Media Clips: The Burglar in the Suitcase – Climate History in an Ice Core

2012 ◽  
Vol 106 (4) ◽  
pp. 250-253
Author(s):  
Kristyn K. Wilson ◽  
Chris Achong

Students analyze items from the media to answer mathematical questions related to the article. The first clip this month uses dimensional analysis and problem solving; the second involves fitting a sinusoid to global warming data.

Author(s):  
Philip Jenkins

My own interest in the topics of this book dates back a good many years. In fact, it predates the emergence of the modern field of climate history, or the identification of global warming as an incipient menace. In saying that, I am claiming no status as a prodigy, still less a prophet. Rather, in my teenage years, I read a great deal of speculative fiction, science fiction, in which themes of climate change and cataclysm have long percolated, at least since the latter years of the nineteenth century. We can debate how accurate the scientific analyses or predictions were in many of these works—in many cases, the level of accurate knowledge was minimal—but those works had the inordinate advantage of thinking through the human and cultural consequences of catastrophe, commonly speculating about religious dimensions. Obviously, some works succeeded better than others in that regard, but the essential project was critically important. If we are foretelling that the world will be assailed by lethal menaces, then we cannot fail to go on to imagine what the political or cultural consequences would or should be....


Author(s):  
David W. Orr

In our final hour (2003), cambridge university astronomer Martin Rees concluded that the odds of global civilization surviving to the year 2100 are no better than one in two. His assessment of threats to humankind ranging from climate change to a collision of Earth with an asteroid received good reviews in the science press, but not a peep from any political leader and scant notice from the media. Compare that nonresponse to a hypothetical story reporting, say, that the president had had an affair. The blow-dried electronic pundits, along with politicians of all kinds, would have spared no effort to expose and analyze the situation down to parts per million. But Rees’s was only one of many credible and well-documented warnings from scientists going back decades, including the Fourth Assessment Report from the Intergovernmental Panel on Climate Change (2007). All were greeted with varying levels of denial, indifference, and misinterpretation, or were simply ignored altogether. It is said to be a crime to cause panic in a crowded theater by yelling “fire” without cause, but is it less criminal not to warn people when the theater is indeed burning? My starting point is the oddly tepid response by U.S. leaders at virtually all levels to global warming, more accurately described as “global destabilization.” I will be as optimistic as a careful reading of the evidence permits and assume that leaders will rouse themselves to act in time to stabilize and then reduce concentrations of greenhouse gases below the level at which we lose control of the climate altogether by the effects of what scientists call “positive carbon cycle feedbacks.” Even so, with a warming approaching or above 2°C we will not escape severe social, economic, and political trauma. In an e-mail to the author on November 19, 2007, ecologist and founder of the Woods Hole Research Center George Woodwell puts it this way: . . . There is an unfortunate fiction abroad that if we can hold the temperature rise to 2 or 3 degrees C we can accommodate the changes. The proposition is the worst of wishful thinking.


2000 ◽  
Vol 30 ◽  
pp. 69-75 ◽  
Author(s):  
A. Savvin ◽  
R. Greve ◽  
R. Calov ◽  
B. Mügge ◽  
K. Hutter

AbstractThe modern dynamic and thermodynamic state of the entire Antarctic ice sheet is computed for a 242 200 year paleoclimatic simulation with the three-dimensional polythermal ice-sheet model SICOPOLIS. The simulation is driven by a climate history derived from the Vostok ice core and the SPECMAP sea-level record. In a 872 km × 436 km region in western Dronning Maud Land (DML), where a deep ice core is planned for EPICA, new high-resolution ice-thickness data are used to compute an improved bedrock topography and a locally refined numerical grid is applied which extends earlier work (Calov and others, 1998). The computed fields of basal temperature, age and shear deformation, together with the measured accumulation rates, give valuable information for the selection of a drill site suitable for obtaining a high-resolution climate record for the last glacial cycle. Based on these results, a possible drill site at 73°59′ S, 00°00′ E is discussed, for which the computed depth profiles of temperature, age, velocity and shear deformation are presented. The geographic origin of the ice column at this position extends 320 km upstream and therefore does not leave the DML region.


1970 ◽  
Vol 3 (5) ◽  
pp. 15-24 ◽  
Author(s):  
Jack D Ives

Himalayan Delusions: Who’s kidding who and why — Science at the service of media, politics and the development agencies. EDITOR’S NOTE: Jack Ives’ article, drawn from his new book Himalayan Perceptions, is a cautionary tale that might almost be read as a gloss on Peter Weingart’s “Moment of truth for science” (see page 11-14). Ives begins by recounting the life and times of the “Theory of Himalayan Environmental Degradation,” a grossly exaggerated but convenient “theory of everything” that suited almost everybody’s agenda — from the media (always hungry for neatly packaged disaster scenarios), to the politicians (happy to point fingers conveniently away from their own failings), to the developers (ready and willing to focus their energies in the pleasant hills of Nepal rather than the steamy lowlands of Bangladesh and India), to the scientists (eager for fame and funding). True to Weingart’s prediction, there was a scientific reaction to the alarmist theories: the Mohonk Conference successfully rallied a generation of “montologists” to investigate critically the bases for predictions of Himalayan deforestation and subcontinental flooding. As a result, the theory was effectively debunked. Unfortunately, it seems to rear its head now and then — most notably in China. And, even more unfortunately, there seems to be a ready supply of successor theories. One media favorite is the impending catastrophic collapse of glacial lakes swollen by glaciers retreating in the face of global warming. Let’s hope that Weingart’s optimism is justified: melting glaciers and glacial lake outburst floods (GLOFs) obviously deserve scientific attention. The question is, will the media and politicians pay any attention at all if researchers predict something less than a super-catastrophe? Himalayan Journal of Sciences 3(5) 2005 p.15-25


2002 ◽  
Vol 35 ◽  
pp. 45-51 ◽  
Author(s):  
Robert Mulvaney ◽  
Hans Oerter ◽  
David A. Peel ◽  
Wolfgang Graf ◽  
Carol Arrowsmith ◽  
...  

AbstractTwo medium-depth ice cores were retrieved from Berkner Island by a joint project between the Alfred-Wegener-Institut and the British Antarctic Survey in the 1994/95 field season. A 151m deep core from the northern dome (Reinwarthhöhe) of Berkner Island spans 700 years, while a 181 m deep core from the southern dome (Thyssenhöhe) spans approximately 1200 years. Both cores display clear seasonal cycles in electrical conductivity measurements, allowing dating by annual-layer counting and the calculation of accumulation profiles. Stable-isotope measurements (both δ18O and δD), together with the accumulation data, allow us to estimate changes in climate for most of the past millennium: the data show multi-decadal variability around a generally stable long-termmean. In addition, a full suite of major chemistry measurements is available to define the history of aerosol deposition at these sites: again, there is little evidence that the chemistry of the sites has changed over the past six centuries. Finally, we suggest that the southern dome, with an ice thickness of 950 m, is an ideal site from which to gain a climate history of the late stages of the last glacial and the deglaciation for comparison with the records from the deep Antarctic ice cores, and with other intermediate-depth cores such as Taylor Dome and Siple Dome.


2020 ◽  
Author(s):  
Daniele FIlippi ◽  
Chiara Giorio

<p>The Beyond EPICA Oldest Ice (BEOI) project will drill an ice core dating back to 1.5 million-years (1.5 Myr) ago. This ice core is of particular interest to the scientific community as it will be the only one covering the climate history of the Mid Pleistocene Transition, when glacial-interglacial cycles changed from a 40 Kyr to 100 Kyr cyclicity, and for which causes are not well understood currently. Obtaining useful climatic information beyond 800 Kyr represents an analytical challenge due to the fact that the deepest section of the ice core is very compact and the amount of sample available is very low.</p><p>Current analytical methods for the determination of organics in ice are characterized by a large number of steps that requires large amounts of sample for a single analysis. This results in the loss of the high time resolution desired from ice cores which is particularly problematic for deeper (i.e. older) records where the ice is more compact.</p><p>This work aims at combining the growing field of microfluidics with improvements to conventional mass spectrometry to allow for continuous analysis of organics in ice cores, melted in continuous on a melting-head. In fact, microfluidic is a powerful technology in which, only a small amount of liquid (10<sup>-9</sup>-10<sup>-18</sup> liters) is manipulated and controlled with an extremely high precision. The method invokes a three-step process: (1) the melted ice core sample is sent to a nebulizer to produce aerosol, then (2) the aerosol is dried to remove water content and concentrate the sample, and (3) the aerosol is sent to a mass spectrometer for continuous analysis through a modified electrospray ionization (ESI) probe.</p><p>This novel system, once operational, can be applied to a range of ice cores but is especially useful for older ice cores given the stratification of deeper segments. It will allow the research community to measure organic compounds with a high time resolution, even in the oldest of ice, to retrieve paleoclimatic information that would otherwise be lost using traditional methods.</p>


2005 ◽  
Vol 17 (4) ◽  
pp. 487-495 ◽  
Author(s):  
ERIC W. WOLFF

Antarctic ice cores have become a unique and powerful resource for studies of climate change. They contain information on past climate, on forcing factors such as greenhouse gas concentrations, and on numerous other environmental parameters. For recent centuries, sites with high snow accumulation are chosen. They have, for example, provided the only direct evidence that carbon dioxide concentrations have increased by over 30% over the last two centuries. They have provided key datasets for other greenhouse gases, and for other forcings such as solar and volcanic. Over longer timescales, the Vostok ice core has shown how greenhouse gas concentrations and climate have closely tracked one another over the last 400 000 years. Other cores have shown detailed spatial and temporal detail of climate transitions, including the Antarctic response during rapid climate events such as Dansgaard-Oeschger events. The new core from Dome C has extended the range of ice cores back beyond 800 000 years, and even older ice could be obtained in future projects.


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