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The Discovery of Global Warming May 2011
Past Climate Cycles: Ice Age Speculations To understand climate change, the obvious first step would be to explain the colossal coming and going of ice ages. Scientists devised ingenious techniques to recover evidence from the distant past, first from deposits left on land, then also from sea floor sediments, and then still better by drilling deep into ice. These paleoclimatologists succeeded brilliantly, discovering a strangely regular pattern of glacial cycles. The pattern pointed to a surprising answer, so precise that some ventured to predict future changes. The timing of the cycles was apparently set by minor changes in sunlight caused by slow variations of the Earth's orbit. Just how that could regulate the ice ages remained uncertain, for the climate system turned out to be dauntingly complex. In particular, it turned out that"greenhouse" gases like carbon dioxide played a surprisingly powerful role in governing global climate. One lesson was clear: the system is delicately poised, so that a little stimulus might drive a great change. (There is a separate essay on shorter-term climate fluctuations, lasting a few years to a century or so, possibly related to Variations of the Sun.) Keywords: climate change, global warming, ice ages,greenhouse effect, CO2, carbon dioxide, methane, CH4, paleoclimate
| Subsections: Evidence and Speculations (to 1954) - Reliable Dates and Temperatures (1955-1971) -Theories Confirmed (1971-1980) - Glimpsing a Greenhouse Future (1980s to Present)
"The origin of these climatic trends... is a difficult subject: by long tradition the happy hunting ground for robust speculation, it suffers because so few can separate fact from fancy." — G.S. Callendar(1)
It was an incredible claim, yet the evidence was eloquent. The scraped-down rock beds, the boulders perched wildly out of place, the bizarre deposits of gravel found all around northern Europe and the northern United States, all these looked exactly like the effects of Alpine glaciers — only far, far larger. By the late 19th century, after passionate debate, most scientists accepted the incredible. Long ago (although not very long as geological time went, for Stone Age humans had lived through it), northern regions had been buried kilometers deep in continental sheets of ice. This Ice Age stood as evidence of a prodigious climate change. | - LINKS - =>CO2 greenhouse
Toward the end of the 19th century, field studies by geologists turned up another fact, almost as surprising and controversial. There had been not one Ice Age but several. The stupendous ice sheets had slowly ground south and retreated, time and again. The series of glacial periods had alternated with times of warmer climate, each cycle lasting many tens of thousands of years. German geologists, meticulously studying the scars left by ancient rivers on what were now hillsides in the Alps, worked out a scheme of four major cycles.(1a) |
Geologists turned up evidence that the past few million years, during which the ice sheets cycled back and forth, was an unusual time in the Earth's history. They gave it a name of its own, the Pleistocene epoch. Before that there had been long eras of less turbulent climate, when fossils of tropical plants and animals had been deposited in regions that were now frigid. Much farther back there had been a few other relatively brief epochs of glaciation, revealed by very ancient ice-scraped rocks and gravel deposits. Most geologists concluded that the planet’s climate had at least two possible states. The most common condition was long temperate epochs, like the balmy times of the dinosaurs. Much rarer were glacial epochs like our own, lasting a few millions of years, in which periods of glaciation alternated with warmer "interglacial" periods like the present. This essay does not cover studies of the very remote past, before the Pleistocene. | =>CO2 greenhouse =>Simple models
What could explain the change from a warm to a glacial epoch, and the cycling of ice ages within a glacial epoch? A solution to the puzzle would bring deep satisfaction and eternal fame to whoever solved it. Perhaps the solution would also tell when the next ice age might descend upon humanity — and would reveal mechanisms that could produce other kinds of climate change.. |
Evidence and Speculations (to 1954) |
From the mid-19th to the mid-20th century, many theories were offered to explain the ice ages and other climate changes. None amounted to more than plausible hand-waving. Most favored were ideas about how the uplift of mountain ranges, or other reconfigurations of the Earth's surface, would alter the circulation of ocean currents and the pattern of winds. Other theories ranged from the extraterrestrial, such as a long-term cyclical variation of solar energy, to the deep Earth, such as massive volcanic eruptions. All these theories shared a problem. Given that something had put the Earth into a state conducive to glaciation, what made the ice sheets grow and then retreat, over and over again? None of the theories could readily explain the cycles. | Full discussion in <=Simple models <=Solar variation <=Aerosols =>Climatologists
Many things in the natural world come and go in cycles, so it was natural for people to suppose that there was a regular pattern to the ebb and flow of ice sheets. After all, there was evidence — convincing to many meteorologists, although doubted by as many more — that temperature and rainfall varied in regular cycles on human timescales of decades or centuries. The glacial periods of the ice ages likewise seemed to follow a cyclical pattern, on a far grander timescale. A series of repeated advances and retreats of the ice was visible in channels carved by glacial streams and in the fossil shorelines of lakes in regions that were now dry. If the pattern of advance and retreat could be measured and understood, it would give a crucial clue to the mystery of ice ages. | <=Chaos theory
Simple observations of surface features were joined by inventive methods for measuring what a region's climate had been like thousands or even millions of years ago. In particular, from the early 20th century forward, a few scientists in Sweden and elsewhere developed the study of ancient pollens ("palynology"). The tiny but amazingly durable pollen grains are as various as sea shells, with baroque lumps and apertures characteristic of the type of plant that produced them. One could dig up soil from lake beds or peat deposits, dissolve away in acids everything but the sturdy pollen, and after some hours at a microscope know what kinds of flowers, grasses or trees had lived in the neighborhood at the time the layer of lake-bed or peat was formed. That told scientists much about the ancient climate. We had no readings from rain gauges and thermometers 50,000 years ago, but pollen served as an accurate "proxy." |
Studying ancient pollens, scientists found again a sequence of colder and warmer spells, glacial and interglacial periods. The most recent ice age had ended ten thousand years or so ago. Other ingenious studies showed that a particularly warm period had followed. For example, fossil hoards of nuts collected by squirrels revealed that five thousand or so years ago, hazel trees had grown farther north in Sweden than at present. Were we drifting toward another ice age?(2) | <=>Rapid change
The problem that researchers set themselves was to find a pattern in the timing of the changes. Unfortunately, there were no tools to accurately determine dates so far in the past; any figure might be wrong by thousands of years. That did not stop people from seeing regular patterns. An example was a 1933 study of ancient beach deposits by W.M. Davis. As the continental ice sheets formed and then melted, they had locked up and then released so much water that the oceans had dropped and risen many tens of meters. Wave-carved fossil shores stood as testimony of the different sea levels. Davis believed he saw a pattern, in which the warm interglacial periods were long. Our own time seemed near to the preceding ice age, so he concluded that the Earth ought to get warmer for a while before it cooled again. When this was added to reports that the climate of the 1930s was measurably getting warmer, predictions appeared in Science magazine and in the public press that "The poles may become useful and inhabited places."(3) | <=>Public opinion
The pattern of past changes, no matter how accurately geologists might measure it, would always be suspect until a plausible theory explained it. Of all the proposed theories, only one was bound by its very nature to give regular cycles of change. This theory promised, moreover, to give the timing of past changes precisely from basic physical principles, and to predict future ice ages. The history of the measurement of ancient climates is inseparable from the history of this "astronomical" theory. |
In the mid 19th century, James Croll, a self-taught British amateur scientist, published calculations of how the gravitational pulls of the Sun, Moon, and planets subtly affect the Earth's motion and orientation. The inclination of the Earth's axis and the shape of its orbit around the Sun oscillate gently in cycles lasting tens of thousands or hundreds of thousands of years. During some periods the Northern Hemisphere would get slightly less sunlight during the winter than it would get during other centuries. Snow would accumulate. Croll argued that this would change the pattern of trade winds, leading to the deflection of warming currents like the Gulf Stream, and finally a self-sustaining ice age. The timing of such changes could be calculated exactly using classical mechanics (at least in principle, for the mathematics were thorny). Croll believed that the timing of the astronomical cycles, tens to hundreds of thousands of years long, roughly matched the timing of ice ages.(4*) | =>Simple models =>The oceans
Most scientists found Croll's ideas unconvincing, and his timing of the ice ages wholly wrong.(5) Nevertheless a few enthusiasts pursued his astronomical theory. It became almost plausible in the hands of the Serbian engineer Milutin Milankovitch. Working in the 1920s and 1930s, he not only improved the tedious calculations of the varying distances and angles of the Sun's radiation, but also applied an important new idea. Suppose there was a particular season when the sunlight falling in a given hemisphere was so weak, even in the summer, that the snow that fell in high latitudes in winter did not all melt away? It would build up, year after year. As others had pointed out, a covering of snow would reflect away enough sunlight to help keep a region cold, giving an amplifying feedback. Under such circumstances, a snowfield could grow over the centuries into a continental ice sheet. Milankovitch was encouraged by Wladimir Köppen, an eminent climatologist, who pointed out that the sensitive zone would lie between the latitudes of 55 and 65 degrees north (where moraines marked the edge of past continental ice sheets). Milankovitch ground through calculations for the slow variations of the angle that sunlight fell in that particular zone, especially in summer. Comparing the calculations with geological evidence for the timing of past ice ages, Köppen pronounced a good match.(6) | <=Simple models = Milestone
"The possibility of dating the varying episodes of the Pleistocene ice ages by correlating them with the [Milankovitch] radiation curve appealed to a number of workers," a meteorologist reported in 1940. "Correlations with the radiation curve were found everywhere."(7) It was also encouraging that even the tiny changes in solar radiation that came with the eleven-year sunspot cycle had some effect on weather — at least according to some studies. By the 1940s, some climate textbooks were teaching that Milankovitch's theory gave a plausible solution to the problem of timing the ice ages.(8) | <=Solar variation
Supporting evidence came from "varves," a Swedish word for the pairs of layers seen in the mud covering the bottom of northern lakes. Each year the spring runoff laid down a thin layer of silt followed by a settling of finer particles. From bogs and outcrops where the beds of fossil lakes were exposed, or cores of slick clay drilled out of living lakes, researchers painstakingly counted and measured the layers. Some reported finding a 21,000-year cycle of changes. That approximately matched the timing for a wobbling of the Earth's axis which Milankovitch had calculated as a crucial element (namely, the precession of the equinoxes, in fact a combination of 19,000- and 23,000-year cycles).(9) |
Most geologists, however, dismissed the astronomical theory. For contrary to the optimistic Köppen, they could not fit Milankovitch’s timing to the accepted sequence of four ice ages. A generation of geologists had laboriously constructed this sequence from studies around the world of surface features, such as the gravel deposits (moraines) that marked where glaciers had halted. The Milankovitch theory, wrote one authority condescendingly in 1957, had served a useful function as "a dogma of faith" that had stimulated research, but compared with the actual glacial record, the orbital chronology "must be stamped as illusory." Another problem lay in the fact that ice sheets had spread at the same time in the Northern and Southern Hemispheres. Since the astronomical theory relied upon an increase in the sunlight falling on one hemisphere along with a decrease on the other hemisphere, many experts considered the world-wide pattern of ice ages a devastating refutation.(10) Finally, there was a basic physical argument against the theory which seemed insurmountable. |
One reviewer — who had himself seen 21,000-year variations in lake deposits — explained at a 1952 conference that it was a problem of magnitudes. The computed variations in the angle and intensity of incoming sunlight were only tiny changes, "insufficient to explain the periods of glaciation."(11) Meanwhile, the studies that had found correlations between sunspot cycles and weather had all turned out wrong, giving an air of cranky unreliability to every connection between solar radiation variations and climate. That same year, a leading American planetary scientist wrote a European colleague to ask how the astronomical theory stood over there, remarking that "People I have consulted in this country... are not impressed by this work." His correspondent replied, "I have discussed the question of the appraisal of Milankovitch's theory with colleagues here. They are of the opinion that the theory cannot account for past changes. The effects are too small and the chronology of the occurrence of glaciation is so uncertain that any correspondence... appears fortuitous."(12) So what had caused the ice ages? That was still anybody's guess. | <=Solar variation
Reliable Dates and Temperatures (1955-1971) TOP OF PAGE |
The tool that would unlock the secret was constructed in the 1950s, although it took scientists a decade to make full use of it. This tool was radiocarbon dating. It could tell with surprising precision the age of features like a glacial moraine. You only needed to dig out fragments of trees or other organic material that had been buried thousands of years ago, and measure the fraction of the radioactive isotope carbon-14 in them. Of course researchers had to devise and test a number of laboratory techniques before they could get trustworthy results. Once that was done, they could assign a timescale to the climate fluctuations that had previously been sketched out by various traditional means. The best of these means, in the 1950s, was pollen science. The study of ancient climates had turned out to be invaluable for identifying strata as an aid to oil exploration, and that had paid for specialists who brought the technique to a high degree of refinement.(13) Carbon-14 measurements could now assign accurate dates to the palynologists’ tables of cool and warm periods in northern regions. For example, dating of lake deposits in the Western United States showed surprisingly regular cycles of drought and flood — which seemed to match the 21,000-year cycle predicted by Milankovitch. But other carbon-14 dates seemed altogether out of step with the Milankovitch timetable. | <=Carbon dates
The swift postwar development of nuclear science meanwhile fostered another highly promising technique. In 1947, the nuclear chemist Harold Urey discovered a way to measure ancient temperatures. The key was in the oxygen built into fossil sea shells. The amount of heavier or lighter oxygen isotopes that an organism took up from sea water varied according to the water's temperature when it was alive, so the ratio (O18/O16 ) served as a proxy thermometer.(14) This ingenious method was taken up by Cesare Emiliani, a geology student from Italy working in Urey's laboratory at the University of Chicago. Emiliani measured the oxygen isotopes in the microscopic shells of foraminifera, a kind of ocean plankton. Tracking the shells layer by layer in long cores of clay extracted from the seabed, he found a record of temperature variations. Emiliani's 1955 paper, a landmark of paleoclimatology, provided the world's first high-quality record of ice age temperatures.(15) | <=Uses of shells
Historians usually treat techniques as a stodgy foundation, unseen beneath the more exciting story of scientific ideas. Yet techniques are often crucial, and controversial. The stories of two especially important cases are explored in short essays on Uses of Radiocarbon Dating and Temperatures from Fossil Shells. |
Emiliani tentatively identified the rises and dips of temperatures with the geologists' traditional chronology of the past three glacial periods. His efforts were motivated largely by a desire to learn something about the evolution of the human race, which had surely been powerfully influenced by the climate shocks of the ice ages. But his results turned out to tell less about the causes of human evolution than about the causes of climate change. To get a timescale connecting the temperature changes with depth down the core, he made carbon-14 measurements covering the top few tens of thousands of years (farther back there was too little of the isotope to measure). That gave him an estimate for how fast sediments accumulated on the seabed at that point. Emiliani now found a rough correlation with the varying amount of sunlight that, according to Milankovitch's astronomical calculations, struck high northern latitudes in summer. To get the match he had to figure in a lag of about five thousand years. That seemed reasonable, considering how long it would take a mass of ice to react. "A causal connection is suggested but not proved," Emiliani concluded.(16*) |
The chemist Hans Suess, another graduate of Urey's lab, took the lead in improving the carbon-14 chronology. He reported, among other things, that the last ice age had come to a surprisingly abrupt end, starting sometime around 15,000 years ago. Looking farther back, Suess found hints of a roughly 40,000-year cycle, which sounded like the 41,000-year cycle that Milankovitch had computed for slight variations in the inclination of the Earth's axis.(17) Emiliani too, reporting a cycle of roughly 50,000 years, was increasingly confident that orbital changes set the timing of ice ages.(18) His curves, however, did not match up with the canonical four ice ages. | <=Carbon dates =>Rapid change
To resolve the issue, Emiliani began urging colleagues to launch a major program and pull up truly long cores, a hundred-meter record covering many hundreds of thousands of years. But for a long time the drillers' crude techniques were incapable of extracting long, undisturbed cores from the slimy ooze. As one of them remarked ruefully, "one does not make wood carvings with a butcher's knife."(19) |
In the early 1960s suggestive new evidence was dug up (literally) by the geochemist Wallace Broecker and collaborators. Ancient coral reefs were perched at various elevations above the present sea level on islands that geological forces were gradually uplifting. The fossil reefs gave witness to how sea level had risen and fallen as ice sheets built up on the continents and melted away. The coral could be dated by hacking out samples and measuring their uranium and other radioactive isotopes. These isotopes decayed over millennia on a timescale that had been accurately measured in nuclear laboratories. Unlike carbon-14, the decay was slow enough so there was still enough left to measure after hundreds of thousands of years. As a check, the sea level changes could be set alongside the oxygen-isotope temperature changes measured in deep-sea cores. Again the orbital cycles emerged, plainer than ever. At a conference on climate change held in Boulder, Colorado in 1965, Broecker announced that "The Milankovitch hypothesis can no longer be considered just an interesting curiosity."(20) People at the conference began to speculate on how the calculated changes in sunlight, although they seemed insignificantly small, might somehow trigger ice ages. That could happen if the climate system were so delicately balanced that a small push could prompt it to switch between different states. | <=>Chaos theory <=>The oceans <=>Rapid change
Meanwhile oceanographers managed to extract a fine set of cores that reached back more than 400,000 years. Analyzing the cores, Emiliani announced he could not make the data fit the traditional ice ages timetable at all. He rejected the entire scheme, painstakingly worked out around the end of the 19th century in Europe and accepted by generations of geologists, of a Pleistocene epoch comprising four major glacial advances alternating with long and equable interglacial periods. Emiliani said the interglacials had been briefer, and had been complicated by irregular rises and falls of temperature, making dozens of ice ages.(21) Many other scientists found his chronology dubious, but he defended his position tenaciously. Most significantly, he believed the sequence correlated rather well with the complex Milankovitch curve of summer sunlight at high northern latitude. Calculating how the cycle should continue in the future, in 1966 Emiliani predicted that "a new glaciation will begin within a few thousand years."(22) It was a step toward what would soon become widespread public concern about future cooling. | Deep-sea cores CLICK FOR FULL IMAGE =>Public opinion =>Modern temp's = Milestone
Seldom was such work straightforward. Geologists defended their traditional chronology passionately and skillfully. For a few years they held their ground, for it turned out that Emiliani's data on oxygen isotopes taken up in plankton shells did not directly measure ocean temperatures after all. Emiliani fiercely defended his position, but other workers in the late 1960s convinced the scientific community that he was mistaken. When water was withdrawn from the oceans to form continental ice sheets, the heavier and lighter isotopes evaporated and fell as rain or snow in different proportions. The way plankton absorbed oxygen at a given temperature mattered less than what proportion of each isotope was available in the sea water as ice sheets came and went. |
Yet in a deeper sense Emiliani was vindicated. Whatever the forces that changed the isotope ratio, its rise and fall did represent the coming and going of ice ages. "Emiliani's 'paleotemperature' curve," the new findings revealed, "...may be renamed a 'paleoglaciation' curve."(23*) |
These changes did turn out to correlate with ocean surface temperatures. New evidence for that came from scientists who took a census of the particular species of foraminifera, recognizing that the assemblage of different species varied with the temperature of the water where the animals had lived. The data confirmed that there had been dozens of major glaciations during the past couple of million years, not the four or so enshrined in textbooks. Corroborating evidence came from a wholly different type of record. In a brick-clay quarry in Czechoslovakia, George Kukla noticed how wind-blown dust had built up into deep layers of soil (what geologists call "loess"). Although Kukla could not get dates that matched Emiliani's, the multiple repetitions of advance and retreat of ice sheets were immediately visible in the colored bands of different types of loess. It was one of the few cases in this story where traditional field geology, tramping around with your eyes open, paid a big dividend. | <=Uses of shells =>Rapid change
In 1968, still more complete and convincing evidence came from an expedition that Broecker and a few others took to Barbados. Terraces of ancient coral covered much of the island, rising to hundreds of meters above the present sea level. The dates for when the coral reefs had been living (125,000, 105,000, and 82,000 years ago) closely matched dates from Milankovitch cycles for times when the ice sheets should have been melted and the seas at their highest (127,000, 106,000, and 82,000 years ago). The dating matched, that is, so long as one looked for the times when the maximum amount of sunlight struck a particular band of mid-northern latitudes during the summer. "The often-discredited hypothesis of Milankovitch," declared Broecker and his collaborators, "must be recognized as the number-one contender in the climatic sweepstakes."(24*) |
Since the Milankovitch cycles could be computed directly from celestial mechanics, one could project them forward in time, as Emiliani had done in 1966. In 1972, presenting more Caribbean cores, he again advised that "the present episode of amiable climate is coming to an end." Thus "we may soon be confronted with... a runaway glaciation." (He meant "soon" as geologists reckoned time, in centuries or millennia.) However, he added, greenhouse effect warming caused by human emissions might overwhelm the orbital shifts, so we might instead face "a runaway deglaciation."(25) |
Some other scientists agreed that the current interglacial warm period had peaked 6,000 or so years ago, and should be approaching its natural end. A prominent example was Kukla, continuing his study of loess layers in Czechoslovakia. He could now date the layers thanks to a new technique provided by other scientists. Geological and oceanographic studies had shown that over the course of millions of years, from time to time the Earth's entire magnetic field flipped: the North magnetic pole became the South magnetic pole and vice-versa. These reverses were recorded where layers of sediment or volcanic lava had entombed the direction of the magnetic field at the time. Geologists had worked out a chronology in lava flows, dated by the faint radioactivity of an isotope of potassium that decayed very slowly.(26) If even one magnetic-field reversal could be identified in any set of layers, it pinned down the timing of the entire sequence. When the loess layers were dated in this fashion, Milankovitch cycles turned up. Extrapolating the cycles into the future, Kukla thought the next shift to an ice age "is due very soon." (To geologists of the time, "very soon" meant within a few thousand years, although Kukla and a few others thought cooling might possibly become severe within a century or two.)(Link from below) (27) | <=External input =>Aerosols
If the climate experts of the time seem to have been a bit preoccupied with ice ages, that fitted their training and interests. For a hundred years their field had concerned itself above all with the ice ages. Their techniques, from pollen studies to sea floor drilling, were devoted to measuring the swings between warm and glacial epochs. Home at their desks, they occupied themselves with figuring how glacial-period climates had differed from the present, and attacking the grand challenge of explaining what might cause the swings. Now that they were beginning to turn their attention from the past to the future, the most natural meaning to attach to "climate change" was the next swing into cold.(28) |
In 1972, a group of leading glacial-epoch experts met at Brown University to discuss how and when the present warm interglacial period might end. A large majority agreed that "the natural end of our warm epoch is undoubtedly near." Near, that is, as geologists reckoned time. Unless there were impacts from future human activity, they thought that serious cooling "must be expected within the next few millennia or even centuries."(29) But many other scientists doubted these conclusions. They hesitated to accept the Milankovitch theory at all unless they could get definitive proof from some entirely different kind of evidence. | <=>Rapid change
Theories Confirmed (1971-1980) TOP OF PAGE |
The Greenland ice sheet is a daunting sight. Most investigators first come to it by air, past colossal bare cliffs where unimaginable quantities of ice pour down to the sea in a slow-motion flood. Beyond that the landscape rises and rises, over entire mountain ranges hidden under ice, to a limitless plain of gently undulating white. Greenland had played an important role in the 19th-century controversy over the ice ages. A few geologists had dared to postulate the existence, in the distant past, of seas of solid ice kilometers thick. Then astonished explorers of Greenland found just such a thing beneath their skis. | <=Simple models
In the late 1950s scientists came back to Greenland, hoping to find the key to the history of climate change. The logistics were arduous. But there was good support thanks to the International Geophysical Year — backed up by the United States government's concern to master the Arctic regions that lay on the shortest air routes to the Soviet Union. At Camp Century, Greenland, workers drilled short cores from the ice to demonstrate that it could be done. An improved drill, brought onto the ice in 1961, produced glistening cores 5 inches in diameter in segments several feet long. This was no small feat in a land where removing your gloves for a few minutes to adjust something might cost you the skin on your fingertips, if not entire fingers. After another five years of difficult work, organized by the U.S. Army's Cold Regions Research and Engineering Laboratory, the drill at Camp Century reached bedrock. The hole reached down some 1.4 kilometers (7/8 of a mile), bringing up ice as much as 100,000 years old.(30*) Two years later, in 1968, another long core of ancient ice was retrieved from a site even colder and more remote: Byrd Station in West Antarctica.(31) | <=International Camp Century <=>Rapid change
Much could be read from these cores. For example, individual layers with a lot of acidic dust pointed to past volcanic eruptions. Individual eruptions could be assigned dates simply by counting the annual layers of ice.(32) (Known eruptions like the destruction of Pompeii in the year 79 gave a check on the counts.) Farther down the layers became blurred, but approximate dates could still be assigned. Deep in the ice there were large amounts of mineral dust, evidence that during the last ice age the world had been windier, with storms carrying dust clear from China. Still better, ancient air had been trapped and preserved as bubbles in the ice, a million tiny time capsules packed with information about past climates. However, for a long time nobody could figure out how to extract and measure the fossil air reliably. | =>Aerosols <=>CO2 greenhouse
In the early years, the most useful work was done from the ice itself. The method had been worked out back in 1954 by an ingenious Danish scientist, Willi Dansgaard. He showed that the ratio of oxygen isotopes (O18/O16) in the ice measured the temperature of the clouds at the time the snow had fallen — the warmer the air, the more of the heavy isotope got into the ice crystals.(33) It was an exhilarating day for the researchers at Camp Century, making measurements along each cylinder of ice after it was pulled up from the borehole, when they saw the isotope ratios change and realized they had reached the last ice age. The preliminary study of the ice cores, published in 1969, showed variations that indicated an average temperature change of perhaps 10°C (that is, 18°F). Some cycles were tentatively identified, including one with a 13,000 year length.(34) Comparison of the Greenland and Antarctic cores showed that the climate changes were truly global, coming at essentially the same time in both hemispheres. That put a strict constraint on theories about the cause of cycles.(35) | <=Uses of shells
There is a supplementary site on the History of Greenland Ice Drilling, with some documentation of the U.S. "GISP" projects of the 1980s. |
Ice core studies also confirmed a feature that researchers had already noticed in deep-sea cores: the glacial cycle followed a sawtooth curve. In each cycle, a spurt of rapid warming was followed by a more gradual, irregular descent back into the cold over tens of thousands of years. A closer look showed that temperatures tended to cluster at the two ends of the curve. It seemed that the climate system had two fairly stable modes, brief warmth and more enduring cold, with relatively rapid shifts between them. Warm intervals like the past few thousand years normally did not last long.(36) Beyond such fascinating hints, however, the Greenland ice cores could say little about long-term cycles. They were too short to reach past a single glacial cycle. And the ice flowed like tar at great depths, confusing the record. In the 1970s, despite the arduous efforts of the ice drillers, the most reliable data were still coming from deep-sea cores. | <=Rapid change A glacial cycle =>Rapid change =>The oceans
That work too was strenuous and hazardous, manhandling long wet pipes on a heaving deck. Oceanographers (like ice drillers) lived close together for weeks or months at a time under Spartan conditions, far from their families. The teams might function smoothly — or not. Either way, the scientists labored long hours, for the problems were stimulating, the results could be exciting, and dedication to work seemed normal with everyone around them doing the same. | Deep-sea drilling
To make it worthwhile, scientists had to draw on all their knowledge and luck to find the right places to drill on the ocean bed. In these few places, layers of silt had built up unusually swiftly and steadily and without disturbance. Meanwhile, drilling techniques were finally worked out that could extract the continuous hundred-meter cores of clay that Emiliani had been asking for since the 1950s. Improved techniques for measuring the layers gave data good enough for thorough analysis. |
The most prominent feature turned out to be a 100,000-year cycle — evidently a key to the entire climate puzzle. Several earlier studies had tentatively identified this long-term cycle. Corroboration was in hand from Kukla's loess layers in Czechoslovakia, at the opposite end of the world from some of the deep-sea cores. Here too the 100,000-year cycle stood out.(37) |
Yet nobody could be entirely sure. Radiocarbon decayed too rapidly to give dates going back more than a few tens of thousands of years. A deeper timescale could only be estimated by measuring lengths down a core, and it was uncertain whether the sediments were laid down at a uniform rate. For a decade controversy had smoldered between Emiliani, as usual sticking by his original position, and other scientists who felt that his chronology was seriously in error. According to their data, the prominent cycle he had seen and attributed to the 41,000-year orbital shifts was actually the 100,000-year cycle.(38) Here again Emiliani had been bogged down by erroneous assumptions, yet somehow had muddled through to the fundamental truth that Milankovitch cycles were real. |
In 1973, Nicholas (Nick) Shackleton nailed it all down for certain. What made it possible was the new magnetic-reversal dates established by radioactive potassium, plus Shackleton's uncommon combination of technical expertise in different fields. A splendid deep-sea core had been pulled — "one of the best and most complete records of the entire Pleistocene that is known" — the famous core Vema 28-238 (named after the Lamont Observatory's oceanographic research vessel, a converted luxury yacht). It reached back over a million years, and included the most recent reversal of the Earth's magnetic field, which geologists dated at a bit over 700,000 years ago. This calibrated the chronology for the entire core. As a further benefit, Shackleton managed to extract and analyze the rare foraminifera that lived in the deep sea, and which reflected basic oceanic changes independent of the fluctuating sea-surface temperatures. The deep-sea forams showed the same isotopic variations as surface ones, confirming that the variations gave a record of the withdrawal of water to form ice sheets. When Shackleton showed his graph of long-term change to a roomful of climate scientists, a spontaneous cheer went up.(39*) | <=Climatologists
The core Vema 28-238 and a few others contained such a long run of consistent data that it was possible to analyze the numbers with a mathematically sophisticated "frequency-domain" calculation, a well-established technique for picking out the lengths of cycles in a set of data.(40) Detailed measurements and numerical calculations found a set of favored frequencies, a spectrum of regular cycles visible amid the noise of random fluctuations. The first unimpeachable results (well, almost unimpeachable) were achieved in 1976 by James Hays, John Imbrie and Shackleton. The trio not only analyzed the oxygen-isotope record in selected cores from the Indian Ocean, but checked their curves against temperatures deduced from the assemblage of foraminifera species found in each layer. | <=Uses of shells
The long cores proved beyond doubt what Emiliani had stoutly maintained — there had been not four major ice ages, but dozens. The analysis showed cycles with lengths roughly 20,000 and 40,000 years, and especially the very strong cycle around 100,000 years, all in agreement with Milankovitch calculations.(41) Extrapolating the curves ahead, the group predicted cooling for the next 20,000 years. As Emiliani, Kukla, and other specialists had already concluded several years earlier, the Earth was gradually — indeed, perhaps quite soon as geologists reckoned time — heading into a new ice age (see above). | =>Modern temp's =>Public opinion =>Rain-making =>Simple models = Milestone
These results, like so many in paleoclimatology, were promptly called into question.(42) For one thing, there was no solid reason to suppose that our current interglacial period would be of average length and was therefore nearing its end. (And in fact, as noted below, improved orbital calculations and paleoclimate data would eventually show that the natural end of the current interglacial is tens of thousands of years away.) But the main results withstood all criticism. Confirmation came from other scientists who likewise found cycles near twenty and forty thousand years, give or take a few thousand. The most impressive analysis remained the pioneering work of Hays, Imbrie, and Shackleton. They could even split the 20,000 year cycle into a pair of cycles with lengths of 19,000 and 23,000 years — exactly what the best new astronomical calculations predicted. By the late 1970s, most scientists were convinced that orbital variations acted as a "pacemaker" to set the timing of ice ages.(43) Science magazine reported in 1978 that the evidence for the Milankovitch theory was now "convincing," and the theory "has recently gained widespread acceptance as a factor" in climate change.(44) | =>Chaos theory
Yet the cause of the ice ages remained more a mystery than ever. How could the "pacemaker" possibly work? The variation in the intensity of sunlight that was computed for the 100,000-year astronomical cycle came from a minor change in orbital eccentricity — a slight stretching of the Earth's path around the sun out of a perfect circle. It was a particularly tiny variation; the changes it caused should be trivial compared with the shorter-term and larger orbital shifts, not to mention all the other influences on climate. Yet it was the 100,000-year cycle that dominated the record. Scientists began to turn from hunting down cycles to searching for the physical mechanisms that could make the climate system respond so dramatically to subtle changes in sunlight. As a reviewer admitted, "failures to support the Milankovitch theory may only reflect the inadequacies of the models."(45) A number of people took up the challenge, devising elaborate numerical models that took into account the sluggish dynamics of continental ice sheets. It seemed likely that eventually the modelers would produce a suite of feedbacks that would entirely explain the schedule of the ice ages. | <=Simple models
Glimpsing a Greenhouse Future (1980s to Present) TOP OF PAGE |
During the 1980s, the work advanced steadily with few surprises. Ocean drilling in particular, pursued on an international scale, produced ever better cores. A costly project dedicated to "spectral mapping" (SPECMAP) yielded a spectrum of cycles that matched the astronomical calculations with gratifying precision going back hundreds of millennia. Five separate cores confirmed that variations in the Earth's orbit drove the coming and going of ice ages.(46) But an unexpected finding brought in a new complication. The prominent 100,000-year cycle (due to changes in the orbit's eccentricity) had dominated climate change only during the most recent million years. During a long earlier phase of the Pleistocene epoch, the rise and decay of ice sheets had followed the 41,000-year cycle (related to shifts in the inclination of the Earth's axis).(47) Milankovitch and his followers had originally expected that this cycle would have a much stronger effect than the feeble 100,000-year shifts. They had recognized, however, that the 41,000-year variations in sunlight might still have been too small to cause ice ages without some kind of amplification. The experts understood that "the response characteristics of the Earth's climate system have themselves evolved," so that the details of cycling could well change.(48) The shift in the dominant cycle surely gave a clue, if an enigmatic one, to the variety of feedback mechanisms at work. | <=The oceans
Meanwhile ice drillers, reaching ever farther into the past at locations where the flow of ice in the depths did not introduce too much confusion, joined the deep-sea drillers as a main source of information. The ice and seabed climate curves were found to go up and down in fine agreement, and researchers began to combine data from both sources in a single discussion. The most striking news from the ice was evidence that the level of carbon dioxide gas (CO2) in the atmosphere had risen and fallen more or less in time with the temperature. |
The outstanding record was extracted by a French-Soviet team at the Soviets' Vostok Station in Antarctica. It was a truly heroic feat of technology, wrestling with drills stuck a kilometer down, at temperatures so low that a puff of breath fell to the ground in glittering crystals. Vostok had been established during the 1957-58 International Geophysical Year at the most remote spot on the planet. Supplies were brought once a year by a train of vehicles that clawed across hundreds of kilometers of ice. Underfunded and threadbare, the station was fueled by the typically Russian combination of cigarettes, vodka, and stubborn persistence. ("What do you do for recreation?" "Wash... you have a bath once every ten days.") At one point the generator failed; the crew survived by huddling in an ice cave heated by candles.(49) | Vostok, Antarctica
The effort paid off. While the Greenland record reached into the most recent ice age, by 1985 the Antarctic team had pulled up cores of ice stretching clear through the cold period and into the preceding warm period—a complete glacial cycle.(50) During the cold period, the CO2 level had been much lower than during the warm periods before and after. Indeed the curves of gas level and temperature tracked one another remarkably closely. Measurements in ice cores of an even more potent greenhouse gas, methane, showed a similar rise and fall that matched the rise and fall of temperature.(51) This work fulfilled the old dream that studying the different climates of the past could be almost like putting the Earth on a laboratory bench, switching conditions back and forth and observing the consequences. | <=CO2 greenhouse <=Other gases =>Venus & Mars =>Biosphere <=Government
The Vostok team pointed out that the swings in greenhouse gas levels might be amplifying the effect of the orbital shifts. A small rise or fall in temperature seemed likely to cause a rise or fall in the gas levels (for example, when seawater got warmer it would evaporate some CO2 into the atmosphere, whereas it would absorb the gas during a cooling period). More or less greenhouse gases in the atmosphere would make for further changes in temperature, which would in turn raise or lower the gas levels some more... and so on. It was the first truly plausible theory for how minor shifts of sunlight could make the entire planet's temperature lurch back and forth. | <=CO2 greenhouse
The changes in the atmosphere also answered the old persuasive objection to Milankovitch's theory — if the timing of ice ages was set by variations in the sunlight falling on a given hemisphere, why didn't the Southern Hemisphere get warmer as the Northern Hemisphere cooled, and vice-versa? The answer was that changes in atmospheric CO2 and methane physically linked the two hemispheres, powerfully warming or cooling the planet as a whole.(52*) | =>Simple models
Variations over 420,000 years of CO2, methane(CH4), and temperature, from the Vostok ice core after it reached bedrock (1999): four complete glacial cycles. Age in years Before Present, older to right. Adapted from Petit et al., Nature 399:429-36 (1999).
Looking at the rhythmic curves of past cycles, one could hardly resist the temptation to extrapolate into the future. By the late 1980s, most calculations had converged on the familiar prediction that the natural Milankovitch cycle should bring a mild but steady cooling over the next few thousand years. As climate models and studies of past ice ages improved, however, worries about a swift descent into the next great glaciation — what many in the 1970s had tentatively expected — died away. Improved calculations said that the next ice age would not come naturally within the next ten thousand years or so. The calculations were backed up in 2004 by data from a heroic new drilling effort in Antarctica that brought up ice spanning the past eight glacial cycles. Among these was an unusually long previous cycle where the orbital elements had been similar to those in our own cycle.(53*) |
The scientists who published these calculations always added a caveat. In the Antarctic record, atmospheric CO2 levels over the past 750,000 years had cycled between about 180 and 280 parts per million. The level in the late 20th century had now climbed above 370 and kept climbing. (The other main greenhouse gas, methane, was soaring even farther above any level seen in the long ice record.) Greenhouse warming and other human influences seemed strong enough to overwhelm any natural trend. One environmental scientist, William Ruddiman, even argued that the rise of human agriculture had already counteracted the gradual cooling that should have come during the past several thousand years in the normal descent from a post-glacial temperature peak.(53a) As emissions climbed exponentially, we might not only cancel the next ice age, but launch our planet into an altogether new climate regime. |
The ice cores themselves gave convincing evidence of the threat, according to analyses published in the early 1990s. The "climate sensitivity" — the response of temperature to changes in carbon dioxide — could be measured for the last glacial maximum. The answer was in the same range that computer models were predicting for our future, namely, a few degrees of warming if the CO2 level doubled. That raised confidence that the models could not be far wrong.(53b) | =>Models (GCMs) =>CO2 greenhouse
In climate science, where everything is subtle and complex, it is rare for an issue to be entirely settled. By the late 1980s, it did seem to be an established fact that ice ages were timed by orbital variations. But what kind of feedbacks amplified the effect? Some people challenged whether any of this was really understood. The cycles, most scientists now agreed, involved not only orbital variations in solar irradiation, but also a variety of geological effects. First came the massive creation, settling and flow of continental ice sheets, which naturally would work on a timescale of tens of thousands of years. But large-scale physical and chemical changes in the oceans might be important too. New evidence gave a particularly crucial role to changes in CO2 and other greenhouse gases, changes apparently driven not just by geochemistry and ocean circulation, but still more by changes in biological activity. And of course the biosphere depended in turn on climate — and not just temperature, but also trickier matters like fertilization of the seas by minerals eroded from glacial era deserts. Further unexpected influences were added to the list of possibilities almost every year.(54) It would take much more study to determine just what combination of effects determined the shape of glacial cycles. | <=CO2 greenhouse
In 1992, a more fundamental challenge was raised by the ingenious exploitation of a novel source of data: layers of calcite laid down in the desert oasis of Devils Hole, Nevada. The layers showed glacial and interglacial periods much like those seen in the ice cores. But the dating (using uranium isotopes) failed to agree with Milankovitch calculations. The authors suggested that the timing of ice ages followed no regular cycle at all, but was driven wholly by "internal nonlinear feedbacks within the atmosphere-ice sheet-ocean system."(55) A vigorous controversy followed, but in the end most climate scientists stuck by the Milankovitch theory. The Devils Hole measurements looked solid, but didn't they represent only a strictly local effect? |
By 2001 it was shown that the Nevada temperatures were indeed a local effect, related to currents in the Pacific Ocean. But the controversy had highlighted the value of new types of data and the complexities of the global system. As two experts reviewing the problem put it, "climate is too complicated to be predicted by a single parameter."(56) The faint variations of summer sunlight in Northern latitudes were effective only because the astronomical schedule somehow resonated with other factors — the dynamics of continental ice sheets and tropical ocean currents, the bio-geochemical CO2 system, and who knew what else. The more precise the data got, the less precise seemed the match between sunlight in the Northern Hemisphere and ice age cycles; probably Southern Hemisphere sunlight and other Milankovitch features played a role. Evidently when orbital effects served as a pacemaker, it was by adjusting the timing of greater forces working through their own complex cycles. As one reviewer said, "The sheer number of explanations for the 100,000-year cycle... seems to have dulled the scientific community into a semipermanent state of wariness about accepting any particular explanation."(57) | <=>Simple models
The grand puzzle of the ice ages stood only half solved — except insofar as scientists now understood that nobody would ever jump up with a neat single solution. There would instead be a long collective trudge through the intricacies of field data and models, gradually increasing our knowledge of all the interacting forces that drive climate cycles. The invaluable fruit of a century of ice ages research was the recognition of how complex and powerful all the feedbacks could be. |
An important clue came from some especially good ice core records that timed precisely the changes in the levels of CO2 and methane. The levels apparently rose or fell a few centuries after a rise or fall in temperature. At first this lag puzzled scientists, but they quickly realized that this was just what they should have expected. For it strongly confirmed that the Milankovitch-cycle orbital changes initiated a powerful feedback loop. The close of a glacial era came when a shift in sunlight caused a slight rise of temperature, and that evidently raised the gas levels over the next few centuries. The greenhouse effect then slowly drove the planet's temperature a bit higher, which drove a further rise in the gas levels... and so forth. On the other hand, when the sunlight in key latitudes weakened, that would not only bring more ice and snow, but also a shift from emission to absorption of gases, eventually causing a further fall in temperature... and so forth.(58) | =>CO2 greenhouse
Our current situation was altogether different. The warming was not started by a small shift of sunlight, as in previous epochs. Our addition of gases to the atmosphere was initiating the process, with the temperature rise lagging behind the rise of gas levels. Emissions were climbing at a far swifter rate than anything in the Pleistocene record, so the lag was measured not in centuries, but mere decades. And already by the 1980s the levels of greenhouse gases had climbed far higher than anything seen for many millions of years. Even if we stopped our emissions, would feedbacks drive things higher on their own? There were disturbing signs that feedbacks were indeed kicking in. Drying forests and warmer seawater were getting less efficient at taking CO2 out of the air, and methane was seen bubbling up from Arctic wetlands. | <=CO2 greenhouse
By the start of the 21st century, it was clear that the connection between global temperature and greenhouse gas levels was a major geological force. All through the Pleistocene, the greenhouse gas feedback had turned the planet's orbital cycles from minor climate variations to grand transformations that affected all life on the planet. The geological record gave a striking verification, with wholly independent methods and data, of the processes that computer models were predicting would bring a rapid and severe global warming — a disruption of climate exceeding anything seen since the emergence of the human species. | =>Models (GCMs)
RELATED: Home Simple Models of Climate The Carbon Dioxide Greenhouse Effect Changing Sun, Changing Climate Supplement: Temperatures from Fossil Shells
NOTES
1. Callendar (1961), p. 1. BACK 1a. The history is reviewed by Imbrie and Imbrie (1986); the scheme of four ice ages was propounded by Albrecht Penck, Penck and Brückner (1901-1909). BACK 2. Nuts: G. Andersson in 1902 as cited in Lamb (1977), p. 397; for the history overall, see Lamb pp. 193, 378ff. and Webb (1980). BACK 3. Davis (1933). BACK 4. Croll (1864); Croll (1875); Croll predicted glaciation when the Earth was at aphelion in winter. But summer aphelion (with the distant Sun less likely to melt the snow away) was more likely to do it, as pointed out by Murphy (1876); Croll (1886) defends his views; Imbrie and Imbrie (1979), pp. 77-88. BACK 5. For example, Arrhenius (1896), p. 274; Brooks (1922), p. 18-19. BACK 6. Milankovitch (1920) ; Milankovitch (1930), see pp. 118-21 for additional history; Milankovitch (1941) ; for this history I have used Imbrie and Imbrie (1986). BACK 7. Simpson (1939-40), p. 203. BACK 8. E.g., Landsberg (1941, rev. ed. 1947, 1960), pp. 191-92. BACK 9. Bradley (1929) ; Zeuner (1946 [4th ed., 1958]). BACK 10. "dogma... illusory," Öpik (1957); "This theory has been answered devastatingly by... Sir George Simpson," Wexler (1952), p. 74. BACK 11. van Woerkom (1953); see also Science Newsletter (1952); similarly, "the changes of solar radiation due to changes in the Earth's orbit are always too small to be of practical importance," Simpson (1939-40), p. 209. BACK 12. Kuiper to H. Sverdrup, 28 May 1952, and reply, 11 June 1952, Box 11, G.P. Kuiper files, Special Collections, U. Ariz., kindly reported to me by Ron Doel.; similarly, the theory "has failed utterly," Humphreys (1920), pp. 564-66, quote p. 568, on the Croll theory, but repeated without change in the 3rd (1940) edition, p. 586, without reference to Milankovitch. BACK 13. Faegri et al. (1964); Manten (1966). BACK 14. Urey (1947). BACK 15. Emiliani (1955); see Emiliani (1958). BACK 16. The effect was never expected to correlate with sunlight in the Southern Hemisphere, which is mostly ocean where snow would never accumulate. Emiliani (1955), p. 509; see also Emiliani (1958); on evolution, Emiliani (1958) p. 63. BACK 17. Suess (1956). BACK 18. Emiliani and Geiss (1959). BACK 19. Hsü (1992), pp. 30-32, 220. BACK 20. Quote: Broecker (1968), p. 139; for early work, see Broecker (1966). For a detailed account of this and following events see Broecker and Kunzig (2008), pp. 46-56. BACK 21. Emiliani (1966). BACK 22. Emiliani (1966). BACK 23. Dansgaard and Tauber (1969). Later work found many further refinements; any large change in precipitation or in ecosystems that processed oxygen would alter the oxygen-isotope ratio throughout the global atmosphere. For example, certain abrupt global climate changes thousands of years ago (Dansgaard-Oeschger events, see the essay on Ocean Currents) included large changes in monsoon rainfall over Asia, which produced noticeable isotope shifts, Severinghaus et al. (2009). BACK 24. "sweepstakes": Broecker et al. (1968) p. 300; as 125, 105, and 82,000 in Mesolella et al. (1969); see also summary in Broecker and van Donk (1970) .On this and the history of ice-age cycle observations in general see Broecker (2010), ch. 1. An important confirmation, using boreholes drilled in Barbados reefs now drowned, was Fairbanks and Matthews (1978); the objection that the sea level changes might be due to local uplift in Barbados, and not a world-wide phenomenon, was refuted by an expedition to another fine set of coral terraces on a rarely visited coast of New Guinea, Bloom et al. (1974); for discussion Berger (1988). BACK 25. Emiliani (1972). BACK 26. Glen (1982). BACK 27. Kukla and Kocí (1972), p. 383. BACK 28. Chambers and Brain (2002), p. 239. BACK 29. Kukla et al. (1972), p. 191; Kukla and Matthews (1972); "large majority" according to Flohn (1974), p. 385. BACK 30. The first long core (411m), using a drill developed by B. Lyle Hansen, was extracted at another site in Greenland in 1956: Dansgaard et al. (1973); for brief history and references, see also Langway et al. (1985); Levenson (1989) pp. 40-41; for a firsthand account, Alley (2000). BACK 31. Epstein et al. (1970). BACK 32. Hamilton and Seliga (1972). BACK 33. Dansgaard (1954); Dansgaard (1964); for further bibliography on gases in ice, see Broecker (1995), pp. 279-84. BACK 34. Dansgaard et al. (1969). Exciting day: oral history interview of Klaus Hammer by Finn Aaserud, 1993, GISP interviews, records of Study of Multi-Institutional Collaborations, AIP. Extensive autobiographical histories: Langway (2008), Dansgaard (2005). BACK 35. Epstein et al. (1970). BACK 36. Newell (1974); using results of Johnsen et al. (1972). BACK 37. Kukla and Kocí (1972); see Schneider and Londer (1984), p. 53. BACK 38. Broecker and van Donk (1970); cf. Ericson and Wollin (1968), using foram temperatures. BACK 39. Later revised to 780,000. Shackleton and Opdyke (1973), quote p. 40. They determined temperatures by oxygen isotopes. Opdyke did the magnetic work. Cheer: John Imbrie, oral history interview by Ron Doel, 1997, AIP; see Imbrie and Imbrie (1979), p. 164. BACK 40. For history and comments, see Imbrie (1982); Imbrie and Imbrie (1979). BACK 41. Hays et al. (1976); for other work, see Imbrie et al. (1975). BACK 42. Evans and Freeland (1977). BACK 43. Hays et al. (1976); Berger (1977); other data: Berger (1978); see review, Berger (1988). BACK 44. Kerr (1978). BACK 45. Shift of emphasis: paraphrase of Imbrie (1982), p. 408; for example, see North and Coakley (1979); review: North et al. (1981), p. 107. BACK 46. Imbrie et al. (1984). The definitive "SPECMAP" chronology was published by Martinson et. al. (1987) BACK 47. Pisias and Moore (1981); Ruddiman et al. (1986). BACK 48. Imbrie (1982), p. 411. BACK 49. Quote: J.-R. Petit in Walker (2000). For additional details see Broecker (2010), ch. 1. BACK 50. Lorius et al.(1985); Barnola et al.(1987); Genthon et al. (1987). BACK 51. Stauffer et al. (1988). BACK 52. E.g., Pisias and Shackleton (1984); "The existence of the 100-kyr [kiloyear] cycle and the synchronism between Northern and Southern Hemisphere climates may have their origin in the large glacial-interglacial CO2 changes." Genthon et al. (1987), p. 414. BACK 53. E.g., Berger (1988), p. 649; see Falkowski et al. (2000); Berger and Loutre (2002) discusses a long interglacial. The new Antarctic "Dome C" record of climate went back 750,000 years. EPICA community members (2004). On the drilling see Flannery (2005), p. 58. See also reports in Science (November 25, 2005): 1285-87, 1313-21. BACK 53a. Ruddiman (2005); Ruddiman (2006). Evidence against the hypothesis was advanced by Elsig et al. (2009). BACK 53b. Lorius et al. (1990); Hoffert and Covey (1992). BACK 54. A review of ice sheets (which added yet another factor, permafrost thawing beneath a sheet) is Clark et al. (1999). BACK 55. Winograd et al. (1992), p. 255; Ludwig et al. (1992). BACK 56. Pacific currents: Herbert et al. (2001); "too complicated:" Karner and Muller (2000). BACK 57. Reviewer: Crowley (2002), p. 1474; see also Wunsch (2004); Drysdale et al. (2009). An attempt at a comprehensive theory: Chang et al. (2009). BACK 58. Shackleton (2000); changes of CO2 preceding changes in ice sheet volume were reported in Shackleton and Pisias (1985). The feedback is mentioned or assumed in many of the references cited above, e.g., see quote by Genthon; Lorius et al. (1990) remarked that Greenland drilling then underway "should allow a better determination of the relative timing (phase lag) of climate and greenhouse forcing" (p. 145), but the wider community had thought little about a lag. A recent summary noting some of the complexities is Severinghaus (2009). BACK copyright © 2003-2011 Spencer Weart & American Institute of Physics