Discover emerging neighborhood talent in music, food, drinks, and the More. 2) Considering new sweet spot for subscriptions - e. g. lower hardware acquisition costs but higher subscription costs (why? The digital edition of The New York Times (NYT) is available for current students, staff, and faculty. You can play New York Times Mini Crossword online, but if you need it on your phone, you can download it from these links: Renaissance New York Times Square Hotel. If you're looking for a bigger, harder and full sized crossword, we also put all the answers for NYT Crossword Here, that could help you to solve them and If you ever have any problem with solutions or anything else, feel free to ask us in the comments. How to cancel membership the gym. Crossword clue NYT": Answer: ABDAY. If you want some other answer clues, check: NYT Mini January 12 2023 Answers. Here's the answer for "Crunch time at the gym?
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Ways to postpone such a climatic shift are conceivable, however—old-fashioned dam-and-ditch construction in critical locations might even work. There is, increasingly, international cooperation in response to catastrophe—but no country is going to be able to rely on a stored agricultural surplus for even a year, and any country will be reluctant to give away part of its surplus. Meaning of three sheets to the wind. They might not be the end of Homo sapiens—written knowledge and elementary education might well endure—but the world after such a population crash would certainly be full of despotic governments that hated their neighbors because of recent atrocities. Twice a year they sink, carrying their load of atmospheric gases downward. Whereas the familiar consequences of global warming will force expensive but gradual adjustments, the abrupt cooling promoted by man-made warming looks like a particularly efficient means of committing mass suicide.
When this happens, something big, with worldwide connections, must be switching into a new mode of operation. They even show the flips. 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. But just as vaccines and antibiotics presume much knowledge about diseases, their climatic equivalents presume much knowledge about oceans, atmospheres, and past climates. North-south ocean currents help to redistribute equatorial heat into the temperate zones, supplementing the heat transfer by winds. The sheet in 3 sheets to the wind crosswords eclipsecrossword. The fact that excess salt is flushed from surface waters has global implications, some of them recognized two centuries ago. Indeed, were another climate flip to begin next year, we'd probably complain first about the drought, along with unusually cold winters in Europe. Large-scale flushing at both those sites is certainly a highly variable process, and perhaps a somewhat fragile one as well. 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.
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. Or divert eastern-Greenland meltwater to the less sensitive north and west coasts. The saying three sheets to the wind. Perish for that reason. But the regional record is poorly understood, and I know at least one reason why. In the Labrador Sea, flushing failed during the 1970s, was strong again by 1990, and is now declining.
The Great Salinity Anomaly, a pool of semi-salty water derived from about 500 times as much unsalted water as that released by Russell Lake, was tracked from 1968 to 1982 as it moved south from Greenland's east coast. But our current warm-up, which started about 15, 000 years ago, began abruptly, with the temperature rising sharply while most of the ice was still present. Door latches suddenly give way. When there has been a lot of evaporation, surface waters are saltier than usual. These carry the North Atlantic's excess salt southward from the bottom of the Atlantic, around the tip of Africa, through the Indian Ocean, and up around the Pacific Ocean. A remarkable amount of specious reasoning is often encountered when we contemplate reducing carbon-dioxide emissions. At the same time that the Labrador Sea gets a lessening of the strong winds that aid salt sinking, Europe gets particularly cold winters. Just as an El Niño produces a hotter Equator in the Pacific Ocean and generates more atmospheric convection, so there might be a subnormal mode that decreases heat, convection, and evaporation. A lake surface cooling down in the autumn will eventually sink into the less-dense-because-warmer waters below, mixing things up. Present-day Europe has more than 650 million people. For Europe to be as agriculturally productive as it is (it supports more than twice the population of the United States and Canada), all those cold, dry winds that blow eastward across the North Atlantic from Canada must somehow be warmed up.
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. 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. 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. Then not only Europe but also, to everyone's surprise, the rest of the world gets chilled. But to address how all these nonlinear mechanisms fit together—and what we might do to stabilize the climate—will require some speculation. Berlin is up at about 52°, Copenhagen and Moscow at about 56°.
A gentle pull on a trigger may be ineffective, but there comes a pressure that will suddenly fire the gun. Nothing like this happens in the Pacific Ocean, but the Pacific is nonetheless affected, because the sink in the Nordic Seas is part of a vast worldwide salt-conveyor belt. 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. By 250, 000 years ago Homo erectushad died out, after a run of almost two million years. The modern world is full of objects and systems that exhibit "bistable" modes, with thresholds for flipping. The back and forth of the ice started 2. Although the sun's energy output does flicker slightly, the likeliest reason for these abrupt flips is an intermittent problem in the North Atlantic Ocean, one that seems to trigger a major rearrangement of atmospheric circulation. A brief, large flood of fresh water might nudge us toward an abrupt cooling even if the dilution were insignificant when averaged over time. But we can't assume that anything like this will counteract our longer-term flurry of carbon-dioxide emissions. Thus the entire lake can empty quickly. They are utterly unlike the changes that one would expect from accumulating carbon dioxide or the setting adrift of ice shelves from Antarctica.
In 1970 it arrived in the Labrador Sea, where it prevented the usual salt sinking. The high state of climate seems to involve ocean currents that deliver an extraordinary amount of heat to the vicinity of Iceland and Norway. 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. Stabilizing our flip-flopping climate is not a simple matter.
Oslo is nearly at 60°N, as are Stockholm, Helsinki, and St. Petersburg; continue due east and you'll encounter Anchorage. Three scenarios for the next climatic phase might be called population crash, cheap fix, and muddling through. It was initially hoped that the abrupt warmings and coolings were just an oddity of Greenland's weather—but they have now been detected on a worldwide scale, and at about the same time. We might create a rain shadow, seeding clouds so that they dropped their unsalted water well upwind of a given year's critical flushing sites—a strategy that might be particularly important in view of the increased rainfall expected from global warming. "Southerly" Rome lies near the same latitude, 42°N, as "northerly" Chicago—and the most northerly major city in Asia is Beijing, near 40°. Now only Greenland's ice remains, but the abrupt cooling in the last warm period shows that a flip can occur in situations much like the present one. What could possibly halt the salt-conveyor belt that brings tropical heat so much farther north and limits the formation of ice sheets? It's happening right now:a North Atlantic Oscillation started in 1996. It has excellent soils, and largely grows its own food.