Articles | Volume 16, issue 6
https://doi.org/10.5194/tc-16-2301-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-16-2301-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
15 Jun 2022
Research article |
| 15 Jun 2022
| 15 Jun 2022
Chronostratigraphy of the Larsen blue-ice area in northern Victoria Land, East Antarctica, and its implications for paleoclimate
Giyoon Lee
School of Earth and Environmental Sciences, Seoul National University, Seoul, South Korea
Jinho Ahn
CORRESPONDING AUTHOR
School of Earth and Environmental Sciences, Seoul National University, Seoul, South Korea
Hyeontae Ju
Research Unit of Frontier Exploration, Korea Polar Research Institute, Incheon, South Korea
Florian Ritterbusch
School of Physical Sciences, University of Science and Technology of China, Hefei, China
Ikumi Oyabu
Meteorology and Glaciology Group, Division for Advanced Research Promotion, National Institute of Polar Research, Tokyo, Japan
Christo Buizert
College of Earth, Ocean, and Atmospheric Sciences, Oregon State
University (OSU), Corvallis, OR, USA
Songyi Kim
Division of Glacial Environment Research, Korea Polar Research Institute, Incheon, South Korea
Jangil Moon
Division of Glacial Environment Research, Korea Polar Research Institute, Incheon, South Korea
Sambit Ghosh
School of Earth and Environmental Sciences, Seoul National University, Seoul, South Korea
Kenji Kawamura
Meteorology and Glaciology Group, Division for Advanced Research Promotion, National Institute of Polar Research, Tokyo, Japan
Department of Polar Science, School of Multidisciplinary Sciences, The Graduate University for Advanced Studies (SOKENDAI), Tachikawa, Japan
Japan Agency for Marine-Earth Science and Technology (JAMSTEC),
Yokosuka, Japan
Zheng-Tian Lu
School of Physical Sciences, University of Science and Technology of China, Hefei, China
Sangbum Hong
Division of Glacial Environment Research, Korea Polar Research Institute, Incheon, South Korea
Chang Hee Han
Division of Glacial Environment Research, Korea Polar Research Institute, Incheon, South Korea
Soon Do Hur
Division of Glacial Environment Research, Korea Polar Research Institute, Incheon, South Korea
Wei Jiang
School of Physical Sciences, University of Science and Technology of China, Hefei, China
Guo-Min Yang
School of Physical Sciences, University of Science and Technology of China, Hefei, China
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EGUsphere, https://doi.org/10.5194/egusphere-2024-1003, https://doi.org/10.5194/egusphere-2024-1003, 2024
This preprint is open for discussion and under review for Climate of the Past (CP).
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We use a series of spectral techniques to quantify the strength of high-frequency climate variability in Northeastern Greenland to 50,000 ka before present. Importantly, we find that variability consistently decreases hundreds of years prior to Dansgaard-Oeschger warming events. Model simulations suggest a change in North Atlantic sea ice behavior contributed to this pattern, thus providing new information on the conditions which proceeded abrupt climate change during the Last Glacial Period.
Kumiko Goto-Azuma, Remi Dallmayr, Yoshimi Ogawa-Tsukagawa, Nobuhiro Moteki, Tatsuhiro Mori, Sho Ohata, Yutaka Kondo, Makoto Koike, Motohiro Hirabayashi, Jun Ogata, Kyotaro Kitamura, Kenji Kawamura, Koji Fujita, Sumito Matoba, Naoko Nagatsuka, Akane Tsushima, Kaori Fukuda, and Teruo Aoki
EGUsphere, https://doi.org/10.5194/egusphere-2024-1496, https://doi.org/10.5194/egusphere-2024-1496, 2024
This preprint is open for discussion and under review for Atmospheric Chemistry and Physics (ACP).
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We developed a continuous flow analysis system to analyse an ice core from northwest Greenland, and coupled it with an improved BC measurement technique. This coupling allowed accurate high-resolution analyses of BC particles' size distributions and concentrations with diameters between 70 nm and 4 μm for the past 350 years. Our results provide crucial insights into BC's climatic effects. We also found that previous ice core studies substantially underestimated the BC mass concentrations.
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The Cryosphere, 18, 1647–1652, https://doi.org/10.5194/tc-18-1647-2024, https://doi.org/10.5194/tc-18-1647-2024, 2024
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The age of the surface blue ice in the Grove Mountains area is dated to be about 140 000 years, and one meteorite found here is 260 000 years old. It is inferred that the Grove Mountains blue-ice area holds considerable potential for paleoclimate studies.
Ryo Inoue, Teruo Aoki, Shuji Fujita, Shun Tsutaki, Hideaki Motoyama, Fumio Nakazawa, and Kenji Kawamura
EGUsphere, https://doi.org/10.5194/egusphere-2024-769, https://doi.org/10.5194/egusphere-2024-769, 2024
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We measured the snow specific surface area (SSA) at ~2150 surfaces between the coast near Syowa Station and Dome Fuji, East Antarctica, in 2021–2022 summer. The observed SSA less depends on elevation between 15 and 500 km from the coast and increases toward the dome area beyond the range. SSA varies depending on surface morphologies and meteorological events. The spatial variation of SSA can be explained by snow metamorphism, snowfall frequency, and wind-driven inhibition of snow deposition.
Frédéric Parrenin, Marie Bouchet, Christo Buizert, Emilie Capron, Ellen Corrick, Russell Drysdale, Kenji Kawamura, Amaëlle Landais, Robert Mulvaney, Ikumi Oyabu, and Sune Rasmussen
EGUsphere, https://doi.org/10.5194/egusphere-2023-2911, https://doi.org/10.5194/egusphere-2023-2911, 2024
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The Paleochrono1 probablistic dating model allows to derive a common and optimized chronology for several paleoclimatic sites from various archives (ice cores, speleothems, marine cores, lake cores, etc.). It combines prior sedimentation scenarios with chronological information such as dated horizons, dated intervals, stratigraphic links and (for ice cores) Delta-depth observations. Paleochrono1 is available under the MIT open-source license.
Ryo Inoue, Shuji Fujita, Kenji Kawamura, Ikumi Oyabu, Fumio Nakazawa, Hideaki Motoyama, and Teruo Aoki
The Cryosphere, 18, 425–449, https://doi.org/10.5194/tc-18-425-2024, https://doi.org/10.5194/tc-18-425-2024, 2024
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We measured the density, microstructural anisotropy, and specific surface area (SSA) of six firn cores collected within 60 km of Dome Fuji, Antarctica. We found a lack of significant density increase, development of vertically elongated microstructures, and a rapid decrease in SSA in the top few meters due to the metamorphism driven by water vapor transport under a temperature gradient. We highlight the significant spatial variability in the properties, which depends on the accumulation rate.
Vasilii V. Petrenko, Segev BenZvi, Michael Dyonisius, Benjamin Hmiel, Andrew M. Smith, and Christo Buizert
EGUsphere, https://doi.org/10.5194/egusphere-2023-3126, https://doi.org/10.5194/egusphere-2023-3126, 2024
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This manuscript presents the concept for a new proxy for past variations in the galactic cosmic ray flux (GCR). Past variations in GCR flux are important to understand for interpretation of records of isotopes produced by cosmic rays; these records are used for reconstructing solar variations and past land ice extent. The proxy involves using measurements of 14CO in ice cores, which should provide an uncomplicated and precise estimate of past GCR flux variations for the past few thousand years.
Romilly Harris Stuart, Amaëlle Landais, Laurent Arnaud, Christo Buizert, Emilie Capron, Marie Dumont, Quentin Libois, Robert Mulvaney, Anaïs Orsi, Ghislain Picard, Frédéric Prié, Jeffery Severinghaus, Barbara Stenni, and Patricia Martinerie
EGUsphere, https://doi.org/10.5194/egusphere-2023-2585, https://doi.org/10.5194/egusphere-2023-2585, 2023
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The influence of local accumulation rate and temperature on δO2/N2 ice core records, a key dating tool, are not fully understood, but required for a full mechanistic understanding. We show evidence that mean δO2/N2 is strongly dependent on local accumulation rate and temperature, in addition to the well documented insolation dependence. Snowpack modelling is used to investigate which physical properties drive the mechanistic dependence on these local parameters.
Jenna A. Epifanio, Edward J. Brook, Christo Buizert, Erin C. Pettit, Jon S. Edwards, John M. Fegyveresi, Todd A. Sowers, Jeffrey P. Severinghaus, and Emma C. Kahle
The Cryosphere, 17, 4837–4851, https://doi.org/10.5194/tc-17-4837-2023, https://doi.org/10.5194/tc-17-4837-2023, 2023
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The total air content (TAC) of polar ice cores has long been considered a potential proxy for past ice sheet elevation. This study presents a high-resolution record of TAC from the South Pole ice core. The record reveals orbital- and millennial-scale variability that cannot be explained by elevation changes. The orbital- and millennial-scale changes are likely a product of firn grain metamorphism near the surface of the ice sheet, due to summer insolation changes or local accumulation changes.
Marie Bouchet, Amaëlle Landais, Antoine Grisart, Frédéric Parrenin, Frédéric Prié, Roxanne Jacob, Elise Fourré, Emilie Capron, Dominique Raynaud, Vladimir Ya Lipenkov, Marie-France Loutre, Thomas Extier, Anders Svensson, Etienne Legrain, Patricia Martinerie, Markus Leuenberger, Wei Jiang, Florian Ritterbusch, Zheng-Tian Lu, and Guo-Min Yang
Clim. Past, 19, 2257–2286, https://doi.org/10.5194/cp-19-2257-2023, https://doi.org/10.5194/cp-19-2257-2023, 2023
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A new federative chronology for five deep polar ice cores retrieves 800 000 years of past climate variations with improved accuracy. Precise ice core timescales are key to studying the mechanisms linking changes in the Earth’s orbit to the diverse climatic responses (temperature and atmospheric greenhouse gas concentrations). To construct the chronology, new measurements from the oldest continuous ice core as well as glaciological modeling estimates were combined in a statistical model.
Benjamin Hmiel, Vasilii V. Petrenko, Christo Buizert, Andrew M. Smith, Michael N. Dyonisius, Philip Place, Bin Yang, Quan Hua, Ross Beaudette, Jeffrey P. Severinghaus, Christina Harth, Ray F. Weiss, Lindsey Davidge, Melisa Diaz, Matthew Pacicco, James A. Menking, Michael Kalk, Xavier Faïn, Alden Adolph, Isaac Vimont, and Lee T. Murray
The Cryosphere Discuss., https://doi.org/10.5194/tc-2023-121, https://doi.org/10.5194/tc-2023-121, 2023
Revised manuscript accepted for TC
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The main aim of this research is to improve understanding of carbon-14 that is produced by cosmic rays in ice sheets. Measurements of carbon-14 in ice cores can provide a range of useful information (age of ice, past atmospheric chemistry, past cosmic ray intensity). Our results show that almost all (approx. 95 %) of carbon-14 that is produced in the upper layer of ice sheets is rapidly lost to the atmosphere. Our results also provide better estimates of carbon-14 production rates in deeper ice.
Benoit S. Lecavalier, Lev Tarasov, Greg Balco, Perry Spector, Claus-Dieter Hillenbrand, Christo Buizert, Catherine Ritz, Marion Leduc-Leballeur, Robert Mulvaney, Pippa L. Whitehouse, Michael J. Bentley, and Jonathan Bamber
Earth Syst. Sci. Data, 15, 3573–3596, https://doi.org/10.5194/essd-15-3573-2023, https://doi.org/10.5194/essd-15-3573-2023, 2023
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The Antarctic Ice Sheet Evolution constraint database version 2 (AntICE2) consists of a large variety of observations that constrain the evolution of the Antarctic Ice Sheet over the last glacial cycle. This includes observations of past ice sheet extent, past ice thickness, past relative sea level, borehole temperature profiles, and present-day bedrock displacement rates. The database is intended to improve our understanding of past Antarctic changes and for ice sheet model calibrations.
Takashi Obase, Ayako Abe-Ouchi, Fuyuki Saito, Shun Tsutaki, Shuji Fujita, Kenji Kawamura, and Hideaki Motoyama
The Cryosphere, 17, 2543–2562, https://doi.org/10.5194/tc-17-2543-2023, https://doi.org/10.5194/tc-17-2543-2023, 2023
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We use a one-dimensional ice-flow model to examine the most suitable core location near Dome Fuji (DF), Antarctica. This model computes the temporal evolution of age and temperature from past to present. We investigate the influence of different parameters of climate and ice sheet on the ice's basal age and compare the results with ground radar surveys. We find that the local ice thickness primarily controls the age because it is critical to the basal melting, which can eliminate the old ice.
Christo Buizert, Sarah Shackleton, Jeffrey P. Severinghaus, William H. G. Roberts, Alan Seltzer, Bernhard Bereiter, Kenji Kawamura, Daniel Baggenstos, Anaïs J. Orsi, Ikumi Oyabu, Benjamin Birner, Jacob D. Morgan, Edward J. Brook, David M. Etheridge, David Thornton, Nancy Bertler, Rebecca L. Pyne, Robert Mulvaney, Ellen Mosley-Thompson, Peter D. Neff, and Vasilii V. Petrenko
Clim. Past, 19, 579–606, https://doi.org/10.5194/cp-19-579-2023, https://doi.org/10.5194/cp-19-579-2023, 2023
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It is unclear how different components of the global atmospheric circulation, such as the El Niño effect, respond to large-scale climate change. We present a new ice core gas proxy, called krypton-86 excess, that reflects past storminess in Antarctica. We present data from 11 ice cores that suggest the new proxy works. We present a reconstruction of changes in West Antarctic storminess over the last 24 000 years and suggest these are caused by north–south movement of the tropical rain belt.
Michael N. Dyonisius, Vasilii V. Petrenko, Andrew M. Smith, Benjamin Hmiel, Peter D. Neff, Bin Yang, Quan Hua, Jochen Schmitt, Sarah A. Shackleton, Christo Buizert, Philip F. Place, James A. Menking, Ross Beaudette, Christina Harth, Michael Kalk, Heidi A. Roop, Bernhard Bereiter, Casey Armanetti, Isaac Vimont, Sylvia Englund Michel, Edward J. Brook, Jeffrey P. Severinghaus, Ray F. Weiss, and Joseph R. McConnell
The Cryosphere, 17, 843–863, https://doi.org/10.5194/tc-17-843-2023, https://doi.org/10.5194/tc-17-843-2023, 2023
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Cosmic rays that enter the atmosphere produce secondary particles which react with surface minerals to produce radioactive nuclides. These nuclides are often used to constrain Earth's surface processes. However, the production rates from muons are not well constrained. We measured 14C in ice with a well-known exposure history to constrain the production rates from muons. 14C production in ice is analogous to quartz, but we obtain different production rates compared to commonly used estimates.
Ikumi Oyabu, Kenji Kawamura, Shuji Fujita, Ryo Inoue, Hideaki Motoyama, Kotaro Fukui, Motohiro Hirabayashi, Yu Hoshina, Naoyuki Kurita, Fumio Nakazawa, Hiroshi Ohno, Konosuke Sugiura, Toshitaka Suzuki, Shun Tsutaki, Ayako Abe-Ouchi, Masashi Niwano, Frédéric Parrenin, Fuyuki Saito, and Masakazu Yoshimori
Clim. Past, 19, 293–321, https://doi.org/10.5194/cp-19-293-2023, https://doi.org/10.5194/cp-19-293-2023, 2023
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We reconstructed accumulation rate around Dome Fuji, Antarctica, over the last 5000 years from 15 shallow ice cores and seven snow pits. We found a long-term decreasing trend in the preindustrial period, which may be associated with secular surface cooling and sea ice expansion. Centennial-scale variations were also found, which may partly be related to combinations of volcanic, solar and greenhouse gas forcings. The most rapid and intense increases of accumulation rate occurred since 1850 CE.
Jinhwa Shin, Jinho Ahn, Jai Chowdhry Beeman, Hun-Gyu Lee, Jaemyeong Mango Seo, and Edward J. Brook
Clim. Past, 18, 2063–2075, https://doi.org/10.5194/cp-18-2063-2022, https://doi.org/10.5194/cp-18-2063-2022, 2022
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We present a new and highly resolved atmospheric CO2 record from the Siple Dome ice core, Antarctica, over the early Holocene (11.7–7.4 ka). Atmospheric CO2 decreased by ~10 ppm from 10.9 to 7.3 ka, but the decrease was punctuated by local minima at 11.1, 10.1, 9.1, and 8.3 ka. We found millennial CO2 variability of 2–6 ppm, and the millennial CO2 variations correlate with proxies for solar forcing and local climate in the Southern Ocean, North Atlantic, and eastern equatorial Pacific.
Shun Tsutaki, Shuji Fujita, Kenji Kawamura, Ayako Abe-Ouchi, Kotaro Fukui, Hideaki Motoyama, Yu Hoshina, Fumio Nakazawa, Takashi Obase, Hiroshi Ohno, Ikumi Oyabu, Fuyuki Saito, Konosuke Sugiura, and Toshitaka Suzuki
The Cryosphere, 16, 2967–2983, https://doi.org/10.5194/tc-16-2967-2022, https://doi.org/10.5194/tc-16-2967-2022, 2022
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We constructed an ice thickness map across the Dome Fuji region, East Antarctica, from improved radar data and previous data that had been collected since the late 1980s. The data acquired using the improved radar systems allowed basal topography to be identified with higher accuracy. The new ice thickness data show the bedrock topography, particularly the complex terrain of subglacial valleys and highlands south of Dome Fuji, with substantially high detail.
Jacob D. Morgan, Christo Buizert, Tyler J. Fudge, Kenji Kawamura, Jeffrey P. Severinghaus, and Cathy M. Trudinger
The Cryosphere, 16, 2947–2966, https://doi.org/10.5194/tc-16-2947-2022, https://doi.org/10.5194/tc-16-2947-2022, 2022
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The composition of air bubbles in Antarctic ice cores records information about past changes in properties of the snowpack. We find that, near the South Pole, thinner snowpack in the past is often due to steeper surface topography, in which faster winds erode the snow and deposit it in flatter areas. The slope and wind seem to also cause a seasonal bias in the composition of air bubbles in the ice core. These findings will improve interpretation of other ice cores from places with steep slopes.
Taku Umezawa, Satoshi Sugawara, Kenji Kawamura, Ikumi Oyabu, Stephen J. Andrews, Takuya Saito, Shuji Aoki, and Takakiyo Nakazawa
Atmos. Chem. Phys., 22, 6899–6917, https://doi.org/10.5194/acp-22-6899-2022, https://doi.org/10.5194/acp-22-6899-2022, 2022
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Greenhouse gas methane in the Arctic atmosphere has not been accurately reported for 1900–1980 from either direct observations or ice core reconstructions. By using trace gas data from firn (compacted snow layers above ice sheet), air samples at two Greenland sites, and a firn air transport model, this study suggests a likely range of the Arctic methane reconstruction for the 20th century. Atmospheric scenarios from two previous studies are also evaluated for consistency with the firn data sets.
Ikumi Oyabu, Kenji Kawamura, Tsutomu Uchida, Shuji Fujita, Kyotaro Kitamura, Motohiro Hirabayashi, Shuji Aoki, Shinji Morimoto, Takakiyo Nakazawa, Jeffrey P. Severinghaus, and Jacob D. Morgan
The Cryosphere, 15, 5529–5555, https://doi.org/10.5194/tc-15-5529-2021, https://doi.org/10.5194/tc-15-5529-2021, 2021
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We present O2/N2 and Ar/N2 records from the Dome Fuji ice core through the bubbly ice, bubble–clathrate transition, and clathrate ice zones without gas-loss fractionation. The insolation signal is preserved through the clathrate formation. The relationship between Ar/Ν2 and Ο2/Ν2 suggests that the fractionation for the bubble–clathrate transition is mass independent, while the bubble close-off process involves a combination of mass-independent and mass-dependent fractionation for O2 and Ar.
Sarah Shackleton, James A. Menking, Edward Brook, Christo Buizert, Michael N. Dyonisius, Vasilii V. Petrenko, Daniel Baggenstos, and Jeffrey P. Severinghaus
Clim. Past, 17, 2273–2289, https://doi.org/10.5194/cp-17-2273-2021, https://doi.org/10.5194/cp-17-2273-2021, 2021
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In this study, we measure atmospheric noble gases trapped in ice cores to reconstruct ocean temperature during the last glaciation. Comparing the new reconstruction to other climate records, we show that the ocean reached its coldest temperatures before ice sheets reached maximum volumes and atmospheric CO2 reached its lowest concentrations. Ocean cooling played a major role in lowering atmospheric CO2 early in the glaciation, but it only played a minor role later.
Raffaello Nardin, Mirko Severi, Alessandra Amore, Silvia Becagli, Francois Burgay, Laura Caiazzo, Virginia Ciardini, Giuliano Dreossi, Massimo Frezzotti, Sang-Bum Hong, Ishaq Khan, Bianca Maria Narcisi, Marco Proposito, Claudio Scarchilli, Enricomaria Selmo, Andrea Spolaor, Barbara Stenni, and Rita Traversi
Clim. Past, 17, 2073–2089, https://doi.org/10.5194/cp-17-2073-2021, https://doi.org/10.5194/cp-17-2073-2021, 2021
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The first step to exploit all the potential information buried in ice cores is to produce a reliable age scale. Based on chemical and isotopic records from the 197 m Antarctic GV7(B) ice core, accurate dating was achieved and showed that the archive spans roughly the last 830 years. The relatively high accumulation rate allowed us to use the non-sea-salt sulfate seasonal pattern to count annual layers. The accumulation rate reconstruction exhibited a slight increase since the 18th century.
Ikumi Oyabu, Kenji Kawamura, Kyotaro Kitamura, Remi Dallmayr, Akihiro Kitamura, Chikako Sawada, Jeffrey P. Severinghaus, Ross Beaudette, Anaïs Orsi, Satoshi Sugawara, Shigeyuki Ishidoya, Dorthe Dahl-Jensen, Kumiko Goto-Azuma, Shuji Aoki, and Takakiyo Nakazawa
Atmos. Meas. Tech., 13, 6703–6731, https://doi.org/10.5194/amt-13-6703-2020, https://doi.org/10.5194/amt-13-6703-2020, 2020
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Air in polar ice cores provides information on past atmosphere and climate. We present a new method for simultaneously measuring eight gases (CH4, N2O and CO2 concentrations; isotopic ratios of N2 and O2; elemental ratios between N2, O2 and Ar; and total air content) from single ice-core samples with high precision.
Jenna A. Epifanio, Edward J. Brook, Christo Buizert, Jon S. Edwards, Todd A. Sowers, Emma C. Kahle, Jeffrey P. Severinghaus, Eric J. Steig, Dominic A. Winski, Erich C. Osterberg, Tyler J. Fudge, Murat Aydin, Ekaterina Hood, Michael Kalk, Karl J. Kreutz, David G. Ferris, and Joshua A. Kennedy
Clim. Past, 16, 2431–2444, https://doi.org/10.5194/cp-16-2431-2020, https://doi.org/10.5194/cp-16-2431-2020, 2020
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A new ice core drilled at the South Pole provides a 54 000-year paleo-environmental record including the composition of the past atmosphere. This paper describes the gas chronology for the South Pole ice core, based on a high-resolution methane record. The new gas chronology, in combination with the existing ice age scale from Winski et al. (2019), allows a model-independent reconstruction of the delta age record.
James E. Lee, Edward J. Brook, Nancy A. N. Bertler, Christo Buizert, Troy Baisden, Thomas Blunier, V. Gabriela Ciobanu, Howard Conway, Dorthe Dahl-Jensen, Tyler J. Fudge, Richard Hindmarsh, Elizabeth D. Keller, Frédéric Parrenin, Jeffrey P. Severinghaus, Paul Vallelonga, Edwin D. Waddington, and Mai Winstrup
Clim. Past, 16, 1691–1713, https://doi.org/10.5194/cp-16-1691-2020, https://doi.org/10.5194/cp-16-1691-2020, 2020
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The Roosevelt Island ice core was drilled to investigate climate from the eastern Ross Sea, West Antarctica. We describe the ice age-scale and gas age-scale of the ice core for 0–763 m (83 000 years BP). Old ice near the bottom of the core implies the ice dome existed throughout the last glacial period and that ice streaming was active in the region. Variations in methane, similar to those used as evidence of early human influence on climate, were observed prior to significant human populations.
Anders Svensson, Dorthe Dahl-Jensen, Jørgen Peder Steffensen, Thomas Blunier, Sune O. Rasmussen, Bo M. Vinther, Paul Vallelonga, Emilie Capron, Vasileios Gkinis, Eliza Cook, Helle Astrid Kjær, Raimund Muscheler, Sepp Kipfstuhl, Frank Wilhelms, Thomas F. Stocker, Hubertus Fischer, Florian Adolphi, Tobias Erhardt, Michael Sigl, Amaelle Landais, Frédéric Parrenin, Christo Buizert, Joseph R. McConnell, Mirko Severi, Robert Mulvaney, and Matthias Bigler
Clim. Past, 16, 1565–1580, https://doi.org/10.5194/cp-16-1565-2020, https://doi.org/10.5194/cp-16-1565-2020, 2020
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We identify signatures of large bipolar volcanic eruptions in Greenland and Antarctic ice cores during the last glacial period, which allows for a precise temporal alignment of the ice cores. Thereby the exact timing of unexplained, abrupt climatic changes occurring during the last glacial period can be determined in a global context. The study thus provides a step towards a full understanding of elements of the climate system that may also play an important role in the future.
Jinyoung Jung, Sang-Bum Hong, Meilian Chen, Jin Hur, Liping Jiao, Youngju Lee, Keyhong Park, Doshik Hahm, Jung-Ok Choi, Eun Jin Yang, Jisoo Park, Tae-Wan Kim, and SangHoon Lee
Atmos. Chem. Phys., 20, 5405–5424, https://doi.org/10.5194/acp-20-5405-2020, https://doi.org/10.5194/acp-20-5405-2020, 2020
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Characteristics of atmospheric sulfur and organic carbon species in marine aerosols and the environmental factors influencing their distributions were investigated over the Southern Ocean and the Amundsen Sea, Antarctica, during austral summer. The simultaneous measurements of chemical species in aerosols as well as the chemical and biological properties of seawater in the Amundsen Sea allowed for a better understanding of the effect of the ocean ecosystem on marine aerosols.
Ji-Woong Yang, Jinho Ahn, Go Iwahana, Sangyoung Han, Kyungmin Kim, and Alexander Fedorov
The Cryosphere, 14, 1311–1324, https://doi.org/10.5194/tc-14-1311-2020, https://doi.org/10.5194/tc-14-1311-2020, 2020
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Thawing permafrost may lead to decomposition of soil carbon and nitrogen and emission of greenhouse gases. Thus, methane and nitrous oxide compositions in ground ice may provide information on their production mechanisms in permafrost. We test conventional wet and dry extraction methods. We find that both methods extract gas from the easily extractable parts of the ice and yield similar results for mixing ratios. However, both techniques are unable to fully extract gas from the ice.
Dominic A. Winski, Tyler J. Fudge, David G. Ferris, Erich C. Osterberg, John M. Fegyveresi, Jihong Cole-Dai, Zayta Thundercloud, Thomas S. Cox, Karl J. Kreutz, Nikolas Ortman, Christo Buizert, Jenna Epifanio, Edward J. Brook, Ross Beaudette, Jeffrey Severinghaus, Todd Sowers, Eric J. Steig, Emma C. Kahle, Tyler R. Jones, Valerie Morris, Murat Aydin, Melinda R. Nicewonger, Kimberly A. Casey, Richard B. Alley, Edwin D. Waddington, Nels A. Iverson, Nelia W. Dunbar, Ryan C. Bay, Joseph M. Souney, Michael Sigl, and Joseph R. McConnell
Clim. Past, 15, 1793–1808, https://doi.org/10.5194/cp-15-1793-2019, https://doi.org/10.5194/cp-15-1793-2019, 2019
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A deep ice core was recently drilled at the South Pole to understand past variations in the Earth's climate. To understand the information contained within the ice, we present the relationship between the depth and age of the ice in the South Pole Ice Core. We found that the oldest ice in our record is from 54 302 ± 519 years ago. Our results show that, on average, 7.4 cm of snow falls at the South Pole each year.
Youngjoon Jang, Sang Bum Hong, Christo Buizert, Hun-Gyu Lee, Sang-Young Han, Ji-Woong Yang, Yoshinori Iizuka, Akira Hori, Yeongcheol Han, Seong Joon Jun, Pieter Tans, Taejin Choi, Seong-Joong Kim, Soon Do Hur, and Jinho Ahn
The Cryosphere, 13, 2407–2419, https://doi.org/10.5194/tc-13-2407-2019, https://doi.org/10.5194/tc-13-2407-2019, 2019
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We can learn how human activity altered atmospheric air from the interstitial air in the porous snow layer (firn) on top of glaciers. However, old firn air (> 55 years) was observed only at sites where surface temperatures and snow accumulation rates are very low, such as the South Pole. In this study, we report an unusually old firn air with CO2 age of 93 years from Styx Glacier, near the Ross Sea coast in Antarctica. We hypothesize that the large snow density variations increase firn air ages.
Laurie Menviel, Emilie Capron, Aline Govin, Andrea Dutton, Lev Tarasov, Ayako Abe-Ouchi, Russell N. Drysdale, Philip L. Gibbard, Lauren Gregoire, Feng He, Ruza F. Ivanovic, Masa Kageyama, Kenji Kawamura, Amaelle Landais, Bette L. Otto-Bliesner, Ikumi Oyabu, Polychronis C. Tzedakis, Eric Wolff, and Xu Zhang
Geosci. Model Dev., 12, 3649–3685, https://doi.org/10.5194/gmd-12-3649-2019, https://doi.org/10.5194/gmd-12-3649-2019, 2019
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As part of the Past Global Changes (PAGES) working group on Quaternary Interglacials, we propose a protocol to perform transient simulations of the penultimate deglaciation for the Paleoclimate Modelling Intercomparison Project (PMIP4). This design includes time-varying changes in orbital forcing, greenhouse gas concentrations, continental ice sheets as well as freshwater input from the disintegration of continental ice sheets. Key paleo-records for model-data comparison are also included.
Jens Mühle, Cathy M. Trudinger, Luke M. Western, Matthew Rigby, Martin K. Vollmer, Sunyoung Park, Alistair J. Manning, Daniel Say, Anita Ganesan, L. Paul Steele, Diane J. Ivy, Tim Arnold, Shanlan Li, Andreas Stohl, Christina M. Harth, Peter K. Salameh, Archie McCulloch, Simon O'Doherty, Mi-Kyung Park, Chun Ok Jo, Dickon Young, Kieran M. Stanley, Paul B. Krummel, Blagoj Mitrevski, Ove Hermansen, Chris Lunder, Nikolaos Evangeliou, Bo Yao, Jooil Kim, Benjamin Hmiel, Christo Buizert, Vasilii V. Petrenko, Jgor Arduini, Michela Maione, David M. Etheridge, Eleni Michalopoulou, Mike Czerniak, Jeffrey P. Severinghaus, Stefan Reimann, Peter G. Simmonds, Paul J. Fraser, Ronald G. Prinn, and Ray F. Weiss
Atmos. Chem. Phys., 19, 10335–10359, https://doi.org/10.5194/acp-19-10335-2019, https://doi.org/10.5194/acp-19-10335-2019, 2019
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We discuss atmospheric concentrations and emissions of the strong greenhouse gas perfluorocyclobutane. A large fraction of recent emissions stem from China, India, and Russia, probably as a by-product from the production of fluoropolymers and fluorochemicals. Most historic emissions likely stem from developed countries. Total emissions are higher than what is being reported. Clearly, more measurements and better reporting are needed to understand emissions of this and other greenhouse gases.
Eunho Jang, Ki-Tae Park, Young Jun Yoon, Tae-Wook Kim, Sang-Bum Hong, Silvia Becagli, Rita Traversi, Jaeseok Kim, and Yeontae Gim
Atmos. Chem. Phys., 19, 7595–7608, https://doi.org/10.5194/acp-19-7595-2019, https://doi.org/10.5194/acp-19-7595-2019, 2019
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We reported long-term observations (from 2009 to 2016) of the nanoparticles measured at the Antarctic Peninsula (62.2° S, 58.8° W), and satellite-derived estimates of the biological characteristics were analyzed to identify the link between new particle formation and marine biota. The key finding from this research is that the formation of nanoparticles was strongly associated not only with the biomass of phytoplankton but, more importantly, also its taxonomic composition in the Antarctic Ocean.
Jai Chowdhry Beeman, Léa Gest, Frédéric Parrenin, Dominique Raynaud, Tyler J. Fudge, Christo Buizert, and Edward J. Brook
Clim. Past, 15, 913–926, https://doi.org/10.5194/cp-15-913-2019, https://doi.org/10.5194/cp-15-913-2019, 2019
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Atmospheric CO2 was likely an important amplifier of global-scale orbitally-driven warming during the last deglaciation. However, the mechanisms responsible for the rise in CO2, and the coherent rise in Antarctic isotopic temperature records, are under debate. Using a stochastic method, we detect variable lags between coherent changes in Antarctic temperature and CO2. This implies that the climate mechanisms linking the two records changed or experienced modulations during the deglaciation.
Mai Winstrup, Paul Vallelonga, Helle A. Kjær, Tyler J. Fudge, James E. Lee, Marie H. Riis, Ross Edwards, Nancy A. N. Bertler, Thomas Blunier, Ed J. Brook, Christo Buizert, Gabriela Ciobanu, Howard Conway, Dorthe Dahl-Jensen, Aja Ellis, B. Daniel Emanuelsson, Richard C. A. Hindmarsh, Elizabeth D. Keller, Andrei V. Kurbatov, Paul A. Mayewski, Peter D. Neff, Rebecca L. Pyne, Marius F. Simonsen, Anders Svensson, Andrea Tuohy, Edwin D. Waddington, and Sarah Wheatley
Clim. Past, 15, 751–779, https://doi.org/10.5194/cp-15-751-2019, https://doi.org/10.5194/cp-15-751-2019, 2019
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We present a 2700-year timescale and snow accumulation history for an ice core from Roosevelt Island, Ross Ice Shelf, Antarctica. We observe a long-term slightly decreasing trend in accumulation during most of the period but a rapid decline since the mid-1960s. The latter is linked to a recent strengthening of the Amundsen Sea Low and the expansion of regional sea ice. The year 1965 CE may thus mark the onset of significant increases in sea-ice extent in the eastern Ross Sea.
Laurie Menviel, Emilie Capron, Aline Govin, Andrea Dutton, Lev Tarasov, Ayako Abe-Ouchi, Russell Drysdale, Philip Gibbard, Lauren Gregoire, Feng He, Ruza Ivanovic, Masa Kageyama, Kenji Kawamura, Amaelle Landais, Bette L. Otto-Bliesner, Ikumi Oyabu, Polychronis Tzedakis, Eric Wolff, and Xu Zhang
Clim. Past Discuss., https://doi.org/10.5194/cp-2018-106, https://doi.org/10.5194/cp-2018-106, 2018
Preprint withdrawn
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The penultimate deglaciation (~ 138–128 ka), which represents the transition into the Last Interglacial period, provides a framework to investigate the climate and environmental response to large changes in boundary conditions. Here, as part of the PAGES-PMIP working group on Quaternary Interglacials, we propose a protocol to perform transient simulations of the penultimate deglaciation as well as a selection of paleo records for upcoming model-data comparisons.
Benjamin Birner, Christo Buizert, Till J. W. Wagner, and Jeffrey P. Severinghaus
The Cryosphere, 12, 2021–2037, https://doi.org/10.5194/tc-12-2021-2018, https://doi.org/10.5194/tc-12-2021-2018, 2018
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Ancient air enclosed in bubbles of the Antarctic ice sheet is a key source of information about the Earth's past climate. However, a range of physical processes in the snow layer atop an ice sheet may change the trapped air's chemical composition before it is occluded in the ice. We developed the first detailed 2-D computer simulation of these processes and found a new method to improve the reconstruction of past climate from air in ice cores bubbles.
Nancy A. N. Bertler, Howard Conway, Dorthe Dahl-Jensen, Daniel B. Emanuelsson, Mai Winstrup, Paul T. Vallelonga, James E. Lee, Ed J. Brook, Jeffrey P. Severinghaus, Taylor J. Fudge, Elizabeth D. Keller, W. Troy Baisden, Richard C. A. Hindmarsh, Peter D. Neff, Thomas Blunier, Ross Edwards, Paul A. Mayewski, Sepp Kipfstuhl, Christo Buizert, Silvia Canessa, Ruzica Dadic, Helle A. Kjær, Andrei Kurbatov, Dongqi Zhang, Edwin D. Waddington, Giovanni Baccolo, Thomas Beers, Hannah J. Brightley, Lionel Carter, David Clemens-Sewall, Viorela G. Ciobanu, Barbara Delmonte, Lukas Eling, Aja Ellis, Shruthi Ganesh, Nicholas R. Golledge, Skylar Haines, Michael Handley, Robert L. Hawley, Chad M. Hogan, Katelyn M. Johnson, Elena Korotkikh, Daniel P. Lowry, Darcy Mandeno, Robert M. McKay, James A. Menking, Timothy R. Naish, Caroline Noerling, Agathe Ollive, Anaïs Orsi, Bernadette C. Proemse, Alexander R. Pyne, Rebecca L. Pyne, James Renwick, Reed P. Scherer, Stefanie Semper, Marius Simonsen, Sharon B. Sneed, Eric J. Steig, Andrea Tuohy, Abhijith Ulayottil Venugopal, Fernando Valero-Delgado, Janani Venkatesh, Feitang Wang, Shimeng Wang, Dominic A. Winski, V. Holly L. Winton, Arran Whiteford, Cunde Xiao, Jiao Yang, and Xin Zhang
Clim. Past, 14, 193–214, https://doi.org/10.5194/cp-14-193-2018, https://doi.org/10.5194/cp-14-193-2018, 2018
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Temperature and snow accumulation records from the annually dated Roosevelt Island Climate Evolution (RICE) ice core show that for the past 2 700 years, the eastern Ross Sea warmed, while the western Ross Sea showed no trend and West Antarctica cooled. From the 17th century onwards, this dipole relationship changed. Now all three regions show concurrent warming, with snow accumulation declining in West Antarctica and the eastern Ross Sea.
Alan M. Seltzer, Christo Buizert, Daniel Baggenstos, Edward J. Brook, Jinho Ahn, Ji-Woong Yang, and Jeffrey P. Severinghaus
Clim. Past, 13, 1323–1338, https://doi.org/10.5194/cp-13-1323-2017, https://doi.org/10.5194/cp-13-1323-2017, 2017
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To explore whether the oxygen-18 to oxygen-16 ratio of atmospheric O2 is sensitive to the position of the tropical rain belts, we (1) present a record of ice core bubble oxygen isotope measurements from two Antarctic ice cores, and (2) examine the sensitivity of oxygen isotopes in precipitation, weighted by photosynthesis, to the location of oxygen production over the modern-day seasonal cycle. We find a strong modern relationship and discuss implications for past shifts in tropical rainfall.
Ji-Woong Yang, Jinho Ahn, Edward J. Brook, and Yeongjun Ryu
Clim. Past, 13, 1227–1242, https://doi.org/10.5194/cp-13-1227-2017, https://doi.org/10.5194/cp-13-1227-2017, 2017
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The early Holocene climate is characterized as an interglacial boundary condition without substantial human influence. Here we present a high-resolution CH4 record covering the early Holocene. The results show that abrupt cooling in Greenland and southward migration of ITCZ were able to induce an ~20 ppb CH4 decrease on a millennial timescale. The inter-polar difference exhibits a gradual increase during the early Holocene, implying the strengthening of northern extratropical emission.
Daniel Baggenstos, Thomas K. Bauska, Jeffrey P. Severinghaus, James E. Lee, Hinrich Schaefer, Christo Buizert, Edward J. Brook, Sarah Shackleton, and Vasilii V. Petrenko
Clim. Past, 13, 943–958, https://doi.org/10.5194/cp-13-943-2017, https://doi.org/10.5194/cp-13-943-2017, 2017
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We present measurements of the gas composition in trapped air bubbles in ice samples taken from Taylor Glacier, Antarctica. We can show that ice from the entire last glacial cycle (125 000 years ago to the present) is exposed at the surface of this glacier and that the atmospheric record contained in the air bubbles is well preserved. Taylor Glacier therefore provides an easily accessible archive of ancient ice that allows for studies of trace components that require large ice volumes.
Léa Gest, Frédéric Parrenin, Jai Chowdhry Beeman, Dominique Raynaud, Tyler J. Fudge, Christo Buizert, and Edward J. Brook
Clim. Past Discuss., https://doi.org/10.5194/cp-2017-71, https://doi.org/10.5194/cp-2017-71, 2017
Revised manuscript has not been submitted
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In this manuscript, we place the atmospheric CO2 and Antarctic temperature records onto a common age scale during the last deglaciation. Moreover, we evaluate the phase relationship between those two records in order to discuss possible climatic and carbon cycle scenarios. Indeed, this phase relationship is central to determine the role of the former in past (and therefore future) climatic variations. This scientific problem was even discussed by some policy makers (e.g., in the USA senate).
Hyo-Jin Eom, Dhrubajyoti Gupta, Hye-Rin Cho, Hee Jin Hwang, Soon Do Hur, Yeontae Gim, and Chul-Un Ro
Atmos. Chem. Phys., 16, 13823–13836, https://doi.org/10.5194/acp-16-13823-2016, https://doi.org/10.5194/acp-16-13823-2016, 2016
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Summertime and wintertime Antarctic sea spray aerosol (SSA) samples with a drastic chlorophyll-a level contrast were investigated on a single-particle basis. X-ray analysis showed that the contents of C, O, Ca, S, and Si were more elevated, whereas Cl was more depleted for the summertime sample. The combined application of RMS and ATR-FTIR imaging showed Mg hydrate salts of alanine and Mg salts of fatty acids were major organic species in nascent Antarctic SSAs.
Christo Buizert and Jeffrey P. Severinghaus
The Cryosphere, 10, 2099–2111, https://doi.org/10.5194/tc-10-2099-2016, https://doi.org/10.5194/tc-10-2099-2016, 2016
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The upper 50–100 m of the world's ice sheets consists of the firn layer, a porous layer of snow that is slowly compacted by overlying snow. Understanding air movement inside the firn is critical for ice core climate reconstructions. Buizert and Severinghaus identify and describe a new mechanism of firn air movement. High- and low-pressure systems force air movement in the firn that drives strong mixing, called dispersion. Dispersion is the main mechanism for air mixing in the deep firn.
Rachael H. Rhodes, Xavier Faïn, Edward J. Brook, Joseph R. McConnell, Olivia J. Maselli, Michael Sigl, Jon Edwards, Christo Buizert, Thomas Blunier, Jérôme Chappellaz, and Johannes Freitag
Clim. Past, 12, 1061–1077, https://doi.org/10.5194/cp-12-1061-2016, https://doi.org/10.5194/cp-12-1061-2016, 2016
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Local artifacts in ice core methane data are superimposed on consistent records of past atmospheric variability. These artifacts are not related to past atmospheric history and care should be taken to avoid interpreting them as such. By investigating five polar ice cores from sites with different conditions, we relate isolated methane spikes to melt layers and decimetre-scale variations as "trapping signal" associated with a difference in timing of air bubble closure in adjacent firn layers.
Ikumi Oyabu, Yoshinori Iizuka, Eric Wolff, and Margareta Hansson
Clim. Past Discuss., https://doi.org/10.5194/cp-2016-42, https://doi.org/10.5194/cp-2016-42, 2016
Manuscript not accepted for further review
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This study presented the chemical compositions of non-volatile particles around the last termination in the Dome C ice core by using the sublimation-EDS method. The major soluble salt particles are CaSO4, Na2SO4, and NaCl, and time-series changes in the composition of these salts are similar to those for the Dome Fuji ice core. However, some differences occurred. The sulfatization rate of NaCl at Dome C is higher than that at Dome Fuji.
Michael Sigl, Tyler J. Fudge, Mai Winstrup, Jihong Cole-Dai, David Ferris, Joseph R. McConnell, Ken C. Taylor, Kees C. Welten, Thomas E. Woodruff, Florian Adolphi, Marion Bisiaux, Edward J. Brook, Christo Buizert, Marc W. Caffee, Nelia W. Dunbar, Ross Edwards, Lei Geng, Nels Iverson, Bess Koffman, Lawrence Layman, Olivia J. Maselli, Kenneth McGwire, Raimund Muscheler, Kunihiko Nishiizumi, Daniel R. Pasteris, Rachael H. Rhodes, and Todd A. Sowers
Clim. Past, 12, 769–786, https://doi.org/10.5194/cp-12-769-2016, https://doi.org/10.5194/cp-12-769-2016, 2016
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Here we present a chronology (WD2014) for the upper part (0–2850 m; 31.2 ka BP) of the West Antarctic Ice Sheet (WAIS) Divide ice core, which is based on layer counting of distinctive annual cycles preserved in the elemental, chemical and electrical conductivity records. We validated the chronology by comparing it to independent high-accuracy, absolutely dated chronologies. Given its demonstrated high accuracy, WD2014 can become a reference chronology for the Southern Hemisphere.
Shin'ya Nakano, Kazue Suzuki, Kenji Kawamura, Frédéric Parrenin, and Tomoyuki Higuchi
Nonlin. Processes Geophys., 23, 31–44, https://doi.org/10.5194/npg-23-31-2016, https://doi.org/10.5194/npg-23-31-2016, 2016
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This paper proposes a technique for dating an ice core. The proposed technique employs a hybrid method combining the sequential Monte Carlo method and the Markov chain Monte Carlo method, which is referred to as the particle Markov chain Monte Carlo method. The sequential Monte Carlo method, which is also known as the particle filter, is widely used for nonlinear time-series analysis. This paper demonstrates the usefulness of the approach in time-series analysis for dating an ice core.
A. Svensson, S. Fujita, M. Bigler, M. Braun, R. Dallmayr, V. Gkinis, K. Goto-Azuma, M. Hirabayashi, K. Kawamura, S. Kipfstuhl, H. A. Kjær, T. Popp, M. Simonsen, J. P. Steffensen, P. Vallelonga, and B. M. Vinther
Clim. Past, 11, 1127–1137, https://doi.org/10.5194/cp-11-1127-2015, https://doi.org/10.5194/cp-11-1127-2015, 2015
A. Ghosh, P. K. Patra, K. Ishijima, T. Umezawa, A. Ito, D. M. Etheridge, S. Sugawara, K. Kawamura, J. B. Miller, E. J. Dlugokencky, P. B. Krummel, P. J. Fraser, L. P. Steele, R. L. Langenfelds, C. M. Trudinger, J. W. C. White, B. Vaughn, T. Saeki, S. Aoki, and T. Nakazawa
Atmos. Chem. Phys., 15, 2595–2612, https://doi.org/10.5194/acp-15-2595-2015, https://doi.org/10.5194/acp-15-2595-2015, 2015
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Atmospheric CH4 increased from 900ppb to 1800ppb during the period 1900–2010 at a rate unprecedented in any observational records. We use bottom-up emissions and a chemistry-transport model to simulate CH4. The optimized global total CH4 emission, estimated from the model–observation differences, increased at fastest rate during 1940–1990. Using δ13C of CH4 measurements we attribute this emission increase to biomass burning. Total CH4 lifetime is shortened by 4% over the simulation period.
F. Parrenin, S. Fujita, A. Abe-Ouchi, K. Kawamura, V. Masson-Delmotte, H. Motoyama, F. Saito, M. Severi, B. Stenni, R. Uemura, and E. Wolff
Clim. Past Discuss., https://doi.org/10.5194/cpd-11-377-2015, https://doi.org/10.5194/cpd-11-377-2015, 2015
Revised manuscript has not been submitted
C. Buizert, K. M. Cuffey, J. P. Severinghaus, D. Baggenstos, T. J. Fudge, E. J. Steig, B. R. Markle, M. Winstrup, R. H. Rhodes, E. J. Brook, T. A. Sowers, G. D. Clow, H. Cheng, R. L. Edwards, M. Sigl, J. R. McConnell, and K. C. Taylor
Clim. Past, 11, 153–173, https://doi.org/10.5194/cp-11-153-2015, https://doi.org/10.5194/cp-11-153-2015, 2015
S. O. Rasmussen, P. M. Abbott, T. Blunier, A. J. Bourne, E. Brook, S. L. Buchardt, C. Buizert, J. Chappellaz, H. B. Clausen, E. Cook, D. Dahl-Jensen, S. M. Davies, M. Guillevic, S. Kipfstuhl, T. Laepple, I. K. Seierstad, J. P. Severinghaus, J. P. Steffensen, C. Stowasser, A. Svensson, P. Vallelonga, B. M. Vinther, F. Wilhelms, and M. Winstrup
Clim. Past, 9, 2713–2730, https://doi.org/10.5194/cp-9-2713-2013, https://doi.org/10.5194/cp-9-2713-2013, 2013
K. Kawamura, J. P. Severinghaus, M. R. Albert, Z. R. Courville, M. A. Fahnestock, T. Scambos, E. Shields, and C. A. Shuman
Atmos. Chem. Phys., 13, 11141–11155, https://doi.org/10.5194/acp-13-11141-2013, https://doi.org/10.5194/acp-13-11141-2013, 2013
H. Fischer, J. Severinghaus, E. Brook, E. Wolff, M. Albert, O. Alemany, R. Arthern, C. Bentley, D. Blankenship, J. Chappellaz, T. Creyts, D. Dahl-Jensen, M. Dinn, M. Frezzotti, S. Fujita, H. Gallee, R. Hindmarsh, D. Hudspeth, G. Jugie, K. Kawamura, V. Lipenkov, H. Miller, R. Mulvaney, F. Parrenin, F. Pattyn, C. Ritz, J. Schwander, D. Steinhage, T. van Ommen, and F. Wilhelms
Clim. Past, 9, 2489–2505, https://doi.org/10.5194/cp-9-2489-2013, https://doi.org/10.5194/cp-9-2489-2013, 2013
A. Svensson, M. Bigler, T. Blunier, H. B. Clausen, D. Dahl-Jensen, H. Fischer, S. Fujita, K. Goto-Azuma, S. J. Johnsen, K. Kawamura, S. Kipfstuhl, M. Kohno, F. Parrenin, T. Popp, S. O. Rasmussen, J. Schwander, I. Seierstad, M. Severi, J. P. Steffensen, R. Udisti, R. Uemura, P. Vallelonga, B. M. Vinther, A. Wegner, F. Wilhelms, and M. Winstrup
Clim. Past, 9, 749–766, https://doi.org/10.5194/cp-9-749-2013, https://doi.org/10.5194/cp-9-749-2013, 2013
T. Kobashi, D. T. Shindell, K. Kodera, J. E. Box, T. Nakaegawa, and K. Kawamura
Clim. Past, 9, 583–596, https://doi.org/10.5194/cp-9-583-2013, https://doi.org/10.5194/cp-9-583-2013, 2013
Related subject area
Discipline: Glaciers | Subject: Ice Cores
Temporal markers in a temperate ice core: insights from 3H and 137Cs profiles from the Adamello Glacier
Review article: Melt-affected ice cores for polar research in a warming world
Impact of subsurface crevassing on the depth–age relationship of high-Alpine ice cores extracted at Col du Dôme between 1994 and 2012
Fifty years of firn evolution on Grigoriev ice cap, Tien Shan, Kyrgyzstan
Climate change is rapidly deteriorating the climatic signal in Svalbard glaciers
Identifying atmospheric processes favouring the formation of bubble-free layers in the Law Dome ice core, East Antarctica
Early Holocene ice on the Begguya plateau (Mt. Hunter, Alaska) revealed by ice core 14C age constraints
A quantitative method of resolving annual precipitation for the past millennia from Tibetan ice cores
Acoustic velocity measurements for detecting the crystal orientation fabrics of a temperate ice core
Brief communication: New evidence further constraining Tibetan ice core chronologies to the Holocene
Giant dust particles at Nevado Illimani: a proxy of summertime deep convection over the Bolivian Altiplano
Physical properties of shallow ice cores from Antarctic and sub-Antarctic islands
Stable water isotopes and accumulation rates in the Union Glacier region, Ellsworth Mountains, West Antarctica, over the last 35 years
Apparent discrepancy of Tibetan ice core δ18O records may be attributed to misinterpretation of chronology
Age ranges of the Tibetan ice cores with emphasis on the Chongce ice cores, western Kunlun Mountains
Elena Di Stefano, Giovanni Baccolo, Massimiliano Clemenza, Barbara Delmonte, Deborah Fiorini, Roberto Garzonio, Margit Schwikowski, and Valter Maggi
The Cryosphere, 18, 2865–2874, https://doi.org/10.5194/tc-18-2865-2024, https://doi.org/10.5194/tc-18-2865-2024, 2024
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Rising temperatures are impacting the reliability of glaciers as environmental archives. This study reports how meltwater percolation affects the distribution of tritium and cesium, which are commonly used as temporal markers in dating ice cores, in a temperate glacier. Our findings challenge the established application of radionuclides for dating mountain ice cores and indicate tritium as the best choice.
Dorothea Elisabeth Moser, Elizabeth R. Thomas, Christoph Nehrbass-Ahles, Anja Eichler, and Eric Wolff
The Cryosphere, 18, 2691–2718, https://doi.org/10.5194/tc-18-2691-2024, https://doi.org/10.5194/tc-18-2691-2024, 2024
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Increasing temperatures worldwide lead to more melting of glaciers and ice caps, even in the polar regions. This is why ice-core scientists need to prepare to analyse records affected by melting and refreezing. In this paper, we present a summary of how near-surface melt forms, what structural imprints it leaves in snow, how various signatures used for ice-core climate reconstruction are altered, and how we can still extract valuable insights from melt-affected ice cores.
Susanne Preunkert, Pascal Bohleber, Michel Legrand, Adrien Gilbert, Tobias Erhardt, Roland Purtschert, Lars Zipf, Astrid Waldner, Joseph R. McConnell, and Hubertus Fischer
The Cryosphere, 18, 2177–2194, https://doi.org/10.5194/tc-18-2177-2024, https://doi.org/10.5194/tc-18-2177-2024, 2024
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Ice cores from high-elevation Alpine glaciers are an important tool to reconstruct the past atmosphere. However, since crevasses are common at these glacier sites, rigorous investigations of glaciological conditions upstream of drill sites are needed before interpreting such ice cores. On the basis of three ice cores extracted at Col du Dôme (4250 m a.s.l; French Alps), an overall picture of a dynamic crevasse formation is drawn, which disturbs the depth–age relation of two of the three cores.
Horst Machguth, Anja Eichler, Margit Schwikowski, Sabina Brütsch, Enrico Mattea, Stanislav Kutuzov, Martin Heule, Ryskul Usubaliev, Sultan Belekov, Vladimir N. Mikhalenko, Martin Hoelzle, and Marlene Kronenberg
The Cryosphere, 18, 1633–1646, https://doi.org/10.5194/tc-18-1633-2024, https://doi.org/10.5194/tc-18-1633-2024, 2024
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In 2018 we drilled an 18 m ice core on the summit of Grigoriev ice cap, located in the Tien Shan mountains of Kyrgyzstan. The core analysis reveals strong melting since the early 2000s. Regardless of this, we find that the structure and temperature of the ice have changed little since the 1980s. The probable cause of this apparent stability is (i) an increase in snowfall and (ii) the fact that meltwater nowadays leaves the glacier and thereby removes so-called latent heat.
Andrea Spolaor, Federico Scoto, Catherine Larose, Elena Barbaro, Francois Burgay, Mats P. Bjorkman, David Cappelletti, Federico Dallo, Fabrizio de Blasi, Dmitry Divine, Giuliano Dreossi, Jacopo Gabrieli, Elisabeth Isaksson, Jack Kohler, Tonu Martma, Louise S. Schmidt, Thomas V. Schuler, Barbara Stenni, Clara Turetta, Bartłomiej Luks, Mathieu Casado, and Jean-Charles Gallet
The Cryosphere, 18, 307–320, https://doi.org/10.5194/tc-18-307-2024, https://doi.org/10.5194/tc-18-307-2024, 2024
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We evaluate the impact of the increased snowmelt on the preservation of the oxygen isotope (δ18O) signal in firn records recovered from the top of the Holtedahlfonna ice field located in the Svalbard archipelago. Thanks to a multidisciplinary approach we demonstrate a progressive deterioration of the isotope signal in the firn core. We link the degradation of the δ18O signal to the increased occurrence and intensity of melt events associated with the rapid warming occurring in the archipelago.
Lingwei Zhang, Tessa R. Vance, Alexander D. Fraser, Lenneke M. Jong, Sarah S. Thompson, Alison S. Criscitiello, and Nerilie J. Abram
The Cryosphere, 17, 5155–5173, https://doi.org/10.5194/tc-17-5155-2023, https://doi.org/10.5194/tc-17-5155-2023, 2023
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Physical features in ice cores provide unique records of past variability. We identified 1–2 mm ice layers without bubbles in surface ice cores from Law Dome, East Antarctica, occurring on average five times per year. The origin of these bubble-free layers is unknown. In this study, we investigate whether they have the potential to record past atmospheric processes and circulation. We find that the bubble-free layers are linked to accumulation hiatus events and meridional moisture transport.
Ling Fang, Theo M. Jenk, Dominic Winski, Karl Kreutz, Hanna L. Brooks, Emma Erwin, Erich Osterberg, Seth Campbell, Cameron Wake, and Margit Schwikowski
The Cryosphere, 17, 4007–4020, https://doi.org/10.5194/tc-17-4007-2023, https://doi.org/10.5194/tc-17-4007-2023, 2023
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Understanding the behavior of ocean–atmosphere teleconnections in the North Pacific during warm intervals can aid in predicting future warming scenarios. However, majority ice core records from Alaska–Yukon region only provide data for the last few centuries. This study introduces a continuous chronology for Denali ice core from Begguya, Alaska, using multiple dating methods. The early-Holocene-origin Denali ice core will facilitate future investigations of hydroclimate in the North Pacific.
Wangbin Zhang, Shugui Hou, Shuang-Ye Wu, Hongxi Pang, Sharon B. Sneed, Elena V. Korotkikh, Paul A. Mayewski, Theo M. Jenk, and Margit Schwikowski
The Cryosphere, 16, 1997–2008, https://doi.org/10.5194/tc-16-1997-2022, https://doi.org/10.5194/tc-16-1997-2022, 2022
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This study proposes a quantitative method to reconstruct annual precipitation records at the millennial timescale from the Tibetan ice cores through combining annual layer identification based on LA-ICP-MS measurement with an ice flow model. The reliability of this method is assessed by comparing our results with other reconstructed and modeled precipitation series for the Tibetan Plateau. The assessment shows that the method has a promising performance.
Sebastian Hellmann, Melchior Grab, Johanna Kerch, Henning Löwe, Andreas Bauder, Ilka Weikusat, and Hansruedi Maurer
The Cryosphere, 15, 3507–3521, https://doi.org/10.5194/tc-15-3507-2021, https://doi.org/10.5194/tc-15-3507-2021, 2021
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In this study, we analyse whether ultrasonic measurements on ice core samples could be employed to derive information about the particular ice crystal orientation in these samples. We discuss if such ultrasonic scans of ice core samples could provide similarly detailed results as the established methods, which usually destroy the ice samples. Our geophysical approach is minimally invasive and could support the existing methods with additional and (semi-)continuous data points along the ice core.
Shugui Hou, Wangbin Zhang, Ling Fang, Theo M. Jenk, Shuangye Wu, Hongxi Pang, and Margit Schwikowski
The Cryosphere, 15, 2109–2114, https://doi.org/10.5194/tc-15-2109-2021, https://doi.org/10.5194/tc-15-2109-2021, 2021
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We present ages for two new ice cores reaching bedrock, from the Zangser Kangri (ZK) glacier in the northwestern Tibetan Plateau and the Shulenanshan (SLNS) glacier in the western Qilian Mountains. We estimated bottom ages of 8.90±0.57/0.56 ka and 7.46±1.46/1.79 ka for the ZK and SLNS ice core respectively, constraining the time range accessible by Tibetan ice cores to the Holocene.
Filipe G. L. Lindau, Jefferson C. Simões, Barbara Delmonte, Patrick Ginot, Giovanni Baccolo, Chiara I. Paleari, Elena Di Stefano, Elena Korotkikh, Douglas S. Introne, Valter Maggi, Eduardo Garzanti, and Sergio Andò
The Cryosphere, 15, 1383–1397, https://doi.org/10.5194/tc-15-1383-2021, https://doi.org/10.5194/tc-15-1383-2021, 2021
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Information about the past climate variability in tropical South America is stored in the snow layers of the tropical Andean glaciers. Here we show evidence that the presence of very large aeolian mineral dust particles at Nevado Illimani (Bolivia) is strictly controlled by the occurrence of summer storms in the Bolivian Altiplano. Therefore, based on the snow dust content and its composition of stable water isotopes, we propose a new proxy for information on previous summer storms.
Elizabeth Ruth Thomas, Guisella Gacitúa, Joel B. Pedro, Amy Constance Faith King, Bradley Markle, Mariusz Potocki, and Dorothea Elisabeth Moser
The Cryosphere, 15, 1173–1186, https://doi.org/10.5194/tc-15-1173-2021, https://doi.org/10.5194/tc-15-1173-2021, 2021
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Here we present the first-ever radar and ice core data from the sub-Antarctic islands of Bouvet Island, Peter I Island, and Young Island. These islands have the potential to record past climate in one of the most data-sparse regions on earth. Despite their northerly location, surface melting is generally low, and the upper layer of the ice at most sites is undisturbed. We estimate that a 100 m ice core drilled on these islands could capture climate over the past 100–200 years.
Kirstin Hoffmann, Francisco Fernandoy, Hanno Meyer, Elizabeth R. Thomas, Marcelo Aliaga, Dieter Tetzner, Johannes Freitag, Thomas Opel, Jorge Arigony-Neto, Christian Florian Göbel, Ricardo Jaña, Delia Rodríguez Oroz, Rebecca Tuckwell, Emily Ludlow, Joseph R. McConnell, and Christoph Schneider
The Cryosphere, 14, 881–904, https://doi.org/10.5194/tc-14-881-2020, https://doi.org/10.5194/tc-14-881-2020, 2020
Shugui Hou, Wangbin Zhang, Hongxi Pang, Shuang-Ye Wu, Theo M. Jenk, Margit Schwikowski, and Yetang Wang
The Cryosphere, 13, 1743–1752, https://doi.org/10.5194/tc-13-1743-2019, https://doi.org/10.5194/tc-13-1743-2019, 2019
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The apparent discrepancy between the Holocene δ18O records of the Guliya and the Chongce ice cores may be attributed to a possible misinterpretation of the Guliya ice core chronology.
Shugui Hou, Theo M. Jenk, Wangbin Zhang, Chaomin Wang, Shuangye Wu, Yetang Wang, Hongxi Pang, and Margit Schwikowski
The Cryosphere, 12, 2341–2348, https://doi.org/10.5194/tc-12-2341-2018, https://doi.org/10.5194/tc-12-2341-2018, 2018
Short summary
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We present multiple lines of evidence indicating that the Chongce ice cores drilled from the northwestern Tibetan Plateau reaches back only to the early Holocene. This result is at least, 1 order of magnitude younger than the nearby Guliya ice core (~30 km away from the Chongce ice core drilling site) but similar to other Tibetan ice cores. Thus it is necessary to explore multiple dating techniques to confirm the age ranges of the Tibetan ice cores.
Cited articles
Aarons, S. M., Aciego, S. M., Gabrielli, P., Delmonte, B., Koornneef, J. M.,
Wegner, A., and Blakowski, M. A.: The impact of glacier retreat from the
Ross Sea on local climate: Characterization of mineral dust in the Taylor
Dome ice core, East Antarctica, Earth Planet. Sc. Lett., 444, 34–44,
https://doi.org/10.1016/j.epsl.2016.03.035, 2016.
Aarons, S. M., Aciego, S. M., Arendt, C. A., Blakowski, M. A., Steigmeyer,
A., Gabrielli, P., Sierra-Hernández, M. R., Beaudon, E., Delmonte, B.,
Baccolo, G., May, N. W., and Pratt, K. A.: Dust composition changes from
Taylor Glacier (East Antarctica) during the last glacial-interglacial
transition: A multi-proxy approach, Quaternary Sci. Rev., 162, 60–71,
https://doi.org/10.1016/j.quascirev.2017.03.011, 2017.
Aciego, S. M., Cuffey, K. M., Kavanaugh, J. L., Morse, D. L., and
Severinghaus, J. P.: Pleistocene ice and paleo-strain rates at Taylor
Glacier, Antarctica, Quaternary Res., 68, 303–313,
https://doi.org/10.1016/j.yqres.2007.07.013, 2007.
Ahn, J., Brook, E. J., and Howell, K.: A high-precision method for
measurement of paleoatmospheric CO2 in small polar ice samples, J.
Glaciol., 55, 499–506, https://doi.org/10.3189/002214309788816731, 2009.
Azuma, N., Nakawo, A., Higashi, A., and Nishio, F.: Flow pattern near Massif
A in the Yamato bare ice field estimated from the structures and the
mechanical properites of a shallow ice core, Mem. Natl. Inst. Polar Res., 39, 173–183, 1985.
Baggenstos, D., Bauska, T. K., Severinghaus, J. P., Lee, J. E., Schaefer, H., Buizert, C., Brook, E. J., Shackleton, S., and Petrenko, V. V.: Atmospheric gas records from Taylor Glacier, Antarctica, reveal ancient ice with ages spanning the entire last glacial cycle, Clim. Past, 13, 943–958, https://doi.org/10.5194/cp-13-943-2017, 2017.
Baggenstos, D., Severinghaus, J. P., Mulvaney, R., McConnell, J. R., Sigl,
M., Maselli, O., Petit, J. R., Grente, B., and Steig, E. J.: A horizontal ice
core from Taylor Glacier, its implication for Antarctic climate history, and
an improved Taylor Dome ice core time scale, Paleoceanography and
Paleoclimatology, 33, 778–794, https://doi.org/10.1029/2017PA003297, 2018.
Bauska, T., Baggenstos, D., Brook, E. J., Mix, A. C., Marcott, S. A.,
Petrenko, V. V., Schaefer, H., Severinghaus, J. P., and Lee, J. E.: Carbon
isotopes characterize rapid changes in atmospheric carbon dioxide during the
last deglaciation, P. Natl. Acad. Sci. USA, 113, 3465–3470,
https://doi.org/10.1073/pnas.1513868113, 2016.
Bazin, L., Landais, A., Lemieux-Dudon, B., Toyé Mahamadou Kele, H.,
Veres, D., Parrenin, F., Martinerie, P., Ritz, C., Capron, E., Lipenkov, V.
Y., Loutre, M.-F., Raynaud, D., Vinther, B. M., Svensson, A. M., Rasmussen,
S. O., Severi, M., Blunier, T., Leuenberger, M. C., Fischer, H.,
Masson-Delmotte, V., Chappellaz, J. A., and Wolff, E. W.: AICC2012
chronology for ice core EDC, PANGAEA [data set],
https://doi.org/10.1594/PANGAEA.824865, 2013a.
Bazin, L., Landais, A., Lemieux-Dudon, B., Toyé Mahamadou Kele, H.,
Veres, D., Parrenin, F., Martinerie, P., Ritz, C., Capron, E., Lipenkov, V.
Y., Loutre, M.-F., Raynaud, D., Vinther, B. M., Svensson, A. M., Rasmussen,
S. O., Severi, M., Blunier, T., Leuenberger, M. C., Fischer, H.,
Masson-Delmotte, V., Chappellaz, J. A., and Wolff, E. W.: delta Deuterium
measured on ice core EDC on AICC2012 chronology, PANGAEA [data set],
https://doi.org/10.1594/PANGAEA.824891, 2013b.
Bazin, L., Landais, A., Lemieux-Dudon, B., Toyé Mahamadou Kele, H.,
Veres, D., Parrenin, F., Martinerie, P., Ritz, C., Capron, E., Lipenkov, V.
Y., Loutre, M.-F., Raynaud, D., Vinther, B. M., Svensson, A. M., Rasmussen,
S. O., Severi, M., Blunier, T., Leuenberger, M. C., Fischer, H.,
Masson-Delmotte, V., Chappellaz, J. A., and Wolff, E. W.: δ18O
measured on ice core TALDICE on AICC2012 chronology, PANGAEA [data set],
https://doi.org/10.1594/PANGAEA.824890, 2013c.
Bazin, L., Landais, A., Lemieux-Dudon, B., Toyé Mahamadou Kele, H.,
Veres, D., Parrenin, F., Martinerie, P., Ritz, C., Capron, E., Lipenkov, V.
Y., Loutre, M.-F., Raynaud, D., Vinther, B. M., Svensson, A. M., Rasmussen,
S. O., Severi, M., Blunier, T., Leuenberger, M. C., Fischer, H.,
Masson-Delmotte, V., Chappellaz, J. A., and Wolff, E. W.: Methane measured
on ice core EDC on AICC2012 chronology, PANGAEA [data set],
https://doi.org/10.1594/PANGAEA.824883, 2013d.
Bender, M.: Concentration and Isotopic Composition of O2 and N2 in Trapped
Gases of the Vostok Ice Core, U.S. Antarctic Program (USAP) Data Center [data set],
https://doi.org/10.7265/N5862DCW, 2002.
Bender, M., Labeyrie, L. D., Raynaud, D., and Lorius, C.: Isotopic
composition of atmospheric O2 in ice linked with deglaciation and
global primary productivity, Nature, 318, 349–352,
https://doi.org/10.1038/318349a0, 1985.
Bender, M. L., Barnett, B., Dreyfus, G., Jouzel, J., and Porcelli, D.: The
contemporary degassing rate of 40Ar from the solid Earth, P. Natl.
Acad. Sci. USA., 105, 8232–8237, https://doi.org/10.1073/pnas.0711679105,
2008.
Bender, M. L., Burgess, E., Alley, R. B., Barnett, B., and Clow, G. D.: On
the nature of the dirty ice at the bottom of the GISP2 ice core, Earth.
Planet. Sc. Lett., 299, 466–473,
https://doi.org/10.1016/j.epsl.2010.09.033, 2010.
Bereiter, B., Eggleston, S., Schmitt, J., Nehrbass-Ahles, C., Stocker, T.
F., Fischer, H., Kipfstuhl, S., and Chappellaz, J.: Revision of the EPICA
Dome C CO2 record from 800 to 600 kyr before present, Geophys. Res.
Lett., 42, 542–549, https://doi.org/10.1002/2014GL061957, 2015.
Bindschadler, R., Vornberger, P., Fleming, A., Fox, A., Mullins, J., Binnie,
D., Paulsen, S. J., Granneman, B., and Gorodetzky, D.: The Landsat image
mosaic of Antarctica, Remote Sens. Environ., 112, 4214–4226,
https://doi.org/10.1016/j.rse.2008.07.006, 2008.
Bintanja, R.: On the glaciological, meteorological, and climatological
significance of Antarctic blue ice areas, Rev. Geophys., 37, 337–359,
https://doi.org/10.1029/1999RG900007, 1999.
Blunier, T. and Brook, E. J.: Timing of millennial-scale climate change in
Antarctica and Greenland during the last glacial period, Science, 291,
109–112, https://doi.org/10.1126/science.291.5501.109, 2001.
Blunier, T., Spahni, R., Barnola, J.-M., Chappellaz, J., Loulergue, L., and Schwander, J.: Synchronization of ice core records via atmospheric gases, Clim. Past, 3, 325–330, https://doi.org/10.5194/cp-3-325-2007, 2007.
Borgorodsky, V. V., Bentley, C. R., and Gudmandsen, P. E.: Radioglaciology, 1st edn.,
Glaciology and Quaternary Geology, Springer Netherlands, ISBN 978-94-010-8830-5, https://doi.org/10.1007/978-94-009-5275-1, 1985.
Buizert, C.: The ice core gas age-ice age difference as a proxy for surface
temperature, Geophys. Res. Lett., 48, e2021GL094241.
https://doi.org/10.1029/2021GL094241, 2021.
Buizert, C., Baggenstos, D., Jiang, W., Purtschert, R., Petrenko, V. V., Lu,
Z.-T., Müller, P., Kuhl, T., Lee, J., Severinghaus, J. P., and Brook, E.
J.: Radiometric 81Kr dating identifies 120,000-year-old ice at Taylor
Glacier, Antarctica, P. Natl. Acad. Sci. USA., 111, 6876–6881,
https://doi.org/10.1073/pnas.1320329111, 2014.
Buizert, C., Cuffey, K. M., Severinghaus, J. P., Baggenstos, D., Fudge, T. J., Steig, E. J., Markle, B. R., Winstrup, M., Rhodes, R. H., Brook, E. J., Sowers, T. A., Clow, G. D., Cheng, H., Edwards, R. L., Sigl, M., McConnell, J. R., and Taylor, K. C.: The WAIS Divide deep ice core WD2014 chronology – Part 1: Methane synchronization (68–31 ka BP) and the gas age–ice age difference, Clim. Past, 11, 153–173, https://doi.org/10.5194/cp-11-153-2015, 2015.
Buizert, C., Sigl, M., Severi, M., Markle, B. R., Wettstein, J. J.,
McConnell, J. R., Pedro, J. B., Sodemann, H., Goto-Azuma, K., Kawamura, K.,
Fuita, S., Motoyama, H., Hirabayashi, M., Uemura, R., Stenni, B., Parrenin,
F., He, F., Fudge, T. J., and Steig, E. J.: Abrupt ice-age shifts in
southern westerly winds and Antarctic climate forced from the north, Nature,
563, 681–685, https://doi.org/10.1038/s41586-018-0727-5, 2018.
Buizert, C., Fudge, T. J., Roberts, W. H. G., Steig, E. J., Sherriff-Tadano,
S., Ritz, C., Lefebvre, E., Edwards, J., Kawamura, K., Oyabu, I., Motoyama,
H., Kahle, E. C., Jones, T. R., Abe-Ouchi, A., Obase, T., Martin, C., Corr,
H., Severinghaus, J. P., Beaudette, R., Epifanio, J. A., Brook, E. J.,
Martin, K., Chappellaz, J., Aoki, S., Nakazawa, T., Sower, T. A., Alley, R.
B., Ahn, J., Sigl, M., Severi, M., Dunbar, N. W., Svensson, A., Fegyveresi,
J. M., He, C., Liu, Z., Zhu, J., Otto-Bliesner, B. L., Lipenkov, V. Y.,
Kageyama, M., and Schwander, J.: Antarctic surface temperature and elevation
during the Last Glacial Maximum, Science, 372, 1097–1101, https://doi.org/10.1126/science.abd2897, 2021.
Capron, E., Landais, A., Leieux-Dudon, B., Schilt, A., Masson-Delmotte, V.,
Buiron, D., Chappellaz, J., Dahl-Jensen, D., Johnsen, S., Leuenberger, M.,
Loulergue, L., and Oerter, H.: Synchronising EDML and NorthGRIP ice cores
using δ18O of atmospheric oxygen (δ18Oatm)
and CH4 measurements over MIS5 (80–123 kyr), Quaternary Sci. Rev., 29,
222–234, https://doi.org/10.1016/j.quascirev.2009.07.014, 2010.
Cassidy, W., Harvey, R., Schutt, J., Delisle, G., and Yanai, K.: The
meteorite collection sites of Antarctica, Meteoritics, 27, 490–525,
https://doi.org/10.1111/j.1945-5100.1992.tb01073.x, 1992.
Chalk, T. B., Hain, M. P., Foster, G. L., Rohling, E. J., Sexton, P. F.,
Badger, M. P. S., Cherry, S. G., Hasenfratz, A. P., Haug, G. H., Jaccard, S.
L., Martínez-García, A., Pälike, H., Pancost, R. D., and
Wilson, P. A.: Causes of ice age intensification across the Mid-Pleistocene
Transition, P. Natl. Acad. Sci. USA., 114, 13114–13119,
https://doi.org/10.1073/pnas.1702143114, 2017.
Conway, H., Hall, B. L., Denton, G. H., Gades, A. M., and Waddington, E. D.:
Past and future grounding-line retreat of the west Antarctic ice sheet,
Science, 286, 280–283, https://doi.org/10.1126/science.286.5438.280, 1999.
Craig, H., Horibe, Y., and Sowers, T.: Gravitational Separation of Gases and
Isotopes in Polar Ice Caps, Science, 242, 1675–1678, https://doi.org/10.1126/science.242.4886.1675, 1988.
Crotti, I., Landais, A., Stenni, B., Bazin, L, Parrenin, F., Frezzotti, M.,
Ritterbusch, F., Lu, Z.-T., Jiang, W., Yang, G.-M., Fourré, E., Orsi,
A., Jacob, R., Minster, B., Prié, F., Dreossi, G., and Barbante, C.: An
extension of the TALDICE ice core age scale reaching back to MIS 10.1,
Quaternary Sci. Rev., 266, 107078,
https://doi.org/10.1016/j.quascirev.2021.107078, 2021.
Curzio, P., Folco, L., Laurenzi, M. A., Mellini, M., and Zeoli, A.: A tephra
chronostratigraphic framework for the Frontier Mountain blue-ice field
(northern Victoria Land, Antarctica), Quaternary Sci. Rev., 27, 602–620,
https://doi.org/10.1016/j.quascirev.2007.11.017, 2008.
Dansgaard, W., White, J., and Johnsen, S.: The abrupt termination of the
Younger Dryas climate event, Nature, 339, 532–534,
https://doi.org/10.1038/339532a0, 1989.
Delisle, G. and Sievers, J.: Sub-ice topography and meteorite finds near
the Allan Hills and the Near Western ice field, Victoria Land, Antarctica,
J. Geophys. Res.-Planet., 96, 15577–15587,
https://doi.org/10.1029/91JE01117, 1991.
Delmas, R. J., Ascencio, J.-M, and Legrand, M.: Polar ice evidence that
atmospheric CO2 20,000 yr BP was 50 % of present, Nature, 284,
155–157, https://doi.org/10.1038/284155a0, 1980.
Dlugokencky, E. J., Myers, R. C., Lang, P. M., Masarie, K. A., Crotwell, A.
M., Thoning, K. W., Hall, B. D., Elkins, J. W., and Steele, L. P.:
Conversion of NOAA atmospheric dry air CH4 mole fractions to a
gravimetrically prepared standard scale, J. Geophys. Res., 110, D18306,
https://doi.org/10.1029/2005JD006035, 2005.
Dunbar, N. W., McIntosh, W. C., and Esser, R. P.: Physical setting and
tephrochronology of the summit caldera ice record at Mount Moulton, West
Antarctica, Geol. Soc. Am. Bull., 120, 796–812,
https://doi.org/10.1130/B26140.1, 2008.
Elderfield, H., Ferretti, P., Greaves, M., Crowhurst, S., McCave, I. N.,
Hodell, D., and Piotrowski, A. M.: Evolution of Ocean Temperature and Ice
Volume Through the Mid-Pleistocene Climate Transition, Science, 337,
704–709, https://doi.org/10.1126/science.1221294, 2012.
EPICA Community Members: Eight glacial cycles from an Antarctic ice
core, Nature, 429, 623–628, https://doi.org/10.1038/nature02599, 2004.
Extier, T., Landais, A., Bréant, C., Prié, F., Bazin, L., Dreyfus,
G., Roche, D. M., and Leuenberger, M.: δ18Oatm records
between 100–800 ka from EPICA Dome C ice core, PANGAEA [data set],
https://doi.org/10.1594/PANGAEA.887323, 2018a.
Extier, T., Landais, A., Bréant, C., Prié, F., Bazin, L., Dreyfus,
G., Roche, D. M., and Leuenberger, M.: On the use of δ18Oatm for ice core dating, Quaternary Sci. Rev., 185, 244–257,
https://doi.org/10.1016/j.quascirev.2018.02.008, 2018b.
Fischer, H., Severinghaus, J., Brook, E., Wolff, E., Albert, M., Alemany, O., Arthern, R., Bentley, C., Blankenship, D., Chappellaz, J., Creyts, T., Dahl-Jensen, D., Dinn, M., Frezzotti, M., Fujita, S., Gallee, H., Hindmarsh, R., Hudspeth, D., Jugie, G., Kawamura, K., Lipenkov, V., Miller, H., Mulvaney, R., Parrenin, F., Pattyn, F., Ritz, C., Schwander, J., Steinhage, D., van Ommen, T., and Wilhelms, F.: Where to find 1.5 million yr old ice for the IPICS “Oldest-Ice” ice core, Clim. Past, 9, 2489–2505, https://doi.org/10.5194/cp-9-2489-2013, 2013.
Fogwill, C. J., Turney, C. S. M., Menviel, L., Baker, A., Weber, M. E.,
Ellis, B., Thomas, Z. A., Golledge, N. R., Etheridge, D., Rubino, M.,
Thornton., D. P., Van Ommen, T. D., Moy, A. D., Curran, M. A. J., Davies,
S., Bird, M. I., Munksgaard, N. C., Rootes, C. M., Millman, H., Vohra, J.,
Rivera, A., Mackintosh, A., Pike, J., Hall, I. R., Bagshaw, E. A., Rainsley,
E., Bronk-Ramsey, C., Montenari, M., Cage, A. G., Harris, M. R. P., Jones,
R., Power, A., Love, J., Young, J., Weyrich, L. S., and Cooper, A.: Southern
Ocean carbon sink enhanced by sea-ice feedbacks at the Antarctic Cold
Reversal, Nat. Geosci., 13, 489–497,
https://doi.org/10.1038/s41561-020-0587-0, 2020.
Folco, L., Welten, K. C., Jull, A. J. T., Nishiizumi, K., and Zeoli, A.:
Meteorites constrain the age of Antarctic ice at the Frontier Mountain blue
ice field (northern Victoria Land), Earth Planet Sc. Lett., 248, 209–216,
https://doi.org/10.1016/j.epsl.2006.05.022, 2006.
Gardner, A. S., Moholdt, G., Scambos, T., Fahnstock, M., Ligtenberg, S., van den Broeke, M., and Nilsson, J.: Increased West Antarctic and unchanged East Antarctic ice discharge over the last 7 years, The Cryosphere, 12, 521–547, https://doi.org/10.5194/tc-12-521-2018, 2018.
Goujon, C., Barnola, J.-M., and Ritz, C.: Modeling the densification of
polar firn including heat diffusion: Application to close-off
characteristics and gas isotopic fractionation for Antarctica and Greenland
sites, J. Geophys. Res., 108, 4792, https://doi.org/10.1029/2002JD003319,
2003.
Hall, B. D., Crotwell, A. M., Kitzis, D. R., Mefford, T., Miller, B. R., Schibig, M. F., and Tans, P. P.: Revision of the World Meteorological Organization Global Atmosphere Watch (WMO/GAW) CO2 calibration scale, Atmos. Meas. Tech., 14, 3015–3032, https://doi.org/10.5194/amt-14-3015-2021, 2021.
Harvey, R.: The Origin and Significance of Antarctic Meteorites,
Geochemistry, 63, 93–147, https://doi.org/10.1078/0009-2819-00031, 2003.
Herron, M. M. and Langway, C. C.: Firn densification: An empirical model,
J. Glaciol., 25, 373–385, https://doi.org/10.3189/S0022143000015239, 1980.
Higgins, J. A., Kurbatov, A. V., Spaulding, N. E., Brook, E., Introne, D.
S., Chimiak, L. M., Yan, Y., Mayewski, P. A., and Bender, M. L.: Atmospheric
composition 1 million years ago from blue ice in the Allan Hills,
Antarctica, P. Natl. Acad. Sci. USA., 112, 6887–6891,
https://doi.org/10.1073/pnas.1420232112, 2015.
Hu, J., Yan, Y., Yeung, L. Y., and Dee, S. G.: Sublimation origin of
negative deuterium excess observed in snow and ice samples from McMurdo Dry
Valleys and Allan Hills Blue Ice Areas, East Antarctica, J.
Geophys. Res.-Atmos. [preprint],
https://doi.org/10.1002/essoar.10508105.1, 4 October 2021.
Hui, F., Ci, T., Cheng, X., Scambo, T. A., Liu, Y., Zhang, Y., Chi, Z.,
Huang H., Wang, X., Wang, F., Zhao, C., Jin, Z., and Wang, K.: Mapping
blue-ice areas in Antarctica using ETM+ and MODIS data, Ann. Glaciol., 55,
129–137, https://doi.org/10.3189/2014AoG66A069, 2014.
Ikeda-Fukazawa, T., Fukumizu, K., Kawamura, K., Aoki, S., Nakazawa, T., and
Hondoh, T.: Effects of molecular diffusion on trapped gas composition in
polar ice cores, Earth Planet. Sc. Lett., 299, 183–192,
https://doi.org/10.1016/j.epsl.2004.11.011, 2005.
Jang, Y., Han, Y., Ryu, Y., Moon, J., Ju, H.-T., Yang, J.-W., Lee, H.-G.,
Jun, S. J., Lee, J., Hur, S. D., Lee, J. I., and Ahn, J.: A preliminary
study for blue ice in Victoria Land, East Antarctica, Journal of the
Geological Society of Korea, 53, 567–580,
https://doi.org/10.14770/jgsk.2017.53.4.567, 2017.
Jiang, W., Bailey, K., Lu, Z.-T., Mueller, P., O'Connor, T. P., Cheng,
C.-F., Hu, S.-M., Purtschert, R., Sturchio, N. C., Sun, Y. R., Williams, W.
D., and Yang, G.-M.: An atom counter for measuring 81Kr and 85Kr
in environmental samples, Geochim. Cosmochim. Ac., 91, 1–6,
https://doi.org/10.1016/j.gca.2012.05.019, 2012.
Jiang, W., Hu, S.-M., Lu, Z.-T., Ritterbusch, F., and Yang, G.: Latest
development of radiokrypton dating – A tool to find and study
paleogroundwater, Quatern. Int., 547, 166–171,
https://doi.org/10.1016/j.quaint.2019.04.025, 2020.
Jouzel, J., Alley, R. B., Cuffey, K. M., Dansgaard, W., Grootes, P.,
Hoffmann, G., Johnsen, S. J., Koster, R. D., Peel, D., Shuman, C. A.,
Stievenard, M., Stuiver, M., and White, J.: Validity of the temperature
reconstruction from water isotopes in ice cores, J. Geophys. Res., 102,
26471–26487, https://doi.org/10.1029/97JC01283, 1997.
Korotkikh, E. V., Mayewski, P. A., Handley, M. J., Sneed, S. B., Introne, D.
S., Kurbatov, A. V., Dunbar, N. W., and McIntosh, W. C.: The last
interglacial as represented in the glaciochemical record from Mount Moulton
Blue Ice Area, West Antarctica, Quaternary Sci. Rev., 30, 1940–1947,
https://doi.org/10.1016/j.quascirev.2011.04.020, 2011.
Landais, A., Caillon, N., Severinghaus, J., Jouzel, J., and Masson-Delmotte,
V.: Analyses isotopiques à haute précision de l'air piégé
dans les glaces polaires pour la quantification des variations rapides de
température: méthodes et limites, Notes des activités
instrumentales de l'IPSL, 39, https://hal.archives-ouvertes.fr/hal-03263858/document (last access: 6 June 2022), 2003.
Landais, A., Dreyfus, G., Capron, E., Masson-Delmotte, V., Sanchez-Goñi,
M. F., Desprat, S., Hoffmann, G., Jouzel, J., Leuenberger, M., and Johnsen,
S.: What drives the millennial and orbital variations of δ18Oatm?, Quaternary Sci. Rev., 29, 235–246,
https://doi.org/10.1016/j.quascirev.2009.07.005, 2010.
Landais, A., Dreyfus, G. B., Capron, E., Jouzel, J., Masson-Delmotte, V.,
Roche, D. M., Prié, F., Caillon, N., Chappellaz, J., Leuenberger, M.,
Lourantou, A., Parrenin, F., Raynaud, D., and Teste, G.: EPICA Dome C Ice
Core Terminations I and II Air Isotopes and CO2 Data, NOAA/WDS for
Paleoclimatology [data set],
https://www.ncei.noaa.gov/pub/data/paleo/icecore/antarctica/epica_domec/edc2013d18oatm.txt (last access: 1 September 2021), 2013.
Landais, A., Masson-Delmotte, V., Stenni, B., Selmo, E., Roche, D.M.,
Jouzel, J., Lambert, F., Guillevic, M., Bazin, L., Arzel, O., Vinther, B.,
Gkinis, V., and Popp, T.: A review of the bipolar see–saw from synchronized
and high resolution ice core water stable isotope records from Greenland and
East Antarctica, Quaternary Sci. Rev., 114, 18–32,
https://doi.org/10.1016/j.quascirev.2015.01.031, 2015.
Lisiecki, L. E. and Raymo, M. E.: A Pliocene-Pleistocene stack of 57
globally distributed benthic δ18O records, Paleoceanography,
20, PA1003, https://doi.org/10.1029/2004pa001071, 2005.
Loosli, H. H. and Oeschger, H.: 37Ar and 81Kr in the atmosphere,
Earth Planet Sc. Lett., 7, 67–71,
https://doi.org/10.1016/0012-821X(69)90014-4, 1969.
Lourantou, A., Chappellaz, J., Barnola J.-M., Masson-Delmotte, V., and
Raynaud, D.: Changes in atmospheric CO2 and its carbon isotopic ratio
during the penultimate deglaciation, Quaternary Sci. Rev., 29, 1983–1992,
https://doi.org/10.1016/j.quascirev.2010.05.002, 2010.
Lu, Z.-T., Schlosser, P., Smethie Jr., W. M., Sturchio, N. C., Fischer, T.
P., Kennedy, B. M., Purtschert, R., Severinghaus, J. P., Solomon, D. K.,
Tanhua, T., and Yokochi, R.: Tracer applications of noble gas radionuclides
in the geosciences, Earth-Sci. Rev., 138, 196–214,
https://doi.org/10.1016/j.earscirev.2013.09.002, 2014.
Lüthi, D., Floch, M. L., Bereiter, B., Blunier, T., Barnola, J.-M., Siegenthaler, U., Raynaud, D., Jouzel, J., Fischer, H., Kawamura, K., and Stocker, T. F.: High-resolution carbon dioxide concentration record 650,000–800,000 years before present, Nature, 453, 379–382, https://doi.org/10.1038/nature06949, 2008.
Marcott, S. A., Bauska, T. K., Buizert, C., Steig, E. J., Rosen, J. L.,
Cuffey, K. M., Fudge, T. J., Severinghaus, J. P., Ahn, J., Kalk, M. L.,
McConnell, J. R., Sowers, T., Taylor K. C., White, J. W. C., and Brook, E.
J.: Centennial-scale changes in the global carbon cycle during the last
deglaciation, Nature, 514, 616–619, https://doi.org/10.1038/nature13799,
2014.
Masson-Delmotte, V., Hou, S., Ekaykin, A., Jouzel, J., Aristarain, A.,
Bernardo, R. T., Bromwich, D., Cattani, O., Delmotte, M., Falourd, S.,
Frezzotti, M., Gallée, H., Genoni, L., Isaksson, E., Landais, A.,
Helsen, M. M., Hoffmann, G., Lopez, J., Morgan, V., Motoyama, H., Noone, D.,
Oerter, H., Petit, J. R., Royer, A., Uemura, R., Schmidt, G. A., Schlosser,
E., Simões, J. C., Steig, E. J., Stenni, B., Stievenard, M., Van Den
Broeke, M. R., Van De Wal, R. S. W., Van De Berg, W. J., Vimeux, F., and White,
J. W. C.: A review of Antarctic surface snow isotopic composition:
Observations, atmospheric circulation, and isotopic modeling, J. Climate,
21, 3359–3387, https://doi.org/10.1175/2007JCLI2139.1, 2008.
Masson-Delmotte, V., Buiron, D., Ekaykin, A., Frezzotti, M., Gallée, H., Jouzel, J., Krinner, G., Landais, A., Motoyama, H., Oerter, H., Pol, K., Pollard, D., Ritz, C., Schlosser, E., Sime, L. C., Sodemann, H., Stenni, B., Uemura, R., and Vimeux, F.: A comparison of the present and last interglacial periods in six Antarctic ice cores, Clim. Past, 7, 397–423, https://doi.org/10.5194/cp-7-397-2011, 2011.
Matsuoka, K., Skoglund, A., and Roth, G.: Quanarctica, Norwegian
Polar Institute [data set], https://doi.org/10.21334/npolar.2018.8516e961, 2018.
Matsuoka, K., Skoglund, A., Roth, G., de Pomereu, J., Griffiths, H.,
Headland, R., Herried, B., Katsumata, K., Le Brocq, A., Licht, K., Morgan,
F., Neff, P. D., Ritz, C., Scheinert, M., Tamura, T., Van de Putte, A., van
den Broeke, M., von Deschwanden, A., Deschamps-Berger, C., Van Liefferinge,
B., Tronstad, S., and Melvær, Y.: Quantarctica, an integrated mapping
environment for Antarctica, the Southern Ocean, and sub-Antarctic islands,
Environ. Model. Softw., 140, 105015,
https://doi.org/10.1016/j.envsoft.2021.105015, 2021.
Menking, J. A., Brook, E. J., Shackleton, S. A., Severinghaus, J. P., Dyonisius, M. N., Petrenko, V., McConnell, J. R., Rhodes, R. H., Bauska, T. K., Baggenstos, D., Marcott, S., and Barker, S.: Spatial pattern of accumulation at Taylor Dome during Marine Isotope Stage 4: stratigraphic constraints from Taylor Glacier, Clim. Past, 15, 1537–1556, https://doi.org/10.5194/cp-15-1537-2019, 2019.
Monnin, E., Indermühle, A., Dällenbach, A., Flückiger, J.,
Stauffer, B., Stocker, T. F., Raynaud, D., and Barnola, J.-M.: Atmospheric
CO2 concentrations over the last glacial termination, Science, 291,
112–114, https://doi.org/10.1126/science.291.5501.112, 2001.
Monnin, E., Steig, E. J., Siegenthaler, U., Kawamura, K., Schwander, J.,
Stauffer, B., Stocker, T. F., Morse, D. L., Barnola, J.-M., Bellier, B.,
Raynaud, D., and Fischer, H.: Evidence for substantial accumulation rate
variability in Antarctica during the Holocene, through synchronization of
CO2 in the Taylor Dome, Dome C and DML ice cores, Earth Planet Sc.
Lett., 224, 45–54, https://doi.org/10.1016/j.epsl.2004.05.007, 2004.
Morse, D. L., Waddington, E. D., and Steig, E. J.: Ice age storm
trajectories inferred from radar stratigraphy at Taylor Dome, Antarctica,
Geophys. Res. Lett., 25, 3383–3386, https://doi.org/10.1029/98GL52486,
1998.
Mouginot, J., Scheuchl, B., and Rignot, E.: Mapping of Ice Motion in
Antarctica Using Synthetic-Aperture Radar Data, Remote Sensing, 4,
2753–2767, https://doi.org/10.3390/rs4092753, 2012.
Nakawo, M., Nagoshi, M., and Mae S.: Stratigraphic record of an ice core
from the Yamato meteorite ice field, Antarctica, Ann. Glaciol., 10,
126–129, https://doi.org/10.3189/S0260305500004298, 1988.
Oeschger, H.: Accelerator mass spectrometry and ice core research, Nucl.
Instrum. Meth. B., 29, 196–202,
https://doi.org/10.1016/0168-583X(87)90235-7, 1987.
Oyabu, I., Kawamura, K., Kitamura, K., Dallmayr, R., Kitamura, A., Sawada, C., Severinghaus, J. P., Beaudette, R., Orsi, A., Sugawara, S., Ishidoya, S., Dahl-Jensen, D., Goto-Azuma, K., Aoki, S., and Nakazawa, T.: New technique for high-precision, simultaneous measurements of CH4, N2O and CO2 concentrations; isotopic and elemental ratios of N2, O2 and Ar; and total air content in ice cores by wet extraction, Atmos. Meas. Tech., 13, 6703–6731, https://doi.org/10.5194/amt-13-6703-2020, 2020.
Oyabu, I., Kawamura, K., Uchida, T., Fujita, S., Kitamura, K., Hirabayashi, M., Aoki, S., Morimoto, S., Nakazawa, T., Severinghaus, J. P., and Morgan, J. D.: Fractionation of
Parrenin, F., Barker, S., Blunier, T., Chappellaz, J., Jouzel, J., Landais, A., Masson-Delmotte, V., Schwander, J., and Veres, D.: On the gas-ice depth difference (Δdepth) along the EPICA Dome C ice core, Clim. Past, 8, 1239–1255, https://doi.org/10.5194/cp-8-1239-2012, 2012.
Petit, J. R., Jouzel, J., Raynaud, D., Barkov, N. I., Barnola, J.-M., Basile,
I., Bender, M., Chappellaz, J., Davis, M., Delaygue, G. Delmotte, M.,
Kotlyakov, V. M., Legrand, M., Lipenkov, V. Y., Lorius, C., PÉpin, L.,
Ritz, C., Saltzman, E., and Stievenard, M.: Climate and atmospheric history
of the past 420,000 years from the Vostok ice core, Antarctica, Nature, 399,
429–436, https://doi.org/10.1038/20859, 1999.
Petrenko, V. V., Severinghaus, J. P., Brook, E. J., Reeh, N., and Schaefer,
H.: Gas records from the West Greenland ice margin covering the Last Glacial
Termination: a horizontal ice core, Quaternary Sci. Rev., 25, 865–875,
https://doi.org/10.1016/j.quascirev.2005.09.005, 2006.
Reeh, N., Oerter, H., and Thomsen, H. H.: Comparison between Greenland
ice-margin and ice-core oxygen-18 records, Ann. Glaciol., 35, 136–144,
https://doi.org/10.3189/172756402781817365, 2002.
Reynolds, J. M.: Dielectric Behaviour of Firn and Ice from the Antarctic
Peninsula, Antarctica, J. Glaciol., 31, 253–262,
https://doi.org/10.3189/S0022143000006584, 1985.
Rhodes, R. H., Brook, E. J., Blunier, T., McConnell, J. R., and Romanini,
D.: Experiment-time-integrated CH4 data from all 3 instruments,
calibrated and corrected for solubility and gravitational effects of the
WAIS-Divide ice core, Antarctica, PANGAEA [data set],
https://doi.org/10.1594/PANGAEA.875980, 2017.
Rignot, E., Mouginot, J., and Scheuchl, B.: Ice Flow of the Antarctic Ice
Sheet, Science, 333, 1427–1430, https://doi.org/10.1126/science.1208336, 2011.
Schaefer, H., Whiticar, M. J., Brook, E. J., Petrenko, V. V., Ferretti, D.
F., and Severinghaus J. P.: Ice record of δ13C for atmospheric
CH4 across the Younger Dryas-Preboreal transition, Science, 313,
1109–1112, https://doi.org/10.1126/science.1126562, 2006.
Schaefer, H., Petrenko, V. V., Brook, E. J., Severinghaus, J. P., Reeh, N.,
Melton, J. R., and Mitchell, L.: Ice stratigraphy at the Pâkitsoq ice
margin, West Greenland, derived from gas records, J. Glaciol., 55, 411–421,
https://doi.org/10.3189/002214309788816704, 2009.
Schmitt, J., Schneider, R., Elsig, J., Leuenberger, D., Lourantou, A.,
Chappellaz, J., Köhler, P., Joos, F., Stocker, T. F., Leuenberger, M.,
and Fischer, H.: Carbon isotope constraints on the deglacial CO2 rise
from ice cores, Science, 336, 711–714, https://doi.org/10.1126/science.1217161, 2012.
Schwander, J. and Stauffer, B.: Age difference between polar ice and the
air trapped in its bubbles, Nature, 311, 45–47,
https://doi.org/10.1038/311045a0, 1984.
Schwander, J., Sowers, T., Barnola, J.-M., Blunier, T., Fuchs, A., and
Malaizé B.: Age scale of the air in the summit ice: Implication for
glacial-interglacial temperature change, J. Geophys. Res., 102,
19483–19493, https://doi.org/10.1029/97JD01309, 1997.
Seltzer, A. M., Buizert, C., Baggenstos, D., Brook, E. J., Ahn, J., Yang, J.-W., and Severinghaus, J. P.: Does δ18O of O2 record meridional shifts in tropical rainfall?, Clim. Past, 13, 1323–1338, https://doi.org/10.5194/cp-13-1323-2017, 2017.
Severi, M., Udisti, R., Becagli, S., Stenni, B., and Traversi, R.: Volcanic synchronisation of the EPICA-DC and TALDICE ice cores for the last 42 kyr BP, Clim. Past, 8, 509–517, https://doi.org/10.5194/cp-8-509-2012, 2012.
Severinghaus, J. P.: Low-res δ15N and δ18O of O2 in the WAIS Divide 06A Deep
Core, U.S. Antarctic Program (USAP) Data Center [data set], https://doi.org/10.7265/N5S46PWD, 2015.
Severinghaus, J. P., Sowers, T., Brook, E. J., Alley, R. B., and Bender, M.
L.: Timing of abrupt climate change at the end of the Younger Dryas interval
from thermally fractionated gases in polar ice, Nature, 391, 141–146,
https://doi.org/10.1038/34346, 1998.
Severinghaus, J. P., Beaudette, R., Headly, M. A., Taylor, K., and Brook, E.
J.: Oxygen-18 of O2 Records the Impact of Abrupt Climate Change on the
Terrestrial Biosphere, Science, 324, 1431–1434, https://doi.org/10.1126/science.1169473, 2009.
Shin, J.: Atmospheric CO2 variations on millennial time scales during
the early Holocene, MS thesis, School of Earth and Environmental Sciences,
Seoul National University, South Korea, https://s-space.snu.ac.kr/bitstream/10371/131380/1/000000017635.pdf (last access: 6 June 2022), 2014.
Ship, S., Anderson, J., and Domack, E.: Late Pleistocene–Holocene retreat
of the West Antarctic Ice-Sheet system in the Ross Sea: part 1 –
Geophysical results, Geol. Soc. Am. Bull., 111, 1486–1516,
https://doi.org/10.1130/0016-7606(1999)111<1486:LPHROT>2.3.CO;2,
1999.
Siegenthaler, U., Stocker, T. F., Monnin, E., Lüthi, D., Schwander, J.,
Staffer, B., Raynaud, D., Barnola, J.-M., Fischer, H., Masson-Delmotte, V.,
and Jouzel, J.: Stable carbon cycle–climate relationship during the late
Pleistocene, Science, 310, 1313–1317, https://doi.org/10.1126/science.1120130, 2005.
Sigl, M., Fudge, T. J., Winstrup, M., Cole-Dai, J., Ferris, D., McConnell, J. R., Taylor, K. C., Welten, K. C., Woodruff, T. E., Adolphi, F., Bisiaux, M., Brook, E. J., Buizert, C., Caffee, M. W., Dunbar, N. W., Edwards, R., Geng, L., Iverson, N., Koffman, B., Layman, L., Maselli, O. J., McGwire, K., Muscheler, R., Nishiizumi, K., Pasteris, D. R., Rhodes, R. H., and Sowers, T. A.: The WAIS Divide deep ice core WD2014 chronology – Part 2: Annual-layer counting (0–31 ka BP), Clim. Past, 12, 769–786, https://doi.org/10.5194/cp-12-769-2016, 2016.
Sinisalo, A., Grinsted, A., Moore, J., Meijer, H., Martma, T., and Van De
Wal, R. S. W.: Inferences from stable water isotopes on the Holocene
evolution of Scharffenbergbotnen blue-ice area, East Antarctica, J.
Glaciol., 53, 427–434, https://doi.org/10.3189/002214307783258495, 2007.
Sinisalo, A. and Moore, J. C.: Antarctic blue ice area – towards extracting
palaeoclimate information, Antarct. Sci., 22, 99–115,
https://doi.org/10.1017/S0954102009990691, 2010.
Sowers, T., Bender, M., Raynaud, D., and Korotkevich, Y. S.: δ15N of N2 in air trapped in polar ice: A tracer of gas transport in the firn and a possible constraint on ice age-gas age differences, J. Geophys. Res., 97, 15683–15697, https://doi.org/10.1029/92jd01297, 1992.
Sowers, T., Bender, M., Labeyrie, L., Martinson, D., Jouzel, J., Raynaud,
D., Pichon, J. J., and Korotkevich, Y. S.: A 135,000-year Vostok-Sepcmap
Common temporal framework, Paleoceanography, 8, 737–766,
https://doi.org/10.1029/93PA02328, 1993.
Spaulding, N. E., Higgins, J. A., Kurbatov, A. V., Bender, M. L., Arcone, S.
A., Campbell, S., Dunbar, N. W., Chimiak, L. M., Introne, D. S., and
Mayewski, P. A.: Climate archives from 90 to 250 ka in horizontal and
vertical ice cores from the Allan Hills Blue Ice Area, Antarctica,
Quaternary Res., 80, 562–574, https://doi.org/10.1016/j.yqres.2013.07.004,
2013.
Steffensen, J. P., Andersen, K. K., Bigler, M., Clausen, H. B., Dahl-Jensen,
D., Fischer, H., Goto-Azuma, K., Hansson, M., Johnsen, S. J., Jouzel, J.,
Masson-Delmotte, V., Popp, T., Rasmussen, S. O., Röthlisberger, R.,
Ruth, U., Stauffer, B., Siggaard-Andersen, M.-L., Sveinbjörnsdóttir,
Á. E., Svensson, A., and White, J. W. C.: High-resolution Greenland ice
core data show abrupt climate change happens in few years, Science, 321,
680–684, https://doi.org/10.1126/science.1157707, 2008.
Stenni, B., Buiron, D., Frezzotti, M., Albani, S., Barbante, C., Bard, E.,
Barnola, J. M., Baroni, M., Baumgartner, M., Bonazza, M., Capron, E.,
Castellano, E., Chappellaz, J., Delmonte, B., Falourd, S., Genoni, L.,
lacumin, P., Jouzel, J., Kipfstuhl, S., Landais, A., Lemieux-Dudon, B.,
Maggi, V., Masson-Delmotte, V., Mazzola, C., Minster, B., Montagnat, M.,
Mulvaney, R., Narcisi, B., Oerter, H., Parrenin, F., Petit, J. R., Ritz, C.,
Scarchilli, C., Schilt, A., Schüpbach, S., Schwander, J., Selmo, E.,
Severi, M., Stocker, T. F., and Udisti, R.: Expression of the bipolar
see-saw in Antarctic climate records during the last deglaciation, Nat.
Geosci., 4, 46–49, https://doi.org/10.1038/ngeo1026, 2011.
Tian, L., Ritterbusch, F., Gu J.-Q., Hu, S.-M., Jiang, W., Lu, Z.-T., Wang,
D., and Yang, G.-M.: 81Kr Dating at the Guliya Ice Cap, Tibetan
Plateau, Geohys. Res. Lett., 46, 6636–6643,
https://doi.org/10.1029/2019GL082464, 2019.
Tollenaar, V., Zekollari, H., Lhermitte, S., Tax, D. M. J., Debaille, V.,
Goderis, S., Claeys, P., and Pattyn, F.: Unexplored Antarctic meteorite
collection sites revealed through machine learning, Science Advances, 8, eabj8138,
https://doi.org/10.1126/sciadv.abj8138, 2022.
Turney, C., Fogwill, C., Van Ommen, T. D., Moy, A. D., Etheridge, D.,
Rubino, M., Curran, M. A. J., and Rivera, A.: Late Pleistocene and early
Holocene change in the Weddell Sea: a new climate record from the Patriot
Hills, Ellsworth Mountains, West Antarctica, J. Quaternary Sci., 28,
697–704, https://doi.org/10.1002/jqs.2668, 2013.
Van Ommen, T., Morgan, V., and Curran, M.: Deglacial and Holocene changes in
accumulation at Law Dome, East Antarctica, Ann. Glaciol., 39, 359–365,
https://doi.org/10.3189/172756404781814221, 2004.
Veres, D., Bazin, L., Landais, A., Toyé Mahamadou Kele, H., Lemieux-Dudon, B., Parrenin, F., Martinerie, P., Blayo, E., Blunier, T., Capron, E., Chappellaz, J., Rasmussen, S. O., Severi, M., Svensson, A., Vinther, B., and Wolff, E. W.: The Antarctic ice core chronology (AICC2012): an optimized multi-parameter and multi-site dating approach for the last 120 thousand years, Clim. Past, 9, 1733–1748, https://doi.org/10.5194/cp-9-1733-2013, 2013.
Welten, K. C., Folco, L., Nishiizumi, K., Caffee, M. W., Grimberg, A.,
Meier, M. M. M., and Kober, F.: Meteoritic and bedrock constraints on the
glacial history of Frontier Mountain in northern Victoria Land, Antarctica,
Earth Planet. Sc. Lett., 270, 308–315,
https://doi.org/10.1016/j.epsl.2008.03.052, 2008.
Whillans, I. M. and Cassidy, W. A.: Catch a falling star: Meteorites and old
ice, Science, 222, 55–57, https://doi.org/10.1126/science.222.4619.55, 1983.
Yan, Y., Bender, M. L., Brook, E. J., Clifford, H. M., Kemeny, P. C.,
Kurbatov, A. V., Mackay, S., Mayewski, P. A., Ng, J., Severinghaus J. P.,
and Higgins, J. A.: Two-million-year-old snapshots of atmospheric gases from
Antarctic ice, Nature, 574, 663–666,
https://doi.org/10.1038/s41586-019-1692-3, 2019.
Yan, Y., Spaulding, N. E., Bender, M. L., Brook, E. J., Higgins, J. A., Kurbatov, A. V., and Mayewski, P. A.: Enhanced moisture delivery into Victoria Land, East Antarctica, during the early Last Interglacial: implications for West Antarctic Ice Sheet stability, Clim. Past, 17, 1841–1855, https://doi.org/10.5194/cp-17-1841-2021, 2021.
Yang, J.-W.: Paleoclimate reconstruction from greenhouse gas and borehole
temperature of polar ice cores, and study on the origin of greenhouse gas in
permafrost ice wedges, PhD thesis, School of Earth and Environmental
Sciences, Seoul National University, South Korea, https://s-space.snu.ac.kr/bitstream/10371/152926/1/000000154664.pdf (last access: 9 June 2022), 2019.
Yau A. M., Bender, M. L., Marchant, D. R., and Mackay, S. L.: Geochemical
analyses of air from an ancient debris-covered glacier, Antarctica, Quat.
Geochronol., 28, 29–39, https://doi.org/10.1016/j.quageo.2015.03.008, 2015.
Yokoyama, Y., Anderson, J. B., Yamane, M., Simkins, L. M., Miyairi, Y.,
Yamazaki, T., Koizumi, M., Suga, H., Kusahara, K., Prothro, L., and Hasumi,
H.: Widespread collapse of the Ross Ice Shelf during the late Holocene, P.
Natl. Acad. Sci. USA, 113, 2354–2359,
https://doi.org/10.1073/pnas.1516908113, 2016.
Zappala, J. C., Baggenstos, D., Gerber, C., Jiang, W., Kennedy, B. M., Lu,
Z.-T., Masarik, J., Mueller, P., Purtschert, R., and Visser, A.: Atmospheric
81Kr as an Integrator of Cosmic-Ray Flux on the Hundred-Thousand-Year
Time Scale, Geophys. Res. Lett., 47, e2019GL086381, https://doi.org/10.1029/2019GL086381,
2020.
Zekollari, H., Goderis, S., Debaille, V., van Ginneken, M., Gattacceca, J.,
Team, A., Jull, A. J. T., Lenaerts, J. T. M., Yamaguchi, A., Huybrechts, P., and
Claeys, P.: Unravelling the high-altitude Nansen blue ice field meteorite
trap (East Antarctica) and implications for regional paleo-conditions,
Geochim. Cosmochim. Ac., 248, 289–310,
https://doi.org/10.1016/j.gca.2018.12.035, 2019.
Short summary
Blue-ice areas (BIAs) have several advantages for reconstructing past climate. However, the complicated ice flow in the area hinders constraining the age. We applied state-of-the-art techniques and found that the ages cover the last deglaciation period. Our study demonstrates that the BIA in northern Victoria Land may help reconstruct the past climate during the termination of the last glacial period.
Blue-ice areas (BIAs) have several advantages for reconstructing past climate. However, the...
