Murray Beats Fellow Vet Wawrinka In Cincy S Playoff – The Sheet In 3 Sheets To The Wind Crossword

'There is part of it I think when you announce that you're retiring that I would imagine psychologically it's quite difficult, as well. "He was a little bit sharper than me out there. Serena Williams: The career of a tennis icon.

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Murray took the opening set in a tie-break before seeing age-old rival Wawrinka level the contest as muscle cramps took their toll on the 35-year-old. I got unfortunate with the ab injury, which was not bad but it was enough to sort of disrupt me in the buildup to that, " Murray said after the match. Croatian Marin Cilic's resurgent season continued with a routine 6-3 6-3 win over Jaume Munar and Argentine Diego Schwartzman found his form late to beat Alex Molcan 5-7 6-4 6-2. Sign up for our emails. The week after Madrid takes the players back to sea level for the season's third and final Masters 1000 event on clay. Although the contrast between yellow balls and the blue background was wonderful for television, the bleached-then-dyed clay particles created a treacherously slippery surface. Defense alone, though, is not sufficient to guarantee wins. US Open: Andy Murray sweat tests come back clear as cause of cramp remains unknown ahead ahead of Flushing Meadows | Tennis News. Dimitrov won 27 of his 31 first serve points in his 6-3 6-3 win over Andrew Harris in the first round. Today, in the words of Nadal's characteristically blunt uncle and first coach, Toni Nadal, "Rafael is not a tennis player but an injured person who plays tennis. Playing with a bazooka-hitting style similar to Khachanov's, Basilashvili is capable of playing wonderful matches en route to a Round of 16 finish or perhaps even a quarterfinal. In part because he has struggled with health issues, Khachanov opened 2019 with relatively weak results. Twenty-two-year-old Karen Khachanov of Russia can be a joy to watch on a tennis court if one is not rooting for his opponent.

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What a Championships that promises to be next summer. The story of Djokovic - tennis' GOAT in waiting I News in brief. His match against Nadal on at the 2018 U. The "Prince of Clay" – Dominic Thiem. Nadal opened 2019 by reaching the Australian Open final without dropping a set only eleven weeks after pre-season ankle surgery. Stan Wawrinka to face Alex Bolt in busy Friday at the Murray River Open in Melbourne. Tournament: Open Parc Auvergne-Rhone-Alpes (Lyon). Former world number one Murray, 35, won 7-6 (7-3) 5-7 7-5 in the first-round match against his 37-year-old rival. He said: 'I think pretty much every tennis player in their career has cramped usually in these sorts of conditions that we have had [in Cincinnati]. "It's been a big surprise to me.

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Kyrgios fires sharp reply after being called out for slating rival. The unmatched topspin he applies to his shots, especially to his forehand with the distinctive "lariat" follow-through. Murray beats fellow vet wawrinka in cincy and nky. But he met his match in 18th-ranked Wawrinka, with the 34-year-old taking one hour and 59 minutes to edge closer to a first title since winning the Geneva Open in May 2017. Following his first round triumph, the Scot admitted he is feeling the best he has "in a really long time".

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Khachanov's blistering power and big serve have garnered him some impressive results. World number 18 Stan Wawrinka will face Australia's Alex Bolt before a possible quarter final clash against either Jeremy Chardy or Taylor Fritz. Norrie has since gone on to become a Top 15 staple four titles in the last two years—including the BNP Paribas Open last fall—and a maiden Wimbledon semifinal only three weeks ago. The slipperiness influences tactics (for example, it's especially profitable on clay to aim a shot behind a moving opponent) and profoundly affects a player's timing. Trivia: The "footprint" of space around Court Philippe Chatrier, the main stadium court, is the largest of any tournament court in the world. Agence France-Presse | Sunday September 27, 2020Opening day will see 2018 champion Simona Halep start her bid for a third major while 40-year-old Venus Williams kicks off her 23rd French Open. "I didn't play since the US Open, so to be in a final here after a month away is great for me. Frances Tiafoe has recorded one of his best wins this year by beating Italy's Matteo Berrettini in the opening round at the Cincinnati Masters. "It's just not been consistent enough and consistency is what matters over the course of the year. Leon Smith comments on Andy Murray's inclusion on GB David Cup team. Andy Murray beats Stan Wawrinka in Cincinnati to set up all-Scottish tie with Cameron Norrie. Consequently, it is much more difficult on clay than on a hard or grass court for a player to hit an unreturnable shot. And it became clear he will keep playing for as long as he can still land high-profile victories like this one. Both players were pushed deep into a third set in the opening round, but Norrie struggling against one of the game's most talented youngsters in Holger Rune is more understandable than Murray being outplayed for much of the match by fellow veteran Stan Wawrinka, who has won just three matches all year.

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That was an encouraging result, but it's too early to declare the streaky Shapovalov's slump over, while Paul's playing the best tennis of his career at the moment. Andy Murray wins thrilling veteran battle over Stan Wawrinka in Cincinnati. "It's not been easy these last few years to stay fit and healthy and play enough tennis to get matches to learn from and to build confidence and to get my body sort of physically like robust enough to compete week in, week out. Murray beats fellow vet wawrinka in cincy. Singles players: 48.

"But at least I know now it is more down to either conditioning or hydration or food-related. Murray has reached the final in each of the year's first three majors, losing to world number one Novak Djokovic in Australia and Paris before beating Milos Raonic at Wimbledon. Murray beats fellow vet wawrinka in cincy nc. Wawrinka earlier ended Italian teenager Jannik Sinner's fine run in Belgium, the Swiss veteran defeating the 18-year-old 6-3, 6-2 to reach his 30th career final. Meanwhile, the seventh-seeded Pegula has been cranking out deep runs consistently, reaching the semifinals or better in three of her last four WTA 1000 events. Former world number one Andy Murray reached his first final in more than two and a half years on Saturday and admitted it was a "big surprise".

The Scot will now go into that match, first up on Louis Armstrong Stadium on Monday, unsure as to the cause of his recent problems but is hopeful he will be ready to compete at the tournament where he broke his Grand Slam duck a decade ago. This will be the first action of the tournament for top-eight seeds, who had first-round byes, while all the other players had to win a main draw match to get to this point. 1 and two-time Grand Slam champion certainly has the talent to take out the recent Wimbledon champ here. Emma Raducanu will only become stronger for Wimbledon 2023. The Canadian player reached three ATP Tour finals in Rotterdam, Marseille and Cologne finishing runner-up each time in 2019 and scored 23 wins to 19 defeats. 16th-seeded Bulgarian Grigor Dimitrov was another round-of-64 casualty, beaten 7-6 (7-4) 6-3 by Denis Shapovalov of Canada. The men's clay tennis season opened in the week of April 8 with 250-level (i. e., fourth tier, if the Majors are first-tier) tournaments in Houston and Marrakech. Open and last month in Indian Wells). "I tried to take the ball on a little more and finish points at the net.

Any meltwater coming in behind the dam stayed there. History is full of withdrawals from knowledge-seeking, whether for reasons of fundamentalism, fatalism, or "government lite" economics. When the ice cores demonstrated the abrupt onset of the Younger Dryas, researchers wanted to know how widespread this event was. A gentle pull on a trigger may be ineffective, but there comes a pressure that will suddenly fire the gun. Counting those tree-ring-like layers in the ice cores shows that cooling came on as quickly as droughts. In Greenland a given year's snowfall is compacted into ice during the ensuing years, trapping air bubbles, and so paleoclimate researchers have been able to glimpse ancient climates in some detail. Thus we might dig a wide sea-level Panama Canal in stages, carefully managing the changeover. More rain falling in the northern oceans—exactly what is predicted as a result of global warming—could stop salt flushing. Three scenarios for the next climatic phase might be called population crash, cheap fix, and muddling through. Like bus routes or conveyor belts, ocean currents must have a return loop. What is three sheets to the wind. Though combating global warming is obviously on the agenda for preventing a cold flip, we could easily be blindsided by stability problems if we allow global warming per se to remain the main focus of our climate-change efforts. These northern ice sheets were as high as Greenland's mountains, obstacles sufficient to force the jet stream to make a detour.

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The fjords of Greenland offer some dramatic examples of the possibilities for freshwater floods. The sheet in 3 sheets to the wind crossword clue. A cheap-fix scenario, such as building or bombing a dam, presumes that we know enough to prevent trouble, or to nip a developing problem in the bud. The only reason that two percent of our population can feed the other 98 percent is that we have a well-developed system of transportation and middlemen—but it is not very robust. This was posited in 1797 by the Anglo-American physicist Sir Benjamin Thompson (later known, after he moved to Bavaria, as Count Rumford of the Holy Roman Empire), who also posited that, if merely to compensate, there would have to be a warmer northbound current as well. The last abrupt cooling, the Younger Dryas, drastically altered Europe's climate as far east as Ukraine.

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Timing could be everything, given the delayed effects from inch-per-second circulation patterns, but that, too, potentially has a low-tech solution: build dams across the major fjord systems and hold back the meltwater at critical times. Plummeting crop yields would cause some powerful countries to try to take over their neighbors or distant lands—if only because their armies, unpaid and lacking food, would go marauding, both at home and across the borders. Twenty thousand years ago a similar ice sheet lay atop the Baltic Sea and the land surrounding it. To keep a bistable system firmly in one state or the other, it should be kept away from the transition threshold. We have to discover what has made the climate of the past 8, 000 years relatively stable, and then figure out how to prop it up. Alas, further warming might well kick us out of the "high state. " It then crossed the Atlantic and passed near the Shetland Islands around 1976. Abortive responses and rapid chattering between modes are common problems in nonlinear systems with not quite enough oomph—the reason that old fluorescent lights flicker. Term 3 sheets to the wind. From there it was carried northward by the warm Norwegian Current, whereupon some of it swung west again to arrive off Greenland's east coast—where it had started its inch-per-second journey. In almost four decades of subsequent research Henry Stommel's theory has only been enhanced, not seriously challenged. Perish for that reason. Thermostats tend to activate heating or cooling mechanisms abruptly—also an example of a system that pushes back. The population-crash scenario is surely the most appalling. 5 million years ago, which is also when the ape-sized hominid brain began to develop into a fully human one, four times as large and reorganized for language, music, and chains of inference.

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Again, the difference between them amounts to nine to eighteen degrees—a range that may depend on how much ice there is to slow the responses. We need more well-trained people, bigger computers, more coring of the ocean floor and silted-up lakes, more ships to drag instrument packages through the depths, more instrumented buoys to study critical sites in detail, more satellites measuring regional variations in the sea surface, and perhaps some small-scale trial runs of interventions. Only the most naive gamblers bet against physics, and only the most irresponsible bet with their grandchildren's resources. Rather than a vigorous program of studying regional climatic change, we see the shortsighted preaching of cheaper government at any cost. There is also a great deal of unsalted water in Greenland's glaciers, just uphill from the major salt sinks. Of particular importance are combinations of climate variations—this winter, for example, we are experiencing both an El Niño and a North Atlantic Oscillation—because such combinations can add up to much more than the sum of their parts. Because such a cooling would occur too quickly for us to make readjustments in agricultural productivity and supply, it would be a potentially civilization-shattering affair, likely to cause an unprecedented population crash. We puzzle over oddities, such as the climate of Europe. They even show the flips. When this happens, something big, with worldwide connections, must be switching into a new mode of operation. In Broecker's view, failures of salt flushing cause a worldwide rearrangement of ocean currents, resulting in—and this is the speculative part—less evaporation from the tropics. At the same time that the Labrador Sea gets a lessening of the strong winds that aid salt sinking, Europe gets particularly cold winters.

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Flying above the clouds often presents an interesting picture when there are mountains below. Keeping the present climate from falling back into the low state will in any case be a lot easier than trying to reverse such a change after it has occurred. For a quarter century global-warming theorists have predicted that climate creep is going to occur and that we need to prevent greenhouse gases from warming things up, thereby raising the sea level, destroying habitats, intensifying storms, and forcing agricultural rearrangements. Up to this point in the story none of the broad conclusions is particularly speculative. When there has been a lot of evaporation, surface waters are saltier than usual. Canada's agriculture supports about 28 million people. But the ice ages aren't what they used to be. In discussing the ice ages there is a tendency to think of warm as good—and therefore of warming as better. When that annual flushing fails for some years, the conveyor belt stops moving and so heat stops flowing so far north—and apparently we're popped back into the low state. Unlike most ocean currents, the North Atlantic Current has a return loop that runs deep beneath the ocean surface. To see how ocean circulation might affect greenhouse gases, we must try to account quantitatively for important nonlinearities, ones in which little nudges provoke great responses. We can design for that in computer models of climate, just as architects design earthquake-resistant skyscrapers. Ancient lakes near the Pacific coast of the United States, it turned out, show a shift to cold-weather plant species at roughly the time when the Younger Dryas was changing German pine forests into scrublands like those of modern Siberia.

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Coring old lake beds and examining the types of pollen trapped in sediment layers led to the discovery, early in the twentieth century, of the Younger Dryas. To the long list of predicted consequences of global warming—stronger storms, methane release, habitat changes, ice-sheet melting, rising seas, stronger El Niños, killer heat waves—we must now add an abrupt, catastrophic cooling. Ways to postpone such a climatic shift are conceivable, however—old-fashioned dam-and-ditch construction in critical locations might even work. Thus the entire lake can empty quickly. I call the colder one the "low state. " In the Labrador Sea, flushing failed during the 1970s, was strong again by 1990, and is now declining. That increased quantities of greenhouse gases will lead to global warming is as solid a scientific prediction as can be found, but other things influence climate too, and some people try to escape confronting the consequences of our pumping more and more greenhouse gases into the atmosphere by supposing that something will come along miraculously to counteract them. There seems to be no way of escaping the conclusion that global climate flips occur frequently and abruptly.

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It's the high state that's good, and we may need to help prevent any sudden transition to the cold low state. But the regional record is poorly understood, and I know at least one reason why. Even the tropics cool down by about nine degrees during an abrupt cooling, and it is hard to imagine what in the past could have disturbed the whole earth's climate on this scale. That's how our warm period might end too. This cold period, known as the Younger Dryas, is named for the pollen of a tundra flower that turned up in a lake bed in Denmark when it shouldn't have. Computer models might not yet be able to predict what will happen if we tamper with downwelling sites, but this problem doesn't seem insoluble. We now know that there's nothing "glacially slow" about temperature change: superimposed on the gradual, long-term cycle have been dozens of abrupt warmings and coolings that lasted only centuries. By 1961 the oceanographer Henry Stommel, of the Woods Hole Oceanographic Institution, in Massachusetts, was beginning to worry that these warming currents might stop flowing if too much fresh water was added to the surface of the northern seas. Recovery would be very slow. Greenland's east coast has a profusion of fjords between 70°N and 80°N, including one that is the world's biggest. Oslo is nearly at 60°N, as are Stockholm, Helsinki, and St. Petersburg; continue due east and you'll encounter Anchorage. Water falling as snow on Greenland carries an isotopic "fingerprint" of what the temperature was like en route. And in the absence of a flushing mechanism to sink cooled surface waters and send them southward in the Atlantic, additional warm waters do not flow as far north to replenish the supply. Present-day Europe has more than 650 million people.

We must be careful not to think of an abrupt cooling in response to global warming as just another self-regulatory device, a control system for cooling things down when it gets too hot. Then, about 11, 400 years ago, things suddenly warmed up again, and the earliest agricultural villages were established in the Middle East. By 125, 000 years ago Homo sapienshad evolved from our ancestor species—so the whiplash climate changes of the last ice age affected people much like us. Fjords are long, narrow canyons, little arms of the sea reaching many miles inland; they were carved by great glaciers when the sea level was lower. Implementing it might cost no more, in relative terms, than building a medieval cathedral. Or divert eastern-Greenland meltwater to the less sensitive north and west coasts. We are in a warm period now. In 1970 it arrived in the Labrador Sea, where it prevented the usual salt sinking. We might, for example, anchor bargeloads of evaporation-enhancing surfactants (used in the southwest corner of the Dead Sea to speed potash production) upwind from critical downwelling sites, letting winds spread them over the ocean surface all winter, just to ensure later flushing. Within the ice sheets of Greenland are annual layers that provide a record of the gases present in the atmosphere and indicate the changes in air temperature over the past 250, 000 years—the period of the last two major ice ages. Temperature records suggest that there is some grand mechanism underlying all of this, and that it has two major states. "Southerly" Rome lies near the same latitude, 42°N, as "northerly" Chicago—and the most northerly major city in Asia is Beijing, near 40°. Perish in the act: Those who will not act. A meteor strike that killed most of the population in a month would not be as serious as an abrupt cooling that eventually killed just as many.

The last warm period abruptly terminated 13, 000 years after the abrupt warming that initiated it, and we've already gone 15, 000 years from a similar starting point. Suppose we had reports that winter salt flushing was confined to certain areas, that abrupt shifts in the past were associated with localized flushing failures, andthat one computer model after another suggested a solution that was likely to work even under a wide range of weather extremes. A lake formed, rising higher and higher—up to the height of an eight-story building.

Sat, 01 Jun 2024 00:15:09 +0000