Articles | Volume 17, issue 3
https://doi.org/10.5194/cp-17-1341-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-17-1341-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
21 Jun 2021
Research article |
| 21 Jun 2021
| 21 Jun 2021
Variations in mineralogy of dust in an ice core obtained from northwestern Greenland over the past 100 years
Naoko Nagatsuka
CORRESPONDING AUTHOR
National Institute of Polar Research, Tokyo 190-8518, Japan
Kumiko Goto-Azuma
National Institute of Polar Research, Tokyo 190-8518, Japan
Department of Polar Science, The Graduate University for Advanced Studies, SOKENDAI, Tokyo 190-8518, Japan
Akane Tsushima
Graduate School of Science, Chiba University, Chiba 277-0882, Japan
Koji Fujita
Graduate School of Environmental Studies, Nagoya University, Nagoya 464-8601, Japan
Sumito Matoba
Institute of Low Temperature Science, Hokkaido University, Sapporo 060-0819, Japan
Yukihiko Onuma
Institute of Industrial Science, University of Tokyo, Kashiwa 277-8574, Japan
Remi Dallmayr
Alfred Wegener Institute, Am Alten Hafen 26, 27568 Bremerhaven, Germany
Moe Kadota
Institute of Low Temperature Science, Hokkaido University, Sapporo 060-0819, Japan
Graduate School of Environmental Science, Hokkaido University, Sapporo 060-0810, Japan
Motohiro Hirabayashi
National Institute of Polar Research, Tokyo 190-8518, Japan
Jun Ogata
National Institute of Polar Research, Tokyo 190-8518, Japan
Yoshimi Ogawa-Tsukagawa
National Institute of Polar Research, Tokyo 190-8518, Japan
Kyotaro Kitamura
National Institute of Polar Research, Tokyo 190-8518, Japan
Masahiro Minowa
Graduate School of Environmental Studies, Nagoya University, Nagoya 464-8601, Japan
Yuki Komuro
National Institute of Polar Research, Tokyo 190-8518, Japan
Hideaki Motoyama
National Institute of Polar Research, Tokyo 190-8518, Japan
Department of Polar Science, The Graduate University for Advanced Studies, SOKENDAI, Tokyo 190-8518, Japan
Teruo Aoki
National Institute of Polar Research, Tokyo 190-8518, Japan
Department of Polar Science, The Graduate University for Advanced Studies, SOKENDAI, Tokyo 190-8518, Japan
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Earth Syst. Sci. Data, 15, 5207–5226, https://doi.org/10.5194/essd-15-5207-2023, https://doi.org/10.5194/essd-15-5207-2023, 2023
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Earth Syst. Sci. Data, 15, 5079–5091, https://doi.org/10.5194/essd-15-5079-2023, https://doi.org/10.5194/essd-15-5079-2023, 2023
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Earth Syst. Sci. Data, 15, 2517–2532, https://doi.org/10.5194/essd-15-2517-2023, https://doi.org/10.5194/essd-15-2517-2023, 2023
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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
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The Cryosphere, 16, 2985–3003, https://doi.org/10.5194/tc-16-2985-2022, https://doi.org/10.5194/tc-16-2985-2022, 2022
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Hitoshi Matsui, Tatsuhiro Mori, Sho Ohata, Nobuhiro Moteki, Naga Oshima, Kumiko Goto-Azuma, Makoto Koike, and Yutaka Kondo
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Yota Sato, Koji Fujita, Hiroshi Inoue, Akiko Sakai, and Karma
The Cryosphere, 16, 2643–2654, https://doi.org/10.5194/tc-16-2643-2022, https://doi.org/10.5194/tc-16-2643-2022, 2022
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Tobias Erhardt, Matthias Bigler, Urs Federer, Gideon Gfeller, Daiana Leuenberger, Olivia Stowasser, Regine Röthlisberger, Simon Schüpbach, Urs Ruth, Birthe Twarloh, Anna Wegner, Kumiko Goto-Azuma, Takayuki Kuramoto, Helle A. Kjær, Paul T. Vallelonga, Marie-Louise Siggaard-Andersen, Margareta E. Hansson, Ailsa K. Benton, Louise G. Fleet, Rob Mulvaney, Elizabeth R. Thomas, Nerilie Abram, Thomas F. Stocker, and Hubertus Fischer
Earth Syst. Sci. Data, 14, 1215–1231, https://doi.org/10.5194/essd-14-1215-2022, https://doi.org/10.5194/essd-14-1215-2022, 2022
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The datasets presented alongside this manuscript contain high-resolution concentration measurements of chemical impurities in deep ice cores, NGRIP and NEEM, from the Greenland ice sheet. The impurities originate from the deposition of aerosols to the surface of the ice sheet and are influenced by source, transport and deposition processes. Together, these records contain detailed, multi-parameter records of past climate variability over the last glacial period.
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.
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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Pavel Talalay, Yazhou Li, Laurent Augustin, Gary D. Clow, Jialin Hong, Eric Lefebvre, Alexey Markov, Hideaki Motoyama, and Catherine Ritz
The Cryosphere, 14, 4021–4037, https://doi.org/10.5194/tc-14-4021-2020, https://doi.org/10.5194/tc-14-4021-2020, 2020
Xavier Fettweis, Stefan Hofer, Uta Krebs-Kanzow, Charles Amory, Teruo Aoki, Constantijn J. Berends, Andreas Born, Jason E. Box, Alison Delhasse, Koji Fujita, Paul Gierz, Heiko Goelzer, Edward Hanna, Akihiro Hashimoto, Philippe Huybrechts, Marie-Luise Kapsch, Michalea D. King, Christoph Kittel, Charlotte Lang, Peter L. Langen, Jan T. M. Lenaerts, Glen E. Liston, Gerrit Lohmann, Sebastian H. Mernild, Uwe Mikolajewicz, Kameswarrao Modali, Ruth H. Mottram, Masashi Niwano, Brice Noël, Jonathan C. Ryan, Amy Smith, Jan Streffing, Marco Tedesco, Willem Jan van de Berg, Michiel van den Broeke, Roderik S. W. van de Wal, Leo van Kampenhout, David Wilton, Bert Wouters, Florian Ziemen, and Tobias Zolles
The Cryosphere, 14, 3935–3958, https://doi.org/10.5194/tc-14-3935-2020, https://doi.org/10.5194/tc-14-3935-2020, 2020
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We evaluated simulated Greenland Ice Sheet surface mass balance from 5 kinds of models. While the most complex (but expensive to compute) models remain the best, the faster/simpler models also compare reliably with observations and have biases of the same order as the regional models. Discrepancies in the trend over 2000–2012, however, suggest that large uncertainties remain in the modelled future SMB changes as they are highly impacted by the meltwater runoff biases over the current climate.
Yukihiko Onuma, Nozomu Takeuchi, Sota Tanaka, Naoko Nagatsuka, Masashi Niwano, and Teruo Aoki
The Cryosphere, 14, 2087–2101, https://doi.org/10.5194/tc-14-2087-2020, https://doi.org/10.5194/tc-14-2087-2020, 2020
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Surface snow albedo is substantially reduced by organic impurities, such as microbes that live in the snow. We present the temporal changes of surface albedo, snow grain size, and inorganic and organic impurities observed on a snowpack in northwest Greenland during summer and our attempt to reproduce the changes in albedo with a physically based snow albedo model coupled with a snow algae model. To our knowledge, this is the first report proposing such a coupled albedo model in Greenland.
Adrien Gilbert, Anna Sinisalo, Tika R. Gurung, Koji Fujita, Sudan B. Maharjan, Tenzing C. Sherpa, and Takehiro Fukuda
The Cryosphere, 14, 1273–1288, https://doi.org/10.5194/tc-14-1273-2020, https://doi.org/10.5194/tc-14-1273-2020, 2020
Ambarish Pokhrel, Kimitaka Kawamura, Bhagawati Kunwar, Kaori Ono, Akane Tsushima, Osamu Seki, Sumio Matoba, and Takayuki Shiraiwa
Atmos. Chem. Phys., 20, 597–612, https://doi.org/10.5194/acp-20-597-2020, https://doi.org/10.5194/acp-20-597-2020, 2020
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A 180 m long (ca. 274 year) ice core was drilled in the saddle of the Aurora Peak in Alaska (63.52° N, 146.54° W; elevation: 2,825 m). The ice core samples were derived with O-bis-(trimethylsilyl)trifluoroacetamide with 1 % trimethylsilyl chloride and pyridine followed by gas-chromatography–mass-spectrometry analyses. Levoglucosan, dehydroabietic acid and vanillic acid are reported for the first time from the alpine glacier to better understand historical biomass burning.
Shun Tsutaki, Koji Fujita, Takayuki Nuimura, Akiko Sakai, Shin Sugiyama, Jiro Komori, and Phuntsho Tshering
The Cryosphere, 13, 2733–2750, https://doi.org/10.5194/tc-13-2733-2019, https://doi.org/10.5194/tc-13-2733-2019, 2019
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We investigate thickness change of Bhutanese glaciers during 2004–2011 using repeat GPS surveys and satellite-based observations. The thinning rate of Lugge Glacier (LG) is > 3 times that of Thorthormi Glacier (TG). Numerical simulations of ice dynamics and surface mass balance (SMB) demonstrate that the rapid thinning of LG is driven by both negative SMB and dynamic thinning, while the thinning of TG is minimised by a longitudinally compressive flow regime.
Damiano Della Lunga, Hörhold Maria, Birthe Twarloh, Behrens Melanie, Dallmayr Remi, Erhardt Tobias, Jensen Camille Marie, and Wilhelms Frank
The Cryosphere Discuss., https://doi.org/10.5194/tc-2019-215, https://doi.org/10.5194/tc-2019-215, 2019
Preprint withdrawn
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The extent of sea ice plays a major role in the present Arctic warming, and it is possibly one of its first victims, since it has been predicted to disappear in the near future, if warming proceed. Our manuscript validates ice core proxies for the reconstruction of the variability of sea ice extent around Greenland in the last 600 years, and simultanesouly infers the evolution of the proxy-sources with time. Understanding past sea ice extent variability, is thus crucial in predicting its future.
Satoru Yamaguchi, Masaaki Ishizaka, Hiroki Motoyoshi, Sent Nakai, Vincent Vionnet, Teruo Aoki, Katsuya Yamashita, Akihiro Hashimoto, and Akihiro Hachikubo
The Cryosphere, 13, 2713–2732, https://doi.org/10.5194/tc-13-2713-2019, https://doi.org/10.5194/tc-13-2713-2019, 2019
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The specific surface area (SSA) of solid precipitation particles (PPs) includes detailed information of PP. This work is based on field measurement of SSA of PPs in Nagaoka, the city with the heaviest snowfall in Japan. The values of SSA strongly depend on wind speed (WS) and wet-bulb temperature (Tw) on the ground. An equation to empirically estimate the SSA of fresh PPs with WS and Tw was established and the equation successfully reproduced the fluctuation of SSA in Nagaoka.
Koji Fujita, Sumito Matoba, Yoshinori Iizuka, Nozomu Takeuchi, and Teruo Aoki
Clim. Past Discuss., https://doi.org/10.5194/cp-2019-97, https://doi.org/10.5194/cp-2019-97, 2019
Revised manuscript not accepted
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This study presents a novel method for reconstructing summer temperatures from ice-layer thickness and annual accumulation in an ice core using an energy balance model. The method calculates a lookup table by considering heat conduction and meltwater refreezing in firn. We applied the method to four ice cores in different climates. Sensitivity analyses reveal that the annual temperature range, amount of annual precipitation, and firn albedo significantly affect the estimated summer temperature.
Sauvik Santra, Shubha Verma, Koji Fujita, Indrajit Chakraborty, Olivier Boucher, Toshihiko Takemura, John F. Burkhart, Felix Matt, and Mukesh Sharma
Atmos. Chem. Phys., 19, 2441–2460, https://doi.org/10.5194/acp-19-2441-2019, https://doi.org/10.5194/acp-19-2441-2019, 2019
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The present study provided information on specific glaciers over the Hindu Kush Himalayan region identified as being vulnerable to BC-induced impacts (affected by high BC-induced snow albedo reduction in addition to being sensitive to BC-induced impacts), thus impacting the downstream hydrology. The source-specific contribution to atmospheric BC aerosols by emission sources led to identifying the potential emission source, which was distinctive over south and north to 30° N.
Yukihiko Onuma, Nozomu Takeuchi, Sota Tanaka, Naoko Nagatsuka, Masashi Niwano, and Teruo Aoki
The Cryosphere, 12, 2147–2158, https://doi.org/10.5194/tc-12-2147-2018, https://doi.org/10.5194/tc-12-2147-2018, 2018
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Snow algal bloom can substantially increase melt rates of the snow due to the effect of albedo reduction on the snow surface. In this study, the temporal changes in algal abundance on the snowpacks of Greenland Glacier were studied in order to reproduce snow algal growth using a numerical model. Our study demonstrates that a simple numerical model could simulate the temporal variation in snow algal abundance on the glacier throughout the summer season.
Masashi Niwano, Teruo Aoki, Akihiro Hashimoto, Sumito Matoba, Satoru Yamaguchi, Tomonori Tanikawa, Koji Fujita, Akane Tsushima, Yoshinori Iizuka, Rigen Shimada, and Masahiro Hori
The Cryosphere, 12, 635–655, https://doi.org/10.5194/tc-12-635-2018, https://doi.org/10.5194/tc-12-635-2018, 2018
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We present a high-resolution regional climate model called NHM–SMAP applied to the Greenland Ice Sheet (GrIS). The model forced by JRA-55 reanalysis is evaluated using in situ data from automated weather stations, stake measurements,
and ice core obtained from 2011 to 2014. By utilizing the model, we highlight that the choice of calculation schemes for vertical water movement in snow and firn has an effect of up to 200 Gt/year in the yearly accumulated GrIS-wide surface mass balance estimates.
Damodar Lamsal, Koji Fujita, and Akiko Sakai
The Cryosphere, 11, 2815–2827, https://doi.org/10.5194/tc-11-2815-2017, https://doi.org/10.5194/tc-11-2815-2017, 2017
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This study presents the geodetic mass balance of Kanchenjunga Glacier, a heavily debris-covered glacier in the easternmost Nepal Himalaya, between 1975 and 2010 using high-resolution DEMs. The rate of elevation change positively correlates with elevation and glacier velocity, and significant surface lowering is observed at supraglacial ponds. A difference in pond density would strongly affect the different geodetic mass balances of the Kanchenjunga and Khumbu glaciers.
Keiichiro Hara, Sumito Matoba, Motohiro Hirabayashi, and Tetsuhide Yamasaki
Atmos. Chem. Phys., 17, 8577–8598, https://doi.org/10.5194/acp-17-8577-2017, https://doi.org/10.5194/acp-17-8577-2017, 2017
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To obtain knowledge about sea-salt chemistry in polar regions, we made simultaneous measurements and sampling of aerosols, frost flowers, and brine around northwestern Greenland during winter–spring. Our results show sea-salt enrichment in frost flowers and snow. Also, the fractionated sea-salt particles were suspended in the atmosphere over sea-ice areas. From the field evidence and results from earlier studies, we propose and describe sea-salt cycles in seasonal sea-ice areas.
Koji Fujita, Hiroshi Inoue, Takeki Izumi, Satoru Yamaguchi, Ayako Sadakane, Sojiro Sunako, Kouichi Nishimura, Walter W. Immerzeel, Joseph M. Shea, Rijan B. Kayastha, Takanobu Sawagaki, David F. Breashears, Hiroshi Yagi, and Akiko Sakai
Nat. Hazards Earth Syst. Sci., 17, 749–764, https://doi.org/10.5194/nhess-17-749-2017, https://doi.org/10.5194/nhess-17-749-2017, 2017
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We create multiple DEMs from photographs taken by helicopter and UAV and reveal the deposit volumes over the Langtang village, which was destroyed by avalanches induced by the Gorkha earthquake. Estimated snow depth in the source area is consistent with anomalously large snow depths observed at a neighboring glacier. Comparing with a long-term observational data, we conclude that this anomalous winter snow amplified the disaster induced by the 2015 Gorkha earthquake in Nepal.
Anna Dittmann, Elisabeth Schlosser, Valérie Masson-Delmotte, Jordan G. Powers, Kevin W. Manning, Martin Werner, and Koji Fujita
Atmos. Chem. Phys., 16, 6883–6900, https://doi.org/10.5194/acp-16-6883-2016, https://doi.org/10.5194/acp-16-6883-2016, 2016
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For a better understanding of the stable water isotope data from ice cores, recent time periods have to be analysed, where both measurements and model simulations are available. This was done for Dome Fuji by combining observations, synoptic analysis, back trajectories, and isotopic modelling. It was found that a more northerly moisture source does not necessarily mean a larger temperature difference between source area and deposition site and thus precipitation more depleted in heavy isotopes.
Takeshi Kinase, Kazuyuki Kita, Yoshimi Tsukagawa-Ogawa, Kumiko Goto-Azuma, and Hiroto Kawashima
Atmos. Meas. Tech., 9, 1939–1945, https://doi.org/10.5194/amt-9-1939-2016, https://doi.org/10.5194/amt-9-1939-2016, 2016
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The influence of temperature and time for the melting snow samples on the measurement of mass concentration and its size distribution of black carbon (BC) in snow have not been understood enough. We evaluated the effect of the melting temperature and time with experiments. We also derived the best conditions of temperature and time for melting snow samples for the measurement of BC in snow by a single-particle soot photometer (SP2).
H. Nagai, K. Fujita, A. Sakai, T. Nuimura, and T. Tadono
The Cryosphere, 10, 65–85, https://doi.org/10.5194/tc-10-65-2016, https://doi.org/10.5194/tc-10-65-2016, 2016
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Digital glacier inventories are invaluable data sets for revealing the characteristics of glacier distribution. However, quantitative comparison of present inventories was not performed. Here, we present a new inventory manually delineated from Advanced Land Observing Satellite (ALOS) imagery and compare it with existing inventories for the Bhutan Himalaya. Quantification of overlapping among available glacier outlines suggests consistency and recent improvement of their delineation quality.
T. Kobashi, T. Ikeda-Fukazawa, M. Suwa, J. Schwander, T. Kameda, J. Lundin, A. Hori, H. Motoyama, M. Döring, and M. Leuenberger
Atmos. Chem. Phys., 15, 13895–13914, https://doi.org/10.5194/acp-15-13895-2015, https://doi.org/10.5194/acp-15-13895-2015, 2015
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We find that argon/nitrogen ratios of trapped air in the GISP2 ice core on “gas ages” are significantly negatively correlated with accumulation rate changes over the past 6000 years. Lines of evidence indicate that changes in overloading pressure at bubble closeoff depths induced the gas fractionation in closed bubbles. Further understanding of the fractionation processes may lead to a new proxy for the past temperature and accumulation rate.
S. Fujita, F. Parrenin, M. Severi, H. Motoyama, and E. W. Wolff
Clim. Past, 11, 1395–1416, https://doi.org/10.5194/cp-11-1395-2015, https://doi.org/10.5194/cp-11-1395-2015, 2015
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
M. Niwano, T. Aoki, S. Matoba, S. Yamaguchi, T. Tanikawa, K. Kuchiki, and H. Motoyama
The Cryosphere, 9, 971–988, https://doi.org/10.5194/tc-9-971-2015, https://doi.org/10.5194/tc-9-971-2015, 2015
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A physical snowpack model SMAP and in situ meteorological and snow data obtained at site SIGMA-A on the northwest Greenland ice sheet are used to assess surface energy balance during the extreme near-surface snowmelt event around 12 July 2012. We determined that the main factor for the melt event observed at the SIGMA-A site was low-level clouds accompanied by a significant temperature increase, which induced surface heating via cloud radiative forcing in the polar region.
T. Nuimura, A. Sakai, K. Taniguchi, H. Nagai, D. Lamsal, S. Tsutaki, A. Kozawa, Y. Hoshina, S. Takenaka, S. Omiya, K. Tsunematsu, P. Tshering, and K. Fujita
The Cryosphere, 9, 849–864, https://doi.org/10.5194/tc-9-849-2015, https://doi.org/10.5194/tc-9-849-2015, 2015
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We present a new glacier inventory for high-mountain Asia named “Glacier Area Mapping for Discharge from the Asian Mountains” (GAMDAM). Glacier outlines were delineated manually using 356 Landsat ETM+ scenes in 226 path-row sets from the period 1999–2003, in conjunction with a digital elevation model and high-resolution Google EarthTM imagery. Our GAMDAM Glacier Inventory includes 87,084 glaciers covering a total area of 91,263 ± 13,689 km2 throughout high-mountain Asia.
A. Sakai, T. Nuimura, K. Fujita, S. Takenaka, H. Nagai, and D. Lamsal
The Cryosphere, 9, 865–880, https://doi.org/10.5194/tc-9-865-2015, https://doi.org/10.5194/tc-9-865-2015, 2015
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Among meteorological elements, precipitation has a large spatial variability and less observation, particularly in high-mountain Asia, although precipitation in mountains is an important parameter for hydrological circulation. Based on the GAMDAM glacier inventory, we estimated precipitation contributing to glacier mass at the median elevation of glaciers, which is presumed to be at equilibrium-line altitude, by tuning adjustment parameters of precipitation.
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
A. Tsushima, S. Matoba, T. Shiraiwa, S. Okamoto, H. Sasaki, D. J. Solie, and K. Yoshikawa
Clim. Past, 11, 217–226, https://doi.org/10.5194/cp-11-217-2015, https://doi.org/10.5194/cp-11-217-2015, 2015
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A 180.17-m ice core was drilled at Aurora Peak in the central part of the Alaska Range, Alaska, in 2008. The ice core age was determined by annual counts of δD and seasonal cycles of Na+. Here, we show that the chronology of the Aurora Peak ice core from 95.61 m to the top corresponds to the period from 1900 to the summer season of 2008, with a dating error of ±3 years. Our results suggest that temporal variations in δD and annual accumulation rates are strongly related to shifts in PDO Index.
K. Fujita and A. Sakai
Hydrol. Earth Syst. Sci., 18, 2679–2694, https://doi.org/10.5194/hess-18-2679-2014, https://doi.org/10.5194/hess-18-2679-2014, 2014
K. Osada, S. Ura, M. Kagawa, M. Mikami, T. Y. Tanaka, S. Matoba, K. Aoki, M. Shinoda, Y. Kurosaki, M. Hayashi, A. Shimizu, and M. Uematsu
Atmos. Chem. Phys., 14, 1107–1121, https://doi.org/10.5194/acp-14-1107-2014, https://doi.org/10.5194/acp-14-1107-2014, 2014
Y. Motizuki, Y. Nakai, K. Takahashi, M. Igarashi, H. Motoyama, and K. Suzuki
The Cryosphere Discuss., https://doi.org/10.5194/tcd-8-769-2014, https://doi.org/10.5194/tcd-8-769-2014, 2014
Revised manuscript has not been submitted
J. Chappellaz, C. Stowasser, T. Blunier, D. Baslev-Clausen, E. J. Brook, R. Dallmayr, X. Faïn, J. E. Lee, L. E. Mitchell, O. Pascual, D. Romanini, J. Rosen, and S. Schüpbach
Clim. Past, 9, 2579–2593, https://doi.org/10.5194/cp-9-2579-2013, https://doi.org/10.5194/cp-9-2579-2013, 2013
T. Kobashi, K. Goto-Azuma, J. E. Box, C.-C. Gao, and T. Nakaegawa
Clim. Past, 9, 2299–2317, https://doi.org/10.5194/cp-9-2299-2013, https://doi.org/10.5194/cp-9-2299-2013, 2013
H. Nagai, K. Fujita, T. Nuimura, and A. Sakai
The Cryosphere, 7, 1303–1314, https://doi.org/10.5194/tc-7-1303-2013, https://doi.org/10.5194/tc-7-1303-2013, 2013
K. Fujita, A. Sakai, S. Takenaka, T. Nuimura, A. B. Surazakov, T. Sawagaki, and T. Yamanokuchi
Nat. Hazards Earth Syst. Sci., 13, 1827–1839, https://doi.org/10.5194/nhess-13-1827-2013, https://doi.org/10.5194/nhess-13-1827-2013, 2013
Y. Zhang, Y. Hirabayashi, K. Fujita, S. Liu, and Q. Liu
The Cryosphere Discuss., https://doi.org/10.5194/tcd-7-2413-2013, https://doi.org/10.5194/tcd-7-2413-2013, 2013
Revised manuscript not accepted
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
Related subject area
Subject: Proxy Use-Development-Validation | Archive: Ice Cores | Timescale: Holocene
An age scale for new climate records from Sherman Island, West Antarctica
An annually resolved chronology for the Mount Brown South ice cores, East Antarctica
The new Kr-86 excess ice core proxy for synoptic activity: West Antarctic storminess possibly linked to Intertropical Convergence Zone (ITCZ) movement through the last deglaciation
A multi-ice-core, annual-layer-counted Greenland ice-core chronology for the last 3800 years: GICC21
How precipitation intermittency sets an optimal sampling distance for temperature reconstructions from Antarctic ice cores
Five thousand years of fire history in the high North Atlantic region: natural variability and ancient human forcing
Cryptotephra from the Icelandic Veiðivötn 1477 CE eruption in a Greenland ice core: confirming the dating of volcanic events in the 1450s CE and assessing the eruption's climatic impact
A first chronology for the East Greenland Ice-core Project (EGRIP) over the Holocene and last glacial termination
High-frequency climate variability in the Holocene from a coastal-dome ice core in east-central Greenland
Greenland temperature and precipitation over the last 20 000 years using data assimilation
Holocene atmospheric iodine evolution over the North Atlantic
The SP19 chronology for the South Pole Ice Core – Part 1: volcanic matching and annual layer counting
Novel automated inversion algorithm for temperature reconstruction using gas isotopes from ice cores
Particle shape accounts for instrumental discrepancy in ice core dust size distributions
Temperature and mineral dust variability recorded in two low-accumulation Alpine ice cores over the last millennium
Regional climate signal vs. local noise: a two-dimensional view of water isotopes in Antarctic firn at Kohnen Station, Dronning Maud Land
Synchronizing the Greenland ice core and radiocarbon timescales over the Holocene – Bayesian wiggle-matching of cosmogenic radionuclide records
A method for analysis of vanillic acid in polar ice cores
Dating a tropical ice core by time–frequency analysis of ion concentration depth profiles
A new Himalayan ice core CH4 record: possible hints at the preindustrial latitudinal gradient
Causes of Greenland temperature variability over the past 4000 yr: implications for northern hemispheric temperature changes
Greenland ice core evidence of the 79 AD Vesuvius eruption
Deglaciation records of 17O-excess in East Antarctica: reliable reconstruction of oceanic normalized relative humidity from coastal sites
Isobel Rowell, Carlos Martin, Robert Mulvaney, Helena Pryer, Dieter Tetzner, Emily Doyle, Hara Madhav Talasila, Jilu Li, and Eric Wolff
Clim. Past, 19, 1699–1714, https://doi.org/10.5194/cp-19-1699-2023, https://doi.org/10.5194/cp-19-1699-2023, 2023
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We present an age scale for a new type of ice core from a vulnerable region in West Antarctic, which is lacking in longer-term (greater than a few centuries) ice core records. The Sherman Island core extends to greater than 1 kyr. We provide modelling evidence for the potential of a 10 kyr long core. We show that this new type of ice core can be robustly dated and that climate records from this core will be a significant addition to existing regional climate records.
Tessa R. Vance, Nerilie J. Abram, Alison S. Criscitiello, Camilla K. Crockart, Aylin DeCampo, Vincent Favier, Vasileios Gkinis, Margaret Harlan, Sarah L. Jackson, Helle A. Kjær, Chelsea A. Long, Meredith K. Nation, Chris T. Plummer, Delia Segato, Andrea Spolaor, and Paul T. Vallelonga
Clim. Past Discuss., https://doi.org/10.5194/cp-2023-52, https://doi.org/10.5194/cp-2023-52, 2023
Revised manuscript accepted for CP
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This study presents the chronologies from the new Mount Brown South ice cores, from East Antarctica, which were developed by counting annual layers in the ice core data and aligning these to volcanic sulfate signatures. The uncertainty in the dating is quantified, and we discuss initial results from seasonal cycle analysis and mean annual concentrations. The chronologies will underpin the development of new proxy records for East Antarctica spanning the past millennium.
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.
Giulia Sinnl, Mai Winstrup, Tobias Erhardt, Eliza Cook, Camilla Marie Jensen, Anders Svensson, Bo Møllesøe Vinther, Raimund Muscheler, and Sune Olander Rasmussen
Clim. Past, 18, 1125–1150, https://doi.org/10.5194/cp-18-1125-2022, https://doi.org/10.5194/cp-18-1125-2022, 2022
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A new Greenland ice-core timescale, covering the last 3800 years, was produced using the machine learning algorithm StratiCounter. We synchronized the ice cores using volcanic eruptions and wildfires. We compared the new timescale to the tree-ring timescale, finding good alignment both between the common signatures of volcanic eruptions and of solar activity. Our Greenlandic timescales is safe to use for the Late Holocene, provided one uses our uncertainty estimate.
Thomas Münch, Martin Werner, and Thomas Laepple
Clim. Past, 17, 1587–1605, https://doi.org/10.5194/cp-17-1587-2021, https://doi.org/10.5194/cp-17-1587-2021, 2021
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We analyse Holocene climate model simulation data to find the locations of Antarctic ice cores which are best suited to reconstruct local- to regional-scale temperatures. We find that the spatial decorrelation scales of the temperature variations and of the noise from precipitation intermittency set an effective sampling length scale. Following this, a single core should be located at the
target site for the temperature reconstruction, and a second one optimally lies more than 500 km away.
Delia Segato, Maria Del Carmen Villoslada Hidalgo, Ross Edwards, Elena Barbaro, Paul Vallelonga, Helle Astrid Kjær, Marius Simonsen, Bo Vinther, Niccolò Maffezzoli, Roberta Zangrando, Clara Turetta, Dario Battistel, Orri Vésteinsson, Carlo Barbante, and Andrea Spolaor
Clim. Past, 17, 1533–1545, https://doi.org/10.5194/cp-17-1533-2021, https://doi.org/10.5194/cp-17-1533-2021, 2021
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Human influence on fire regimes in the past is poorly understood, especially at high latitudes. We present 5 kyr of fire proxies levoglucosan, black carbon, and ammonium in the RECAP ice core in Greenland and reconstruct for the first time the fire regime in the high North Atlantic region, comprising coastal east Greenland and Iceland. Climate is the main driver of the fire regime, but at 1.1 kyr BP a contribution may be made by the deforestation resulting from Viking colonization of Iceland.
Peter M. Abbott, Gill Plunkett, Christophe Corona, Nathan J. Chellman, Joseph R. McConnell, John R. Pilcher, Markus Stoffel, and Michael Sigl
Clim. Past, 17, 565–585, https://doi.org/10.5194/cp-17-565-2021, https://doi.org/10.5194/cp-17-565-2021, 2021
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Volcanic eruptions are a key source of climatic variability, and greater understanding of their past influence will increase the accuracy of future projections. We use volcanic ash from a 1477 CE Icelandic eruption in a Greenlandic ice core as a temporal fix point to constrain the timing of two eruptions in the 1450s CE and their climatic impact. Despite being the most explosive Icelandic eruption in the last 1200 years, the 1477 CE event had a limited impact on Northern Hemisphere climate.
Seyedhamidreza Mojtabavi, Frank Wilhelms, Eliza Cook, Siwan M. Davies, Giulia Sinnl, Mathias Skov Jensen, Dorthe Dahl-Jensen, Anders Svensson, Bo M. Vinther, Sepp Kipfstuhl, Gwydion Jones, Nanna B. Karlsson, Sergio Henrique Faria, Vasileios Gkinis, Helle Astrid Kjær, Tobias Erhardt, Sarah M. P. Berben, Kerim H. Nisancioglu, Iben Koldtoft, and Sune Olander Rasmussen
Clim. Past, 16, 2359–2380, https://doi.org/10.5194/cp-16-2359-2020, https://doi.org/10.5194/cp-16-2359-2020, 2020
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We present a first chronology for the East Greenland Ice-core Project (EGRIP) over the Holocene and last glacial termination. After field measurements and processing of the ice-core data, the GICC05 timescale is transferred from the NGRIP core to the EGRIP core by means of matching volcanic events and common patterns (381 match points) in the ECM and DEP records. The new timescale is named GICC05-EGRIP-1 and extends back to around 15 kyr b2k.
Abigail G. Hughes, Tyler R. Jones, Bo M. Vinther, Vasileios Gkinis, C. Max Stevens, Valerie Morris, Bruce H. Vaughn, Christian Holme, Bradley R. Markle, and James W. C. White
Clim. Past, 16, 1369–1386, https://doi.org/10.5194/cp-16-1369-2020, https://doi.org/10.5194/cp-16-1369-2020, 2020
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An ice core drilled on the Renland ice cap (RECAP) in east-central Greenland contains a continuous climate record dating through the last glacial period. Here we present the water isotope record for the Holocene, in which high-resolution climate information is retained for the last 8 kyr. We find that the RECAP water isotope record exhibits seasonal and decadal variability which may reflect sea surface conditions and regional climate variability.
Jessica A. Badgeley, Eric J. Steig, Gregory J. Hakim, and Tyler J. Fudge
Clim. Past, 16, 1325–1346, https://doi.org/10.5194/cp-16-1325-2020, https://doi.org/10.5194/cp-16-1325-2020, 2020
Juan Pablo Corella, Niccolo Maffezzoli, Carlos Alberto Cuevas, Paul Vallelonga, Andrea Spolaor, Giulio Cozzi, Juliane Müller, Bo Vinther, Carlo Barbante, Helle Astrid Kjær, Ross Edwards, and Alfonso Saiz-Lopez
Clim. Past, 15, 2019–2030, https://doi.org/10.5194/cp-15-2019-2019, https://doi.org/10.5194/cp-15-2019-2019, 2019
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This study provides the first reconstruction of atmospheric iodine levels in the Arctic during the last 11 700 years from an ice core record in coastal Greenland. Dramatic shifts in iodine level variability coincide with abrupt climatic transitions in the North Atlantic. Since atmospheric iodine levels have significant environmental and climatic implications, this study may serve as a past analog to predict future changes in Arctic climate in response to global warming.
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.
Michael Döring and Markus C. Leuenberger
Clim. Past, 14, 763–788, https://doi.org/10.5194/cp-14-763-2018, https://doi.org/10.5194/cp-14-763-2018, 2018
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We present a novel approach for ice-core-based temperature reconstructions, which is based on gas-isotope data measured on enclosed air bubbles in ice cores. The processes of air movement and enclosure are highly temperature dependent due to heat diffusion in and densification of the snow and ice. Our method inverts a model, which describes these processes, to desired temperature histories. This paper examines the performance of our novel approach on different synthetic isotope-data scenarios.
Marius Folden Simonsen, Llorenç Cremonesi, Giovanni Baccolo, Samuel Bosch, Barbara Delmonte, Tobias Erhardt, Helle Astrid Kjær, Marco Potenza, Anders Svensson, and Paul Vallelonga
Clim. Past, 14, 601–608, https://doi.org/10.5194/cp-14-601-2018, https://doi.org/10.5194/cp-14-601-2018, 2018
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Ice core dust size distributions are more often measured today by an Abakus laser sensor than by the more technically demanding but also very accurate Coulter counter. However, Abakus measurements consistently give larger particle sizes. We show here that this bias exists because the particles are flat and elongated. Correcting for this gives more accurate Abakus measurements. Furthermore, the shape of the particles can be extracted from a combination of Coulter counter and Abakus measurements.
Pascal Bohleber, Tobias Erhardt, Nicole Spaulding, Helene Hoffmann, Hubertus Fischer, and Paul Mayewski
Clim. Past, 14, 21–37, https://doi.org/10.5194/cp-14-21-2018, https://doi.org/10.5194/cp-14-21-2018, 2018
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The Colle Gnifetti (CG) glacier is the only drilling site in the European Alps offering ice core records back to some 1000 years. We aim to fully exploit these unique long-term records by establishing a reliable long-term age scale and an improved ice core proxy interpretation for reconstructing temperature. Our findings reveal a site-specific temperature-related signal in the trends of the mineral dust proxy Ca2+ that may supplement other proxy evidence over the last millennium.
Thomas Münch, Sepp Kipfstuhl, Johannes Freitag, Hanno Meyer, and Thomas Laepple
Clim. Past, 12, 1565–1581, https://doi.org/10.5194/cp-12-1565-2016, https://doi.org/10.5194/cp-12-1565-2016, 2016
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Ice-core oxygen isotope ratios are a key climate archive to infer past temperatures, an interpretation however complicated by non-climatic noise. Based on 50 m firn trenches, we present for the first time a two-dimensional view (vertical × horizontal) of how oxygen isotopes are stored in Antarctic firn. A statistical noise model allows inferences for the validity of ice coring efforts to reconstruct past temperatures, highlighting the need of replicate cores for Holocene climate reconstructions.
F. Adolphi and R. Muscheler
Clim. Past, 12, 15–30, https://doi.org/10.5194/cp-12-15-2016, https://doi.org/10.5194/cp-12-15-2016, 2016
Short summary
Short summary
Here we employ common variations in tree-ring 14C and Greenland ice core 10Be records to synchronize the Greenland ice core (GICC05) and the radiocarbon (IntCal13) timescale over the Holocene. We propose a transfer function between both timescales that allows continuous comparisons between radiocarbon dated and ice core climate records at unprecedented chronological precision.
M. M. Grieman, J. Greaves, and E. S. Saltzman
Clim. Past, 11, 227–232, https://doi.org/10.5194/cp-11-227-2015, https://doi.org/10.5194/cp-11-227-2015, 2015
M. Gay, M. De Angelis, and J.-L. Lacoume
Clim. Past, 10, 1659–1672, https://doi.org/10.5194/cp-10-1659-2014, https://doi.org/10.5194/cp-10-1659-2014, 2014
S. Hou, J. Chappellaz, D. Raynaud, V. Masson-Delmotte, J. Jouzel, P. Bousquet, and D. Hauglustaine
Clim. Past, 9, 2549–2554, https://doi.org/10.5194/cp-9-2549-2013, https://doi.org/10.5194/cp-9-2549-2013, 2013
T. Kobashi, K. Goto-Azuma, J. E. Box, C.-C. Gao, and T. Nakaegawa
Clim. Past, 9, 2299–2317, https://doi.org/10.5194/cp-9-2299-2013, https://doi.org/10.5194/cp-9-2299-2013, 2013
C. Barbante, N. M. Kehrwald, P. Marianelli, B. M. Vinther, J. P. Steffensen, G. Cozzi, C. U. Hammer, H. B. Clausen, and M.-L. Siggaard-Andersen
Clim. Past, 9, 1221–1232, https://doi.org/10.5194/cp-9-1221-2013, https://doi.org/10.5194/cp-9-1221-2013, 2013
R. Winkler, A. Landais, H. Sodemann, L. Dümbgen, F. Prié, V. Masson-Delmotte, B. Stenni, and J. Jouzel
Clim. Past, 8, 1–16, https://doi.org/10.5194/cp-8-1-2012, https://doi.org/10.5194/cp-8-1-2012, 2012
Cited articles
Allen, V. T. and Johns, W. D.: Clays and clay minerals of New England and
Eastern Canada, GSA Bulletin, 71, 75–86,
https://doi.org/10.1130/0016-7606(1960)71[75:CACMON]2.0.CO;2, 1960.
Amino, T., Iizuka, Y., Matoba, S., Shimada, R., Oshima, N., Suzuki, T.,
Ando, T., Aoki, T., and Fujita, K.: Increasing dust emission from ice free
terrain in southeastern Greenland since 2000, Polar Sci., 27, 100599,
https://doi.org/10.1016/j.polar.2020.100599, 2021.
Bendixen, M., Iversen, L. L., Bjørk, A. A., Elberling, B.,
Westergaard-Nielsen, A., Overeem, I., Barnhart, K. R., Khan, S. A., Box, J.
E., and Abermann, J.: Delta progradation in Greenland driven by increasing
glacial mass loss, Nature, 550, 101–104, https://doi.org/10.1038/nature23873, 2017.
Bergaya, F., Theng, B. K. G., and Legaly, G. (Eds.): Handbook of Clay
Science. Development in Clay Science, Elsevier, Amsterdam, 2006.
Biscaye, P. E.: Mineralogy and sedimentation of recent deep-sea clay in the
Atlantic Ocean and adjacent seas and oceans, GSA Bulletin, 76, 803–832, https://doi.org/10.1130/0016-7606(1965)76[803:MASORD]2.0.CO;2, 1965.
Biscaye, P. E., Grousset, F. E., Revel, M., Van der Gaast, S., Zielinski, G.
A., Vaars, A., and Kukla, G.: Asian provenance of glacial dust (stage 2) in
the Greenland Ice Sheet Project 2 ice core, Summit, Greenland, J. Geophys.
Res., 102, 26765–26781, https://doi.org/10.1029/97JC01249, 1997.
Bory, A. J.-M., Biscaye, P. E., and Grousset, F. E.: Two distinct seasonal
Asian source regions for mineral dust deposited in Greenland (NorthGRIP),
Geophys. Res. Lett., 30, 1167, https://doi.org/10.1029/2002GL016446, 2003a.
Bory, A. J.-M., Biscaye, P. E., Piotrowski, A. M., and Steffensen, J. P.:
Regional variability of ice core dust composition and provenance in
Greenland, Geochem. Geophy. Geosy., 4, 1107, https://doi.org/10.1029/2003GC000627, 2003b.
Box, J. E. and Herrington, A.: Was there a 1930's meltdown of Greenland
glaciers?, American Geophysical Union Fall Meeting, San Francisco, USA,
10–14 December 2007, C11A-0077, 2007.
Box, J. E., Yang, L., Bromwich, D. H., and Bai, L.: Greenland Ice Sheet
Surface Air Temperature Variability: 1840–2007, J. Climate, 22,
4029–4049, https://doi.org/10.1175/2009JCLI2816.1, 2009.
Bullard, J. E. and Austin, M. J.: Dust generation on a proglacial
floodplain, West Greenland, Aeolian Res., 3, 43–54,
https://doi.org/10.1016/j.aeolia.2011.01.002, 2011.
Bullard, J. E. and Mockford, T.: Seasonal and decadal variability of dust
observations in the Kangerlussuaq area, west Greenland, Arct. Antarct. Alp.
Res., 50, S100011, https://doi.org/10.1080/15230430.2017.1415854, 2018.
Capo, R. C., Stewart, B. W., and Chadwick, O. A.: Strontium isotopes as
tracers of ecosystem processes: theory and methods, Geoderma, 82, 197–225,
https://doi.org/10.1016/S0016-7061(97)00102-X, 1998.
Cappelen, J. (Ed.): Denmark – DMI Historical Climate Data Collection
1768–2018, DMI Report 19-02, DMI, Copenhagen, Denmark, 2019.
Clausen, H. B. and Hammer, C. U.: The Laki and Tambora eruptions as revealed
in Greenland ice cores from 11 locations, Ann. Glaciol., 10, 16–22,
https://doi.org/10.3189/S0260305500004092, 1988.
Cremaschi, M.: Paleosols and Ventusols in the Central Po Plain (Northern
Italy), A Study in Quaternary Geology and Soil Development, Unicopli,
Milano, Italy, 1987.
Dallmayr, R., Goto-Azuma, K., Kjær, H. A., Azuma, N, Takata, M.,
Schüpbach, S., and Hirabayashi, M.: A High-Resolution Continuous Flow
Analysis System for Polar Ice Cores, Bull. Glaciol. Res., 34, 11–20, https://doi.org/10.5331/bgr.16R03, 2016.
Darby, D. A.: Kaolinite and other clay minerals in Arctic Ocean sediments,
J. Sediment. Res., 45, 272–279, https://doi.org/10.1306/212F6D34-2B24-11D7-8648000102C1865D, 1975.
De Angelis, M., Steffensen, J. P., Legrand, M., Clausen, H., and Hammer, C.:
Primary aerosol (sea salt and soil dust) deposited in Greenland ice during
the last climatic cycle: Comparison with East Antarctic records, J. Geophys.
Res., 102, 26681–26698, https://doi.org/10.1029/97JC01298, 1997.
Dee, D. P., Uppala, S. M., Simmons, A. J., Berrisford, P., Poli, P.,
Kobayashi, S., and Vitart, F.: The ERA-Interim reanalysis: Configuration and
performance of the data assimilation system, Q. J. Roy. Meteor. Soc., 137, 553–597, https://doi.org/10.1002/qj.828, 2011.
Deer, F. R. S., Howie, R. A., and Zussman, J.: An Introduction to the
Rock-Forming Minerals, Longman, White Plains, New York, USA, 1993.
Devi, S., Bijaksana, S., Fajar, S. J., and Santoso, N. A.: Characterization
of Volcanic Ash From the 2017 Agung Eruption, Bali, Indonesia, IOP Conf.
Ser.: Earth Environ. Sci., 318, 012014, https://doi.org/10.1088/1755-1315/318/1/012014, 2019.
Donarummo, J., Ram, M., and Stoermer, E. F.: Possible deposit of soil dust
from the 1930's U.S. dust bowl identified in Greenland ice, Geophys. Res.
Lett., 30, 1269, https://doi.org/10.1029/2002GL016641, 2003.
Drab, E., Gaudichet, A., and Jaffrezo, J. L.: Mineral particles content in
recent snow at Summit (Greenland), Atmos. Environ., 36, 5365–5367,
https://doi.org/10.1016/S1352-2310(02)00470-3, 2002.
Eyring, V., Bony, S., Meehl, G. A., Senior, C. A., Stevens, B., Stouffer, R. J., and Taylor, K. E.: Overview of the Coupled Model Intercomparison Project Phase 6 (CMIP6) experimental design and organization, Geosci. Model Dev., 9, 1937–1958, https://doi.org/10.5194/gmd-9-1937-2016, 2016.
Faure, G. and Mensing, T. M.: Isotopes, Principles and Applications, John
Wiley & Sons, USA, 2004.
Fuhrer, K., Wolff, E. W., and Johnsen, S. J.: Timescales for dust
variability in the Greenland Ice Core Project (GRIP) ice core in the last
100,000 years, J. Geophys. Res., 104, 31043–31052, https://doi.org/10.1029/1999JD900929, 1999.
Genthon, C. and Armengaud, A.: GCM simulations of atmospheric tracers in the
polar latitudes: South Pole (Antarctica) and Summit (Greenland) cases, Sci.
Total Environ., 160–161, 101–116, https://doi.org/10.1016/0048-9697(95)04348-5, 1995.
Griffin, J. J., Windom, H., and Goldberg, E. D.: The distribution of clay
minerals in the world ocean, Deep-Sea. Res., 15, 433–459, https://doi.org/10.1016/0011-7471(68)90051-X, 1968.
Grumet, N. S., Wake, C. P., Zielinski, G., Fisher, D. A., Koerner, R. M.,
and Jacobs, J. D.: Preservation of glaciochemical time-series in snow and
ice from Penny Ice Cap, Baffin Island, Geophys. Res. Lett., 25, 357–360,
https://doi.org/10.1029/97GL03787, 1998.
Han, C., Hur, S. D., Han, Y., Lee, K. Hong, S., Erhardt, T., Fischer, H.,
Svensson, A. M., Steffensen, J. P., and Vallelonga, P.: High-resolution isotopic evidence for a potential Saharan provenance of Greenland glacial dust, Sci. Rep., 8, 15582, https://doi.org/10.1038/s41598-018-33859-0, 2018.
Hanna, E., Fettweis, X., Mernild, S. H., Cappelen, J., Ribergaard, M. H.,
Shuman, C. A., Steffen, K., Wood, L., and Mote, T. L.: Atmospheric and
oceanic climate forcing of the exceptional Greenland ice sheet surface melt
in summer 2012, Int. J. Climatol., 34, 1022–1037, https://doi.org/10.1002/joc.3743, 2014.
Harris, I. C.: CRU JRA v2.0: A forcings dataset of gridded land surface
blend of Climatic Research Unit (CRU) and Japanese reanalysis (JRA) data;
Jan.1901-Dec.2018, Centre for Environmental Data Analysis, available at:
https://catalogue.ceda.ac.uk/uuid/7f785c0e80aa4df2b39d068ce7351bbb (last access: 20 June 2020), 2019.
Hurrell, J. W: NAO Index Data provided by the Climate Analysis Section, NCAR, Boulder, USA, 2003, available at: https://climatedataguide.ucar.edu/climate-data/hurrell-north-atlantic-oscillation-nao-index-station-based, last access: 27 May 2021 (updated regularly).
Iizuka, Y., Uemura, R., Fujita, K., Hattori, S., Seki, O., Miyamoto, C.,
Suzuki, T., Yoshida, N., Motoyama, H., and Matoba, S.: A 60 year record of
atmospheric aerosol depositions preserved in a high-accumulation dome ice
core, Southeast Greenland, J. Geophys. Res., 123, 574–589,
https://doi.org/10.1002/2017JD026733, 2018.
Ito, A. and Wagai, R.: Global distribution of clay-size minerals on land
surface for biogeochemical and climatological studies, Sci. Data, 4,
170103, https://doi.org/10.1038/sdata.2017.103, 2017.
Kemp, S. J., Ellis, M. A., Mounteney, I., and Kender, S.: Palaeoclimatic
implications of high-resolution clay mineral assemblages preceding and
across the onset of the Palaeocene–Eocene thermal maximum, North Sea Basin,
Clay Miner., 51, 793–813, https://doi.org/10.1180/claymin.2016.051.5.08, 2016.
Kim, H.: Global Soil Wetness Project Phase 3 Atmospheric Boundary Conditions
(Experiment 1), Data Integration and Analysis System (DIAS) [data set],
https://doi.org/10.20783/DIAS.501, 2017.
Kobashi, T., Kawamura, K., Severinghaus, J. P., Barnola, J.-M., Nakaegawa,
T., Vinther, B. M., Johnsen, S. J., and Box, J. E.: High variability of
Greenland surface temperature over the past 4000 years estimated from
trapped air in an ice core, Geophys. Res. Lett., 38, L21501,
https://doi.org/10.1029/2011GL049444, 2011.
Koide, M., Michel, R., Goldberg, E., Herron, M. M., and Langway, C. C.:
Characterization of radioactive fallout from pre- and post-moratorium tests
to polar ice caps, Nature, 296, 544–547, https://doi.org/10.1038/296544a0, 1982.
Kuramoto, T., Goto-Azuma, K., Hirabayashi, M., Miyake, T., Motoyama, H.,
Dahl-Jensen, D., and Steffensen, J. P.: Seasonal variations of snow
chemistry at NEEM, Greenland, Ann. Glaciol., 52, 193–200,
https://doi.org/10.3189/172756411797252365, 2011.
Kurosaki, Y. and Mikami, M.: Recent frequent dust events and their relation
to surface wind in East Asia, Geophys. Res. Lett., 30, 1736,
https://doi.org/10.1029/2003GL017261, 2003.
Kurosaki, Y., Matoba, S., Iizuka, Y., Niwano, M., Tanikawa, T., Ando, T.,
Hori, A., Miyamoto, A., Fujita, S., and Aoki, T.: Reconstruction of sea ice
concentration in northern Baffin Bay using deuterium excess in a coastal ice
core from the northwestern Greenland Ice Sheet, J. Geophys. Res.-Atmos.,
125, e2019JD031668, https://doi.org/10.1029/2019JD031668, 2020.
Lambert, F., Delmonte, B., Petit, J. R., Bigler, M., Kaufmann, P. R.,
Hutterli, M. A., Stocker, T. F., Ruth, U., Steffensen, J. P., and Maggi, V.:
Dust-climate couplings over the past 800,000 years from the EPICA Dome C ice
core, Nature, 452, 616–619, https://doi.org/10.1038/nature06763, 2008.
Legrand, M. and Mayewski, P.: Glaciochemistry of polar ice cores: A review,
Rev. Geophys., 35, 219–243, https://doi.org/10.1029/96RG03527, 1997.
Lupker, M., Aciego, S. M., Bourdon, B., Schwander, J., and Stocker, T. F.:
Isotopic tracing (Sr, Nd, U and Hf) of continental and marine aerosols in an
18th century section of the Dye-3 ice core (Greenland), Earth Planet. Sc.
Lett., 295, 277–286, https://doi.org/10.1016/j.epsl.2010.04.010, 2010.
Maggi, V.: Mineralogy of atmospheric microparticles deposited along the
Greenland Ice Core Project ice core, J. Geophys. Res., 102, 26725–26734,
https://doi.org/10.1029/97JC00613, 1997.
Matoba, S., Narita, H., Motoyama, H., Kamiyama, K., and Watanabe, O.: Ice
core chemistry of Vestfonna Ice Cap in Svalbard, Norway, J. Geophys. Res.,
107, 4721, https://doi.org/10.1029/2002JD002205, 2002.
Matoba, S., Motoyama, H., Fujita, K., Yamasaki, T., Minowa, M., Onuma, Y.,
Komuro, Y., Aoki, T., Yamaguchi, S., Sugiyama, S., and Enomoto, H.:
Glaciological and meteorological observations at the SIGMA-D site,
northwestern Greenland Ice Sheet, Bull. Glaciol. Res., 33, 7–14, https://doi.org/10.5331/bgr.33.7, 2015.
Mayewski, P. A., Meeker, L. D., Twickler, M. S., Whitlow, S., Yang, Q.,
Lyons, W. B., and Prentice, M.: Major features and forcing of high-latitude
northern hemisphere atmospheric circulation using a 110,000-year-long
glaciochemical series, J. Geophys. Res., 102, 26345–26366,
https://doi.org/10.1029/96JC03365, 1997.
Mudroch, A., Zeman, A. J., and San, R.: Identification of mineral particles
in fine grained lacustrine sediments with transmission electron microscope
and x-ray energy dispersive spectroscopy, J. Sediment. Petrol., 47,
244–250, https://doi.org/10.1306/212F713F-2B24-11D7-8648000102C1865D, 1977.
Mueller, J. P. and Bocquier, G.: Dissolution of kaolinites and accumulation
of iron oxides in lateritic-ferruginous nodules: Mineralogical and
microstructural transformations, Geoderma, 37, 113–116,
https://doi.org/10.1016/0016-7061(86)90025-X, 1986.
Nagatsuka, N., Takeuchi, N., Uetake, J., and Shimada, R.: Mineralogical
composition of cryoconite on glaciers in northwest Greenland, Bull. Glaciol. Res., 32, 107–114, https://doi.org/10.5331/bgr.32.107, 2014.
Nagatsuka, N., Matoba, S., Kadota, M., Fujita, K., Tsushima, A., Dallmayr, R., Hirabayashi, M., Ogata, J., Ogawa-Tsukagawa, Y., and Goto-Azuma, K.: Stable isotope, ion concentrations, and mineral dust data from northwestern Greenland ice core (SIGMA-D), 1.00, Arctic Data archive System (ADS) [data set], Japan, https://doi.org/10.17592/001.2021052501, 2021.
Nahon, D. B.: Introduction to the Petrology of Soils and Chemical
Weathering, John Wiley, New York, 1991.
Onuma, Y. and Kim, H.: MIROC6 model output prepared for CMIP6 LS3MIP
land-hist, Version 20200423, Earth System Grid Federation [data set],
https://doi.org/10.22033/ESGF/CMIP6.5622, 2020a.
Onuma, Y. and Kim, H.: MIROC6 model output prepared for CMIP6 LS3MIP
land-hist-cruNcep, Version 20200918, Earth System Grid Federation [data set], https://doi.org/10.22033/ESGF/CMIP6.5627, 2020b.
Onuma, Y. and Kim, H.: MIROC6 model output prepared for CMIP6 LS3MIP
land-hist-princeton, Version 20200918, Earth System Grid Federation [data set], https://doi.org/10.22033/ESGF/CMIP6.5628, 2020c.
Onuma, Y. and Kim, H.: MIROC6 model output prepared for CMIP6 LS3MIP
land-hist-wfdei, Version 20200727, Earth System Grid Federation [data set], https://doi.org/10.22033/ESGF/CMIP6.5629, 2020d.
Oyabu, I., Matoba, S., Yamasaki, T., Kadota, M., and Iizuka, Y.: Seasonal
variations in the major chemical species of snow at the South East Dome in
Greenland, Polar Sci., 10, 36–42, https://doi.org/10.1016/j.polar.2016.01.003, 2016.
Pallister, J. S., Hoblitt, R. P., and Reyes, A. G.: A basalt trigger for the
1991 eruptions of Pinatubo volcano?, Nature, 356, 426–428,
https://doi.org/10.1038/356426a0, 1992.
Parvin, F., Seki, O. Fujita, K., Iizuka, Y., Matoba, S., and Ando, T.:
Assessment for paleoclimatic utility of biomass burning tracers in SE-Dome
ice core, Greenland, Atmos. Environ., 196, 86–94,
https://doi.org/10.1016/j.atmosenv.2018.10.012, 2019.
Petit, J. R., Mounier, L., Jouzel, J., Korotkevich, Y. S., Kotlyakov, V. I.,
and Lorius, C.: Palaeoclimatological and chronological implications of the
Vostok core dust record, Nature, 343, 56–58, https://doi.org/10.1038/343056a0, 1990.
Pye, K.: Aeolian Dust and Dust Deposits, Academic, San Diego, USA, 1987.
Ram, M. and Koenig, G.: Continuous dust concentration profile of
pre-Holocene ice from the Greenland Ice Sheet Project 2 ice core: Dust
stadials, interstadials and the Eemian, J. Geophys. Res., 102, 26641–26648,
https://doi.org/10.1029/96JC03548, 1997.
Ruth, U., Wagenbach, D., Steffensen, J. P., and Bigler, M.: Continuous
record of microparticle concentration and size distribution in the central
Greenland NGRIP ice core during the last glacial period, J. Geophys. Res.,
108, 4098, https://doi.org/10.1029/2002jd002376, 2003.
Schüpbach, S., Fischer, H., Bigler, M., Erhardt, T., Gfeller, G.,
Leuenberger, D., Mini, O., Mulvaney, R., Abram, N. J., Fleet, L., Frey, M.
M., Thomas, E., Svensson, A., Dahl-Jensen, D., Kettner, E., Kjaer, H.,
Seierstad, I., Steffensen, J. P., Rasmussen, S. O., Vallelonga, P.,
Winstrup, M., Wegner, A., Twarloh, B., Wolff, K., Schmidt, K., Goto-Azuma,
K., Kuramoto, T., Hirabayashi, M., Uetake, J., Zheng, J., Bourgeois, J.,
Fisher, D., Zhiheng, D., Xiao, C., Legrand, M., Spolaor, A., Gabrieli, J.,
Barbante, C., Kang, J.-H., Hur, S. D., Hong, S. B., Hwang, H. J., Hong, S.,
Hansson, M., Iizuka, Y., Oyabu, I., Muscheler, R., Adolphi, F., Maselli, O.,
McConnell J., and Wolff, E. W.: Greenland records of aerosol source and
atmospheric lifetime changes from the Eemian to the Holocene, Nat. Commun.,
9, 1476, https://doi.org/10.1038/s41467-018-03924-3, 2018.
Severin, K. P.: Energy dispersive spectrometry of common rock forming
minerals, Kluwer Academic Publishers, Dordrecht, the Netherlands, 2004.
Sheffield, J., Goteti, G., and Wood, E. F.: Development of a 50-Year
High-Resolution Global Dataset of Meteorological Forcings for Land Surface
Modeling, J. Climate, 19, 3088–3111, https://doi.org/10.1175/JCLI3790.1, 2006.
Simonsen, M. F., Baccolo, G., Blunier, T., Borunda, A., Delmonte, B., Frei,
R., Goldstein, S., Grinsted, A., Kjær, H. A., Sowers, T., Svensson, A.,
Vinther, B., Vladimirova, D., Winckler, G., Winstrup, M., and Vallelonga,
P.: East Greenland ice core dust record reveals timing of Greenland ice
sheet advance and retreat, Nat. Commun., 10, 4494,
https://doi.org/10.1038/s41467-019-12546-2, 2019.
Steffensen, J.: The size distribution of microparticles from selected
segments of the Greenland Ice Core Project ice core representing different
climatic periods, J. Geophys. Res., 102, 26755–26763, https://doi.org/10.1029/97JC01490, 1997.
Stein, A. F., Draxler, R. R., Rolph, G. D., Stunder, B. J. B., Cohen, M. D.,
and Ngan, F.: NOAA's HYSPLIT Atmospheric Transport and Dispersion Modeling
System, B. Am. Meteorol. Soc., 96, 2059–2077,
https://doi.org/10.1175/BAMS-D-14-00110.1, 2015.
Svensson, A., Biscaye, P. E., and Grousset, F. E.: Characterization of late
glacial continental dust in the greenland ice core project ice core, J.
Geophys. Res., 105, 4637–4656, https://doi.org/10.1029/1999JD901093, 2000.
Tatebe, H., Ogura, T., Nitta, T., Komuro, Y., Ogochi, K., Takemura, T., Sudo, K., Sekiguchi, M., Abe, M., Saito, F., Chikira, M., Watanabe, S., Mori, M., Hirota, N., Kawatani, Y., Mochizuki, T., Yoshimura, K., Takata, K., O'ishi, R., Yamazaki, D., Suzuki, T., Kurogi, M., Kataoka, T., Watanabe, M., and Kimoto, M.: Description and basic evaluation of simulated mean state, internal variability, and climate sensitivity in MIROC6, Geosci. Model Dev., 12, 2727–2765, https://doi.org/10.5194/gmd-12-2727-2019, 2019.
Taylor, H. E. and Lichte, F. E.: Chemical composition of Mount St. Helens
volcanic ash, Geophys. Res. Lett., 7, 949–952, https://doi.org/10.1029/GL007i011p00949, 1980.
Uppala, S. M., Kallberg, P. W., Simmons, A. J., Andrae, U., daCosta
Bechtold, V., Fiorino, M., Gibson, J. K., Haseler, J., Hernandez, A., Kelly,
G. A., Li, X., Onogi, K., Saarinen, S., Sokka, N., Allan, R. P., Andersson,
E., Arpe, K., Balmaseda, M. A., Beljaars, A. C. M., van de Berg, L., Bidlot,
J., Bormann, N., Caires, S., Chevallier, F., Dethof, A., Dragosavac, M.,
Fisher, M., Fuentes, M., Hagemann, S., Holm, E., Hoskins, B. J., Isaksen,
L., Janssen, P. A. E. M., Jenne, R., McNally, A. P., Mahfouf, J. F.,
Morcrette, J. J., Rayner, N. A., Saunders, R. W., Simon, P., Sterl, A.,
Trenberth, K. E., Untech, A., Vasiljevic, D., Viterbo, P., and Woollen, J.:
The ERA-40 Reanalysis, Q. J. Roy. Meteor. Soc., 131, 2961–3012,
https://doi.org/10.1256/qj.04.176, 2005.
Újvári, G., Stevens, T., Svensson, A., Klötzli, U. S., Manning, C., Németh, T., Kovaìcs, J., Sweeney, M. R., Gocke, M., Wiesenberg, G. L. B., Markovic, S. B., and Zech, M.: Two possible source regions for central
Greenland last glacial dust, Geophys. Res. Lett., 42, 10399–10408,
https://doi.org/10.1002/2015GL066153, 2015.
van den Broeke, M., Bamber, M. J., Ettema, J., Rignot, E., Schrama, E., van
de Berg, W. J., van Meijgaard, E., Velicogna, I., and Wouters, B.:
Partitioning recent Greenland mass loss, Science, 326, 984–986,
https://doi.org/10.1126/science.1178176, 2009.
van den Hurk, B., Kim, H., Krinner, G., Seneviratne, S. I., Derksen, C., Oki, T., Douville, H., Colin, J., Ducharne, A., Cheruy, F., Viovy, N., Puma, M. J., Wada, Y., Li, W., Jia, B., Alessandri, A., Lawrence, D. M., Weedon, G. P., Ellis, R., Hagemann, S., Mao, J., Flanner, M. G., Zampieri, M., Materia, S., Law, R. M., and Sheffield, J.: LS3MIP (v1.0) contribution to CMIP6: the Land Surface, Snow and Soil moisture Model Intercomparison Project – aims, setup and expected outcome, Geosci. Model Dev., 9, 2809–2832, https://doi.org/10.5194/gmd-9-2809-2016, 2016.
Velde, B.: Origin and Mineralogy of Clays: Clays and Environment,
Springer-Verlag, New York, 1995.
Weedon, G. P., Balsamo, G., Bellouin, N., Gomes, S., Best, M. J., and
Viterbo, P.: The WFDEI meteorological forcing data set: WATCH Forcing Data
methodology applied to ERA Interim reanalysis data, Water Resour. Res., 50,
7505–7514, https://doi.org/10.1002/2014WR015638, 2014.
Whitlow, S., Mayewski, P. A., and Dibb, J. E.: A comparison of major
chemical species seasonal concentration and accumulation at the South Pole
and Summit, Greenland, Atmos. Environ., 26A, 2045–2054,
https://doi.org/10.1016/0960-1686(92)90089-4, 1992.
Wilson, T. R. S.: Salinity and the major elements of sea water, Chap. 6, in:
Chemical Oceanography, 2nd edn., edited by: Riley, J. P. and Skirrow, G.,
Academic Press, Orland, 1, 365–413, 1975.
Woollings, T., Hannachi, A., Hoskins, B., and Turner, A.: A regime view of
the North Atlantic Oscillation and its response to anthropogenic forcing, J.
Climate, 23, 1291–1307, https://doi.org/10.1175/2009JCLI3087.1, 2010.
Wu, G., Zhang, X., Zhang, C., and Xu, T.: Mineralogical and morphological
properties of individual dust particles in ice cores from the Tibetan
Plateau, J. Glaciol., 62, 46–53, https://doi.org/10.1017/jog.2016.8, 2016.
Yokoo, Y., Nakano, T., Nishikawa, M., and Quan, H.: Mineralogical variation
of Sr—Nd isotopic and elemental compositions in loess and desert sand from
the central Loess Plateau in China as a provenance tracer of wet and dry
deposition in the northwestern Pacific, Chem. Geol., 204, 45–62,
https://doi.org/10.1016/j.chemgeo.2003.11.004, 2004.
Zhang, P., Jeong, J. H., Yoon, J. H., Kim, H., Wang, S. Y. S., Linderholm,
H. W., Fang, K., Wu, X., and Chen, D.: Abrupt shift to hotter and drier
climate over inner East Asia beyond the tipping point, Science, 370,
1095–1099, https://doi.org/10.1126/science.abb3368, 2020.
Short summary
Here we present a first high-temporal-resolution record of mineral composition in a Greenland ice core (SIGMA-D) over the past 100 years using SEM–EDS analysis. Our results show that the ice core dust composition varied on multi-decadal scales, which was likely affected by local temperature changes. We suggest that the ice core dust was constantly supplied from distant sources (mainly northern Canada) as well as local ice-free areas in warm periods (1915 to 1949 and 2005 to 2013).
Here we present a first high-temporal-resolution record of mineral composition in a Greenland...
