Articles | Volume 5, issue 4
https://doi.org/10.5194/tc-5-1057-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/tc-5-1057-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
28 Nov 2011
Research article |
| 28 Nov 2011
Spatial and temporal variability of snow accumulation rate on the East Antarctic ice divide between Dome Fuji and EPICA DML
S. Fujita
National Institute of Polar Research, Research Organization of Information and Systems, Tokyo, Japan
P. Holmlund
Department of Physical Geography and Quaternary Geology, Stockholm University, Stockholm, Sweden
I. Andersson
Division of Geodesy and Geoinformatics, The Royal Inst. of Technology, Stockholm, Sweden
I. Brown
Department of Physical Geography and Quaternary Geology, Stockholm University, Stockholm, Sweden
H. Enomoto
National Institute of Polar Research, Research Organization of Information and Systems, Tokyo, Japan
Kitami Institute of Technology, Kitami, Japan
Y. Fujii
National Institute of Polar Research, Research Organization of Information and Systems, Tokyo, Japan
K. Fujita
Graduate School of Environmental Studies, Nagoya University, Nagoya, Japan
K. Fukui
National Institute of Polar Research, Research Organization of Information and Systems, Tokyo, Japan
now at: Tateyama Caldera Sabo Museum, Toyama, Japan
T. Furukawa
National Institute of Polar Research, Research Organization of Information and Systems, Tokyo, Japan
M. Hansson
Department of Physical Geography and Quaternary Geology, Stockholm University, Stockholm, Sweden
K. Hara
Department of Earth System Science, Faculty of Science, Fukuoka University, Fukuoka, Japan
Y. Hoshina
Graduate School of Environmental Studies, Nagoya University, Nagoya, Japan
M. Igarashi
National Institute of Polar Research, Research Organization of Information and Systems, Tokyo, Japan
Y. Iizuka
Institute of Low Temperature Science, Hokkaido University, Sapporo, Japan
S. Imura
National Institute of Polar Research, Research Organization of Information and Systems, Tokyo, Japan
S. Ingvander
Department of Physical Geography and Quaternary Geology, Stockholm University, Stockholm, Sweden
T. Karlin
Department of Physical Geography and Quaternary Geology, Stockholm University, Stockholm, Sweden
H. Motoyama
National Institute of Polar Research, Research Organization of Information and Systems, Tokyo, Japan
F. Nakazawa
National Institute of Polar Research, Research Organization of Information and Systems, Tokyo, Japan
H. Oerter
Alfred Wegener Institute for Polar and Marine Research, P.O. Box 120161, 27515, Bremerhaven, Germany
L. E. Sjöberg
Division of Geodesy and Geoinformatics, The Royal Inst. of Technology, Stockholm, Sweden
S. Sugiyama
Institute of Low Temperature Science, Hokkaido University, Sapporo, Japan
S. Surdyk
National Institute of Polar Research, Research Organization of Information and Systems, Tokyo, Japan
J. Ström
Department of Applied Environmental Science, Stockholm University, Stockholm, Sweden
R. Uemura
Faculty of Science, Department of Chemistry, Biology, and Marine Science, University of the Ryukyus, Okinawa, Japan
F. Wilhelms
Alfred Wegener Institute for Polar and Marine Research, P.O. Box 120161, 27515, Bremerhaven, Germany
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The Cryosphere, 18, 3067–3079, https://doi.org/10.5194/tc-18-3067-2024, https://doi.org/10.5194/tc-18-3067-2024, 2024
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Cristina Gerli, Sebastian Rosier, G. Hilmar Gudmundsson, and Sainan Sun
The Cryosphere, 18, 2677–2689, https://doi.org/10.5194/tc-18-2677-2024, https://doi.org/10.5194/tc-18-2677-2024, 2024
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Charlotte M. Carter, Michael J. Bentley, Stewart S. R. Jamieson, Guy J. G. Paxman, Tom A. Jordan, Julien A. Bodart, Neil Ross, and Felipe Napoleoni
The Cryosphere, 18, 2277–2296, https://doi.org/10.5194/tc-18-2277-2024, https://doi.org/10.5194/tc-18-2277-2024, 2024
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David B. Bonan, Jakob Dörr, Robert C. J. Wills, Andrew F. Thompson, and Marius Årthun
The Cryosphere, 18, 2141–2159, https://doi.org/10.5194/tc-18-2141-2024, https://doi.org/10.5194/tc-18-2141-2024, 2024
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Antarctic sea ice has exhibited variability over satellite records, including a period of gradual expansion and a period of sudden decline. We use a novel statistical method to identify sources of variability in observed Antarctic sea ice changes. We find that the gradual increase in sea ice is likely related to large-scale temperature trends, and periods of abrupt sea ice decline are related to specific flavors of equatorial tropical variability known as the El Niño–Southern Oscillation.
Rebecca B. Latto, Ross J. Turner, Anya M. Reading, and J. Paul Winberry
The Cryosphere, 18, 2061–2079, https://doi.org/10.5194/tc-18-2061-2024, https://doi.org/10.5194/tc-18-2061-2024, 2024
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The study of icequakes allows for investigation of many glacier processes that are unseen by typical reconnaissance methods. However, detection of such seismic signals is challenging due to low signal-to-noise levels and diverse source mechanisms. Here we present a novel algorithm that is optimized to detect signals from a glacier environment. We apply the algorithm to seismic data recorded in the 2010–2011 austral summer from the Whillans Ice Stream and evaluate the resulting event catalogue.
Rebecca B. Latto, Ross J. Turner, Anya M. Reading, Sue Cook, Bernd Kulessa, and J. Paul Winberry
The Cryosphere, 18, 2081–2101, https://doi.org/10.5194/tc-18-2081-2024, https://doi.org/10.5194/tc-18-2081-2024, 2024
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Seismic catalogues are potentially rich sources of information on glacier processes. In a companion study, we constructed an event catalogue for seismic data from the Whillans Ice Stream. Here, we provide a semi-automated workflow for consistent catalogue analysis using an unsupervised cluster analysis. We discuss the defining characteristics of identified signal types found in this catalogue and possible mechanisms for the underlying glacier processes and noise sources.
Sanne B. M. Veldhuijsen, Willem Jan van de Berg, Peter Kuipers Munneke, and Michiel R. van den Broeke
The Cryosphere, 18, 1983–1999, https://doi.org/10.5194/tc-18-1983-2024, https://doi.org/10.5194/tc-18-1983-2024, 2024
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We use the IMAU firn densification model to simulate the 21st-century evolution of Antarctic firn air content. Ice shelves on the Antarctic Peninsula and the Roi Baudouin Ice Shelf in Dronning Maud Land are particularly vulnerable to total firn air content (FAC) depletion. Our results also underline the potentially large vulnerability of low-accumulation ice shelves to firn air depletion through ice slab formation.
Jan De Rydt and Kaitlin Naughten
The Cryosphere, 18, 1863–1888, https://doi.org/10.5194/tc-18-1863-2024, https://doi.org/10.5194/tc-18-1863-2024, 2024
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The West Antarctic Ice Sheet is losing ice at an accelerating pace. This is largely due to the presence of warm ocean water around the periphery of the Antarctic continent, which melts the ice. It is generally assumed that the strength of this process is controlled by the temperature of the ocean. However, in this study we show that an equally important role is played by the changing geometry of the ice sheet, which affects the strength of the ocean currents and thereby the melt rates.
Allison M. Chartrand, Ian M. Howat, Ian R. Joughin, and Benjamin E. Smith
EGUsphere, https://doi.org/10.5194/egusphere-2024-1132, https://doi.org/10.5194/egusphere-2024-1132, 2024
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This study uses high-resolution remote sensing data to show that shrinking of the West Antarctic Thwaites Glacier’s ice shelf (floating extension) is exacerbated by the presence of sub–ice shelf meltwater channels that form as the glacier transitions from full contact with the bed to fully floating. In mapping these channels, the position of the transition zone, and thinning rates of the Thwaites Glacier, this work elucidates important processes driving its rapid contribution to sea level rise.
Edmund J. Lea, Stewart S. R. Jamieson, and Michael J. Bentley
The Cryosphere, 18, 1733–1751, https://doi.org/10.5194/tc-18-1733-2024, https://doi.org/10.5194/tc-18-1733-2024, 2024
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We use the ice surface expression of the Gamburtsev Subglacial Mountains in East Antarctica to map the horizontal pattern of valleys and ridges in finer detail than possible from previous methods. In upland areas, valleys are spaced much less than 5 km apart, with consequences for the distribution of melting at the bed and hence the likelihood of ancient ice being preserved. Automated mapping techniques were tested alongside manual approaches, with a hybrid approach recommended for future work.
Brad Reed, J. A. Mattias Green, Adrian Jenkins, and G. Hilmar Gudmundsson
EGUsphere, https://doi.org/10.5194/egusphere-2024-673, https://doi.org/10.5194/egusphere-2024-673, 2024
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We use a numerical ice-flow model to simulate the response of a 1940s Pine Island Glacier to changes in melting beneath its ice shelf. A decadal period of warm forcing is sufficient to push the glacier into an unstable, irreversible retreat from its long-term position on a subglacial ridge to an upstream ice plain. This retreat can only be stopped when unrealistic cold forcing is applied. These results show that short warm anomalies can lead to quick and substantial increases in ice flux.
In-Woo Park, Emilia Kyung Jin, Mathieu Morlighem, and Kang-Kun Lee
The Cryosphere, 18, 1139–1155, https://doi.org/10.5194/tc-18-1139-2024, https://doi.org/10.5194/tc-18-1139-2024, 2024
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This study conducted 3D thermodynamic ice sheet model experiments, and modeled temperatures were compared with 15 observed borehole temperature profiles. We found that using incompressibility of ice without sliding agrees well with observed temperature profiles in slow-flow regions, while incorporating sliding in fast-flow regions captures observed temperature profiles. Also, the choice of vertical velocity scheme has a greater impact on the shape of the modeled temperature profile.
Matthew A. Danielson and Philip J. Bart
The Cryosphere, 18, 1125–1138, https://doi.org/10.5194/tc-18-1125-2024, https://doi.org/10.5194/tc-18-1125-2024, 2024
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The post-Last Glacial Maximum (LGM) retreat of the West Antarctic Ice Sheet in the Ross Sea was more significant than for any other Antarctic sector. Here we combined the available dates of retreat with new mapping of sediment deposited by the ice sheet during overall retreat. Our work shows that the post-LGM retreat through the Ross Sea was not uniform. This uneven retreat can cause instability in the present-day Antarctic ice sheet configuration and lead to future runaway retreat.
Trystan Surawy-Stepney, Anna E. Hogg, Stephen L. Cornford, Benjamin J. Wallis, Benjamin J. Davison, Heather L. Selley, Ross A. W. Slater, Elise K. Lie, Livia Jakob, Andrew Ridout, Noel Gourmelen, Bryony I. D. Freer, Sally F. Wilson, and Andrew Shepherd
The Cryosphere, 18, 977–993, https://doi.org/10.5194/tc-18-977-2024, https://doi.org/10.5194/tc-18-977-2024, 2024
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Here, we use satellite observations and an ice flow model to quantify the impact of sea ice buttressing on ice streams on the Antarctic Peninsula. The evacuation of 11-year-old landfast sea ice in the Larsen B embayment on the East Antarctic Peninsula in January 2022 was closely followed by major changes in the calving behaviour and acceleration (30 %) of the ocean-terminating glaciers. Our results show that sea ice buttressing had a negligible direct role in the observed dynamic changes.
Andrew N. Hennig, David A. Mucciarone, Stanley S. Jacobs, Richard A. Mortlock, and Robert B. Dunbar
The Cryosphere, 18, 791–818, https://doi.org/10.5194/tc-18-791-2024, https://doi.org/10.5194/tc-18-791-2024, 2024
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A total of 937 seawater paired oxygen isotope (δ18O)–salinity samples collected during seven cruises on the SE Amundsen Sea between 1994 and 2020 reveal a deep freshwater source with δ18O − 29.4±1.0‰, consistent with the signature of local ice shelf melt. Local mean meteoric water content – comprised primarily of glacial meltwater – increased between 1994 and 2020 but exhibited greater interannual variability than increasing trend.
Qinggang Gao, Louise C. Sime, Alison J. McLaren, Thomas J. Bracegirdle, Emilie Capron, Rachael H. Rhodes, Hans Christian Steen-Larsen, Xiaoxu Shi, and Martin Werner
The Cryosphere, 18, 683–703, https://doi.org/10.5194/tc-18-683-2024, https://doi.org/10.5194/tc-18-683-2024, 2024
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Antarctic precipitation is a crucial component of the climate system. Its spatio-temporal variability impacts sea level changes and the interpretation of water isotope measurements in ice cores. To better understand its climatic drivers, we developed water tracers in an atmospheric model to identify moisture source conditions from which precipitation originates. We find that mid-latitude surface winds exert an important control on moisture availability for Antarctic precipitation.
Claudio Stefanini, Giovanni Macelloni, Marion Leduc-Leballeur, Vincent Favier, Benjamin Pohl, and Ghislain Picard
The Cryosphere, 18, 593–608, https://doi.org/10.5194/tc-18-593-2024, https://doi.org/10.5194/tc-18-593-2024, 2024
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Local and large-scale meteorological conditions have been considered in order to explain some peculiar changes of snow grains on the East Antarctic Plateau from 2000 to 2022, by using remote sensing observations and reanalysis. We identified some extreme grain size events on the highest ice divide, resulting from a combination of conditions of low wind speed and low temperature. Moreover, the beginning of seasonal grain growth has been linked to the occurrence of atmospheric rivers.
Violaine Coulon, Ann Kristin Klose, Christoph Kittel, Tamsin Edwards, Fiona Turner, Ricarda Winkelmann, and Frank Pattyn
The Cryosphere, 18, 653–681, https://doi.org/10.5194/tc-18-653-2024, https://doi.org/10.5194/tc-18-653-2024, 2024
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We present new projections of the evolution of the Antarctic ice sheet until the end of the millennium, calibrated with observations. We show that the ocean will be the main trigger of future ice loss. As temperatures continue to rise, the atmosphere's role may shift from mitigating to amplifying Antarctic mass loss already by the end of the century. For high-emission scenarios, this may lead to substantial sea-level rise. Adopting sustainable practices would however reduce the rate of ice loss.
Lu Zhou, Julienne Stroeve, Vishnu Nandan, Rosemary Willatt, Shiming Xu, Weixin Zhu, Sahra Kacimi, Stefanie Arndt, and Zifan Yang
EGUsphere, https://doi.org/10.5194/egusphere-2024-81, https://doi.org/10.5194/egusphere-2024-81, 2024
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Snow over Antarctic sea ice, influenced by highly variable meteorological conditions and heavy snowfall, has complex stratigraphy and profound impact over the microwave signature. We employ advanced radiation transfer models to analyze the effects of complex snow properties on brightness temperatures over the sea ice in Southern Oceans. Great potential lies in the understanding of snow processes and the application to satellite retrievals.
Srinidhi Gadde and Willem Jan van de Berg
EGUsphere, https://doi.org/10.5194/egusphere-2024-116, https://doi.org/10.5194/egusphere-2024-116, 2024
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Blowing snow sublimation represents the major loss term in the mass balance of Antarctica. In this study, we update the representation of blowing snow in the regional climate model RACMO. With the updates, results compare well with the observations from East Antarctica. Also, continent wide variation of blowing snow compares well with the satellite observations. Hence, the updates provide a clear step forward in producing physically sound and reliable estimate of the mass balance of Antarctica.
Ashleigh Womack, Alberto Alberello, Marc de Vos, Alessandro Toffoli, Robyn Verrinder, and Marcello Vichi
The Cryosphere, 18, 205–229, https://doi.org/10.5194/tc-18-205-2024, https://doi.org/10.5194/tc-18-205-2024, 2024
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Synoptic events have a significant influence on the evolution of Antarctic sea ice. Our current understanding of the interactions between cyclones and sea ice remains limited. Using two ensembles of buoys, deployed in the north-eastern Weddell Sea region during winter and spring of 2019, we show how the evolution and spatial pattern of sea ice drift and deformation in the Antarctic marginal ice zone were affected by the balance between atmospheric and oceanic forcing and the local ice.
Yushi Morioka, Liping Zhang, Thomas L. Delworth, Xiaosong Yang, Fanrong Zeng, Masami Nonaka, and Swadhin K. Behera
The Cryosphere, 17, 5219–5240, https://doi.org/10.5194/tc-17-5219-2023, https://doi.org/10.5194/tc-17-5219-2023, 2023
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Antarctic sea ice extent shows multidecadal variations with its decrease in the 1980s and increase after the 2000s until 2015. Here we show that our climate model can predict the sea ice decrease by deep convection in the Southern Ocean and the sea ice increase by the surface wind variability. These results suggest that accurate simulation and prediction of subsurface ocean and atmosphere conditions are important for those of Antarctic sea ice variability on a multidecadal timescale.
Hélène Seroussi, Vincent Verjans, Sophie Nowicki, Antony J. Payne, Heiko Goelzer, William H. Lipscomb, Ayako Abe-Ouchi, Cécile Agosta, Torsten Albrecht, Xylar Asay-Davis, Alice Barthel, Reinhard Calov, Richard Cullather, Christophe Dumas, Benjamin K. Galton-Fenzi, Rupert Gladstone, Nicholas R. Golledge, Jonathan M. Gregory, Ralf Greve, Tore Hattermann, Matthew J. Hoffman, Angelika Humbert, Philippe Huybrechts, Nicolas C. Jourdain, Thomas Kleiner, Eric Larour, Gunter R. Leguy, Daniel P. Lowry, Chistopher M. Little, Mathieu Morlighem, Frank Pattyn, Tyler Pelle, Stephen F. Price, Aurélien Quiquet, Ronja Reese, Nicole-Jeanne Schlegel, Andrew Shepherd, Erika Simon, Robin S. Smith, Fiammetta Straneo, Sainan Sun, Luke D. Trusel, Jonas Van Breedam, Peter Van Katwyk, Roderik S. W. van de Wal, Ricarda Winkelmann, Chen Zhao, Tong Zhang, and Thomas Zwinger
The Cryosphere, 17, 5197–5217, https://doi.org/10.5194/tc-17-5197-2023, https://doi.org/10.5194/tc-17-5197-2023, 2023
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Mass loss from Antarctica is a key contributor to sea level rise over the 21st century, and the associated uncertainty dominates sea level projections. We highlight here the Antarctic glaciers showing the largest changes and quantify the main sources of uncertainty in their future evolution using an ensemble of ice flow models. We show that on top of Pine Island and Thwaites glaciers, Totten and Moscow University glaciers show rapid changes and a strong sensitivity to warmer ocean conditions.
Raúl R. Cordero, Sarah Feron, Alessandro Damiani, Pedro J. Llanillo, Jorge Carrasco, Alia L. Khan, Richard Bintanja, Zutao Ouyang, and Gino Casassa
The Cryosphere, 17, 4995–5006, https://doi.org/10.5194/tc-17-4995-2023, https://doi.org/10.5194/tc-17-4995-2023, 2023
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We investigate the response of Antarctic sea ice to year-to-year changes in the tropospheric–stratospheric dynamics. Our findings suggest that, by affecting the tropospheric westerlies, the strength of the stratospheric polar vortex has played a major role in recent record-breaking anomalies in Antarctic sea ice.
Alfonso Ferrone, Étienne Vignon, Andrea Zonato, and Alexis Berne
The Cryosphere, 17, 4937–4956, https://doi.org/10.5194/tc-17-4937-2023, https://doi.org/10.5194/tc-17-4937-2023, 2023
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In austral summer 2019/2020, three K-band Doppler profilers were deployed across the Sør Rondane Mountains, south of the Belgian base Princess Elisabeth Antarctica. Their measurements, along with atmospheric simulations and reanalyses, have been used to study the spatial variability in precipitation over the region, as well as investigate the interaction between the complex terrain and the typical flow associated with precipitating systems.
Joel A. Wilner, Mathieu Morlighem, and Gong Cheng
The Cryosphere, 17, 4889–4901, https://doi.org/10.5194/tc-17-4889-2023, https://doi.org/10.5194/tc-17-4889-2023, 2023
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We use numerical modeling to study iceberg calving off of ice shelves in Antarctica. We examine four widely used mathematical descriptions of calving (
calving laws), under the assumption that Antarctic ice shelf front positions should be in steady state under the current climate forcing. We quantify how well each of these calving laws replicates the observed front positions. Our results suggest that the eigencalving and von Mises laws are most suitable for Antarctic ice shelves.
Rebecca J. Sanderson, Kate Winter, S. Louise Callard, Felipe Napoleoni, Neil Ross, Tom A. Jordan, and Robert G. Bingham
The Cryosphere, 17, 4853–4871, https://doi.org/10.5194/tc-17-4853-2023, https://doi.org/10.5194/tc-17-4853-2023, 2023
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Ice-penetrating radar allows us to explore the internal structure of glaciers and ice sheets to constrain past and present ice-flow conditions. In this paper, we examine englacial layers within the Lambert Glacier in East Antarctica using a quantitative layer tracing tool. Analysis reveals that the ice flow here has been relatively stable, but evidence for former fast flow along a tributary suggests that changes have occurred in the past and could change again in the future.
Thorsten Seehaus, Christian Sommer, Thomas Dethinne, and Philipp Malz
The Cryosphere, 17, 4629–4644, https://doi.org/10.5194/tc-17-4629-2023, https://doi.org/10.5194/tc-17-4629-2023, 2023
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Existing mass budget estimates for the northern Antarctic Peninsula (>70° S) are affected by considerable limitations. We carried out the first region-wide analysis of geodetic mass balances throughout this region (coverage of 96.4 %) for the period 2013–2017 based on repeat pass bi-static TanDEM-X acquisitions. A total mass budget of −24.1±2.8 Gt/a is revealed. Imbalanced high ice discharge, particularly at former ice shelf tributaries, is the main driver of overall ice loss.
Julius Garbe, Maria Zeitz, Uta Krebs-Kanzow, and Ricarda Winkelmann
The Cryosphere, 17, 4571–4599, https://doi.org/10.5194/tc-17-4571-2023, https://doi.org/10.5194/tc-17-4571-2023, 2023
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We adopt the novel surface module dEBM-simple in the Parallel Ice Sheet Model (PISM) to investigate the impact of atmospheric warming on Antarctic surface melt and long-term ice sheet dynamics. As an enhancement compared to traditional temperature-based melt schemes, the module accounts for changes in ice surface albedo and thus the melt–albedo feedback. Our results underscore the critical role of ice–atmosphere feedbacks in the future sea-level contribution of Antarctica on long timescales.
Gemma K. O'Connor, Paul R. Holland, Eric J. Steig, Pierre Dutrieux, and Gregory J. Hakim
The Cryosphere, 17, 4399–4420, https://doi.org/10.5194/tc-17-4399-2023, https://doi.org/10.5194/tc-17-4399-2023, 2023
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Glaciers in West Antarctica are rapidly melting, but the causes are unknown due to limited observations. A leading hypothesis is that an unusually large wind event in the 1940s initiated the ocean-driven melting. Using proxy reconstructions (e.g., using ice cores) and climate model simulations, we find that wind events similar to the 1940s event are relatively common on millennial timescales, implying that ocean variability or climate trends are also necessary to explain the start of ice loss.
Christian Wirths, Johannes Sutter, and Thomas Stocker
EGUsphere, https://doi.org/10.5194/egusphere-2023-2233, https://doi.org/10.5194/egusphere-2023-2233, 2023
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We investigated the influence of several regional climate models onto the Antarctic Ice Sheet, when applied as forcing for the Parallel Ice Sheet Model (PISM). Our study shows, that the choice of regional climate model forcing results in uncertainties similar to the ones in future sea level rise projections and affects also the extent of grounding line retreat in West Antarctica.
Maria T. Kappelsberger, Martin Horwath, Eric Buchta, Matthias O. Willen, Ludwig Schröder, Sanne B. M. Veldhuijsen, Peter Kuipers Munneke, and Michiel R. van den Broeke
The Cryosphere Discuss., https://doi.org/10.5194/tc-2023-140, https://doi.org/10.5194/tc-2023-140, 2023
Revised manuscript accepted for TC
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The interannual variations in the height of the Antarctic Ice Sheet (AIS) are mainly due to natural variations in snowfall. Precise knowledge of these variations is important for the detection of any long-term climatic trends in AIS surface elevation. We present a new product that spatially resolves these height variations over the period 1992–2017. The product combines the strengths of atmospheric modeling results and satellite altimetry measurements.
Ann Kristin Klose, Violaine Coulon, Frank Pattyn, and Ricarda Winkelmann
The Cryosphere Discuss., https://doi.org/10.5194/tc-2023-156, https://doi.org/10.5194/tc-2023-156, 2023
Revised manuscript accepted for TC
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We systematically assess the long-term sea-level response from Antarctica to warming projected over the next centuries with two ice-sheet models. We show that this committed Antarctic sea-level contribution is substantially higher than the transient sea-level change projected for the coming decades. A low-emission scenario already poses a considerable risk of multi-meter sea-level increase over the next millennia, while additional East Antarctic ice loss unfolds under the high-emission pathway.
Thomas Dethinne, Quentin Glaude, Ghislain Picard, Christoph Kittel, Patrick Alexander, Anne Orban, and Xavier Fettweis
The Cryosphere, 17, 4267–4288, https://doi.org/10.5194/tc-17-4267-2023, https://doi.org/10.5194/tc-17-4267-2023, 2023
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We investigate the sensitivity of the regional climate model
Modèle Atmosphérique Régional(MAR) to the assimilation of wet-snow occurrence estimated by remote sensing datasets. The assimilation is performed by nudging the MAR snowpack temperature. The data assimilation is performed over the Antarctic Peninsula for the 2019–2021 period. The results show an increase in the melt production (+66.7 %) and a decrease in surface mass balance (−4.5 %) of the model for the 2019–2020 melt season.
Nora Hirsch, Alexandra Zuhr, Thomas Münch, Maria Hörhold, Johannes Freitag, Remi Dallmayr, and Thomas Laepple
The Cryosphere, 17, 4207–4221, https://doi.org/10.5194/tc-17-4207-2023, https://doi.org/10.5194/tc-17-4207-2023, 2023
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Stable water isotopes from firn cores provide valuable information on past climates, yet their utility is hampered by stratigraphic noise, i.e. the irregular deposition and wind-driven redistribution of snow. We found stratigraphic noise on the Antarctic Plateau to be related to the local accumulation rate, snow surface roughness and slope inclination, which can guide future decisions on sampling locations and thus increase the resolution of climate reconstructions from low-accumulation areas.
Bryony I. D. Freer, Oliver J. Marsh, Anna E. Hogg, Helen Amanda Fricker, and Laurie Padman
The Cryosphere, 17, 4079–4101, https://doi.org/10.5194/tc-17-4079-2023, https://doi.org/10.5194/tc-17-4079-2023, 2023
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We develop a method using ICESat-2 data to measure how Antarctic grounding lines (GLs) migrate across the tide cycle. At an ice plain on the Ronne Ice Shelf we observe 15 km of tidal GL migration, the largest reported distance in Antarctica, dominating any signal of long-term migration. We identify four distinct migration modes, which provide both observational support for models of tidal ice flexure and GL migration and insights into ice shelf–ocean–subglacial interactions in grounding zones.
Rajashree Tri Datta, Adam Herrington, Jan T. M. Lenaerts, David P. Schneider, Luke Trusel, Ziqi Yin, and Devon Dunmire
The Cryosphere, 17, 3847–3866, https://doi.org/10.5194/tc-17-3847-2023, https://doi.org/10.5194/tc-17-3847-2023, 2023
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Precipitation over Antarctica is one of the greatest sources of uncertainty in sea level rise estimates. Earth system models (ESMs) are a valuable tool for these estimates but typically run at coarse spatial resolutions. Here, we present an evaluation of the variable-resolution CESM2 (VR-CESM2) for the first time with a grid designed for enhanced spatial resolution over Antarctica to achieve the high resolution of regional climate models while preserving the two-way interactions of ESMs.
Yaowen Zheng, Nicholas R. Golledge, Alexandra Gossart, Ghislain Picard, and Marion Leduc-Leballeur
The Cryosphere, 17, 3667–3694, https://doi.org/10.5194/tc-17-3667-2023, https://doi.org/10.5194/tc-17-3667-2023, 2023
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Positive degree-day (PDD) schemes are widely used in many Antarctic numerical ice sheet models. However, the PDD approach has not been systematically explored for its application in Antarctica. We have constructed a novel grid-cell-level spatially distributed PDD (dist-PDD) model and assessed its accuracy. We suggest that an appropriately parameterized dist-PDD model can be a valuable tool for exploring Antarctic surface melt beyond the satellite era.
Hannah J. Picton, Chris R. Stokes, Stewart S. R. Jamieson, Dana Floricioiu, and Lukas Krieger
The Cryosphere, 17, 3593–3616, https://doi.org/10.5194/tc-17-3593-2023, https://doi.org/10.5194/tc-17-3593-2023, 2023
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This study provides an overview of recent ice dynamics within Vincennes Bay, Wilkes Land, East Antarctica. This region was recently discovered to be vulnerable to intrusions of warm water capable of driving basal melt. Our results show extensive grounding-line retreat at Vanderford Glacier, estimated at 18.6 km between 1996 and 2020. This supports the notion that the warm water is able to access deep cavities below the Vanderford Ice Shelf, potentially making Vanderford Glacier unstable.
Fernando S. Paolo, Alex S. Gardner, Chad A. Greene, Johan Nilsson, Michael P. Schodlok, Nicole-Jeanne Schlegel, and Helen A. Fricker
The Cryosphere, 17, 3409–3433, https://doi.org/10.5194/tc-17-3409-2023, https://doi.org/10.5194/tc-17-3409-2023, 2023
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We report on a slowdown in the rate of thinning and melting of West Antarctic ice shelves. We present a comprehensive assessment of the Antarctic ice shelves, where we analyze at a continental scale the changes in thickness, flow, and basal melt over the past 26 years. We also present a novel method to estimate ice shelf change from satellite altimetry and a time-dependent data set of ice shelf thickness and basal melt rates at an unprecedented resolution.
Hyein Jeong, Adrian K. Turner, Andrew F. Roberts, Milena Veneziani, Stephen F. Price, Xylar S. Asay-Davis, Luke P. Van Roekel, Wuyin Lin, Peter M. Caldwell, Hyo-Seok Park, Jonathan D. Wolfe, and Azamat Mametjanov
The Cryosphere, 17, 2681–2700, https://doi.org/10.5194/tc-17-2681-2023, https://doi.org/10.5194/tc-17-2681-2023, 2023
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We find that E3SM-HR reproduces the main features of the Antarctic coastal polynyas. Despite the high amount of coastal sea ice production, the densest water masses are formed in the open ocean. Biases related to the lack of dense water formation are associated with overly strong atmospheric polar easterlies. Our results indicate that the large-scale polar atmospheric circulation must be accurately simulated in models to properly reproduce Antarctic dense water formation.
Cited articles
Alley, R., Clark, P., Huybrechts, P., and Joughin, I.: Ice-sheet and sea level changes, Science, 310, 456–460, https://doi.org/10.1126/science.1114613, 2005.
Anschütz, H., Müller, K., Isaksson, E., McConnell, J. R., Fischer, H., Miller, H., Albert, M., and Winther, J.-G.: Revisiting sites of the South Pole Queen Maud Land Traverses in East Antarctica: Accumulation data from shallow firn cores, J. Geophys. Res., 114, D24106, https://doi.org/10.1029/2009JD012204, 2009.
Anschütz, H., Sinisalo, A., Isaksson, E., McConnell, J. R., Hamran, S.-E., Bisiaux, M. M., Pasteris, D., Neumann, T. A. and Winther, J.-G.: Variation of accumulation rates over the last eight centuries on the East Antarctic Plateau derived from volcanic signals in ice cores, J. Geophys. Res., 116, D20103, https://doi.org/10.1029/2011JD015753, 2011
Arthern, R. J., Winebrenner, D. P., and Vaughan, D.G.: Antarctic snow accumulation mapped using polarization of 4.3-cm wavelength microwave emission, J. Geophys. Res, 111, D06107, https://doi.org/10.1029/2004JD005667, 2006.
Bamber, J. L., Gomez-Dans, J. L., and Griggs, J. A.: Antarctic 1 km Digital Elevation Model (DEM) from Combined ERS-1 Radar and ICESat Laser Satellite Altimetry, in: National Snow and Ice Data Center. Digital media, Boulder, Colorado USA, 2009.
Birnbaum, G., Freitag, J., Brauner, R., König-Langlo, Schulz, G. E., Schulz, E., Kipfstuhl, S., Oerter, H., Reijmer, C. H., Schlosser, E., Faria, S. H., Ries, H., Loose, B., Herber, A., Duda, M. G., Powers, J. G., Manning, K. W., and Van den Broeke, M. R.: Strong-wind events and their influence on the formation of snow dunes: Observations from Kohnen Station, Dronning Maud Land, Antarctica, J. Glaciol., 56, 891–902, https://doi.org/10.3189/002214310794457272, 2010.
Braaten, D. A.: Direct measurements of episodic snow accumulation on the Antarctic polar plateau, J. Geophys. Res., 105, 10,119–10,128, https://doi.org/10.1029/2000JD900099, 2000.
Bromwich, D. H., Snowfall in high southern latitudes, Rev. Geophys., 26, 149–168, https://doi.org/10.1029/RG026i001p00149, 1988.
Bromwich, D. H., Guo, Z., Bai, L., and Chen, Q.-S.: Modeled Antarctic precipitation. Part I: Spatial and temporal variability, J. Climate, 17, 427–447, https://doi.org/10.1175/1520-0442(2004)017<0427:MAPPIS>2.0.CO;2,2004.
Chen, J., Wilson, C., Blankenship, D., and Tapley, B.: Antarctic mass rates from GRACE, Geophys. Res. Lett., 33, L11502, https://doi.org/10.1029/2006GL026369, 2006.
Cole-Dai, J., Mosley-Thompson, E., and Thompson, L. G.: Quantifying the Pinatubo volcanic signal in south polar snow, Geophys. Res. Lett., 24 (21), 2679–2682, https://doi.org/10.1029/97GL02734, 1997.
Cullather, R. I., Bromwich, D. H., and Van Woert M. L.: Spatial and temporal variability of Antarctic Precipitation from atmospheric methods, J. Climate, 11, 334–367, 1998.
Davis, C., Li, Y., McConnell, J., Frey, M., and Hanna, E.: Snowfall-driven growth in East Antarctic ice sheet mitigates recent sea-level rise, Science, 308, 5730, 1898–1901, https://doi.org/10.1126/science.1110662, 2005.
Eisen, O., Frezzotti, M., Genthon, C., Isaksson, E., Magand, O., Van den Broeke, M. R., Dixon, D.A., Ekaykin, A., Holmlund, P., Kameda, T., Karlöf, L., Kaspari, S., Lipenkov, V., Oerter, H., Takahashi, S., and Vaughan, D. G.: Ground-based measurements of spatial and temporal variability of snow accumulation in East Antarctica, Rev. Geophys., 46, RG2001, https://doi.org/10.1029/2006RG000218, 2008.
Endo, Y. and Fujiwara, K.: Characteristics of the snow cover in East Antarctica along the route of the JARE South Pole traverse and factors controlling such characteristics, Polar Res. Cent., Natl. Sci. Mus., Tokyo, 38 pp., 1973.
EPICA Community Members: One-to-one coupling of glacial climate variability in Greenland and Antarctica, Nature, 444, 195–198, https://doi.org/10.1038/nature05301, 2006.
Frezzotti, M., Pourchet, M., Flora, O., Gandolfi, S., Gay, M., Urbini, S., Vincent, C., Becagli, S., Gragnani, R., Proposito, M., Severi, M., Traversi, R., Udisti, R., and Fily, M.: New estimations of precipitation and surface sublimation in East Antarctica from snow accumulation measurements, Climate Dynamics, 23, 803–813, https://doi.org/10.1007/s00382-004-0462-5, 2004.
Frezzotti, M., Pourchet, M., Flora, O., Gandolfi, S., Gay, M., Urbini, S., Vincent, C., Becagli, S., Gragnani, R., Proposito, M., Severi, M., Traversi, R., Udisti, R., and Fily, M.: Spatial and temporal variability of snow accumulation in East Antarctica from traverse data, J. Glaciol., 51, 113–124, https://doi.org/10.3189/172756505781829502, 2005.
Frezzotti, M., Urbini, S., Proposito, M., Scarchilli, C., and Gandolfi, S.: Spatial and temporal variability of surface mass balance near Talos Dome, East Antarctica, J. Geophys. Res., 112, F02032, https://doi.org/10.1029/2006JF000638, 2007.
Fujita, K., and Abe, O.: Stable isotopes in daily precipitation at Dome Fuji, East Antarctica, Geophys. Res. Lett., 33, https://doi.org/10.1029/2006GL026936, 2006.
Fujita, S., Maeno, H., Uratsuka, S., Furukawa, T., Mae, S., Fujii, Y., and Watanabe, O.: Nature of radio-echo layering in the Antarctic ice sheet detected by a two-frequency experiment, J. Geophys. Res., 104(B6), 13013–13024, https://doi.org/10.1029/1999JB900034, 1999.
Fujita, S., Matsuoka, T., Ishida, T., Matsuoka, K., and Mae, S.: A summary of the complex dielectric permittivity of ice in the megahertz range and its applications for radar sounding, in: Physics of Ice Core Records, edited by: Hondoh, T., Hokkaido University Press, Sapporo, 185–212, 2000.
Fujita, S., Azuma, N., Motoyama, H., Kameda, T., Narita, H., Fujii, Y., Watanabe, O.: Electrical measurements from the 2503-m Dome F Antarctic ice core, Ann. Glaciol., 35, 313–320, https://doi.org/10.3189/172756402781816951, 2002a.
Fujita, S., Maeno, H., Furukawa, T., and Matsuoka, K.: Scattering of VHF radio waves from within the top 700 m of the Antarctic ice sheet and its relation to the depositional environment: a case study along the Syowa-Mizuho-Dome F traverse, Ann. Glaciol., 34, 157–164, https://doi.org/10.3189/172756402781817888, 2002b.
Fujita, S., Enomoto, H., Kameda, T., Motoyama, H., and Sugiyama, S.: Changes of surface snow density in a summer in the Antarctic Dome Fuji region, paper presented at SCAR/IASC IPY Open Science Conference, Assoc. of Polar Early Career Sci., St. Petersburg, Russia, 8–11 July 2008.
Furukawa, T., Kamiyama, K., and Maeno, H.: Snow surface features along the traverse route from the coast to Dome Fuji Station, Queen Maud Land, Antarctica, Proc. NIPR Symp. Polar Meteorol. Glaciol., 10, 13–24, 1996.
Giovinetto, M. and Zwally, H.: Spatial distribution of net surface accumulation on the Antarctic ice sheet, Ann. Glaciol., 31, 171–178, https://doi.org/10.3189/172756400781820200, 2000.
Göktas, F., Fischer, H., Oerter, H., Weller, R., Sommer, S., and Miller, H.: A glacio-chemical characterisation of the new EPICA deep-drilling site on Amundsenisen, Dronning Maud Land, Antarctica., Ann. Glaciol., 35, 347–354, https://doi.org/10.3189/172756402781816474, 2002.
Hamran, S.-E. and Aarholt, E.: Glacier study using wavenumber domain synthetic aperture radar, Radio Sci., 28, 559–570, https://doi.org/10.1029/92RS03022, 1993.
Hamran, S.-E., Gjessing, D. T., Hjelmstad, J., and Aarholt, E.: Ground penetrating synthetic pulse radar: Dynamic range and modes of operation, J. Appl. Geophys., 33, 7–14, https://doi.org/10.1016/0926-9851(95)90025-X, 1995.
Haran, T., Bohlander, J., Scambos, T., Painter, T., and Fahnestock, M.: MODIS mosaic of Antarctica (MOA) image map, in: National Snow and Ice Data Center, Digital media, Boulder, Colorado USA, 2005, updated 2006.
Helsen, M., Van den Broeke, M., Van de Wal, R., Van de Berg, W., Van Meijgaard, E., Davis, C., Li, Y., and Goodwin, I.: Elevation changes in Antarctica mainly determined by accumulation variability, Science, 320, 1626–1629, https://doi.org/10.1126/science.1153894, 2008.
Hirasawa, N., Nakamura, H., and Yamanouchi, T.: Abrupt changes in meteorological conditions observed at an inland Antarctic Station in association with wintertime blocking, Geophys. Res. Lett., 27, 1911–1914, https://doi.org/10.1029/1999GL011039, 2000.
Hirasawa, N.: Winter warming-event observed at Dome Fuji Station and synoptic-scale circulation in the Antarctic, Nankyoku Shiryo (Antarctic Record), 54, 292–307, 2010.
Hofstede, C. M., Van de Wal, R. S. W., Kaspers, K. A., Van den Broeke, M. R., Karlöf, L., Winther, J.-G., Isaksson, E., Lappegard, G., Mulvaney, R., Oerter, H., and Wilhelms, F.: Firn accumulation records for the past 1000 years on the basis of dielectric profiling of six cores from Dronning Maud Land, Antarctica, J. Glaciol., 50, 279–291, https://doi.org/10.3189/172756504781830169, 2004.
Holmlund, P. and Fujita, S.: Japanese-Swedish Antarctic Expedition JASE, edited by: Thorén A., Swedish Polar Secretariat Year Book 2008, Stockholm, 18E1, 2009.
Huybrechts, P., Rybak, O., Pattyn, F., and Steinhage, D.: Past and present accumulation rate reconstruction along the Dome Fuji-Kohnen radio echo sounding profile, Dronning Maud Land, East Antarctica, Ann. Glaciol., 50, 112–120, https://doi.org/10.3189/172756409789097513, 2009.
Igarashi, M., Nakai, Y., Motizuki, Y., Takahashi, K., Motoyama, H., and Makishima, K.: Dating of the Dome Fuji shallow ice core based on a record of volcanic eruptions from AD 1260 to AD 2001, Polar Sci., 5, 411–420, https://doi.org/10.1016/j.polar.2011.08.001, 2011.
Isaksson, E., Karlén, W., Gundestrup, N., Mayewski, P., Whitlow, S., and Twickler, M.: A century of accumulation and temperature changes in Dronning Maud Land, Antarctica, J. Geophys. Res., 101, 7085–7094, https://doi.org/10.1029/95JD03232, 1996.
Isaksson, E., Van den Broeke, M. R., Winther, J.-G., Karlöf, L., Pinglot, J. F., and Gundestrup, N.: Accumulation and proxy-temperature variability in Dronning Maud Land, Antarctica, determined from shallow firn cores, Ann. Glaciol., 29, 17–22, https://doi.org/10.3189/172756499781821445, 1999.
Japan Meteorological Agency: Antarctic Meteorological Data Vol. 44, obtained by the 44th Japanese Antarctic Research Expedition at Syowa Station and Dome Fuji Station in 2003, CD-ROM, Japan Meteorological Agency, Tokyo, 2005.
Kameda, T., Motoyama, H., Fujita, S., and Takahashi, S.: Temporal and spatial variability of surface mass balance at Dome Fuji, East Antarctica, by the stake method from 1995 to 2006, J. Glaciol., 54, 107–116, https://doi.org/10.3189/002214308784409062, 2008.
Karlöf, L., Isaksson, E., Winther, J.-G., Gundestrup, N., Meijer, H. A. J., Mulvaney, R., Pourchet, M., Hofstede, C.,Lappegard, G., Pettersson, R., Van den Broeke, M., and Van de Wal, R. S. W.: Accumulation variability over a small area in East Dronning Maud Land, Antarctica, as determined from shallow firn cores and snow pits: Some implications for ice-core records, J. Glaciol., 51, 343–352, https://doi.org/10.3189/172756505781829232, 2005.
Kawamura, K., Parrenin, F., Lisiecki, L., Uemura, R., Vimeux, F., Severinghaus, J. P., Hutterli, M.A., Nakazawa, T., Aoki, S., Jouzel, J., Raymo, M.E., Matsumoto, K., Nakata, H., Motoyama, H., Fujita, S., Azuma, K., Fujii, Y. and Watanabe, O.: Northern Hemisphere forcing of climatic cycles over the past 360,000 years implied by accurately dated Antarctic ice cores, Nature, 448, 912–916, https://doi.org/10.1038/nature06015, 2007.
Keller, L. M., Lazzara, M. A., Thom, J. E., Weidner, G. A., and Stearns, C. R.: Antarctic Automatic Weather Station Data for the calendar year 2009, Space Science and Engineering Center, University of Wisconsin, Madison, Wisconsin, 2010.
Kikuchi, T.: Prevailing Windfield, in: Antarctica: East Queen Maud Land-Enderby Land Glaciological Folio, Sheet 2, National Institute of Polar Research, Tokyo, Japan, 1997.
King, J. C. and Turner, J.: Antarctic Meteorology and Climatology, 409 pp., Cambridge Univ. Press, New York, 1997.
Kovacs, A., Gow, A. J., and Morey, R. M.: The in-situ dielectric constant of polar firn revisited, Cold Reg. Sci. Technol., 23, 245–256, https://doi.org/10.1016/0165-232X(94)00016-Q, 1995.
Krinner, G., Magand, O., Simmonds, I., Genthon, C. and Dufresne, J.-L.: Simulated Antarctic precipitation and surface mass balance at the end of the twentieth and twenty-first centuries, Clim. Dyn., 28, 215–230, https://doi.org/10.1007/s00382-006-0177-x, 2007.
Legrand, M. and Wagenbach, D.: Impact of Cerro Hudson and Pinatubo volcanic eruptions on the Antarctic air and snow chemistry, J. Geophys. Res., 104, 1581–1596, https://doi.org/10.1029/1998JD100032, 1999.
Lemke, P., Ren, J., Alley, R. B., Allison, I., Carrasco, J., Flato, G., Fujii, Y., Kaser, G., Mote, P., Thomas, R. H., and Zhang, T.: Observations: Changes in Snow, Ice and Frozen Ground, in: Climate change 2007: the physical science basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, edited by: Solomon, S., Qin, D., Manning, M., Chen, Z., Marquis, M., Averyt, K. B., Tignor, M., and Miller, H. L., Cambridge University Press, Cambridge, 2007.
Matsuoka, K., Maeno, H., Uratsuka, S., Fujita, S., Furukawa, T., and Watanabe, O.: A ground-based, multi-frequency ice-penetrating radar system, Ann. Glaciol., 34, 171–176, https://doi.org/10.3189/172756402781817400, 2002.
Monaghan, A., Bromwich, D., Fogt, R., Wang, S., Mayewski, P., Dixon, D., Ekaykin, A., Frezzotti, M., Goodwin, I., Isaksson, E., Kaspari, S., Morgan, V., Oerter, H., Van Ommen, T., Van Der Veen, C. and Wen, J..: Insignificant change in Antarctic snowfall since the International Geophysical Year, Science, 313, 827–831, https://doi.org/10.1126/science.1128243, 2006.
Motoyama, H., Enomoto, H., Furukawa, T., Kamiyama, K., Shoji, H., Shiraiwa, T., Watanabe, K., Namasu, K., and Ikeda, H.: Preliminary study of ice flow observations along traverse routes from coast to Dome Fuji, East Antarctica by differential GPS method., Nankyoku Shiryo (Antarctic Record), 39, 94–98, 1995.
Moore, J. C., Mulvaney, R., and Paren, J. G.: Dielectric stratigraphy of ice: a new technique for determining total ionic concentrations in polar ice, Geophys. Res. Lett., 16, 1177–1180, https://doi.org/10.1029/GL016i010p01177, 1989.
Mosley-Thompson, E., Paskievitch, J. F., Gow, A. J., and Thompson, L. G.: Late 20th century increase in South Pole snow accumulation, J. Geophys. Res., 104(D4), 3877–3886, https://doi.org/10.1029/1998JD200092, 1999.
Müller, K., Sinisalo, A., Anschütz, H., Hamran, S.-E., Hagen, J.-O., McConnell, J. R., and Pasteris, D. R.: An 860 km surface mass-balance profile on the East Antarctic plateau derived by GPR, Ann. Glaciol., 55, 1–8, https://doi.org/10.3189/172756410791392718, 2010.
Noone, D. and Simmonds, I.: Implications for interpretations of ice-core isotope data from analysis of modelled Antarctic precipitation, Ann. Glaciol., 27, 398–402, 1998.
Noone, D., Turner, J., and Mulvaney, R.: Atmospheric signals and characteristics of accumulation in Dronning Maud Land, Antarctica, J. Geophys. Res., 104, 19191–19211, https://doi.org/10.1029/1999JD900376, 1999.
Oerter, H., Wilhelms, F., Jung-Rothenhäusler, F., Göktas, F., Miller, H., Graf, W., and Sommer, S.: Accumulation rates in Dronning Maud Land, Antarctica, as revealed by dielectric-profiling measurements of shallow firn cores, Ann. Glaciol., 30, 27–34, https://doi.org/10.3189/172756400781820705, 2000.
Oerter, H., Graf, W., Meyer, H., and Wilhelms, F.: The EPICA ice core from Dronning Maud Land: first results from stable-isotope measurements, Ann. Glaciol., 39, 307–312, https://doi.org/10.3189/172756404781814032, 2004.
Parrenin, F., Dreyfus, G., Durand, G., Fujita, S., Gagliardini, O., Gillet, F., Jouzel, J., Kawamura, K., Lhomme, N., Masson-Delmotte, V., Ritz, C., Schwander, J., Shoji, H., Uemura, R., Watanabe, O., and Yoshida, N.: 1-D-ice flow modelling at EPICA Dome C and Dome Fuji, East Antarctica, Clim. Past, 3, 243–259, https://doi.org/10.5194/cp-3-243-2007, 2007.
Pruett, L. E., Kreutz, K. J., Wadleigh, M., Mayewski, P. A., and Kurbatov, A.: Sulfur isotopic measurements from a West Antarctic ice core: implications for sulphate source and transport, Ann. Glaciol., 39, 161–168, https://doi.org/10.3189/172756404781814339, 2004.
Reijmer, C. and Van den Broeke, M. R.: Temporal and spatial variability of the surface mass balance in Dronning Maud Land, Antarctica, as derived from automatic weather stations, J. Glaciol., 49, 512–520, https://doi.org/10.3189/172756503781830494, 2003.
Richardson, C., Aarholt, E., Hamran, S.-E., Holmlund, P., and Isaksson, E.: Spatial distribution of snow in western Dronning Maud Land, East Antarctica, mapped by a ground-based snow radar, J. Geophys. Res., 102, 20343–20353, https://doi.org/10.1029/97JB01441, 1997.
Roe, G. H.: Orographic precipitation, Annu. Rev. Earth Planet. Sci., 33, 645–671, 2005. https://doi.org/10.1146/annurev.earth.33.092203.122541, 2005.
Rotschky, G., Eisen, O., Wilhelms, F., Nixdorf, U., and Oerter, H.: Spatial distribution of surface mass balance on Amundsenisen plateau, Antarctica, derived from ice-penetrating radar studies, Ann. Glaciol., 39, 265–270, https://doi.org/10.3189/172756404781814618, 2004.
Rotschky, G., Holmlund, P., Isaksson, E., Mulvaney, R., Oerter, H., Van den Broecke, M. R., and Winther, J.-G.: A new surface accumulation map for western Dronning Maud Land, Antarctica, from interpretation of point measurements, J. Glaciol., 53, 385–398, https://doi.org/10.3189/002214307783258459, 2007.
Ruth, U., Barnola, J.-M., Beer, J., Bigler, M., Blunier, T., Castellano, E., Fischer, H., Fundel, F., Huybrechts, P., Kaufmann, P., Kipfstuhl, S., Lambrecht, A., Morganti, A., Oerter, H., Parrenin, F., Rybak, O., Severi, M., Udisti, R., Wilhelms, F., and Wolff, E.: "EDML1": a chronology for the EPICA deep ice core from Dronning Maud Land, Antarctica, over the last 150 000 years, Clim. Past, 3, 475–484, https://doi.org/10.5194/cp-3-475-2007, 2007.
Schlosser, E., Duda, M. G., Powers, J. G., and Manning, K. W.: Precipitation regime of Dronning Maud Land, Antarctica, derived from Antarctic Mesoscale Prediction System (AMPS) archive data, J. Geophys. Res., 113, https://doi.org/10.1029/2008JD009968, 2008.
Schlosser, E., Manning, K.W., Powers, J.G., Duda, M.G., Birnbaum, G., and Fujita, K.: Characteristics of high precipitation events in Dronning Maud Land, Antarctica, J. Geophys. Res, 115, https://doi.org/10.1029/2009JD013410, 2010.
Stenni, B., Proposito, M., Gragnani, R., Flora, O., Jouzel, J., Falourd, S., and Frezzotti, M.: Eight centuries of volcanic signal and climate change at Talos Dome (East Antarctica), J. Geophys. Res., 107, 4076, https://doi.org/10.1029/2000JD000317, 2002.
Surdyk, S.: Using microwave brightness temperature to detect short-term surface air temperature changes in Antarctica: An analytical approach, Remote Sens. Environ., 80, 256–271, https://doi.org/10.1016/S0034-4257(01)00308-X, 2002.
Surdyk, S. and Fily, M.: Comparison of the passive microwave spectral signature of the Antarctic ice sheet with ground traverse data, Ann. Glaciol., 17, 161–166, 1993.
Surdyk, S. and Fily, M.: Results of a stratified snow emissivity model based on the wave approach: Application to the Antarctic Ice Sheet, J. Geophys. Res., 100, 8837–8848, https://doi.org/10.1029/94JC03361, 1995.
Takahashi, S., Kameda, T., Enomoto, H., Motoyama, H., and Watanabe, O.: Automatic Weather Station (AWS) data collected by the 33rd to 42nd Japanese Antarctic Research Expeditions during 1993–2001 in: JARE data reports, Meteorology, National Institute of Polar Research, Tokyo, 416 pp., 2004.
Traufetter, F., Oerter, H., Fischer, H., Weller, R., and Miller, H.: Spatio-temporal variability in volcanic sulphate deposition over the past 2 kyr in snow pits and firn cores from Amundsenisen, Dronning Maud Land, Antarctica, J. Glaciol., 50, 137–146, https://doi.org/10.3189/172756504781830222, 2004
Urbini, S., Frezzotti, M., Gandolfi, S., Vincent, C., Scarchilli, C., Vittuari, V., and Fily, M.: Historical behaviour of Dome C and Talos Dome (East Antarctica) as investigated by snow accumulation and ice velocity measurements, Global Planet. Change, 60, 576–588, https://doi.org/10.1016/j.gloplacha.2007.08.002, 2008.
Van de Berg, W., Van den Broeke, M., Reijmer, C., and Van Meijgaard, E.: Reassessment of the Antarctic surface mass balance using calibrated output of a regional atmospheric climate model, J. Geophys. Res., 111, D11104, https://doi.org/10.1029/2005JD006495, 2006.
Van As, M. R., Van den Broeke, M. R., and Helsen, M.: Strong-wind events and their impact on the near-surface climate at Kohnen Station on the Antarctic Plateau, Antarct. Sci., 19, 507–519, https://doi.org/10.1017/S095410200700065X, 2007.
Van den Broeke, M. R. and Van Lipzig, N. P. M.: Factors controlling the near-surface wind field in Antarctica, Mon. Weather Rev., 131, 733–743, https://doi.org/10.1175/1520-0493(2003)131<0733:FCTNSW>2.0.CO;2, 2003.
Van Lipzig, N. P. M., Turner, J., Colwell, S. R., and Van den Broeke, M. R.: The near-surface wind field over the Antarctic continent, Int. J. Climatol., 24, 1973–1982, https://doi.org/10.1002/joc.1090, 2004.
Vaughan, D., Bamber, J., Giovinetto, M., Russell, J., and Cooper, A.: Reassessment of net surface mass balance in Antarctica, J. Climate, 45, 933–946, https://doi.org/10.1175/1520-0442(1999)012<0933:RONSMB>2.0.CO;2, 1999.
Velicogna, I. and Wahr, J.: Measurements of time-variable gravity show mass loss in Antarctica, Science, 311, 1754–1756, https://doi.org/10.1126/science.1123785, 2006.
Watanabe, O.: Distributions of surface features of snow cover in Mizuho Plateau., Mem. Natl Inst. Polar Res. Spec. Issue., 7, 44–62, 1978.
Watanabe, O., Fujii, Y., Motoyama, H., Furukawa, T., Shoji, H., Enomoto, H., Kameda, T., Narita, H., Naruse, R., Hondoh, T., Fujita, S., Mae, S., Azuma, N., Kobayashi, S., Nakawo, M., and Ageta, Y.: Preliminary study of ice core chronology at Dome Fuji, Proc. NIPR Symp. Polar Meteorol. Glaciol., 11, 9–13, 1997.
Watanabe, O., Jouzel, J., Johnsen, S., Parrenin, F., Shoji, H., and Yoshida, N.: Homogeneous climate variability across East Antarctica over the past three glacial cycles, Nature, 422, 509–512, https://doi.org/10.1038/nature01525, 2003.
Wilhelms, F.: Explaining the dielectric properties of firn as a density-and-conductivity mixed permittivity (DECOMP), Geophys. Res. Lett., 32, L16501, https://doi.org/10.1029/2005GL022808, 2005.
Wilhelms, F., Kipfstuhl, J., Miller, H., Heinloth, K., and Firestone, J.: Precise dielectric profiling of ice cores: a new device with improved guarding and its theory, J. Glaciol., 44, 171–174, 1998.
