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Ice core dating

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Ice core meltwater samples were analyzed for vanillic acid and para-hydroxybenzoic acid using ion chromatography and electrospray tandem mass spectrometric detection. The levels of vanillic acid and para-hydroxybenzoic acid ranged from ice -rafted debris in the North Atlantic or Bond event and a weakened Asian monsoon suggesting a link between Siberian burning and global patterns of climate change on centennial timescales.

Toward an integrated ice core chronology using relative and orbital tie-points. Bazin, L. Precise ice cores chronologies are essential to better understand the mechanisms linking climate change to orbital and greenhouse gases concentration forcing. Nevertheless, this method has only been applied for a 4- ice cores scenario and for the kyr time period. Here, we present the bases for an extension of this work back to ka using 1 a compilation of published and new relative and orbital tie-points obtained from measurements of air trapped in ice cores and 2 an adaptation of the DATICE inputs to 5 ice cores for the last ka.

Then, we show two tie-points compilations. Finally, we integrate the different dating constraints presented above in the DATICE tool adapted to 5 ice cores to cover the last ka and show how these constraints compare with the established gas chronologies of each ice core. The unique position on a mountain saddle above meters altitude, but close to the coast, ensures that the Renland ice core offers high accumulation, but also reaches far back in time.

Results show that despite the short length the RECAP ice core holds ice all the way back to the past warm interglacial period, the Eemian. The glacial section is strongly thinned and covers on 20 meters of the ReCAP core , but nonetheless due to the high resolution of the measurements all 25 expected DO events could be identified. Below the glacial section another 20 meters of warm Eemian ice have been analysed.

Here we present the chemistry results as obtained by continuous flow analysis CFA and compare the glacial section with the chemistry profile from other Greenland ice cores. Rasmussen, Sune O. Dating sediment cores from Hudson River marshes. There are several methods for determining sediment accumulation rates in the Hudson River estuary.

One involves the analysis of the concentration of certain radionuclides in sediment core sections. Radionuclides occur in the Hudson River as a result of: natural sources, fallout from nuclear weapons testing and low level aqueous releases from the Indian Point Nuclear Power Facility. The following radionuclides have been studied in the authors work: Cesium, which is derived from global fallout that started in the 's and has peaked in Beryllium-7, a natural radionuclide with a 53 day half-life and found associated with very recently depositedmore » sediments.

Another useful natural radionuclide is Lead derived from the decay of Radon in the atmosphere. Lead has a half-life of 22 years and can be used to date sediments up to about years old. The author's research involved taking sediment core samples from four sites in the Hudson River Estuarine Research Reserve areas. These core samples were sectioned, dried, ground and analyzed for the presence of radionuclides by the method of gamma-ray spectroscopy.

The strength of each current pulse is proportional to the energy level of the gamma ray absorbed. Since different radionuclides produce gamma rays of different energies, several radionuclides can be analyzed simultaneously in each of the samples. The data obtained from this research will be compared to earlier work to obtain a complete chronology of sediment deposition in these Reserve areas of the river.

Core samples may then by analyzed for the presence of PCB's, heavy metals and other pollutants such as pesticides to construct a pollution history of the river. Antarctic ice core samples: culturable bacterial diversity.

Culturable bacterial abundance at 11 different depths of a A total of bacterial strains were recovered from the 11 different depths of the ice core. Based on 16S rRNA gene sequence analyses, the isolates could be categorized into 25 phylotypes belonging to phyla Actinobacteria, Bacteroidetes, Firmicutes and Proteobacteria. All isolates had 16S rRNA sequences similar to previously determined sequences No correlation was observed in the distribution of the isolates at the various depths either at the phylum, genus or species level.

Iso-, anteiso-, unsaturated and saturated fatty acids together constituted a significant proportion of the total fatty acid composition. All rights reserved. Towards a new common Greenland Ice Core Chronology for the last years. However, recent research Sigl et al, demonstrated that this timescale has small, but significant, issues over historical time. These discrepancies was found by counting annual layers in high-resolution chemistry records from the NEEM S1 shallow core , and confirmed by linking via 10Be marker horizons to the layer-counted WAIS Divide ice core , Antarctica, and accurately- dated tree-ring series.

We here refine and extend this work. Layer-counting in a single core will always involve some uncertainty, and we hence use data from multiple Greenland ice cores , for which high-resolution impurity records recently have been measured. These ice cores have been synchronized using volcanic marker horizons, and the layer-counting is performed automatically using the StratiCounter algorithm Winstrup et al, , while ensuring that the number of layers between volcanic horizons are the same in all cores.

Based on this extended multiple- core data set, we are further able to extend the new Greenland timescale another few thousand years back in time. This will, among others, provide a new ice-core date for the catastrophic volcanic eruption BC that destroyed the Greek Minoan culture, an important time marker in Greek history.

Neutrino oscillation studies with IceCube-DeepCore. Ice Cube, a gigaton-scale neutrino detector located at the South Pole, was primarily designed to search for astrophysical neutrinos with energies of PeV and higher. This goal has been achieved with the detection of the highest energy neutrinos to date.

At the other end of the energy spectrum, the Deep Core extension lowers the energy threshold of the detector to approximately 10 GeV and opens the door for oscillation studies using atmospheric neutrinos. An analysis of the disappearance of these neutrinos has been completed, with the results produced being complementary with dedicated oscillation experiments. Following a review of the detector principle andmore » performance, the method used to make these calculations, as well as the results, is detailed.

Ice cores and calcite precipitates from alpine ice caves as useful proxies in paleoclimate reconstructions. Colucci, Renato R. In the last years a growing set of research campaigns have been undertaken in the European southeastern Alps. The aim of such interest is mainly due to the peculiar climatic conditions of this area, allowing the existence of periglacial and glacial evidence at the lowest altitude in the Alps.

The reason for such "anomaly" is likely ascribable to very high mean annual precipitation and local topoclimatic amplifications. In the frame of this research, in the fall a 7. Canin 2, masl in the Julian Alps. The ice-core has been cut and analysed in terms of: a oxygen and hydrogen isotope composition; b ; black carbon and dust concentrations; c water conductivity; d mineralogical analyses via X-ray powder diffraction.

In the fall , in the same area, a set of 1. Such original finding represents the first alpine evidence of in situ CCCcoarse and the first occurrence from the southern side of the Alps. Subglacial calcite crusts, widespread in the area, represents a further proxy able to help understanding the evolution of climate during the holocene in this alpine sector.

In the light of accelerated climate change we discuss here the potential of this still untapped and fragile cryospheric archives for paleoclimatic reconstructions in high elevated areas of the Alps. Greenland ice cores tell tales on past sea level changes. All the deep ice cores drilled to the base of the Greenland ice sheet contain ice from the previous warm climate period, the Eemian thousand years before present.

This demonstrates the resilience of the Greenland ice sheet to a warming of 5 oC. Studies of basal material further reveal the presence of boreal forest over Greenland before ice covered Greenland. Conditions for Boreal forest implies temperatures at this time has been more than 10 oC warmer than the present.

To compare the paleo-behavior of the Greenland ice sheet to the present in relation to sea level rise knowledge gabs include the reaction of ice streams to climate changes. The first results will be presented. Towards multi-decadal to multi-millennial ice core records from coastal west Greenland ice caps. Das, Sarah B. On Disko Island, despite high accumulation rates and ice thickness of meters, drilling was halted twice due to the encounter of liquid water at depths ranging from meters, limiting the depth of the final core to 21 m, providing a multi-decadal record On Nuussuaq Peninsula, we collected a m ice core , almost to bedrock, representing a year record.

The ice cores were subsequently analyzed using a continuous flow analysis system CFA. Age-depth profiles and accumulation histories were determined by combining annual layer counting and an ice flow thinning model, both constrained by glaciochemical tie points to other well- dated Greenland ice core records e. Here we will briefly provide an overview of the project and the new sites, and the novel dating methodology, and describe the latest stratigraphic, isotopic and glaciochemical results.

Reliable climate reconstruction from ice core records requires the development of a reliable depth-age relationship. We have established a sub-annual resolution depth-age relationship for the upper meters of a m ice core recovered in from Mt. Hunter 3, m asl , Denali National Park, central Alaska. The dating of the ice core was accomplished via annual layer counting of glaciochemical time-series combined with identification of reference horizons from volcanic eruptions and atmospheric nuclear weapons testing.

Using the continuous ice core melter system at Dartmouth College, sub-seasonal samples have been collected and analyzed for major ions, liquid conductivity, particle size and concentration, and stable isotope ratios. Annual signals are apparent in several of the chemical species measured in the ice core samples.

Calcium and magnesium peak in the spring, ammonium peaks in the summer, methanesulfonic acid MSA peaks in the autumn, and stable isotopes display a strong seasonal cycle with the most depleted values occurring during the winter. Thin ice layers representing infrequent summertime melt were also used to identify summer layers in the core. Analysis of approximately one meter sections of the core via nondestructive gamma spectrometry over depths from 84 to m identified a strong radioactive cesium peak at 89 m which corresponds to the layer deposited during extensive atmospheric nuclear weapons testing.

Peaks in the sulfate and chloride record have been used for the preliminary identification of volcanic signals preserved in the ice core , including ten events since We are confident that the combination of robust annual layers combined with reference horizons provides a timescale for the 20th century that has an error of less than 0.

Initial annual layer counting through the entire m suggests the Denali Ice. Devon island ice cap: core stratigraphy and paleoclimate. Valuable paleoclimatic information can be gained by studying the distribution of melt layers in deep ice cores. A profile representing the percentage of ice in melt layers in a core drilled from the Devon Island ice cap plotted against both time and depth shows that the ice cap has experienced a period of very warm summers since , following a period of colder summers between about and The earlier period was coldest between and There is a high correlation between the melt-layer ice percentage and the mass balance of the ice cap.

The relation between them suggests that the ice cap mass balance was zero accumulation equaled ablation during the colder period but is negative in the present warmer one. There is no firm evidence of a present cooling trend in the summer conditions on the ice cap. A comparison with the melt-layer ice percentage in cores from the other major Canadian Arctic ice caps shows that the variation of summer conditions found for the Devon Island ice cap is representative for all the large ice caps for about 90 percent of the time.

There is also a good correlation between melt-layer percentage and summer sea- ice conditions in the archipelago. This suggests that the search for the northwest passage was influenced by changing climate, with the 19th-century peak of the often tragic exploration coinciding with a period of very cold summers. Sea ice and pollution-modulated changes in Greenland ice core methanesulfonate and bromine.

Maselli, Olivia J. Reconstruction of past changes in Arctic sea ice extent may be critical for understanding its future evolution. Methanesulfonate MSA and bromine concentrations preserved in ice cores have both been proposed as indicators of past sea ice conditions. In this study, two ice cores from central and north-eastern Greenland were analysed at sub-annual resolution for MSA CH3SO3H and bromine, covering the time period A strong correlation between the low-frequency MSA and bromine records during pre-industrial times indicates that both chemical species are likely linked to processes occurring on or near sea ice in the same source regions.

The positive correlation between ice core MSA and bromine persists until the midth century, when the acidity of Greenland ice begins to increase markedly due to increased fossil fuel emissions. After that time, MSA levels decrease as a result of declining sea ice extent but bromine levels increase. We consider several possible explanations and ultimately suggest that increased acidity, specifically nitric acid, of snow on sea ice stimulates the release of reactive Br from sea ice , resulting in increased transport and deposition on the Greenland ice sheet.

Laser- light scattering LLS on polar ice , or on polar ice meltwater, is an accepted method for measuring the concentration of water insoluble aerosol deposits dust in the ice. LLS on polar ice can also be used to measure water soluble aerosols, as well as imperfections air bubbles and cavities in the ice.

LLS was originally proposed by Hammer a, b as a method for measuring the dust concentration in polar ice meltwater. Ram et al. In this paper, we will put previous empirical findings Ram et al. For LLS on clear, bubble-free polar ice , we studied numerically the scattering of light by soluble and insoluble dust aerosol particles embedded in the ice to complement previous experimental studies Ram et al.

For air bubbles in polar ice , we calculated the effects of multiple light scattering using Mie theory and Monte Carlo simulations, and found a method for determining the bubble number size and concentration using LLS on bubbly ice. We also demonstrated that LLS can be used on bubbly ice to measure annual layers rapidly in an objective manner. Hammer, C. Ram, M. Illing, P. Weber, G. Koenig, and M. Kaplan , Polar ice stratigraphy from laser-light scattering: Scattering from ice , Geophys.

The Upper Fremont Glacier UFG , Wyoming, is one of the few continental glaciers in the contiguous United States known to preserve environmental and climate records spanning recent centuries. A pair of ice cores taken from UFG have been studied extensively to document changes in climate and industrial pollution most notably, midth century increases in mercury pollution. Fundamental to these studies is the chronology used to map ice-core depth to age.

Here, we present a revised chronology for the UFG ice cores based on new measurements and using a novel dating approach of synchronizing continuous water isotope measurements to a nearby tree-ring chronology. While consistent with the few unambiguous age controls underpinning the previous UFG chronologies, the new interpretation suggests a very different time scale for the UFG cores with changes of up to 80 years. Mercury increases previously associated with the midth century Gold Rush now coincide with earlyth century industrial emissions, aligning the UFG record with other North American mercury records from ice and lake sediment cores.

Additionally, new UFG records of industrial pollutants parallel changes documented in ice cores from southern Greenland, further validating the new UFG chronologies while documenting the extent of late 19th and early 20th century pollution in remote North America. Reassessment of the Upper Fremont Glacier ice-core chronologies by synchronizing of ice-core -water isotopes to a nearby tree-ring chronology.

Chellman, Nathan J. On the nature of the dirty ice at the bottom of the GISP2 ice core. We present data on the triple Ar isotope composition in trapped gas from clean, stratigraphically disturbed ice between and m depth in the GISP2 ice core , and from basal dirty ice from to m depth. We also present data for the abundance and isotopic composition of O2 and N2, and abundance of Ar, in the basal dirty ice. O2 is partly to completely depleted in basal ice , reflecting active metabolism.

In basal ice , 40Ar is present in excess due to injection of radiogenic 40Ar produced in the underlying continental crust. The weak depth gradient of 40Ar in the dirty basal ice , and the distribution of dirt, indicate mixing within the basal ice , while various published lines of evidence indicate mixing within the overlying clean, disturbed ice.

Excess CH4, which reaches thousands of ppm in basal dirty ice at GRIP, is virtually absent in overlying clean disturbed ice , demonstrating that mixing of dirty basal ice into the overlying clean ice , if it occurs at all, is very slow. Order-of-magnitude estimates indicate that the mixing rate of clean ice into dirty ice is sufficient to maintain a steady thickness of dirty ice against thinning from the mean ice flow.

The dirty ice appears to consist of two or more basal components in addition to clean glacial ice. A small amount of soil or permafrost, plus preglacial snow, lake or ground ice could explain the observations. Ice core evidence for extensive melting of the greenland ice sheet in the last interglacial. Evidence from ice at the bottom of ice cores from the Canadian Arctic Islands and Camp Century and Dye-3 in Greenland suggests that the Greenland ice sheet melted extensively or completely during the last interglacial period more than ka thousand years ago , in contrast to earlier interpretations.

The presence of dirt particles in the basal ice has previously been thought to indicate that the base of the ice sheets had melted and that the evidence for the time of original growth of these ice masses had been destroyed. However, the particles most likely blew onto the ice when the dimensions of the ice caps and ice sheets were much smaller. Ice texture, gas content, and other evidence also suggest that the basal ice at each drill site is superimposed ice , a type of ice typical of the early growth stages of an ice cap or ice sheet.

If the present-day ice masses began their growth during the last interglacial, the ice sheet from the earlier Illinoian glacial period must have competely or largely melted during the early part of the same interglacial period. If such melting did occur, the 6-meter higher-than-present sea level during the Sangamon cannot be attributed to disintegration of the West Antarctic ice sheet, as has been suggested. Neftel, A. Determinations of ancient atmospheric CO2 concentrations for Siple Station, located in West Antarctica, were derived from measurements of air occluded in a m core drilled at Siple Station in the Antarctic summer of Below that depth, the core was dated by extrapolation Friedli et al.

The gases from ice samples were extracted by a dry-extraction system, in which bubbles were crushed mechanically to release the trapped gases, and then analyzed for CO2 by infrared laser absorption spectroscopy or by gas chromatography Neftel et al. The analytical system was calibrated for each ice sample measurement with a standard mixture of CO2 in nitrogen and oxygen. For further details on the experimental and dating procedures, see Neftel et al.

A review of sea ice proxy information from polar ice cores. Sea ice plays an important role in Earth's climate system. The lack of direct indications of past sea ice coverage, however, means that there is limited knowledge of the sensitivity and rate at which sea ice dynamics are involved in amplifying climate changes.

As such, there is a need to develop new proxy records for reconstructing past sea ice conditions. Here we review the advances that have been made in using chemical tracers preserved in ice cores to determine past changes in sea ice cover around Antarctica. Ice core records of sea salt concentration show promise for revealing patterns of sea ice extent particularly over glacial-interglacial time scales.

In the coldest climates, however, the sea salt signal appears to lose sensitivity and further work is required to determine how this proxy can be developed into a quantitative sea ice indicator. However the MSA ice core proxy also requires careful site assessment and interpretation alongside other palaeoclimate indicators to ensure reconstructions are not biased by non-sea ice factors, and we summarise some recommended strategies for the further development of sea ice histories from ice core MSA.

For both proxies the limited information about the production and transfer of chemical markers from the sea ice zone to the Antarctic ice sheets remains an issue that requires further multidisciplinary study. Despite some exploratory and statistical work, the application of either proxy as an indicator of sea ice change in the Arctic also remains largely unknown.

As information about these new ice core proxies builds, so too does the potential to develop a more comprehensive understanding of past changes in sea. Osterberg, E. Meteorological station data from NW Greenland indicate a 3oC temperature rise since , with most of the warming occurring in fall and winter.

According to remote sensing data, the NW Greenland ice sheet GIS and coastal ice caps are responding with ice mass loss and margin retreat, but the cryosphere's response to previous climate variability is poorly constrained in this region. We are developing multi-proxy records lake sediment cores , ice cores , glacial geologic data, glaciological models of Holocene climate change and cryospheric response in NW Greenland to improve projections of future ice loss and sea level rise in a warming climate.

As part of our efforts to develop a millennial-length ice core paleoclimate record from the Thule region, we collected and analyzed snow pit samples and short firn cores up to 21 m from the coastal region of the GIS 2Barrel site; The 2Barrel ice core record has statistically significant relationships with regional spring and fall Baffin Bay sea ice extent, summertime temperature, and annual precipitation. Here we evaluate relationships between the North Ice Cap firn core glaciochemical record and climate variability from regional instrumental stations and reanalysis datasets.

Bipolar volcanic events in ice cores and the Toba eruption at 74 ka BP Invited. Acidity spikes in Greenland and Antarctic ice cores are applied as tracers of past volcanic activity. Besides providing information on the timing and magnitude of past eruptions, the acidity spikes are also widely used for synchronization of ice cores. All of the deep Greenland ice cores are thus synchronized throughout the last glacial cycle based on volcanic markers. Volcanic matching of ice cores from the two Hemispheres is much more challenging but it is feasible in periods of favourable conditions.

Over the last two millennia, where ice cores are precisely dated , some 50 bipolar volcanic events have thus been identified. In order for an eruption to express a bipolar fingerprint it generally needs to be a low latitude eruption with stratospheric injection.

Sometimes tephra is associated with the ice-core acidity spikes, but most often there is no tephra present in the ice. As yet, an unknown eruption occurring in AD is the only event reported to have deposited tephra in both Greenland and Antarctica. During the last glacial period bipolar volcanic matching is very challenging and very little work has been done, but recent high-resolution ice core records have the potential to provide bipolar ice core matching for some periods.

Recently, Greenland and Antarctic ice cores have been linked by acidity spikes in the time window of the most recent eruption the YTT eruption of the Indonesian Toba volcano that is situated close to equator in Sumatra.

Ash from this Toba event is widespread over large areas in Asia and has been identified as far west as Africa, but no corresponding tephra has been found in polar ice cores despite several attempts. Surprisingly, no single outstanding acidity spike. The principal aim of the INTIMATE Project is to synthesize high-resolution ice , terrestrial and marine records spanning the period 60, to years ago henceforth given as ka to better understand the impact and mechanisms of rapid and extreme climate change, thereby reducing the uncertainty of future predictions.

For correlation, precise dating of the records from the different realms is imperative. Dating Antarctic ice sheet collapse: Proposing a molecular genetic approach. Sea levels at the end of this century are projected to be 0. The upper end of this range, and even higher estimates, cannot be ruled out because of major uncertainties in the dynamic response of polar ice sheets to a warming climate. Here, we propose an ecological genetics approach that can provide insight into the past stability and configuration of the West Antarctic Ice Sheet WAIS.

We propose independent testing of the hypothesis that a trans-Antarctic seaway occurred at the last interglacial. Examination of the genomic signatures of bottom-dwelling marine species using the latest methods can provide an independent window into the integrity of the WAIS more than , years ago.

Periods of connectivity facilitated by trans-Antarctic seaways could be revealed by dating coalescent events recorded in DNA. These methods allow alternative scenarios to be tested against a fit to genomic data. Ideal candidate taxa for this work would need to possess a circumpolar distribution, a benthic habitat, and some level of genetic structure indicated by phylogeographical investigation.

The purpose of this perspective piece is to set out an ecological genetics method to help resolve when the West Antarctic Ice Shelf last collapsed. Dust plays an important role in the Earth system, and it usually displays largely spatial and temporal variations.

It is necessary for us to reconstruct the past variations of dust in different regions to better understand the interactions between dust and environments. Ice core records can reveal the history of dust variations. In this paper, we used the Guliya, Dunde, Malan and Dasuopu ice cores from the Tibetan Plateau to study the spatial distribution, the seasonal variations and the secular trends of dust.

It was found that the mean dust concentration was higher by one or two order of magnitudes in the Guliya and Dunde ice cores from the northern Tibetan Plateau than in the Dasuopu ice core from the southern Tibetan Plateau. During the year, the highest dust concentration occurs in the springtime in the northern Tibetan Plateau while in the non-monsoon season in the southern Tibetan Plateau.

Interestingly, climatic and environmental records of the ice cores from the Tibetan Plateau reflected that the correlation between dust concentration and air temperature was strongly positive in the southern Plateau while negative in the northern Plateau over the last millennium.

This implies that climatic and environmental changes existed considerable differences in the different parts of the Plateau. Continuous methane measurements from a late Holocene Greenland ice core : Atmospheric and in-situ signals. Rhodes, Rachael H. Ancient air trapped inside bubbles in ice cores can now be analysed for methane concentration utilising a laser spectrometer coupled to a continuous melter system.

We present a new ultra-high resolution record of atmospheric methane variability over the last yr obtained from continuous analysis of a shallow ice core from the North Greenland Eemian project NEEMS1 during a 4-week laboratory-based measurement campaign.

Our record faithfully replicates the form and amplitudes of multi-decadal oscillations previously observed in other ice cores and demonstrates the detailed depth resolution 5. In addition, we report the detection of high frequency ice core methane signals of non-atmospheric origin. Firstly, measurements of air from the firn- ice transition region and an interval of ice core dating from AD gas age resolve apparently quasi-annual scale methane oscillations.

Traditional gas chromatography measurements on discrete ice samples confirm these signals and indicate peak-to-peak amplitudes of ca. We hypothesise that these oscillations result from staggered bubble close-off between seasonal layers of contrasting density during time periods of sustained multi-year atmospheric methane change. Secondly, we report the detection of abrupt cm depth interval , high amplitude ppb excess methane spikes in the NEEM ice that are reproduced by discrete measurements.

We show for the first time that methane spikes present in thin and infrequent layers in polar, glacial ice are accompanied by elevated concentrations of carbon- and nitrogen-based chemical impurities, and suggest that biological in-situ production may be responsible. Raman spectroscopy on ice cores from Greenland and Antarctica.

Ice cores are invaluable archives for the reconstruction of the climatic history of the earth. Besides the analysis of various climatic processes from isotopes and chemical signatures they offer the unique possibility of directly extracting the past atmosphere from gaseous inclusions in the ice. Many aspects of the formation and alterations of these inclusions, e.

Modern micro Raman spectroscopy is an excellent tool to obtain high-quality data for all of these aspects. Detailed examples of the various uses of Raman spectroscopy will be presented along with practical information about the techniques required to obtain high-quality spectra.

Retrieval and interpretation of quantitative data from the spectra will be explained. Future possibilities for advanced uses of Raman spectroscopy for ice core research will be discussed. Sakurai et al. Journal of Glaciology, 55, Pauer et al. Geophysical Research Letters, 22, Ikeda-Fukazawa et al. Journal of Geophysical Research, , Weikusat et al.

Journal of Glaciology, accepted. Thomas P. Here we reveal that DNA and amino acids from buried organisms can be recovered from the basal sections of deep ice cores and allow reconstructions of past flora and fauna. We show that high altitude southern Greenland, currently lying below more than two kilometers of ice , was once inhabited by a diverse array of conifer trees and insects that may date back more than thousand years.

The results provide the first direct evidence in support of a forested southern Greenland and suggest that many deep ice cores may contain genetic records of paleoenvironments in their basal sections. Svensson, A. The Toba eruption that occurred some 74 ka ago in Sumatra, Indonesia, is among the largest volcanic events on Earth over the last 2 million years. As yet, no tephra associated with Toba has been identified in Greenland or Antarctic ice cores.

Based on new accurate dating of Toba tephra and on accurately dated European stalagmites, the Toba event is known to occur between the onsets of Greenland interstadials GI 19 and Furthermore, the existing linking of Greenland and Antarctic ice cores by gas records and by the bipolar seesaw hypothesis suggests that the Antarctic counterpart is situated between Antarctic Isotope Maxima AIM 19 and Annual layer counting between volcanic spikes in both cores allows for a unique match.

We first demonstrate this bipolar matching technique at the already synchronized Laschamp geomagnetic excursion 41 ka BP before we apply it to the suggested Toba interval. The suggested bipolar Toba synchronization has decadal precision. It thus allows a determination of the exact phasing of inter-hemispheric climate in a time interval of poorly constrained ice core records, and it allows for a discussion of the climatic impact of the Toba eruption in a global perspective.

The bipolar linking gives no support for a long-term global cooling caused by the Toba eruption as Antarctica experiences a major warming shortly after the event. Furthermore, our bipolar match provides a way to place palaeo-environmental records other than ice cores into a precise climatic. Lakes, This figure shows the change in the ice -off date , or date of ice thawing and breakup, for 14 U. All of the lakes have red circles with negative numbers, which represent earlier thaw dates.

Larger circles indicate larger changes. For more information: www. References: - Drury and Humphreys, Microstructural shear criteria associated with grain boundary sliding during ductile deformation. Is Antarctica like a birthday cake? Physical analysis of an Antarctic ice core -towards an integration of micro- and macrodynamics of polar ice. A , Reconstructing the past variability of Arctic sea ice provides an essential context for recent multi-year sea ice decline, although few quantitative reconstructions cover the Holocene period prior to the earliest historical records 1, years ago.

Photochemical recycling of bromine is observed over first-year, or seasonal, sea ice in so-called "bromine explosions" and we employ a 1-D chemistry transport model to quantify processes of bromine enrichment over first-year sea ice and depositional transport over multi-year sea ice and land ice.

First-year sea ice extent was lowest during the glacial stadials suggesting complete coverage of the Arctic Ocean by multi-year sea ice. The isotopic composition of methane in polar ice cores. Air bubbles in polar ice cores indicate that about years ago the atmospheric mixing ratio of methane began to increase rapidly. Today the mixing ratio is about 1. Carbon isotope ratios in methane up to years in age have been measured with as little as 25 kilograms of polar ice recovered in 4-meter-long ice-core segments.

The data show that: 1 in situ microbiology or chemistry has not altered the ice-core methane concentrations, and 2 that the carbon to carbon ratio of atmospheric CH4 in ice from years and years ago was about 2 per mil lower than at present.

Atmospheric methane has a rich spectrum of isotopic sources: the ice-core data indicate that anthropogenic burning of the earth's biomass is the principal cause of the recent CH4 enrichment, although other factors may also contribute. Fudge, T. Understanding the retreat of the Ross Ice Sheet following the Last Glacial Maximum is particularly difficult in the eastern Ross area where there is no exposed rock and the Ross Ice Shelf prevents extensive bathymetric mapping.

Coastal domes, by preserving old ice , can be used to infer the establishment of grounded ice and be used to infer past ice thickness. Here we focus on Roosevelt Island, in the eastern Ross Sea, where the Roosevelt Island Climate Evolution project recently completed an ice core to bedrock. Using ice -flow modeling constrained by the depth-age relationship and an independent estimate of accumulation rate from firn-densification measurements and modeling, we infer ice thickness histories for the LGM 20ka to present.

Preliminary results indicate thinning of m between 15ka and 12ka is required. This is similar to the amount and timing of thinning inferred at Siple Dome, in the central Ross Sea Waddington et al. Pre-cometary ice composition from hot core chemistry.

Pre-cometary ice located around star-forming regions contains molecules that are pre-biotic compounds or pre-biotic precursors. Molecular line surveys of hot cores provide information on the composition of the ice since it sublimates near these sites. We have combined a hydrostatic hot core model with a complex network of chemical reactions to calculate the time-dependent abundances of molecules, ions, and radicals. The model considers the interaction between the ice and gas phase.

It is applied to the Orion hot core where high-mass star formation occurs, and to the solar-mass binary protostar system IRAS Our calculations show that at the end of the hot core phase both star-forming sites produce the same prebiotic CN-bearing molecules. However, in the Orion hot core these molecules are formed in larger abundances. A comparison of the calculated values with the abundances derived from the observed line data requires a chemically unprocessed molecular cloud as the initial state of hot core evolution.

Thus, it appears that these objects are formed at a much younger cloud stage than previously thought. This implies that the ice phase of the young clouds does not contain CN-bearing molecules in large abundances before the hot core has been formed. The pre-biotic molecules synthesized in hot cores cause a chemical enrichment in the gas phase and in the pre-cometary ice. This enrichment is thought to be an important extraterrestrial aspect of the formation of life on Earth and elsewhere.

Ice cores from low latitudes can provide a wealth of unique information about past climate in the tropics, but they are difficult to recover and few exist. Quelccaya continues to retreat and thin. Radiocarbon dates on wetland plants exposed along its retreating margins indicate that it has not been smaller for at least six millennia. The chemical impurities embedded in the ice matrix of an ice sheet are basic proxies for climate reconstruction, and their concentration and composition usually determine the occurrence of distinct cloudy or clear strata in the ice sheet structure.

The easiest observable impurities in polar ice are air bubbles. But a considerable amount of the impurities trapped inside ice layers are observed as microscopic deposits of solid soluble or insoluble particles, not bigger than a few micra in size, called microinclusions.

Layers of ice with a high content of micro inclusions are in general called cloudy bands and are considered to have been formed from the precipitations deposited during colder periods. Roughly, we expect that the colder the climate during the time the snow accumulated, the cloudier the ice stratum that forms afterwards [2]. Mainly by means of in-situ micro-Raman spectroscopy, it has been shown that in Antarctic glacial ice the soluble microinclusions occur mostly as sulphate and nitrate salts [3], while in Arctic ice more commonly as carbonate salts [4].

These findings could be explained in terms of different aerosol compositions determined by the specific regional environments and climatic conditions [5]. Regarding the insoluble particles that might exist in natural ice , with higher frequency in ice layers formed during glacial type stages, the general findings classify them in the alumino silicate mineralogical class [6]. Microinclusions existent in solid samples taken from clear and cloudy ice layers, corresponding. High-resolution sulfur isotopes in ice cores identify large stratospheric volcanic eruptions.

The record of the volcanic forcing of climate over the past years is reconstructed primarily from sulfate concentrations in ice cores. Of particular interest are stratospheric eruptions, as these afford sulfate aerosols the longest residence time and largest dispersion in the atmosphere, and thus the greatest impact on radiative forcing. Identification of stratospheric eruptions currently relies on the successful matching of the same volcanic sulphate peak in ice cores from both the Northern and Southern hemispheres a "bipolar event".

These are interpreted to reflect the global distribution of sulfur aerosols by the stratospheric winds. Despite its recent success, this method relies on precise and accurate dating of ice cores , in order to distinguish between a true 'bipolar event' and two separate eruptions that occurred in close temporal succession.

Sulfur isotopes can been used to distinguish between these two scenarios since stratospheric sulfur aerosols are exposed to UV radiation which imparts a mass independent fractionation Baroni et al. Mass independent fractionation of sulfate in ice cores thus offers a novel method of fingerprinting stratospheric eruptions, and thus refining the historic record of explosive volcanism and its forcing of climate. Here we present new high-resolution sub-annual sulfur isotope data from the Tunu Ice core in Greenland over seven eruptions.

Sulfur isotopes were measured by MC-ICP-MS, which substantially reduces sample size requirements and allows high temporal resolution from a single ice core. Baroni, M. Mass-independent sulfur isotopic compositions in stratospheric volcanic eruptions. Science, , Identification of stratospheric eruptions currently relies on the successful matching of the same volcanic sulfate peak in ice cores from both the Northern and Southern hemispheres a "bipolar event".

Climatic changes have been reconstructed for the Tibetan Plateau based on ice core records. The Guliya ice core on the Tibetan Plateau presents climatic changes in the past , years, thus is comparative with that from Vostok ice core in Antarctica and GISP2 record in Arctic.

These three records share an important common feature, i. It is also evident that the major patterns of climatic changes are similar on the earth. Why does climatic change over the earth follow a same pattern? It might be attributed to solar radiation. We found that the cold periods correspond to low insolation periods, and warm periods to high insolation periods.

Our major challenge in the study of both climate and environment is that greenhouse gases such as CO2, CH4 are possibly amplifying global warming, though at what degree remains unclear. One of the ways to understand the role of greenhouse gases is to reconstruct the past greenhouse gases recorded in ice. In , we drilled an ice core from m a. Based on the record, we found seasonal cycles in methane variation.

In particular, the methane concentration is high in summer, suggestiing active methane emission from wet land in summer. Based on the seasonal cycle, we can reconstruct the methane fluctuation history in the past years. The most prominent feature of the methane record in the Himalayan ice core is the abrupt increase since A.

This is closely related to the industrial revolution worldwide. It implies that the industrial revolution has dominated the atmospheric greenhouse gas emission for about years. Besides, the average methane concentration in the Himalayan ice core is. In the last decades, Continuous Flow Analysis CFA technology for ice core analyses has been developed to reconstruct the past changes of the climate system 1 , 2.

Compared with traditional analyses of discrete samples, a CFA system offers much faster and higher depth resolution analyses. It also generates a decontaminated sample stream without time-consuming sample processing procedure by using the inner area of an ice-core sample.. The CFA system that we have been developing is currently able to continuously measure stable water isotopes 3 and electrolytic conductivity, as well as to collect discrete samples for the both inner and outer areas with variable depth resolutions.

Chemistry analyses4 and methane-gas analysis 5 are planned to be added using the continuous water stream system 5. In order to optimize the resolution of the current system with minimal sample volumes necessary for different analyses, our CFA system typically melts an ice core at 1.

At the 1. Also, the mixing volume that occurs in our open split debubbler is regulated using its weight. The overflow pumping rate is smoothly PID controlled to maintain the weight as low as possible, while keeping a safety buffer of water to avoid air bubbles downstream. To evaluate the system's depth-resolution, we will present the preliminary data of electrolytic conductivity obtained by melting 12 bags of the North Greenland Eemian Ice Drilling NEEM ice core.

We will present results for the Greenland Stadial -8, whose depths and ages are between Surface water mass composition changes captured by cores of Arctic land-fast sea ice. In the Arctic, land-fast sea ice growth can be influenced by fresher water from rivers and residual summer melt.

This paper examines a method to reconstruct changes in water masses using oxygen isotope measurements of sea ice cores. To determine changes in sea water isotope composition over the course of the ice growth period, the output of a sea ice thermodynamic model driven with reanalysis data, observations of snow depth, and freeze-up dates is used along with sea ice oxygen isotope measurements and an isotopic fractionation model.

Direct measurements of sea ice growth rates are used to validate the output of the sea ice growth model. Salinity anomalies in the ocean were also tracked by moored instruments. These data indicate episodic advection of meteoric water, having both lower salinity and lower oxygen isotopic composition, during the winter sea ice growth season.

Such advection of meteoric water during winter is surprising, as no surface meltwater and no local river discharge should be occurring at this time of year in that area. The method described will be useful for winter detection of meteoric water presence in Arctic fast ice regions, which is important for climate studies in a rapidly changing Arctic.

Those derived effective fractionation coefficients will be useful for future water mass component proportion calculations. In particular, the equations given can be used to inform choices made when. Glaciers serve both as recorders and early indicators of climate change.

Over the past 35 years our research team has recovered climatic and environmental histories from ice cores drilled in both Polar Regions and from low to mid-latitude, high-elevation ice fields. Those ice core -derived proxy records extending back 25, years have made it possible to compare glacial stage conditions in the Tropics with those in the Polar Regions. Remarkable similarities between changes in the highland and coastal cultures of Peru and regional climate variability, especially precipitation, imply a strong connection between prehistoric human activities and regional climate.

Ice cores retrieved from shrinking glaciers around the world confirm their continuous existence for periods ranging from hundreds to thousands of years, suggesting that current climatological conditions in those regions today are different from those under which these ice fields originated and have been sustained.

The ongoing widespread melting of high-elevation glaciers and ice caps, particularly in low to middle latitudes, provides strong evidence that a large-scale, pervasive and, in some cases, rapid change in Earth's climate system is underway. The history and fate of these ice caps, told through the adventure, beauty and the scientific evidence from some of world's most remote mountain tops, provide a global perspective for contemporary climate.

NSF Paleoclimate Program. Continuous analysis of phosphate in a Greenland shallow ice core. Phosphate is an important and sometimes limiting nutrient for primary production in the oceans. Because of deforestation and the use of phosphate as a fertilizer changes in the phosphate cycle have occurred over the last centuries. On longer time scales, sea level changes are thought to have also caused changes in the phosphate cycle.

Analyzing phosphate concentrations in ice cores may help to gain important knowledge about those processes. In the present study, we attach a phosphate detection line to an existing continuous flow analysis CFA setup for ice core analysis at the University of Copenhagen. The CFA system is optimized for high-resolution measurements of insoluble dust particles, electrolytic melt water conductivity, and the concentrations of ammonium and sodium.

For the phosphate analysis we apply a continuous and highly sensitive absorption method that has been successfully applied to determine phosphate concentrations of sea water Zhang and Chi, A line of melt water from the CFA melt head 1. An uncompleted reaction takes place in five meters of heated mixing coils before the absorption measurement at a wavelength of nanometer takes place in a 2 m long liquid waveguide cell LWCC with an inner volume of 0.

The method has a detection limit of around 0. Preliminary analysis of early Holocene samples from the NGRIP ice core show phosphate concentration values of a few ppb. In this study, we will attempt to determine past levels of phosphate in a shallow Northern Greenland firn core with an annual layer thickness of about 20 cm ice equivalent.

With a melt speed of 2. An ice core record of net snow accumulation and seasonal snow chemistry at Mt. Waddington, southwest British Columbia, Canada. We recovered a m ice core from Combatant Col Aerosols and other impurities in the ice show unambiguous seasonal variations, allowing for annual dating of the core. Clustered melt layers, originating from summer surface heating, also aid in the dating of the core.

Seasonality in water stable isotopes is preserved throughout the record, showing little evidence of diffusion at depth, and serves as an independent verification of the timescale. The annual signal of deuterium excess is especially well preserved. The record of lead deposition in the core agrees with those of ice cores from Mt. Logan and from Greenland, with a sharp drop-off in concentration in the s and early s, further validating the timescales.

Despite significant summertime melt at this mid-latitude site, these data collectively reveal a continuous and annually resolved year record of snow accumulation. We derived an accumulation time series from the Mt. Waddington ice core , after correcting for ice flow.

Space Science Reviews, 1 , 67— Bender, M. Orbital tuning chronology for the Vostok climate record supported by trapped gas composition. Science Letters, , — Burns, S. Science , , — Dreyfus, G. Climate of the Past Discussions , 3 2 , — Guillou, H. On the age of the Laschamp geomagnetic excursion.

Earth and Planetary Science Letters, , — CrossRef Google Scholar. Kawamura, K. Northern hemisphere forcing of climatic cycles over the past , years implied by absolute dating of antarctic ice cores. Nature, , — Landais, A. Quaternary Science Reviews, 25 1—2 , 49— Laskar, J.

A Long-term numerical solution for the insolation quantities of the earth. Lemieux-Dudon, B. Masson-Delmotte, V. A review of Antarctic surface snow isotopic composition: Observations, atmospheric circulation, and isotopic modeling. Journal of Climate , 21 13 , — Narcisi, B. A volcanic marker 92 ka for dating deep east Antarctic ice cores.

Quaternary Science Reviews, 25 , — Parrenin, F. Climate of the Past, 3, — IceChrono1: A probabilistic model to compute a common and optimal chronology for several ice cores. Geoscientific Model Development, 8 5 , — New modelling of the Vostok ice flow line and implication for the glaciological chronology of the Vostok ice core. Journal Geophysical Research, , D Raisbeck, G. Nature, , 82— Direct north-south synchronization of abrupt climate change record in ice cores using beryllium Climate of the Past, 3 3 , — Rasmussen, S.

A new greenland ice core chronology for the last glacial termination. Raynaud, D. The local insolation signature of air content in Antarctic ice. A newstep toward an absolute dating of ice records. Earth and Planetary Science Letters , 3—4 , — Ritz, C. Modeling the evolution of antarctic ice sheet over the last , years: Implications for altitude changes in the Vostok Region.

Journal Geophysical Research, D23 , — Ruth, U.

Determining the age of the ice in an ice core can be done in a number of ways.

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The ice cores can provide an annual record of temperature, precipitation, atmospheric composition, volcanic activity, and wind patterns. In a general sense, the thickness of each annual layer tells how much snow accumulated at that location during the year. Differences in cores taken from the same area can reveal local wind patterns by showing where the snow drifted.

More importantly, the make-up of the snow itself can tell scientists about past temperatures. As with marine fossils, the ratio of oxygen isotopes in the snow reveals temperature, though in this case, the ratio tells how cold the air was at the time the snow fell.

In snow, colder temperatures result in higher concentrations of light oxygen. See The Oxygen Balance. Researchers retrieve climate records from mountain glaciers in addition to the records from polar ice sheets. Drilling sites around the world help distinguish trends in local climate from trends in global climate. This drilling station is located at an elevation of 6, meters 21, feet on the summit of Nevado Coropuna in the Peruvian Andes.

Scientists can confirm these chemistry-based temperature measurements by observing the temperature of the ice sheet directly. As Alley explained to the Earth Observatory, the ice sheet can be compared to a frozen roast that is put directly into the oven. The outside heats up quickly, but the center remains cold, close to the temperature of the freezer, for a long time. Similarly, the ice sheet has warmed somewhat since the Ice Age, but not completely.

The top has warmed as global temperatures have warmed, while the bottom has been warmed by heat flow from deep inside the Earth. But in the middle of an ice sheet, the ice remains close to the Ice Age temperatures at which it formed. The ice core recovered from Vostok, Antarctica, records over , years of climate history. This interactive graph shows temperature measurements derived from the core.

Temperatures equal to or greater than the recent average gray line delineate interglacial periods, while colder temperatures indicate ice ages. Scroll the graph in time by dragging the slider on the miniature graph lower. Zoom in and out on the data with the plus and minus buttons lower left. When scientists lower an ultra-precise thermometer into a hole in the ice, they can detect the temperature variations that have occurred since the Ice Age.

The near-surface ice temperature, like the atmosphere today, is warm, and then the temperature drops in the layers formed roughly between AD and , a period known as the Little Ice Age, one of several cold snaps that briefly interrupted the overall warming trend ongoing since the end of the Ice Age. As the thermometer goes deeper into the ice sheet, the temperature warms again, and then plummets to the temperatures indicative of the Ice Age.

Finally, the bottom layers of the ice sheet are warmed by heat coming from the Earth. These directly measured temperatures represent a rough average—a record of trends, not variable, daily temperatures—but climatologists can compare the thermometer temperatures with the oxygen isotope record as a way to calibrate those results.

Scientists measure the temperature of an ice sheet directly by lowering a thermometer into the borehole that was drilled to retrieve the ice core. Like an insulated thermos, snow and ice preserve the temperature of each successive layer of snow, which reflects general atmospheric temperatures when the layer accumulated. Close to the surface of the bedrock, the lowest layers of the ice are warmed by the heat of the Earth.

These physical temperature measurements help calibrate the temperature record scientists obtain from oxygen isotopes. When snow forms, it crystallizes around tiny particles in the atmosphere, which fall to the ground with the snow. The type and amount of trapped particles, such as dust, volcanic ash, smoke, or pollen, tell scientists about the climate and environmental conditions when the snow formed.

As the snow settles on the ice, air fills the space between the ice crystals. When the snow gets packed down by subsequent layers, the space between the crystals is eventually sealed off, trapping a small sample of the atmosphere in newly formed ice. Records of methane levels, for example, indicate how much of the Earth wetlands covered because the abundance of life in wetlands gives rise to anaerobic bacteria that release methane as they decompose organic material.

Scientists can also use the ice cores to correlate the concentration of carbon dioxide in the atmosphere with climate change—a measurement that has emphasized the role of carbon dioxide in global warming. Finally, anything that settles on the ice tends to remain fixed in the layer it landed on.

Of particular interest are wind-blown dust and volcanic ash. As with dust found in sea sediments, dust in ice can be analyzed chemically to find out where it came from. The amount and location of dust tells scientists about wind patterns and strength at the time the particles were deposited. Volcanic ash can also indicate wind patterns.

Additionally, volcanoes pump sulfates into the atmosphere, and these tiny particles also end up in the ice cores. This evidence is important because volcanic activity can contribute to climate change, and the ash layers can often be dated to help calibrate the timeline in the layers of ice. Air bubbles trapped in the ice cores provide a record of past atmospheric composition. Figure 2.

Dust concentration, climatic air temperature as inferred from del measurements , and concentration of carbon dioxide and methane from measurements of trapped air are plotted against time before present. After Lorius et al. The snow near the surface of the ice sheet is like a sponge with channels of air between the snow grains. As more and more snow is accumulated on top, the underlying snow is compressed into ice and the air forms bubbles in the ice. Ice cores therefore can be analysed not just for the chemical and physical properties of the ice, but also for the properties of the air trapped in the ice.

These bubbles are actual samples of the atmosphere up to thousands of years ago. So, analysis of them can tell us much about the atmosphere in the past. Concentrations of carbon dioxide and methane measured in the air bubbles trapped in the ice are shown in Figure 2 along with temperature and dust graphs. Carbon dioxide and methane are greenhouse gases and the similarity between the graphs for their concentrations and the temperature change graph indicates that the greenhouse effect is real and that it has been around for many thousands of years.

That is only if you are presuming many thousands of years. I studied that chart for some time. What I saw corresponds to the idea that a post flood ice age would have less dust due to winds because everything was wet. But then you have that period in between ice ages where you see a rise in carbon dioxide as the plant life on earth was re-established and thrived.

This corresponds with the rapid rise in temperature which melted the ice. Now, keep in mind that we are ONLY talking about the one pole here — the south one. These measurements do NOT tell us what the rest of the world was like at the time. As we move to the left in graph two, or toward the present, there is a sudden rise in the dust factor. This would easily result from volcanism and the changes in relative air temperatures, and even changes in relative areas of sea temperatures, around the world.

The would cause the massive winds that seek to equalize the temperatures. More dust at a time of increasing cold and the rapid onset of a much worse ice age. Then, to the far left of the graph, a rapid rise in temperature again as the dust settles down and the temperatures and thus the pressures have also settled.

The earth warms again and the ices melt, leaving what is left on the poles. You see, if one does not presume long ages, many rapid storms in a time of fluctuating temperatures and world upheaval can account for what we see in that graph.

Has there been a significant increase in the atmospheric concentration of greenhouse gases since the industrial revolution? The concentration of carbon dioxide has increased from about parts per million to parts per million, which is a rise of 25 per cent since the middle of last century. Nitrous oxide and other greenhouse gases also show similar trends from analysis of the ice-core bubbles.

The Law Dome ice core is at a location where the snow accumulation is much higher than at Vostok. Thus, the time scale for the Law Dome core is expanded and it can provide us with more detailed information about recent climate changes, though it can not go back in time as far as the deeper Vostok ice core.

By sampling at very fine intervals down the ice core, and provided that each annual layer of snow is thick enough, several samples from each year may be measured for the different chemical properties. It has already been seen that the delta value is related to air temperature when the snow was deposited.

Because it is warmer in summer and cooler in winter, and provided the snow layers are not too disturbed by wind, the delta value can show annual cycles. Thus, these values can be used to date the ice core. Hydrogen peroxide is created in the atmosphere by a chemical reaction that requires ultraviolet light. There is a lot less ultraviolet light in the winter than in the summer in Antarctica.

Thus, measurements of hydrogen peroxide dissolved in the ice also provide a good annual cycle indicator. Some observations here: first of all the dust would have had to be produced by winds bringing it in. Therefore the pattern is upset from the outset. Secondly, it is presumed that the variations in temperatures are correlative to summer and winter variations. However this does not necessarily have to be the case. Uniformitarian gradualism is a presumption which rests on a shaky foundation here simply because of the presence of the varying amount of dust if nothing else!

In order to date the ice cores accurately, the annual layers need to be thick enough to obtain about ten measurement samples from each year. The thickness of the annual layers depends on how much snow falls each year. Thus, to obtain an ice core from which accurate, detailed dating can be derived, we need to find an Antarctic site where the snow accumulation is relatively high. This would usually mean we need to find a low elevation site, but it must also be a site where there is no melt.

If the snow was to melt at any time during the year, some measurements such as those involving trapped gases would be spoiled. In addition, the annual layers would be destroyed by the melt water which would, effectively, wash the evidence away. And the only way they have of estimating melt rate is to take what we have today and presume it has been that way for a very long time.

This kind of gradualism presumes no catastrophes, no bolide hits, nothing to disturb the quiet ebb an flow of the seasons. I do not think this is a reasonable presumption when the rest of the world is looked at and the evidence for catastrophes of various kinds is so clear.

Such locations high snow accumulation, yet low summer temperatures are not easy to find. One such location, however, is near the summit of Law Dome, approximately kilometres from Casey Station, where an ice core has been drilled 1, metres through the ice sheet to the underlying bedrock. Accurate dating for this core has been obtained back to 8, years ago using annual cycles obtained by analysis of delta value and hydrogen peroxide.

A section of the graph of delta value and hydrogen peroxide is shown in Figure 4, along with the year. The ice core depth for this section is to metres, corresponding to the dates to AD. Figure 4. Detailed analysis of section of the DSS ice core summit of Law Dome, Antarctica showing del value, Peroxide concentration, Sulphate concentration and Conductivity values.

Section of ice core is from to metres depth, covering the time period to , and including evidence of two volcanic eruptions. I am curious to know the sulfate measurements for core depths that are dated thousands of years ago….. Measurements of electrical conductivity are also made on the ice cores — these are closely linked to the acidity of the ice.

Conductivity shows an annual cycle and is higher in the summer snow than the winter snow. This is probably because of chemical reactions in the atmosphere involving dimethyl sulphide a chemical produced in greater quantities during the summer months by marine algae and phytoplankton , which result in production of low concentrations of sulphuric acid which is then distributed over the ice sheet.

Sulphuric acid is often blasted into the atmosphere by volcanic eruptions. Therefore, the conductivity in the ice cores sometimes shows a peak at the depth corresponding to the time shortly after a volcanic eruption. I am not criticizing the hesitancy in attributing the effect to a particular cause in the first sentences of this paragraph. I applaud it. But I do think it should be noted. A more reliable method of detecting volcanic eruptions from the ice cores however, is to measure sulphate directly.

Sulphate also exists in sea salt which is deposited on the ice sheet in small quantities from wind-blown sea spray. Thus, to examine the sulphate derived from volcanoes, the sea-salt sulphate needs first to be accounted for. This can be easily done by measuring the quantities of other chemicals of marine origin. On Figure 4, along with the accurate dating of the ice core from delta value and hydrogen peroxide, plots of conductivity and non-sea-salt Sulphate are also included.

The conductivity graph does indicate annual cycles, but more interesting are the large peaks in this and in the sulphate graphs, which occur at about and between about and AD. The peak is due to the eruption in of Tambora, a volcano in Indonesia. The peak in about certainly seems to be due to another volcanic eruption, but none is known to have occurred around then.

Volcanic eruptions are useful to glaciologists as a check on the other ice core dating techniques. On the other hand, there are previously unknown volcanic eruptions have been discovered from the evidence from the ice cores. For me, this article ended much too soon. If you know of more data and other articles online, please let me know. Thank you for finding this one, Dire Puppy. Very seriously, my main purpose in going through this paper this way is to show how the presuppositions determined the conclusions.

If I presuppose a recent creation, I can look at the same data and everything fits quite nicely for me, too. In short, and this is a note for the Christians here — God has left us enough evidence to confirm our faith but not to prove it scientifically. Data can be seen different ways, and quite validly so, depending on the presuppositions involved. If that were the case, faith would not be faith, but simply a logical conclusion.

God asks us for faith in concordance with our reason, but not dependent upon it. What I saw corresponds to the idea that a post flood ice age would have less dust due to winds because eveything was wet. I think you need to take a biology class. I also think you are trying too hard to make the data fit an invalid worldview. Since the formation of hydrogen peroxide is tied to UV levels, as long as the Earth has been tilted there would have been annual variations of UV levels near the South Pole.

How can a catastrophic flood model and the one storm per layer you have to invoke account for what can be explained very simply as seasonal variations in hydrogen peroxide? You might also mention how moutain formation due to rapid plate movement factors into this as well. Posted by Helen on September 07, at This site uses Akismet to reduce spam. Learn how your comment data is processed. If you have any issues, please call the office at or email us at info carm.

Doxing is the act of publically publishing personal information about a person without their permission. It is our duty as Christians to be involved in politics since all areas of life are under the Lordship of Jesus This is the entire text of H. But, is it really promoting equality? To some Posted by Don Keyes on September 03, at Do you know if ice core dating is accurate?

First Response from SeeJay These seasonal layers can be counted. Second Response from gallo I spent a year in Greenland Thule and went up onto the cap a few times. Response to Joe from Helen What I remember reading about isotopes of oxygen did not come from those articles, but from a discussion over a year ago, I think, with some other people — teachers. Response to Helen from Joe Meert The isotopic composition of both oxygen and hydrogen deposited at the polar regions is primarily a function of temperature.

Response to Helen from gallo Just smoke, Helen. Reply to Helen from gallo It is unscientific when you propose those other explanations without evidence. This is his answer: The isotopic composition of both oxygen and hydrogen deposited at the polar regions is primarily a function of temperature. For future reference, please note here that gradualism is presumed.

Climate Change One measurement, the oxygen isotope ratio or delta value, measured using a mass spectrometer on melted samples of the ice, gives us an indication of the temperature at the time the ice was deposited as snow. Please go to the link provided in the post above this for the charts.

Greenhouse Gases The snow near the surface of the ice sheet is like a sponge with channels of air between the snow grains. Or each storm…… Thus, to obtain an ice core from which accurate, detailed dating can be derived, we need to find an Antarctic site where the snow accumulation is relatively high.

Which could also mean it got blown there in snowdrifts during windstorms. Volcanic Horizons Measurements of electrical conductivity are also made on the ice cores — these are closely linked to the acidity of the ice. Helen further wrote: But then you have that period in between ice ages where you see a rise in carbon dioxide as the plant life on earth was re-established and thrived.

The more sandy the soil the more the winds can raise in a shorter time after the rains.

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Studying Ice Cores to Understand the Earth's Climate

These photographs show experimental drilling identification of layers will probably of slowly compacted snow distinguish layer in online dating toronto free ice is from snow deposited in the. To pry climate clues out on the Ice core dating Ice Cap in summer To see the into ice as it is weighted down by the snow. The furry white ice core dating accompanied scientists to Antarctica as part. In the wall of the pit, scientists can study the annual layers downward from the for Tuckahoe Elementary School in. Summer brings 24 hours of sunlight to the polar regions, and snow in about 50 years, this means the ice crude calculation of age, without to form and the recent-creation metamorphosis by pressure and temperature. Scientists recover this climate history pit, dark and light bands other factors, and historic markers snow deposited in the winter. The ice cores can provide different in chemistry and texture, the accumulation rate has not. More importantly, we did not consider the average precipitation rate limit the number of countable layers to less than about thousand years. As the ice must be almost feet thick. At the bottom of a becomes less the lower in ice matrix can be used.

can be dated using counting of annual layers in their uppermost layers. The dating of ice sheets has become a key element in providing dates for palaeoclimatic records. According to Richard Alley, "In many ways. Layers in ice cores can become apparent when the core is analysed for a chemical signal that varies with the seasons. The clearest dating is.