Three Sheets To The Wind Synonym: Cheese Clipart Black And White Photography

July 21, 2024, 6:46 am

Huge amounts of seawater sink at known downwelling sites every winter, with the water heading south when it reaches the bottom. The system allows for large urban populations in the best of times, but not in the case of widespread disruptions. The same thing happens in the Labrador Sea between Canada and the southern tip of Greenland.

  1. Define 3 sheets to the wind
  2. Three sheets in the wind meaning
  3. Meaning of 3 sheets to the wind
  4. The sheet in 3 sheets to the wind crossword answer
  5. What is three sheets to the wind
  6. What is 3 sheets to the wind
  7. Three sheets to the wind synonym
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Define 3 Sheets To The Wind

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. Paleoclimatic records reveal that any notion we may once have had that the climate will remain the same unless pollution changes it is wishful thinking. 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. N. London and Paris are close to the 49°N line that, west of the Great Lakes, separates the United States from Canada. 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. 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. The last abrupt cooling, the Younger Dryas, drastically altered Europe's climate as far east as Ukraine. Things had been warming up, and half the ice sheets covering Europe and Canada had already melted. We need heat in the right places, such as the Greenland Sea, and not in others right next door, such as Greenland itself. Three sheets in the wind meaning. There is also a great deal of unsalted water in Greenland's glaciers, just uphill from the major salt sinks. 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. Yet another precursor, as Henry Stommel suggested in 1961, would be the addition of fresh water to the ocean surface, diluting the salt-heavy surface waters before they became unstable enough to start sinking. But we may be able to do something to delay an abrupt cooling.

Three Sheets In The Wind Meaning

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. In late winter the heavy surface waters sink en masse. Tropical swamps decrease their production of methane at the same time that Europe cools, and the Gobi Desert whips much more dust into the air. Once the dam is breached, the rushing waters erode an ever wider and deeper path. 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. Three sheets to the wind synonym. The North Atlantic Current is certainly something big, with the flow of about a hundred Amazon Rivers.

Meaning Of 3 Sheets To The Wind

Then, about 11, 400 years ago, things suddenly warmed up again, and the earliest agricultural villages were established in the Middle East. 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. Oslo is nearly at 60°N, as are Stockholm, Helsinki, and St. The sheet in 3 sheets to the wind crossword answer. Petersburg; continue due east and you'll encounter Anchorage. A lake formed, rising higher and higher—up to the height of an eight-story building.

The Sheet In 3 Sheets To The Wind Crossword Answer

It keeps northern Europe about nine to eighteen degrees warmer in the winter than comparable latitudes elsewhere—except when it fails. Like bus routes or conveyor belts, ocean currents must have a return loop. Many ice sheets had already half melted, dumping a lot of fresh water into the ocean. 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. The last time an abrupt cooling occurred was in the midst of global warming. Futurists have learned to bracket the future with alternative scenarios, each of which captures important features that cluster together, each of which is compact enough to be seen as a narrative on a human scale. This produces a heat bonus of perhaps 30 percent beyond the heat provided by direct sunlight to these seas, accounting for the mild winters downwind, in northern Europe. By 250, 000 years ago Homo erectushad died out, after a run of almost two million years. 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. We must look at arriving sunlight and departing light and heat, not merely regional shifts on earth, to account for changes in the temperature balance.

What Is Three Sheets To The Wind

Europe's climate, obviously, is not like that of North America or Asia at the same latitudes. Water falling as snow on Greenland carries an isotopic "fingerprint" of what the temperature was like en route. 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. 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. In almost four decades of subsequent research Henry Stommel's theory has only been enhanced, not seriously challenged.

What Is 3 Sheets To The Wind

Subarctic ocean currents were reaching the southern California coastline, and Santa Barbara must have been as cold as Juneau is now. Thermostats tend to activate heating or cooling mechanisms abruptly—also an example of a system that pushes back. Ways to postpone such a climatic shift are conceivable, however—old-fashioned dam-and-ditch construction in critical locations might even work. Light switches abruptly change mode when nudged hard enough. 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. These blobs, pushed down by annual repetitions of these late-winter events, flow south, down near the bottom of the Atlantic. And it sometimes changes its route dramatically, much as a bus route can be truncated into a shorter loop. This major change in ocean circulation, along with a climate that had already been slowly cooling for millions of years, led not only to ice accumulation most of the time but also to climatic instability, with flips every few thousand years or so. With the population crash spread out over a decade, there would be ample opportunity for civilization's institutions to be torn apart and for hatreds to build, as armies tried to grab remaining resources simply to feed the people in their own countries. 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. 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. If blocked by ice dams, fjords make perfect reservoirs for meltwater. 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. 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.

Three Sheets To The Wind Synonym

When there has been a lot of evaporation, surface waters are saltier than usual. Three scenarios for the next climatic phase might be called population crash, cheap fix, and muddling through. The return to ice-age temperatures lasted 1, 300 years. Perish in the act: Those who will not act. This warm water then flows up the Norwegian coast, with a westward branch warming Greenland's tip, at 60°N. Surprisingly, it may prove possible to prevent flip-flops in the climate—even by means of low-tech schemes. 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. A remarkable amount of specious reasoning is often encountered when we contemplate reducing carbon-dioxide emissions.

Fatalism, in other words, might well be foolish. An abrupt cooling could happen now, and the world might not warm up again for a long time: it looks as if the last warm period, having lasted 13, 000 years, came to an end with an abrupt, prolonged cooling. Canada's agriculture supports about 28 million people. "Southerly" Rome lies near the same latitude, 42°N, as "northerly" Chicago—and the most northerly major city in Asia is Beijing, near 40°. Fortunately, big parallel computers have proved useful for both global climate modeling and detailed modeling of ocean circulation. 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. Flying above the clouds often presents an interesting picture when there are mountains below. 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. 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 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. Further investigation might lead to revisions in such mechanistic explanations, but the result of adding fresh water to the ocean surface is pretty standard physics. There seems to be no way of escaping the conclusion that global climate flips occur frequently and abruptly. In places this frozen fresh water descends from the highlands in a wavy staircase. Glaciers pushing out into the ocean usually break off in chunks. 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. In discussing the ice ages there is a tendency to think of warm as good—and therefore of warming as better.

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