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Mon, 08 Jul 2024 15:19:42 +0000But we can't assume that anything like this will counteract our longer-term flurry of carbon-dioxide emissions. 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. The sheet in 3 sheets to the wind crossword. Were fjord floods causing flushing to fail, because the downwelling sites were fairly close to the fjords, it is obvious that we could solve the problem. Salt circulates, because evaporation up north causes it to sink and be carried south by deep currents. 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. Salt sinking on such a grand scale in the Nordic Seas causes warm water to flow much farther north than it might otherwise do.
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Rather than a vigorous program of studying regional climatic change, we see the shortsighted preaching of cheaper government at any cost. Water is densest at about 39°F (a typical refrigerator setting—anything that you take out of the refrigerator, whether you place it on the kitchen counter or move it to the freezer, is going to expand a little). We could go back to ice-age temperatures within a decade—and judging from recent discoveries, an abrupt cooling could be triggered by our current global-warming trend. Oslo is nearly at 60°N, as are Stockholm, Helsinki, and St. Petersburg; continue due east and you'll encounter Anchorage. Because water vapor is the most powerful greenhouse gas, this decrease in average humidity would cool things globally. The sheet in 3 sheets to the wind crosswords eclipsecrossword. 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. Greenland looks like that, even on a cloudless day—but the great white mass between the occasional punctuations is an ice sheet. Canada lacks Europe's winter warmth and rainfall, because it has no equivalent of the North Atlantic Current to preheat its eastbound weather systems. The same thing happens in the Labrador Sea between Canada and the southern tip of Greenland.
The U. S. Geological Survey took old lake-bed cores out of storage and re-examined them. 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. 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. Meaning of 3 sheets to the wind. I call the colder one the "low state. " Sudden onset, sudden recovery—this is why I use the word "flip-flop" to describe these climate changes. Near a threshold one can sometimes observe abortive responses, rather like the act of stepping back onto a curb several times before finally running across a busy street. Twice a year they sink, carrying their load of atmospheric gases downward. Water falling as snow on Greenland carries an isotopic "fingerprint" of what the temperature was like en route.Meaning Of 3 Sheets To The Wind
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. A lake surface cooling down in the autumn will eventually sink into the less-dense-because-warmer waters below, mixing things up. 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. When there has been a lot of evaporation, surface waters are saltier than usual. Europe is an anomaly. 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. Out of the sea of undulating white clouds mountain peaks stick up like islands. North-south ocean currents help to redistribute equatorial heat into the temperate zones, supplementing the heat transfer by winds. The back and forth of the ice started 2. 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.
Twenty thousand years ago a similar ice sheet lay atop the Baltic Sea and the land surrounding it. Many ice sheets had already half melted, dumping a lot of fresh water into the ocean. Of this much we're sure: global climate flip-flops have frequently happened in the past, and they're likely to happen again. Its snout ran into the opposite side, blocking the fjord with an ice dam. History is full of withdrawals from knowledge-seeking, whether for reasons of fundamentalism, fatalism, or "government lite" economics. The North Atlantic Current is certainly something big, with the flow of about a hundred Amazon Rivers. The cold, dry winds blowing eastward off Canada evaporate the surface waters of the North Atlantic Current, and leave behind all their salt. Natural disasters such as hurricanes and earthquakes are less troubling than abrupt coolings for two reasons: they're short (the recovery period starts the next day) and they're local or regional (unaffected citizens can help the overwhelmed). If Europe had weather like Canada's, it could feed only one out of twenty-three present-day Europeans. When the ice cores demonstrated the abrupt onset of the Younger Dryas, researchers wanted to know how widespread this event was. Only the most naive gamblers bet against physics, and only the most irresponsible bet with their grandchildren's resources. The last abrupt cooling, the Younger Dryas, drastically altered Europe's climate as far east as Ukraine. 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.
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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. The scale of the response will be far beyond the bounds of regulation—more like when excess warming triggers fire extinguishers in the ceiling, ruining the contents of the room while cooling them down. They are utterly unlike the changes that one would expect from accumulating carbon dioxide or the setting adrift of ice shelves from Antarctica. In an abrupt cooling the problem would get worse for decades, and much of the earth would be affected. Indeed, were another climate flip to begin next year, we'd probably complain first about the drought, along with unusually cold winters in Europe. A lake formed, rising higher and higher—up to the height of an eight-story building. Increasing amounts of sea ice and clouds could reflect more sunlight back into space, but the geochemist Wallace Broecker suggests that a major greenhouse gas is disturbed by the failure of the salt conveyor, and that this affects the amount of heat retained. That, in turn, makes the air drier. The return to ice-age temperatures lasted 1, 300 years. It has excellent soils, and largely grows its own food. 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). 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. 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.
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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