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  • 1
    Publication Date: 2023-07-10
    Keywords: Accumulation of snow/ice per year; Age, difference; Age, relative, number of years; Antarctica; Antarctica, west; Core; DML; Dronning Maud Land, Antarctica; Event label; ICEDRILL; Ice drill; Latitude of event; Law_Dome; Longitude of event; Reference/source; Temperature, air, annual mean; WAIS Divide Ice Core; WDC05A
    Type: Dataset
    Format: text/tab-separated-values, 24 data points
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  • 2
    Publication Date: 2023-07-10
    Keywords: Antarctica; Antarctica, west; Carbon dioxide; Carbon dioxide, standard error; Core; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Event label; ICEDRILL; Ice drill; Laboratory; Latitude of event; Law_Dome; Longitude of event; Number of subsamples; WAIS Divide Ice Core; WDC05A
    Type: Dataset
    Format: text/tab-separated-values, 52 data points
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  • 3
    Publication Date: 2024-03-18
    Keywords: Conductivity, electrical, current; DEPTH, ice/snow; DRILL; Drilling/drill rig; GISP; GISP2-B; Greenland Ice Core Projects; GRIP/GISP/NGRIP; Sampling/drilling ice
    Type: Dataset
    Format: text/tab-separated-values, 32323 data points
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  • 4
    Publication Date: 2024-03-18
    Keywords: AGE; Calculated; Conductivity, electrical, ice; DEPTH, ice/snow; DRILL; Drilling/drill rig; GISP; GISP2; Greenland Ice Core Projects; GRIP/GISP/NGRIP; Sampling/drilling ice
    Type: Dataset
    Format: text/tab-separated-values, 5488 data points
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  • 5
    Publication Date: 2024-03-18
    Keywords: Conductivity, electrical, current; DEPTH, ice/snow; DRILL; Drilling/drill rig; GISP; GISP2-D; Greenland Ice Core Projects; GRIP/GISP/NGRIP; Sampling/drilling ice
    Type: Dataset
    Format: text/tab-separated-values, 2372386 data points
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  • 6
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    PANGAEA
    In:  Supplement to: Steig, Eric J; Ding, Quinghua; White, James W C; Küttel, Meinrad; Rupper, Summer B; Neumann, T A; Neff, Peter D; Gallant, Ailie J E; Mayewski, Paul Andrew; Taylor, Kendrick C; Hoffmann, Georg; Dixon, Daniel A; Schoenemann, Spruce W; Markle, Bradley R; Fudge, Tyler J; Schneider, David P; Schauer, Andrew J; Teel, Rebecca P; Vaughn, Bruce H; Burgener, Landon; Williams, Jessica; Korotkikh, Elena (2013): Recent climate and ice-sheet changes in West Antarctica compared with the past 2,000 years. Nature Geoscience, 6(5), 372-375, https://doi.org/10.1038/NGEO1778
    Publication Date: 2024-03-18
    Description: Changes in atmospheric circulation over the past five decades have enhanced the wind-driven inflow of warm ocean water onto the Antarctic continental shelf, where it melts ice shelves from below. Atmospheric circulation changes have also caused rapid warming over the West Antarctic Ice Sheet, and contributed to declining sea-ice cover in the adjacent Amundsen-Bellingshausen seas. It is unknown whether these changes are part of a longer-term trend. Here, we use water-isotope (d18O) data from an array of ice-core records to place recent West Antarctic climate changes in the context of the past two millennia. We find that the d18O of West Antarctic precipitation has increased significantly in the past 50 years, in parallel with the trend in temperature, and was probably more elevated during the 1990s than at any other time during the past 200 years. However, d18O anomalies comparable to those of recent decades occur about 1% of the time over the past 2,000 years. General circulation model simulations suggest that recent trends in d18O and climate in West Antarctica cannot be distinguished from decadal variability that originates in the tropics. We conclude that the uncertain trajectory of tropical climate variability represents a significant source of uncertainty in projections of West Antarctic climate and ice-sheet change.
    Keywords: Antarctica, west; DEPTH, ice/snow; ICEDRILL; Ice drill; WAIS_divide; δ18O, water
    Type: Dataset
    Format: text/tab-separated-values, 601 data points
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  • 7
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    PANGAEA
    In:  Supplement to: Ahn, Jinho; Brook, Edward J; Mitchell, Logan E; Rosen, Julia L; McConnell, Joseph R; Taylor, Kendrick C; Etheridge, David; Rubino, Mauro (2012): Atmospheric CO2 over the last 1000 years: A high-resolution record from the West Antarctic Ice Sheet (WAIS) Divide ice core. Global Biogeochemical Cycles, 26(2), GB2027, https://doi.org/10.1029/2011GB004247
    Publication Date: 2023-12-13
    Description: We report a decadally resolved record of atmospheric CO2 concentration for the last 1000 years, obtained from the West Antarctic Ice Sheet (WAIS) Divide shallow ice core. The most prominent feature of the pre-industrial period is a rapid ~7 ppm decrease of CO2 in a span of ~20-50 years at ~1600 A.D. This observation confirms the timing of an abrupt atmospheric CO2 decrease of ~10 ppm observed for that time period in the Law Dome ice core CO2 records, but the true magnitude of the decrease remains unclear. Atmospheric CO2 variations over the time period 1000-1800 A.D. are statistically correlated with northern hemispheric climate and tropical Indo-Pacific sea surface temperature. However, the exact relationship between CO2 and climate remains elusive due to regional climate variations and/or uneven geographical data density of paleoclimate records. We observe small differences of 0 ~2% (0 ~ 6 ppm) among the high-precision CO2 records from the Law Dome, EPICA Dronning Maud Land and WAIS Divide Antarctic ice cores. However, those records share common trends of CO2 change on centennial to multicentennial time scales, and clearly show that atmospheric CO2 has been increasing above preindustrial levels since ~1850 A.D.
    Keywords: International Polar Year (2007-2008); IPY
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 8
    Publication Date: 2024-04-05
    Description: The West Antarctic Ice Sheet (WAIS) Divide deep ice core WD2014 chronology, consisting of ice age, gas age, delta-age and uncertainties therein. The West Antarctic Ice Sheet Divide (WAIS Divide, WD) ice core is a newly drilled, high-accumulation deep ice core that provides Antarctic climate records of the past ~68 ka at unprecedented temporal resolution. The upper 2850 m (back to 31.2 ka BP; Sigl et al., 2015, Sigl et al., 2016) have been dated using annual-layer counting based on counting of annual layers observed in the chemical, dust and electrical conductivity records. The measurements were interpreted manually and with the aid of two automated methods. We validated the chronology by comparing of the cosmogenic isotope records of 10Be from WAIS Divide and 14C for IntCal13. We demonstrated that over the Holocene WD2014 was consistently accurate to better than 0.5% of the age. The chronology for the deep part of the core (below 2850m; 67.8-31.2 ka BP; Buizert et al., 2015) is based on stratigraphic matching to annual-layer-counted Greenland ice cores using globally well-mixed atmospheric methane. We calculate the WD gas age-ice age difference (Delta age) using a combination of firn densification modeling, ice-flow modeling, and a data set of d15N-N2, a proxy for past firn column thickness. The largest Delta age at WD occurs during the Last Glacial Maximum, and is 525 +/- 120 years. We synchronized the WD chronology to a linearly scaled version of the layer-counted Greenland Ice Core Chronology (GICC05), which brings the age of Dansgaard-Oeschger (DO) events into agreement with the U/Th absolutely dated Hulu Cave speleothem record.
    Keywords: Age, difference; Age, difference error; Age, error; annual-layer-counting; Antarctica; Antarctica, west; Calendar age; Calendar age, standard error; chronology; DEPTH, ice/snow; Gas age; Greenland; ice-core; ICEDRILL; Ice drill; Methane; WAIS; WAIS Divide; WDC-06A; West Antarctic Ice Sheet Divide ice core project
    Type: Dataset
    Format: text/tab-separated-values, 392326 data points
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  • 9
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Ground water 37 (1999), S. 0 
    ISSN: 1745-6584
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Energy, Environment Protection, Nuclear Power Engineering , Geosciences
    Notes: In regions where ground water flow is restricted to sparse, narrow fractures, productive and nonproductive drilling sites frequently are separated by only a few tens of meters. Drilling success rates are low in these areas because favorable drilling sites occur infrequently and are difficult to identify. The drilling success rate can be increased when imagery and surface geophysics are incorporated into the site selection method. We present a method to evaluate the economic benefit of various site selection methods and show that the use of surface geophysics and aerial photography can reduce drilling costs by approximately a factor of two in an area with a low drilling success rate that is characterized by narrow fracture zones covered with several meters of weathered clays and thick vegetation. The benefits are smaller and less certain when social considerations are a strong factor in site selection.
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Ground water monitoring & remediation 9 (1989), S. 0 
    ISSN: 1745-6592
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Energy, Environment Protection, Nuclear Power Engineering , Geosciences
    Notes: The Geonics EM-39 borehole induction tool was field tested to evaluate its performance under controlled conditions. The effects of temperature changes and borehole fluids were found to be negligible under most conditions. The instrument can be calibrated in large bodies of water of known electrical conductivity. When properly calibrated, the ± 5 percent accuracy claimed by the manufacturer is obtainable. A geologic unit must be at least 4m thick for the electrical conductivity of the unit to be accurately measured. Geologic units thinner than 4m thick can be detected if the conductivity contrast to adjacent units is sufficiently large.
    Type of Medium: Electronic Resource
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