

In the past, oil and gas companies mainly used carbon storage and capture for improved oil recovery, which enables companies to extract more oil from depleted reservoirs by pumping in CO2. The improved oil production has been used for decades and has spawned an existing network of pipelines to transport CO2 along the Gulf Coast. The two existing CO2 capture systems in Texas were also built with these measures in mind.

The study shows, however, that falling oil and gas prices and rising federal tax credits, which offset the tax liability of industries to varying degrees depending on the CO2 storage, make carbon storage more attractive for its own sake.

“We used to have only one way: improved oil production,” said former Deputy Energy Secretary Charles McConnell, who is now Executive Director of Carbon Management at the University of Houston and was not involved in the study. “We are now in a different place. Storage in and of itself can now be profitable. “

The paper describes how existing CO2 infrastructure could be used and expanded to promote carbon storage outside of enhanced oil production – with researchers highlighting the subterranean geology off the Gulf Coast as a suitable location for permanent CO2 storage.

The researchers also note that state land in Texas extended up to 10.35 miles offshore instead of the usual 5.45 miles, due to a law that went into effect when Texas was a sovereign nation. The historical act now simplifies ownership and licensing issues.

While the Gulf Coast geology and infrastructure make a winning combination in promoting a carbon storage economy, another important fact, according to the study, is simply the amount of CO2 the region is producing. Texas has the highest emissions of any state. Louisiana is second.

The capture and storage offers a way to stop some of these emissions right at the source, said Meckel. In this way, the technology can help flatten CO2 emissions as lower carbon energy alternatives mature in the marketplace.

“Advancing the capture and storage of CO2 is something we can do now,” said Meckel. “To take a big bite [the carbon] Profile, you have to get started now. “

###

The Ministry of Energy funded the research. The co-authors of the paper are all part of the Gulf Coast Carbon Center. They are Research Associate Alex Bump, Study Director Susan Hovorka, and Program Manager Ramón H. Treviño.

The Bureau of Economic Geology is a research unit of the UT Jackson School of Geosciences.

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Health

Disputes over masks are 75% of the FAA’s recalcitrant passenger complaints on airplanes

A traveler wearing a face mask is seen at Ronald Reagan Washington National Airport in Arlington, Virginia on February 2, 2021.

Ting Shen | Xinhua News Agency | Getty Images

Much of the Federal Aviation Administration’s recalcitrant passenger reports on aircraft come from passengers who refuse to comply with mask requirements to protect against the spread of Covid-19.

About 75% of reports of recalcitrant passengers since Jan. 1 began with people refusing to wear their masks and escalated from there into profanity, screaming matches and even physical violence, the agency said on Tuesday.

The FAA introduced a “zero tolerance” policy with heavy fines earlier this year aimed at curbing unruly passengers after an increase in incidents, but that hasn’t stopped travelers from berating airlines, disrupting flights, and even two to knock teeth out of the mouth of a flight attendant.

“It’s gotten out of hand,” said Paul Hartshorn, spokesman for the Association of Professional Flight Attendants, which represents American Airlines’ more than 20,000 flight attendants. “It really gets to the point where we have to defend ourselves.”

The current federal mask requirements require travelers on trains, buses, commercial flights and at airports to wear face masks. The mandate, which was extended in the spring, currently expires on September 13th.

So far this year, the FAA has fined untrue travelers $ 682,000, identifying potential violations in 540 cases and taking enforcement actions in 83 cases.

The agency on Tuesday released the details of eight cases of recalcitrant travelers fined between $ 7,500 and $ 21,500 for disputes stemming from their refusal to wear masks, including two cases where passengers were other passengers hit.

Flights have been delayed and even diverted due to unruly passengers, many of whom refuse to wear face masks properly or at all. The agency does not disclose the identity of the fined passengers, but does say that passengers have 30 days to appeal the fines.

Health officials generally consider airplane travel safe with regards to Covid, but they have said it depends on passengers’ compliance with mask requirements and other guidelines.

“Although we have seen overall cases of transmissions on airplanes, this is a safe form of travel even from a Covid perspective,” said Dr. Mike Ryan, Executive Director of the World Health Organization’s Emergency Health Program, at a briefing on Monday. “The problem is what happens when you get to your destination, what you’re exposed to, and what you take home.”

Health officials are also warning of unnecessary travel, especially with the advent of the highly contagious Delta variant as many people vacation abroad to make up for more than a year of pandemic lockdown at home.

“Nobody says it is not safe to take a vacation, but we try to say that it is not time to open up to it completely,” said Ryan.

– CNBC’s Leslie Josephs contributed to this report.

Categories
Sport

The Match 2021 dwell golf updates, highlights from Tom Brady & Phil Mickelson vs. Aaron Rodgers & Bryson DeChambeau

After weeks of trash talk between Tom Brady, Phil Mickelson, Aaron Rodgers and Bryson DeChambeau, the two pairs are finally facing off in The Match 4. Brady and Mickelson will team up in hopes of avenging their loss to Tiger Woods and Peyton Manning in The Match 2, which occurred in early 2020.

Meanwhile, DeChambeau and Rodgers will each look to earn a win in their first appearance in The Match. Each player has been dealing with drama over the last few weeks. Rodgers is embroiled in a long-term holdout from Packers camp after an MVP campaign while DeChambeau parted with his caddie Tim Tucker ahead of last weekend’s Rocket Mortgage Classic. DeChambeau failed to make the cut after the change.

Despite that, DeChambeau and Rodgers are still favored to win The Match while Mickelson’s side is listed as the underdog in the event once again. That hasn’t stopped him from winning in the past, as he beat Woods in the first iteration of the event in 2018 despite Woods being heavily favored.

Either side could win the 18-hole, match-play contest that will feature a modified alternate shot format on each hole. It’s just a matter of which side can adjust to the unique conditions of The Reserve at Moonlight Basin, which is at a 7,500-foot altitude and features numerous tee shots that are significantly downhill. That includes the course’s signature hole, a 777-foot Par-5 hole where the tee is a couple hundred yards above the fairway.

Sporting News is tracking live scoring updates and highlights from the 2021 golf match featuring Tom Brady and Phil Mickelson vs. Aaron Rodgers and Bryson DeChambeau. Follow for complete results from The Match 4.

MORE: How much money will The Match winners make?

The Match live updates, highlights from 2021 golf contest

9:48 p.m. — Tom Brady said that golf is “an impossible sport” and spent time recounting his comeback Super Bowl win over the Falcons. He said that was easier than coming back from three-down in five holes at The Match.

9:40 p.m. — For the 14th hole, the golfers are only allowed to use one club for the entirety of the hole. Rodgers draws the 3-wood, Mickelson gets a 4-iron, Brady gets a 7-iron and DeChambeau gets the pitching wedge.

9:36 p.m. — Mickelson converts on the 13th for par to match Rodgers and DeChambeau. With five holes left, Rodgers and DeChambeau are three-up on Brady and Mickelson.

9:31 p.m. — On another note, Larry Fitzgerald said when talking to Baker Mayfield that he wouldn’t crack the top seven on the Browns receiver depth chart. That’s hard to believe even at this stage in Fitzgerald’s Hall of Fame career.

9:27 p.m. — DeChambeau and Rodgers are taking a drop shot after both of their shots landed in a penalty area. That gives a slight advantage to Brady and Mickelson, though Brady’s shot went awry and missed the green.

9:23 p.m. — Mickelson and Brady were in need of a good drive and Mickelson got it into the fairway. Brady missed while “channeling his inner Charles Barkley.” Meanwhile, Rodgers and DeChambeau both missed the fairway. Mickelson and Brady have a good chance to make up one point on this hole.

9:15 p.m. — Rodgers knocks in a birdie putt to give his pairing a win for the third consecutive hole. He and DeChambeau now are three-up on Brady and Mickelson and have birdied the last three holes.

9:08 p.m. — DeChambeau hit his tee shot on the Par-3 12th hole and got it very close to the hole. Mickelson nearly had a similar shot toward the hole, but his stopped right outside the green. DeChambeau and Rodgers have a chance to build a three-hole lead.

9:03 p.m. — DeChambeau and Rodgers have won four of the last six holes and seem to be getting hot at the right time. Rodgers’ driving has been surprisingly good, and that pairing has been using his tee shot more than that of DeChambeau.

9:02 p.m. — Rodgers hits a birdie putt on the 11th hole. That gives the DeChambeau-Rodgers pairing a two-hole lead, the largest lead of the night with seven holes remaining.

8:57 p.m. — Rodgers was asked about his future with the Packers on the TNT broadcast. He was mum on the matter but told Charles Barkley he’d tell the NBA legend his plans in Tahoe next week. That’s the site of the American Century Celebrity Golf Tournament for 2021.

8:52 p.m. — DeChambeau nearly drove the green on the Par-4 11th, which plays 447 yards but is downhill. Rodgers shot from a closer tee and managed to get the ball even closer than his partner.

8:50 p.m. — Brady and Rodgers were playing catch with a football before the 11th hole. 

8:45 p.m. — DeChambeau and Rodgers win the hole after Rodgers holes a short putt. After 10 holes, they are now up one on Brady and Mickelson.

8:41 p.m. — Now, the leg-up belongs to the Rodgers-DeChambeau pairing. DeChambeau lands his chip very close to the hole while Mickelson’s skitters past it and runs away from it. Brady’s putt will be harder than Rodgers’ on the 10th green.

8:34 p.m. — Brady and Rodgers drive the ball well once again, and the golfers will use their tee shots on the 10th hole. Brady’s shot landed particularly close to the green, giving him and Mickelson the early advantage on this hole.

8:30 p.m. — We’re heading to the back nine now. They’ll tee off at the 10th hole in short order.

8:20 p.m. — Both Brady and Rodgers miss mid-length putts, with Rodgers coming up short and Brady’s running just a bit long. After nine holes, we are all square.

8:15 p.m. — We’ve seen foxes, wolves and bears on the Moonlight Basin course today.

8:11 p.m. — On the ninth hole, Mickelson and DeChambeau drove over the green on the 282-yard Par-4. Rodgers and Brady both came up short, but their shots will likely be played. The DeChambeau-Rodgers has used Rodgers’ tee shot on five of the last six holes, 

8:07 p.m. — Charles Barkley delivered a classic line after Mickelson and DeChambeau spent a long time breaking down the final putt on the eighth hole.

Charles Barkley, watching Phil and Bryson talk about putting:

“Could you imagine being in a car with these two guys on a long trip?”

— Dylan Dethier (@dylan_dethier) July 7, 2021

8:04 p.m. — Rodgers and DeChambeau win the eighth hole thanks to their long tee shots, a nice bunker shot from Rodgers and Mickelson and Brady missing the fairway for the first time during The Match. The back-and-forth affair continues, as the pairs are tied up after eight holes.

7:56 p.m. — Officially, DeChambeau’s initial drive went 480 yards. Rodgers’ went 438.

7:51 p.m. — Rodgers and Brady were shooting from 100 yards closer to the hole (677 yards), and Rodgers’ shot was impressive. His went over 400 yards and put his team in good shape to make up their one-hole deficit.

7:49 p.m. — DeChambeau and Mickelson both crushed their tee shots, but Mickelson’s landed in a bunker. DeChambeau actually bought himself a mulligan by donating $100,000 to charity after his got stuck in the rough. However, he sliced that one wide left.

7:45 p.m. — We’re onto the eighth hole, which is really the 17th hole at the course. It’s a whopping 777 yards but plays significantly downhill.

7:42 p.m. — Earlier in the event, Charles Barkley shared a story about Brady’s epic work ethic and how he prepared for his participation in The Match 2.

7:39 p.m. — Brady sinks a 12-foot birdie putt to win the hole for his tandem. That puts Brady and Mickelson up one after seven holes.

7:37 p.m. — Rob Gronkowski has called into The Match and he and Brady are trash-talking Rodgers. Gronkowski is calling Rodgers “slow” and “lazier than he was in retirement.” Meanwhile, Brady called Rodgers “the leader of the Packers… I think.”

7:34 p.m. — Rodgers and Mickelson land on the green at the seventh hole. Nobody gets a hole-in-one, but Mickelson is closest to the hole. Neither Brady nor DeChambeau landed on the green.

7:29 p.m. — Hole 7 features another hole-in-one challenge. Expect the players to target the pin.

7:25 p.m. — Rodgers very nearly sunk an eagle putt to win the sixth hole. He and DeChambeau still earned the victory on the hole, as Brady and Mickelson ran into some bunker problems. After six, we’re tied up.

7:18 p.m. —  Mickelson and Rodgers won the longest drive competition. Each gets $400,000 for charity as a result of their efforts on Hole 6.

7:11 p.m. —  Mickelson and Brady have yet to miss a fairway after Mickelson landed a long drive there on the sixth hole.

7:05 p.m. — Brady and Rodgers both convert to birdie the hole. The hole is halved and Brady and Mickelson maintain a one-hole lead.

7:00 p.m. —  Mickelson and DeChambeau get started with a couple of great shots off the tee. Both are within 10 feet of the hole. Mickelson’s was within five feet of the hole, so $500,000 will be donated to My Brother’s Keeper as a result of the “closest to the pin” challenge for the hole.

6:54 p.m. —  Through four holes, Brady and Mickelson lead. They have been consistent, notching pars on three holes and a birdie on the fourth. Rodgers and DeChambeau have been a bit more up and down, as they’ve gone birdie-par-bogey-par on the first four holes.

6:51 p.m. —  Rodgers told Mickelson that he would walk his putt in. He pulled off the feat and gave his pairing a par mark on the hole. Brady sunk a birdie putt, to put himself and Mickelson up one.

6:47 p.m. —  Lefty chips to within a few feet of the hole. DeChambeau went a bit further than Mickelson’s, who wanted an in-depth analysis from DeChambeau of his approach. Mickelson’s catchphrase so far has been, “We’re not in any rush.”

6:43 p.m. —  Rodgers drive went into the woods, but DeChambeau managed to hit the ball onto the fairway. The shot was an impressive one, though it took quite a long time for the pairing to find the ball, as Mickelson and Brady lamented.

6:34 p.m. —  Brady can’t follow up his great drive with another. His goes left on the dogleg right. Mickelson’s lands in the fairway. Rodgers hits another low shot that bounces off the fairway. DeChambeau slices off the fairway as well. Mickelson’s shot is the best of the bunch.

6:25 p.m. —  Brady and Mickelson emerge as the winners of the third hole. DeChambeau missed a 3-foot putt to split the hole. We’re all square, and Brady is surprised that they were able to pull that off after DeChambeau’s great tee shot.

6:15 p.m. —  Brady and DeChambeau both drove the green at the Par-4, 393-yard third hole. Brady’s shot was incredible and almost as good as DeChambeau’s.

6:11 p.m. —  Rodgers makes par. Mickelson follows suit. The second hole is halved, so the Rodgers-DeChambeau duo maintains a one-point lead.

6:09 p.m. —  Brady hits a nice putt on his second shot to set up a short putt for Mickelson on his next shot. DeChambeau nearly sinks one but sets up Rodgers for a putt similar to Mickelson’s.

6:06 p.m. —  Brady’s shot carries just over the green as he took aim at the flag. Mickelson says, “good shot, partner,” before landing his just off the green and next to a sprinkler head.

6:04 p.m. —  On Hole 2, there’s a hole-in-one challenge in effect. Rodgers manages to drive the green which opens DeChambeau to go for the hole-in-one. DeChambeau’s shot landed in the bunker.

5:57 p.m. — After Rodgers came up short on an approach shot, DeChambeau managed to hole out from just off the green. Mickelson couldn’t make the putt to tie the hole. As such, DeChambeau and Rodgers emerge as the winners of the first hole.

5:50 p.m. —  And now, Rodgers hits. His doesn’t quite reach the fairway, as his shot was a low screamer and had an apex of just 53 feet. DeChambeau launches the ball far down the fairway, well ahead of Mickelson’s. DeChambeau’s shot was the most impressive of the foursome, and he also got in a good shot at Brady, giving him a roll of duck tape for his pants and his mouth. Brady famously ripped his pants during The Match 2.

5:48 p.m. —   Brady hits first off the first tee. He launches the ball off the fairway to the left. Mickelson is next. He hits one nice and easy into the fairway. 

5:45 p.m. —  Rodgers is giving Brady some advice ahead of the event. 

5:36 p.m. —  All right, let’s get this thing started. Brady, Mickelson, Rodgers and DeChambeau are ready to tee off at The Reserve at Moonlight Basin.

5:33 p.m. —  Bryson DeChambeau may be an excellent golfer, but Aaron Rodgers said that he has been working with DeChambeau on his trash talk ahead of The Match. We’ll soon see if he’s made some improvements in that area.

5:28 p.m. —  Mickelson made 15 putts in 30 seconds in a pre-event challenge. Event sponsors will donate 150,000 meals to Feeding America and the Montana Food Bank as a result of Mickelson’s performance.

5:26 p.m. —  Barkley announced that he is donating $100,000 to the Montana Food Bank as part of The Match’s charitable efforts.

5:24 p.m. —  Tom Brady said while warming up that playing football was easier than golf. It’s hard to imagine that many in the world agree with him on that front.

5:12 p.m. —  Charles Barkley participated in The Match 3. Why isn’t he involved in this competition after being part of the winning pair with Mickelson? He explained in typical Barkley fashion on the preshow.

5:06 p.m. —  Former PGA Tour pro and 2008 Masters winner Trevor Immelman says that Bryson DeChambeau should hit some 400-yard tee shots today because of the course elevation along with his PGA Tour-leading 321.9-yard average off the tee.

5:02 p.m. —  Mickelson and Brady talked a lot about their previous Match loss in the intro to the event. Mickelson said they were “hungry” for a win. The underdogs seem to be carrying a chip on their shoulders.

4:55 p.m. —  The four golfers posed for a pre-Match photo. A lot of black, blue and white, but Brady’s red TB12 hat is helping him stand out among the crowd.

4:53 p.m. —  Bryson DeChambeau seems ready for The Match! He showed up to the event in a helicopter.

4:51 p.m. —  While Tom Brady has the advantage over Aaron Rodgers in terms of experience playing The Match, Rodgers is a better golfer than Brady. In fact, Rodgers’ handicap is about 4 1/2 strokes better than Brady’s .

4:42 p.m. —  Charles Barkley actually almost hit the cart during the range battle. It came right after the cart operator heckled him.

4:36 p.m. —  Brady shared a bit of Mickelson’s strategy for The Match on Twitter Tuesday morning. Needless to say, he is focused on going long off the tee at the high-elevation Moonlight Basin course.

4:32 p.m. —  In case you’re wondering, Mickelson won the range battle by hitting the golf cart eight times. Brady, Rodgers and DeChambeau each hit the cart once.

4:31 p.m. —  Moonlight Basin golf course has never been played during a televised event. It’s a beautiful-looking course, so needless to say, we’re looking forward to seeing the golfers in action on it.

4:28 p.m. —  Before The Match starts, the golfers and commentators for the event took part in a range battle event. Every golfer was trying to hit a golf cart located on the driving range. Charles Barkley chirped the cart driver after the driver called out Barkley’s notoriously awkward golf swing.

4:21 p.m. —  There has been plenty of trash talk from all parties involved in The Match this week, but Brady’s did at Rodgers’ rift with the Packers may be one of the best moments of all.

4:18 p.m. —  Apparently, it is windy at Moonlight Basin today. Mickelson tweeted a video of him and Brady getting some warmup shots in, and you can barely hear Mickelson over the sound of the wind.

Tom Brady and Phil Mickelson results

  • Hole 1 (Par 4, 463 yards): Par (loss)
  • Hole 2 (Par 4, 447 yards): Par (tie)
  • Hole 3 (Par 3, 206 yards): Par (win)
  • Hole 4 (Par 5, 566 yards): Birdie (win)
  • Hole 5 (Par 3, 248 yards): Birdie (tie)
  • Hole 6 (Par 5, 559 yards): Par (loss)
  • Hole 7 (Par 3, 184 yards): Birdie (win)
  • Hole 8 (Par 5, 777 yards): Bogey (loss)
  • Hole 9 (Par 4, 282 yards): Par (tie)
  • Hole 10 (Par 4, 427 yards): Par (loss)
  • Hole 11 (Par 4, 447 yards): Par (loss)
  • Hole 12 (Par 3, 190 yards): Par (loss)
  • Hole 13 (Par 4, 470 yards): Par (tie)
  • Hole 14 (Par 4, 443 yards):
  • Hole 15 (Par 5, 590 yards):
  • Hole 16 (Par 3, 223 yards):
  • Hole 17 (Par 5, 777 yards):
  • Hole 18 (Par 4, 354 yards):

MORE: Explaining the format, rules for The Match

Aaron Rodgers and Bryson DeChambeau results

  • Hole 1 (Par 4, 463 yards): Birdie (win)
  • Hole 2 (Par 4, 447 yards): Par (tie)
  • Hole 3 (Par 3, 206 yards): Bogey (loss)
  • Hole 4 (Par 5, 566 yards): Par (loss)
  • Hole 5 (Par 3, 248 yards): Birdie (tie)
  • Hole 6 (Par 5, 559 yards): Birdie (win)
  • Hole 7 (Par 3, 184 yards): Par (loss)
  • Hole 8 (Par 5, 777 yards): Birdie (win)
  • Hole 9 (Par 4, 282 yards): Par (tie)
  • Hole 10 (Par 4, 427 yards): Birdie (win)
  • Hole 11 (Par 4, 447 yards): Birdie (win)
  • Hole 12 (Par 3, 190 yards): Birdie (win)
  • Hole 13 (Par 4, 470 yards): Par (tie)
  • Hole 14 (Par 4, 443 yards):
  • Hole 15 (Par 5, 590 yards):
  • Hole 16 (Par 3, 223 yards):
  • Hole 17 (Par 5, 777 yards):
  • Hole 18 (Par 4, 354 yards):

What time is The Match golf contest today?

  • Start time: 5 p.m. ET / 2 p.m. PT

Live TV coverage of “The Match 4” will begin at 5 p.m. ET from The Reserve at Moonlight Basin in Big Sky, Montana. TNT’s broadcast plans include a pre-show before play begins, so expect Tom Brady, Phil Mickelson, Aaron Rodgers and Bryson DeChambeau to tee off shortly thereafter.

How to watch The Match 2021

  • TV channels:  TNT, TBS and truTV
  • Live stream: TNT app

Three networks in the Turner Sports family will be simulcasting “The Match 4”: TNT, TBS and truTV. Coverage of the event will begin at 5 p.m. ET and will feature play-by-play host Brian Anderson, former “The Match” participant Charles Barkley and other notable analysts.

Categories
Science

Doubtlessly extra underground lakes discovered on Mars

One of the most difficult things to reconcile in science is when new data either complicates or refutes previous knowledge. It is even more difficult when these results have been widely disseminated and made known in the community. But that’s how science works – the theories have to match the data. When a team at JPL analyzed Mars Express data on Mars’ South Pole, they found that the results published in 2018 on underground lakes on Mars may have been more difficult than they originally thought.

This original discovery was announced after scientists found particularly bright spots in radar signals below the surface, which were interpreted as being from liquid water. Located in the region known as the “South Polar Stratified Deposits”, layers of water, dry ice, and dust have mixed for millions of years as the axial tilt of Mars changed. In the lower layers, the temperatures were high enough that sufficient salty water could potentially be liquid.

UT video about the possibility of life (and water) on Mars.

Looking through the data for the entire South Pole of Mars, the JPL scientists noticed the same highly reflective surface in dozens of other places below the surface. Some appeared to be within 1 mile of the surface. Unfortunately, this also means the temperature would be a cool -63 C (-81 F). Even with an enormous amount of perchlorates (a special type of salt found on Mars), water would still freeze at these temperatures.

First, investigators, Jeffrey Plaut and Aditya Khuller from JPL (Khuller is now with ASU) tried to think about other potential sources of heat that could raise the temperature in the areas where they saw the highly reflective features. An obvious candidate would be volcanism, which may be responsible for submarine oceans on other worlds in the solar system. However, there is no other evidence of active volcanism at the South Pole, so the researchers ruled it out as a heat source.

Visualization from the original 2018 study showing the reflected radar signals interpreted as lakes.
Credit Context Card: NASA / Viking; THEMIS Background: NASA / JPL-Caltech / Arizona State University; MARSIS data: ESA / NASA / JPL / ASI / Univ. Rome; R. Orosei et al. 2018

Also, since there is a lack of heat to create liquid water, the researchers have no idea what these highly reflective surfaces could possibly be causing. Could it be lakes caused by heat from an unknown source? Is there any other material that is as reflective to radar as liquid water beneath the surface of Mars? The details of a future manned mission to the Red Planet could literally depend on the answer to these questions. But at the moment there is no satisfactory answer.

Put simply, either there are dozens of underground lakes on Mars that are heated by an as-yet-unknown source, or there could be an unknown material that reflects radar waves as effectively as liquid water, which led scientists to believe that there was liquid water there is available. Or it could be a combination of the two, with liquid water in some warmer pockets while the unknown material is in colder regions. According to other research just reported by UT, there are several possibilities in between.

Points on this map of Mars’ South Pole show where radar reflections were recorded by the MARSIS instrument used by JPL scientists.
Credit – ESA / NASA / JPL-Caltech

Given the importance of water to the success of any human presence on Mars, researchers will want to know where on this spectrum the truth lies. And the only way to find out is to collect even more data. Let’s hope the data we have gathered will answer more questions than it raises next time.

Learn more –
JPL study examines Mars’ underground water signals in more detail
UT – Unfortunately, there are other workable explanations for the underground lakes on Mars
Phys.org – “Lakes” under the South Pole of Mars: A cloudy picture?
Geophysical Research Letters – Characteristics of the Basal Interface of the Mars-South Polar Layer Deposits

Mission statement –
Ice cap at the south pole of Mars, which contains frozen water as well as dry ice.
Credit – ESA / DLR / FU Berlin / Bill Dunford

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Categories
Entertainment

JT shares a couple of tweets after Lil Uzi Vert’s alleged argument with ex-girlfriend Brittany Byrd

Keep it cute or mute it! It was revealed on Friday that Lil Uzi Vert has gotten into an alleged argument with his ex-girlfriend Brittany Byrd. Many were shocked to learn that he allegedly attacked them in a Los Angeles restaurant. While everyone was talking about the incident online, many were waiting for one person to share their opinion. This person is Uzi’s current girlfriend, JT. We all know JT stands by her husband and has spoken loudly about her dislike of Brittany in the past, but in this case, JT has not offered anything online about the incident.

When Uzi was trending online on Friday, JT seemed to know what was going on and apparently responded to online critics who were pestered with their silence. JT tweeted, “When I talk insane! When I’m all crazy! I’m starting to fart voice memos! ”The City Girl didn’t stop there, she tweeted again. “I would change my name to doo doo so that you can keep my name out of your mouth. But you all a bunch of fuckers, so I’d be wasting my time! “

The roommates responded to JT’s tweets in our comment section. One commented: “Lmao. JT just get a publicist! ”Another commented,“ I’ve never read shit like that. ” JT found the post amusing and walked into The Shade Room and left a comment. She wrote: “You are so thirsty!” along with several laughing emojis. JT seemed unimpressed by all of the drama about her husband. Later that evening, she headed out for a fun night out with Yung Miami while attending Saweetie’s Freaknik birthday party in Los Angeles.

JT showed up with an updo and a yellow two-piece set. Miami wore a red romper and birthday girl Saweetie wore a two-piece Louis Vuitton set.

Roommate, do you think JT should have commented on Uzi’s alleged argument or kept silent?

Would you like updates straight to your text inbox? Call us at 917-722-8057 or https://my.community.com/theshaderoom

Categories
Sport

Milwaukee Bucks’ Giannis Antetokounmpo attracts doubtful day for Sport 1 of the NBA Finals in opposition to Phoenix Suns

PHOENIX – Giannis Antetokounmpo is considered dubious for Game 1 of Tuesday’s NBA Finals against the Phoenix Suns after missing the Milwaukee Bucks’ final two games with a hyperextended left knee.

Antetokounmpo was injured in Game 4 of the Eastern Conference final against the Atlanta Hawks.

Bucks coach Mike Budenholzer said Monday that Antetokounmpo will be able to work on the pitch separately from the team’s afternoon training. When asked which specific exercises and movements Antetokounmpo was able to perform painlessly, Budenholzer declined to answer.

2 relatives

“He had a good day,” said Budenholzer. “He’s making good progress.”

The NBA announced that Antetokounmpo was not allowed to speak to reporters on Monday as the status for Game 1 was uncertain.

After a knee injury against the Hawks, Antetokounmpo was able to work on the basketball court for the first time on Saturday. Before that, according to Budenholzer, he could only do exercises in the weight room.

Without their two-time MVP in the last two games of the East Finals, the Bucks prevailed behind the dominant game of Khris Middleton, Jrue Holiday and Brook Lopez.

“When Giannis is out there we can often just give him the ball and let him go to work and let him orchestrate a lot of things out there,” said Middleton. “Without him we have to do it in committee.”

Bobby Portis started in both games that Antetokounmpo missed, while Middleton scored 64 points together and added 60 to Holiday.

Without Antetokounmpo, Holiday believed that he had to fill part of the offensive void and fill part of the void when attacking the basket.

“[I’m trying to] Just keep being aggressive, “said Holiday.” No disappointments because like Giannis [plays], there are no disappointments. He constantly goes to the basket and is aggressive on both ends of the floor. He does so much for this team that I just felt like I was losing, that would be really difficult for us. “

Middleton said he tried to support Antetokounmpo by suggesting the big man not to rush back until he was ready.

“[I told him] don’t rush back and put yourself at greater risk of major injury, “said Middleton.” He’s a guy – he puts so much time and effort into his body to be the best version of himself too. “

Categories
Science

Was World Warming The Reason behind the Nice Northwest Heatwave? Science Says No. – Watts Up With That?

Reposted from The Cliff Mass Weather Blog

During the past week, the Pacific Northwest experienced the most severe heat event of the past century.

All-time high-temperature records were broken throughout the region, often by large margins. Many in the media, several local and national politicians, and some activist environmental scientists have claimed that this event was “driven by” or predominantly forced by human-inspired global warming (usually referred to as “climate change”).But such global warming claims are not supported by the facts and our best scientific understanding.  

Truth and Rigorous Science About Climate Change is Necessary for Wise Decisions
In this blog, I will use observations, modeling, climatological data, and the peer-reviewed scientific literature to demonstrate that human-caused global warming played a very small role in the extreme heat event that we just experienced here in the Pacific Northwest.I will describe the origins of a meteorological black swan eventand how the atmosphere is capable of attaining extreme, unusual conditions without any aid from our species.As you read this, consider that I have actively pursued research on Northwest heatwaves, published several papers in the peer-reviewed literature on this specific topic, and have run both weather prediction and climate models that simulate such events.  This subject is in my wheelhouse.

I also discuss the seriousness of misinformation.   You and others can not make wise decisions when the information provided to you is not based on truth and science.

This is going to be an extended, detailed blog, a necessity if you are going to truly understand the science and the situation.  Superficial, hand-waving arguments will not allow you to comprehend the truth, particularly when so many “facts” communicated in the media and among activists are inconsistent with the best science.

The Event

The maximum temperatures during the heatwave were as high as 30-40 degrees Fahrenheit above normal.    Seattle had a high of 108F,  35F above the normal high of 73F.  Quilluyte on the Washington Coast zoomed to 109F compared to a normal high of 65 (44F above normal).  Throughout the region, all-time temperature records were broken, representing the hottest day on record at many locations. 

The map below shows where the all-time temperature records were broken, mainly west of the Cascade crest.

These high-temperature records occurred in late June, which is atypically early in the summer, with previous high-temperature records occurring roughly a month later when the Pacific Northwest climatologically is at its maximum warmth.

All-Time Records for High Temperatures Broken In WA/OR (red dots)

The Global Warming Background

The Pacific Northwest is warming and human emission of greenhouse gases is probably the origin of much of it.  

To illustrate, the figure below shows the annual average high temperatures for Washington State from 1900 through 2020.  About 1.5 F of warming over 120 years.  The summer warming is nearly the same.   

Let us assume that ALL of this warming is caused by mankind’s greenhouse gas emissions, although some might argue with that assumption.   The warming during the past several decades is consistent with human causation, and climate modeling supports this contention.

So if greenhouse gas warming over Washington State is 1-2F,  how can greenhouse gases cause a huge heatwave that is ten to twenty times greater?  A very good question. Such a ten-times amplification of the global warming signal would require powerful positive feedbacks, which I will demonstrate below are simply not evident.  A global warming origin of increased temperature extremes would also be evident in long-term trends of extreme temperatures, but such trends do not exist.But before we get into such things, you must understand the origins of the extraordinarily high temperatures observed earlier last week.
What Caused the Northwest Heat Wave?
A number of factors came together simultaneously to produce the extreme high temperatures over the Northwest observed last week.  
The key factor in this and previous regional heatwaves is the development of an unusually strong and persistent area of high pressure over the Northwest.   Such high-pressure areas are also called ridges and often extend vertically through great depth (10-30 thousand feet).  
The figure below illustrates what the ridge looked like at 11 AM  last Sunday around 18,000 feet above the surface (500 hPa pressure).  At this level, the ridge was the most intense ever observed over the region (will prove that later).

Map A
High-pressure areas/ridges are associated with warm temperatures during the summer.  First, high-pressure areas possess strong sinking, and sinking causes powerful warming as air is compressed as it descends to the higher pressure that exists at low levels (pressure decreases with height).  Your air pump, very warm after inflating a tire, is a good illustration of this mechanism.  
Ridges also possess southerly (from the south) flow on their western sides (apparent above), bringing subtropical warmth northwards.    
But there is more! 
The sinking air in high-pressure areas prevents clouds, thus allowing maximum solar heating (and the sun is near maximum strength now).  And on the southern side of upper-level ridges there is often easterly (from the east) wind, which can move down the western slopes of terrain barriers, producing even MORE compressional heating as the air descends the slopes.
It is no accident that every major summer heatwave in our region is associated with a ridge of high pressure.   Ridges are veritable heating machines during summer and sometimes are colloquially referred to as heat domes.  The media loves this term.   
The origin of the intense ridge of high pressure of last week is fascinating.
Our ridge appears to have originated in the far western Pacific, where a tropical disturbance rammed into the Pacific jet stream, causing high-amplitude waviness in the jet stream thousands of miles downstream to the east.  The result was a strong ridge over the Northwest, with the waviness also producing a deep trough over the central Pacific (see upper-level map on Wednesday, June 23rd, 500 hPa pressure–about 18,000 ft).

Blue and purple indicate much lower than typical pressures (troughs or lows), red indicates above-average values (ridges or highs). You can see the waviness of the atmosphere over the north Pacific from Asia to North America.The Atmospheric Heat Supercharger
In our heatwave, there was a feature that supercharged the warming west of the Cascade crest and the coastal mountains (e.g., the Olympics):   an approaching upper-atmospheric low-pressure area (or trough) that was west of northern California in Map A above. 

Our high-pressure ridge (“heat dome”) had a potent supercharger.  Picture courtesy of Nick Ares.
Between the offshore trough and the ridge over the Pacific Northwest, there were strong southeasterly (from the southeast) winds that pulled up air from the warm desert Southwest.  This air subsequently descended the western slopes of the Cascades, where the air was further compressed and warmed.  
You can see this “supercharger” in action on Monday afternoon in a forecast map valid for around 5000 ft (850 hPa pressure level).  The colors indicate temperatures (darker red is warmer) and winds are also shown.  You can think of the solid lines as representing the pressure at that level. Note the low offshore and the high to the northeast.  The white arrow shows the warm southeasterly flow that descended the Cascade’s western slopes.

And the impact of the supercharger is seen in the super-warm air (brown colors, 104F, and more) found downstream of the Cascades at 5 PM on Monday, June 28.

Everything had to come together just “right” to give us this extreme event.
Record amplitude of a ridge/high pressure over our region, forced by a tropical disturbance in the western Pacific, that produced a downstream “wave train”.   An environment that allowed the resulting wave to amplify.  The ridge had to be in exactly the right position relative to our terrain.  An upper-level trough had to develop in just the right location offshore and move in the optimal direction to cause strong southeasterly flow, fostering the supercharger noted above.  We needed a period when the sun was very strong.    And a summer stretch without smoke, which has a profound cooling effect.
The meteorological dice had to come up all sixes.  And they did.

This concurrence of a number of factors coming together at one place and time was why the extreme heat occurred, with a very small assist from global warming, which added a few degrees to an already extreme event.
It is important to note that the atmosphere comes up sixes regularly, but not necessarily in the same place.  The atmosphere is churning with all kinds of variability inherent in the physics of the atmosphere (also called natural variability).  
To illustrate this to you, below is a world map of the temperature anomalies (difference from normal) just above the surface (about 800 m in elevation) on Tuesday, June 29th.  You can see our extreme heatwave (red colors), centered over the northwest corner of Washington.  But there are other large temperature anomalies scattered around the world, both warm and cold.    Those are overwhelming NOT the result of global warming, but of natural variability.  I could show you a similar map for a date, in say, 1940.  It would look the same (I checked).
Extreme temperatures happen all the time in a somewhat random fashion.  They just don’t happen where YOU are located very frequently, because so many random mechanisms must come together at the same time to do so.

Natural Variability or Global Warming?   Dealing with Unsupported Claims
Since global warming is much smaller than the magnitude of the heatwave temperature extremes observed last week in the Northwest, those trying to ascribe the extreme temperatures to global warming must prove that global warming somehow amplifies natural variability.   
For example,  some have suggested that the key feature of last week’s heatwave– the extreme amplitude ridge of high pressure aloft– had origins in global warming.   Others have suggested that global warming dries the soils, resulting in less evaporative cooling and warmer temperatures, thus explaining the extremes.
We will evaluate the plausibility of these various mechanisms for amplifying global warming and will show that they can not explain what happened last week.
Does Global Warming “Drought” and Dry Soils Explain the Heatwave? 
One hypothesis starts with global warming causing drought and dry soils over our region.  Then they claim that such dry soils warm the air (less evaporative cooling) enough to explain the high temperatures.  Others suggest that the drought increases high pressure as well.
For reference, the NOAA Drought Monitor graphic for June 22nd shows normal or just slightly dry conditions west of the Cascade crest (where the extreme records were broken), but “drought” conditions over the normally dry region of eastern Washington.  

The claims that the critical extreme ridge of high pressure was caused by dry conditions east of the Cascade crest are problematic for many reasons, including the fact that the origin of the high pressure can be traced to a large-scale amplification of the wave pattern over the entire North Pacific.  Similarly, the claims that dry conditions east of the Cascades were significant in creating the extreme heatwave west of the Cascade crest are also weak.   Let me prove this to you.
Model forecasts were stunningly good for this event.  Even almost a week out, model simulations correctly predicted the development of an extreme high-pressure area over the Northwest and very high surface temperatures.   Modelers like myself can “play god” with such excellent simulations, in this case, by making the soil much moister and seeing what happens.    Would the heatwave go away with the absence of drought and under moister soil moisture conditions?    You are about to find out.
Senior UW graduate student Robert Conrick re-ran the UW WRF weather forecasting model and tripled the soil moisture everywhere.  He turned the region into a veritable swamp!    And what do you think happened to the ridge of high pressure and the heat dome?   Did it disappear?  Did the heatwave go away? 
The answer: virtually nothing happened to the intense high-pressure area.  The heat dome was essentially unchanged.  Surface temperatures over BC and western WA hardly changed.

The figure below shows the height of the ridge at 500 hPa pressure (you can think of this as the pressure at around 18,000 ft.  The left side uses the actual soil moisture last week, the right side shows the same thing with TRIPLE the soil moisture.  Virtually the same heights or pressures.

What about temperatures at the surface?   Even with “biblical” moistening of the soil over the entire domain, temperatures over western Washington and British Columbia, where the heatwave was most severe, hardly changed, cooling by about 1 degrees C (about 2F) or less.

The theory of an unusually dry surface produced by global warming “drought” causing the high pressure “heat dome” or greatly warming low-level temperatures west of the Cascade crest appears unfounded.
This makes physical sense for a number of reasons.  For example,  the lush western side of the Northwest remained relatively moist into the summer.  June’s rainfall was well above normal over most of the region west of the Cascade crest.  As noted in my earlier blog, the trajectories of the air reaching the surface west of the Cascade crest did not come from the surface over eastern Washington or Oregon but subsided (sank) rapidly from aloft.
But there is something else that essentially puts the silver stake into the heart of the unfounded global warming “drought” theory of this event.
Specifically, there is no observed trend towards “drought” over the Pacific Northwest as demanded by the proposed global warming origin of this event.
Below is the observed annual precipitation over Washington State since 1900.   Our region is NOT getting drier.  If anything precipitation has increased a slight amount.

And is spring drought increasing in frequency as suggested by those pushing the global warming hypothesis?  The answer is no.  Below is a long-period plot of the Palmer Drought Index, which considers BOTH temperature and precipitation.  No apparent long-term trend in spring drought…and notice how much worse it was during the 1930s and early 1940s.

So not only does the global warming drought hypothesis for the heatwave fail on a physical basis, but there is no trend in drought, which is a requirement if global warming was the explanation.  

Does Global Warming Produce Stronger Ridges of High Pressure?
Another claim, provided by Professor Michael Mann of Penn. State and published in the New York Times is that global warming produces a weakened, “lazy” jet stream that forces more wave-like undulations and thus more ridging.    This hypothesis has been thoroughly debunked in a number of papers in the peer-reviewed literature (see this article for an example or my blog).  But I need not cite others, since I and my students have investigated this very issue in research sponsored by the National Science Foundation and published the research in the peer-reviewed literature.
For example, Matt Brewer and I looked at global climate models driven by rapidly increasing greenhouse gases and found that high-pressure areas like that seen last week will WEAKEN under global warming.  Just the opposite of what Professor Mann was suggesting.

And last week I examined the frequency of high-amplitude ridging over our region from 1948 to today using NOAA reanalysis gridded data.  I found no trend in the extreme highs aloft.

As further confirmation, Dr. Joe Zagrodnik of Washington State University examined the radiosonde sounding data (balloon-launched weather stations) at Quillaytate on the Washington coast and found no upward trend in the maximum heights (that is big ridges of high pressure) at 500 hPa (around 18,000 ft) at that location.

Dr. Zagrodnk also did not find any trend in extreme high temperatures in the lower troposphere (around 5000 ft).
Bottom line: none of the claims that global warming increases ridging (high pressure)  over time are supported by data or modeling.  Unfortunately, Dr. Mann and others continue to push this unfactual narrative.
Perhaps, The Most Compelling Evidence of All
If global warming was producing extreme heatwaves in our region, such as the event last week, there would be a long-term trend towards more extreme high temperatures.  A single event does not reflect climate, only a trend or changes in long-term average do.
Well-known climatologist (and the official Alabama State climatologist) Dr. John Christy has run the numbers to determine if there are trends in record-breaking extreme temperatures in Washington State or Oregon.  
As shown below, there IS NO INCREASING TREND for more record high temperatures over our region during the past century.  In fact, the past decade (2011-2020) had no all-time records.  I suspect many of you are surprised at this, but it is true.

Total number of stations with temperatures about 99F in our region?  Also no trend

These results are consistent with what others have found.  For example, the U.S. National Climate Assessment found the warmest day of the year over the Northwest actually COOLED between a historic (1901-1960) and a contemporary period (1986-2016).

I had a conversation about these findings with Dr. Nick Bond, Washington State Climatologist.  He told me he was not surprised, and that he and Associate State Climatologist Karin Bumbaco found similar results, published in a peer-reviewed paper.
You may ask why there is little or no upward trend in record high temperatures even though the region and planet are warming.   
There are a number of possibilities.  For example, natural variability may be so dominant that a small amount of global warming is hard to notice.  Or there may be climate feedbacks that work against extremes in a warming world….at least in our area.  I have been researching one of these feedbacks:  the tendency of heat-wave producing easterly flow to weaken under global warming and describe it below. And I can think of several more.
Still not convinced?  Read on.High Resolution, State-of-Science Regional Climate Models Do Not Suggest A Global Warming Origin of the Extreme Heat
One of my major research projects (with Professor Eric Salathe of UW Bothel and supported by Amazon) has been to run high-resolution climate simulations driven by the most realistic global climate models.  And the results are very relevant for this discussion.
Below is a graphic from this work showing the extreme high temperature each year at Seattle Tacoma Airport by an ensemble of 12 regional climate simulations (12-km grid spacing—VERY high resolution for climate work) driven by a highly aggressive (and unrealistic) increase of greenhouse gas emissions (RCP 8.5).  These simulations started in 1970 and each forecast is shown by a different color. The green line is the mean of the regional forecasts and the observed highs are shown by black dots.  I have indicated SeaTac’s high temperatures this year (108F, 42C) by the blue line.

You will notice two important features of these regional climate projections. 
First, and of great importance, there is little upward trend in the extreme high temperatures.  
Second, the most extreme temperatures of the ensembles over the entire period climbed to about  42C (108F).  To do so, required rare, but possible, combinations of several factors.   Improbable, but possible.   You might also notice that the climate model was typically about 1-2C to warm.  I believe that reflects the inability of even my very high-resolution simulations to properly simulate the effects of a narrow, improperly resolved cold Puget Sound. 
Could Global Warming REDUCE Heat Waves West of the Cascade Crest?
Most people assume that global warming can only increase our high temperatures, but it can do the opposite as well.  The Northwest’s mountains and nearby cold water paradoxically might reduce heatwaves over the populated areas west of the Cascade crest under global warming.  
Global warming preferentially warms the interior of western North America compared to the Pacific coast (land warms up much more quickly than the Pacific Ocean).  The heating results in enhanced pressure falls over the interior (warm air is less dense than cold air), which strengthens cool, onshore flow and lessens warm easterly (offshore) flow.   Bad for heatwaves!
All the great heatwaves west of the Cascade crest occurred under strong easterly flow. Both global and regional climate models have shown that global warming lessens heatwave-producing easterly flow.    To illustrate this, consider the figure produced by the research done by my group with Dr. Eric Salathe of UW Bothell.  This plot shows the maximum easterly flow each year simulated by an ensemble (many forecasts) of high-resolution regional climate models.  Importantly, the mean strength of the strong easterly flow (black line) goes DOWN under global warming, working against the kind of heatwave we had last week.


The Evidence is Overwhelming

As I described above, the natural origins of the “black swan” heatwave we experienced last week can be demonstrated in a number of independent ways, from examining the origins and frequency of the ingredients (such as the high-amplitude ridge of high pressure), considering the statistics of warm temperatures  (the lack of trend in extreme high-temperature days), and through high-resolution climate modeling.

The evidence for a predominantly natural origin of the high temperatures records of last week is compelling, with global warming marginally increasing the peak temperatures by perhaps a few degrees.  Without global warming, we still would have experienced the most severe heatwave of the past century.
Politicization and Miscommunication of Science
The inaccurate information being distributed about the origins of this heatwave is very disturbing.
Some of this is being done out of ignorance or laziness, but a few individuals are deceiving the public deliberately.   Science journalism is only a shadow of what it was decades past, and a number of scientists now see social activism as more important than the determination and communication of truth.
Our nation has made costly mistakes when the truth was twisted for political reasons, such as for the Iraq war, when our nation spent trillions of dollars and initiated a war that killed hundreds of thousands of people based on misinformation about non-existent weapons of mass destruction.
We are now making similar mistakes with global warming, with politically inspired misinformation slowing realistic and life-saving steps, such as thinning our forests and restoring natural fire, or proceeding rapidly with nuclear energy.  Hyping global warming puts unrealistic and unnecessary fear into the hearts of our fellow citizens.  Unconscionable.  Global warming is an issue we can deal with, but only if truthful, factual, and science-based information is provided to decision-makers and the nation’s citizens.
I have spent my life trying to understand the weather and climate of our region and it is so frustrating that the media (e.g., KNKX public radio, the Seattle Times, the Seattle Stranger) and local politicians (such as our governor) have placed such a low priority on providing accurate information regarding climate change and other environmental challenges.  
They have put political agendas ahead of truth and we are all the worst for it.

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Categories
Health

Beforehand contaminated individuals would profit from vaccines

Dr. Scott Gottlieb believes people who were previously infected with the coronavirus would continue to benefit from Covid vaccines.

In the interview on Tuesday at CNBC’s Squawk Box, the former Food and Drug Administration commissioner admitted that some people might think that their antibodies, made by the disease, offer adequate protection against future infection or disease and therefore do without the Covid vaccination.

The reason for still getting the vaccine is “twofold,” claimed Gottlieb, who sits on the board of directors at vaccine maker Pfizer.

“First, we believe the vaccine will offer more permanent and broader immunity so it will better protect you from the variants,” he said, alluding to the highly transmissible Delta variant that worries public health officials.

“Second, if you’ve been infected before, and even if you get a single dose of the vaccine – forget to get both doses of the vaccine, just a single dose of the vaccine – you get a very robust immune response,” said Gottlieb.

Pfizer’s vaccine requires two vaccinations for full immune protection, as does Moderna’s vaccine. Johnson & Johnson makes a single-dose vaccine. These are the only three emergency vaccines approved in the US

“It is, so to speak, the best of both worlds if you have previously been infected and vaccinated,” said Gottlieb, who headed the FDA from 2017 to 2019 in the Trump administration. “At least one dose gives you broad, very deep, very lasting immunity based on the data we’ve seen so far. So there are still many compelling reasons why you might want to get vaccinated, even if you’ve been infected before. “

More than 157 million people in the U.S., or 47.4% of the population, are fully vaccinated against Covid, according to the Centers for Disease Control and Prevention. About 182.4 million people, or nearly 55% of the population, received at least one dose.

The pace of admission slowed after an aggressive push this spring to deliver the Covid shots to the Americans. In response, state and local officials – and companies too – launched various promotions to promote vaccination.

Yet some people still hesitate. According to the CDC, less than 30% of residents in about 1,000 counties in the US had been vaccinated by last week.

The increasing presence of the Delta variant in both the US and around the world increases the urgency of calls for more people to get vaccinated. The variant, discovered for the first time in India, has shown that the vaccines are slightly less effective, but still protect against serious diseases.

“We expect increased transmission in these communities when we can’t vaccinate more people,” said CDC Director Dr. Rochelle Walensky on Thursday, referring to the roughly 1,000 US states with low vaccination rates.

“Preliminary data for the past six months suggests 99.5% of deaths from Covid-19 in the states have occurred in unvaccinated people,” she added. “The suffering and loss we are experiencing now are almost entirely avoidable.”

Disclosure: Scott Gottlieb is a CNBC employee and a member of the board of directors of Pfizer, genetic testing startup Tempus, health technology company Aetion Inc., and biotechnology company Illumina. He is also co-chair of the Healthy Sail Panel of Norwegian Cruise Line Holdings and Royal Caribbean.

Categories
Sport

NBA Finals schedule 2021: Full dates, occasions, TV channels & reside streams to observe Bucks vs. Suns

And then there were two.

The Bucks and Suns each won their conference finals series in six games to reach what should be an entertaining NBA Finals. Milwaukee shut the door on Atlanta with Giannis Antetokounmpo out for the final two games, and Phoenix defeated a feisty Clippers squad behind a terrific closeout performance from Chris Paul.

Which team will be the last one standing at the end of a drama- and injury-filled postseason?

Below you’ll find everything you need to know about watching the 2021 NBA Finals.

MORE: Watch NBA Finals games live with fuboTV (7-day trial)

NBA Finals schedule

(All times Eastern)

Date Game Time  National TV
July 6 Game 1 9 p.m. ABC
July 8 Game 2 9 p.m. ABC
July 11 Game 3 8 p.m. ABC
July 14 Game 4 9 p.m. ABC
July 17 Game 5* 9 p.m. ABC
July 20 Game 6* 9 p.m. ABC
July 22 Game 7* 9 p.m. ABC

* If necessary

How to watch NBA Finals games

Every game of the 2021 NBA Finals will be shown exclusively on ABC. The series can also be streamed via Watch ESPN or fuboTV, which offers a free seven-day trial.

MORE: Odds, picks, predictions for 2021 NBA Finals

NBA playoffs 2021: Results from each round

Eastern Conference finals results

(3) Bucks vs. (5) Hawks: Milwaukee wins 4-2

Game Result
Game 1 Hawks 116, Bucks 113
Game 2 Bucks 125, Hawks 91
Game 3 Bucks 113, Hawks 102
Game 4 Hawks 110, Bucks 88
Game 5 Bucks 123, Hawks 112
Game 6 Bucks 118, Hawks 107

Western Conference finals results

(2) Suns vs. (4) Clippers: Phoenix wins 4-2

Game Result
Game 1 Suns 120, Clippers 114 
Game 2 Suns 104, Clippers 103
Game 3 Clippers 106, Suns 92
Game 4 Suns 84, Clippers 80
Game 5 Clippers 116, Suns 102
Game 6 Suns 130, Clippers 103

Eastern Conference second-round results

(1) 76ers vs. (5) Hawks: Atlanta wins 4-3

Game Result
Game 1 Hawks 128, 76ers 124
Game 2 76ers 118, Hawks 102
Game 3 76ers 127, Hawks 111
Game 4 Hawks 103, 76ers 100
Game 5 Hawks 109, 76ers 106
Game 6 76ers 104, Hawks 99
Game 7 Hawks 103, 76ers 96

(2) Nets vs. (3) Bucks: Milwaukee wins 4-3

Game Result
Game 1 Nets 115, Bucks 107
Game 2 Nets 125, Bucks 86
Game 3 Bucks 86, Nets 83
Game 4 Bucks 107, Nets 96
Game 5 Nets 114, Bucks 108
Game 6 Bucks 104, Nets 89
Game 7 Bucks 115, Nets 111 (OT)

Western Conference second-round results

(1) Jazz vs. (4) Clippers: Los Angeles wins 4-2

Game Result
Game 1 Jazz 112, Clippers 109
Game 2 Jazz 117, Clippers 111
Game 3 Clippers 132, Jazz 106
Game 4 Clippers 118, Jazz 104
Game 5 Clippers 119, Jazz 111
Game 6 Clippers 131, Jazz 119

(2) Suns vs. (3) Nuggets: Phoenix wins 4-0

Game Result
Game 1 Suns 122, Nuggets 105
Game 2 Suns 123, Nuggets 98
Game 3 Suns 116, Nuggets 102
Game 4 Suns 125, Nuggets 118

Eastern Conference first-round results

(1) 76ers vs. (8) Wizards: Philadelphia wins 4-1

Game Result
Game 1 76ers 125, Wizards 118
Game 2 76ers 120, Wizards 95
Game 3 76ers 132, Wizards 103
Game 4 Wizards 122, 76ers 114
Game 5 76ers 129, Wizards 112

(2) Nets vs. (7) Celtics: Brooklyn wins 4-1

Game Result
Game 1 Nets 104, Celtics 93
Game 2 Nets 130, Celtics 108
Game 3 Celtics 125, Nets 119
Game 4 Nets 141, Celtics 126
Game 5 Nets 123, Celtics 109

(3) Bucks vs. (6) Heat: Milwaukee wins 4-0

Game Result
Game 1 Bucks 109, Heat 107 (OT)
Game 2 Bucks 132, Heat 98
Game 3 Bucks 113, Heat 84
Game 4 Bucks 120, Heat 103

(4) Knicks vs. (5) Hawks: Atlanta wins 4-1

Game Result
Game 1 Hawks 107, Knicks 105
Game 2 Knicks 101, Hawks 92
Game 3 Hawks 105, Knicks 94
Game 4 Hawks 113, Knicks 96
Game 5 Hawks 103, Knicks 89

Western Conference first-round results

(1) Jazz vs. (8) Grizzlies: Utah wins 4-1

Game Result
Game 1 Grizzlies 112, Jazz 109
Game 2 Jazz 141, Grizzlies 129
Game 3 Jazz 121, Grizzlies 111
Game 4 Jazz 120, Grizzlies 113
Game 5 Jazz 126, Grizzlies 110

(2) Suns vs. (7) Lakers: Phoenix wins 4-2

Game Result
Game 1 Suns 99, Lakers 90
Game 2 Lakers 109, Suns 102
Game 3 Lakers 109, Suns 95
Game 4 Suns 100, Lakers 92
Game 5 Suns 115, Lakers 85
Game 6 Suns 113, Lakers 100

(3) Nuggets vs. (6) Trail Blazers: Denver wins 4-2

Game Result
Game 1 Trail Blazers 123, Nuggets 109
Game 2 Nuggets 128, Trail Blazers 109
Game 3 Nuggets 120, Trail Blazers 115
Game 4 Trail Blazers 115, Nuggets 95
Game 5 Nuggets 147, Trail Blazers 140 (2OT)
Game 6 Nuggets 126, Trail Blazers 115

(4) Clippers vs. (5) Mavericks: Los Angeles wins 4-3

Game Result
Game 1 Mavericks 113, Clippers 103
Game 2 Mavericks 127, Clippers 121
Game 3 Clippers 118, Mavericks 108
Game 4 Clippers 106, Mavericks 81
Game 5 Mavericks 105, Clippers 100
Game 6 Clippers 104, Mavericks 97
Game 7 Clippers 126, Mavericks 111
Categories
Science

Closing the hole on the lacking lithium – Watts Up With That?

Researchers account for some of the lithium missing from our universe

UNIVERSITY OF TOKYO

Research News

IMAGE: AS A BEAM OF BERYLLIUM COMES IN FROM THE LEFT, THE DEUTERON TROJAN HORSE INTERCEPTS IT AT THE TARGET AND DELIVERS ITS NEUTRON SOLDIER. THIS ALLOWS THE DECAY PRODUCTS OF… view more CREDIT: ©2021 HAYAKAWA ET AL.

There is a significant discrepancy between theoretical and observed amounts of lithium in our universe. This is known as the cosmological lithium problem, and it has plagued cosmologists for decades. Now, researchers have reduced this discrepancy by around 10%, thanks to a new experiment on the nuclear processes responsible for the creation of lithium. This research could point the way to a more complete understanding of the early universe.

There is a famous saying that, “In theory, theory and practice are the same. In practice, they are not.” This holds true in every academic domain, but it’s especially common in cosmology, the study of the entire universe, where what we think we should see and what we really see doesn’t always match up. This is largely because many cosmological phenomena are difficult to study due to inaccessibility. Cosmological phenomena are usually out of our reach because of the extreme distances involved, or often they have occurred before the human brain had even evolved to worry about them in the first place — such is the case with the big bang.

Project Assistant Professor Seiya Hayakawa and Lecturer Hidetoshi Yamaguchi from the Center for Nuclear Study at the University of Tokyo, and their international team are especially interested in one area of cosmology where theory and observation are very misaligned, and that is the issue of the missing lithium, the cosmological lithium problem (CLP). In a nutshell, theory predicts that in the minutes following the big bang that created all matter in the cosmos, there should be an abundance of lithium around three times greater than what we actually observe. But Hayakawa and his team accounted for some of this discrepancy and have thus paved the way for research that may one day resolve it entirely.

“13.7 billion years ago, as matter coalesced from the energy of the big bang, common light elements we all recognize — hydrogen, helium, lithium and beryllium — formed in a process we call Big Bang nucleosynthesis (BBN),” said Hayakawa. “However, BBN is not a straightforward chain of events where one thing becomes another in sequence; it is actually a complex web of processes where a jumble of protons and neutrons builds up atomic nuclei, and some of these decay into other nuclei. For example, the abundance of one form of lithium, or isotope — lithium-7 — mostly results from the production and decay of beryllium-7. But it has either been overestimated in theory, underobserved in reality, or a combination of the two. This needs to be resolved in order to really understand what took place way back then.”

Lithium-7 is the most common isotope of lithium, accounting for 92.5% of all observed. However, even though the accepted models of BBN predict the relative amounts of all elements involved in BBN with extreme accuracy, the expected amount of lithium-7 is around three times greater than what is actually observed. This means there is a gap in our knowledge about the formation of the early universe. There are several theoretical and observational approaches which aim to resolve this, but Hayakawa and his team simulated conditions during BBN using particle beams, detectors and an observational method known as the Trojan horse.

“We scrutinized more than ever before one of the BBN reactions, where beryllium-7 and a neutron decay into lithium-7 and a proton. The resulting levels of lithium-7 abundance were slightly lower than anticipated, about 10% lower,” said Hayakawa. “This is a very difficult reaction to observe since beryllium-7 and neutrons are unstable. So we used deuteron, a hydrogen nucleus with an extra neutron, as a vessel to smuggle a neutron into a beryllium-7 beam without disturbing it. This is a unique technique, developed by an Italian group we collaborate with, in which the deuteron is like the Trojan horse in Greek myth, and the neutron is the soldier who sneaks into the impregnable city of Troy without tipping off the guards (destabilizing the sample). Thanks to the new experimental result, we can offer future theoretical researchers a slightly less daunting task when trying to resolve the CLP.”

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Journal article

S. Hayakawa, M. La Cognata, L. Lamia, H. Yamaguchi, D. Kahl, K. Abe, H. Shimizu, L. Yang, O. Beliuskina, S. M. Cha, K. Y. Chae, S. Cherubini, P. Figuera, Z. Ge, M. Gulino, J. Hu, A. Inoue, N. Iwasa, A. Kim, D. Kim, G. Kiss, S. Kubono, M. La Commara, M. Lattuada, E. J. Lee, J. Y. Moon, S. Palmerini, C. Parascandolo, S. Y. Park, V. H. Phong, D. Pierroutsakou, R. G. Pizzone, G. G. Rapisarda, S. Romano, C. Spitaleri, X. D. Tang, O. Trippella, A. Tumino, and N. T. Zhang, “Constraining the Primordial Lithium Abundance: New Cross-Section Measurement of the 7Be + n Reactions Updates the Total 7Be Destruction Rate” Astrophysical Journal Letters,

Funding

This works was supported by JSPS KAKENHI (Grant Nos. 15K17631, 18K13556 and 19K03883). K. Y. C. and S. M. C. were supported by National Research Foundation of Korea (Nos. 2020R1I1A1A01065120, 2020R1A2C1005981, 2019K2A9A2A10018827, and 2016R1A5A1013277). D. K. would like to thank the UK STFC for support. G. G. K. acknowledges the supports by NKFIH (NN128072) and from the Janos Bolyai research fellowship of the Hungarian Academy of Sciences and from UNKP-20-5-DE-2 New National Excellence Program of the Ministry of Human Capacities of Hungary. The authors acknowledge Finanziamenti di Linea 2 and Starting Grant 2020 by University of Catania.

Useful links

Center for Nuclear Study
Istituto Nazionale di Fisica Nucleare – Laboratori Nazionali del Sud
Department of Physics, Sungkyunkwan University

From EurekAlert!

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