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It keeps northern Europe about nine to eighteen degrees warmer in the winter than comparable latitudes elsewhere—except when it fails. Implementing it might cost no more, in relative terms, than building a medieval cathedral. 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. The sheet in 3 sheets to the wind crossword answers. An abrupt cooling got started 8, 200 years ago, but it aborted within a century, and the temperature changes since then have been gradual in comparison. 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. Thus we might dig a wide sea-level Panama Canal in stages, carefully managing the changeover. Then not only Europe but also, to everyone's surprise, the rest of the world gets chilled.

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Recovery would be very slow. This tends to stagger the imagination, immediately conjuring up visions of terraforming on a science-fiction scale—and so we shake our heads and say, "Better to fight global warming by consuming less, " and so forth. What paleoclimate and oceanography researchers know of the mechanisms underlying such a climate flip suggests that global warming could start one in several different ways. Seawater is more complicated, because salt content also helps to determine whether water floats or sinks. History is full of withdrawals from knowledge-seeking, whether for reasons of fundamentalism, fatalism, or "government lite" economics. Pollen cores are still a primary means of seeing what regional climates were doing, even though they suffer from poorer resolution than ice cores (worms churn the sediment, obscuring records of all but the longest-lasting temperature changes). Such a conveyor is needed because the Atlantic is saltier than the Pacific (the Pacific has twice as much water with which to dilute the salt carried in from rivers). Once the dam is breached, the rushing waters erode an ever wider and deeper path. In discussing the ice ages there is a tendency to think of warm as good—and therefore of warming as better. Flying above the clouds often presents an interesting picture when there are mountains below. The sheet in 3 sheets to the wind crossword clue. The last abrupt cooling, the Younger Dryas, drastically altered Europe's climate as far east as Ukraine. 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.

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In late winter the heavy surface waters sink en masse. 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. We may not have centuries to spare, but any economy in which two percent of the population produces all the food, as is the case in the United States today, has lots of resources and many options for reordering priorities. Any meltwater coming in behind the dam stayed there. But the regional record is poorly understood, and I know at least one reason why. Three sheets in the wind meaning. 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. 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. Five months after the ice dam at the Russell fjord formed, it broke, dumping a cubic mile of fresh water in only twenty-four hours. Change arising from some sources, such as volcanic eruptions, can be abrupt—but the climate doesn't flip back just as quickly centuries later. If Europe had weather like Canada's, it could feed only one out of twenty-three present-day Europeans. 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. Thermostats tend to activate heating or cooling mechanisms abruptly—also an example of a system that pushes back. A slightly exaggerated version of our present know-something-do-nothing state of affairs is know-nothing-do-nothing: a reduction in science as usual, further limiting our chances of discovering a way out.

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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. 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. The system allows for large urban populations in the best of times, but not in the case of widespread disruptions. So freshwater blobs drift, sometimes causing major trouble, and Greenland floods thus have the potential to stop the enormous heat transfer that keeps the North Atlantic Current going strong. 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. Stabilizing our flip-flopping climate is not a simple matter.

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Alas, further warming might well kick us out of the "high state. " We are in a warm period now. Feedbacks are what determine thresholds, where one mode flips into another. Europe's climate could become more like Siberia's. 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 need to make sure that no business-as-usual climate variation, such as an El Niño or the North Atlantic Oscillation, can push our climate onto the slippery slope and into an abrupt cooling.

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It has excellent soils, and largely grows its own food. The discovery of abrupt climate changes has been spread out over the past fifteen years, and is well known to readers of major scientific journals such as Scienceand abruptness data are convincing. 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. Then it was hoped that the abrupt flips were somehow caused by continental ice sheets, and thus would be unlikely to recur, because we now lack huge ice sheets over Canada and Northern Europe. Another sat on Hudson's Bay, and reached as far west as the foothills of the Rocky Mountains—where it pushed, head to head, against ice coming down from the Rockies. Whole sections of a glacier, lifted up by the tides, may snap off at the "hinge" and become icebergs. 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. Water falling as snow on Greenland carries an isotopic "fingerprint" of what the temperature was like en route. Civilizations accumulate knowledge, so we now know a lot about what has been going on, what has made us what we are. The U. S. Geological Survey took old lake-bed cores out of storage and re-examined them. 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. Door latches suddenly give way. In the first few years the climate could cool as much as it did during the misnamed Little Ice Age (a gradual cooling that lasted from the early Renaissance until the end of the nineteenth century), with tenfold greater changes over the next decade or two. 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.

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In 1970 it arrived in the Labrador Sea, where it prevented the usual salt sinking. Oslo is nearly at 60°N, as are Stockholm, Helsinki, and St. Petersburg; continue due east and you'll encounter Anchorage. The high state of climate seems to involve ocean currents that deliver an extraordinary amount of heat to the vicinity of Iceland and Norway. 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. But sometimes a glacial surge will act like an avalanche that blocks a road, as happened when Alaska's Hubbard glacier surged into the Russell fjord in May of 1986.

A remarkable amount of specious reasoning is often encountered when we contemplate reducing carbon-dioxide emissions. 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 ice ages aren't what they used to be. 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. One of the most shocking scientific realizations of all time has slowly been dawning on us: the earth's climate does great flip-flops every few thousand years, and with breathtaking speed. Its effects are clearly global too, inasmuch as it is part of a long "salt conveyor" current that extends through the southern oceans into the Pacific. We are near the end of a warm period in any event; ice ages return even without human influences on climate. Present-day Europe has more than 650 million people. It, too, has a salty waterfall, which pours the hypersaline bottom waters of the Nordic Seas (the Greenland Sea and the Norwegian Sea) south into the lower levels of the North Atlantic Ocean. Indeed, we've had an unprecedented period of climate stability. In places this frozen fresh water descends from the highlands in a wavy staircase. Counting those tree-ring-like layers in the ice cores shows that cooling came on as quickly as droughts. Any abrupt switch in climate would also disrupt food-supply routes. Glaciers pushing out into the ocean usually break off in chunks.

There seems to be no way of escaping the conclusion that global climate flips occur frequently and abruptly. 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. A lake surface cooling down in the autumn will eventually sink into the less-dense-because-warmer waters below, mixing things up. We need heat in the right places, such as the Greenland Sea, and not in others right next door, such as Greenland itself. The cold, dry winds blowing eastward off Canada evaporate the surface waters of the North Atlantic Current, and leave behind all their salt. Judging from the duration of the last warm period, we are probably near the end of the current one. The job is done by warm water flowing north from the tropics, as the eastbound Gulf Stream merges into the North Atlantic Current.

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In fact, some of the best looking corsages and boutonnieres feature other flowers like hydrangeas, orchids, lilies and dahlias. There's nothing wrong with making a bold statement by using bright colors mixed together in an unusual way that defies convention while still looking amazing! Prom corsage blue dress.

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