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Liu H, Zheng W, Gao Y, Yang L, Yue F, Huang T, Xie Z. Increased Contribution of Circumpolar Deep Water Upwelling to Methylmercury in the Upper Ocean around Antarctica: Evidence from Mercury Isotopes in the Ornithogenic Sediments. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2024; 58:2762-2773. [PMID: 38294849 DOI: 10.1021/acs.est.3c06923] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 02/01/2024]
Abstract
Upwelling plays a pivotal role in supplying methylmercury (MeHg) to the upper oceans, contributing to the bioaccumulation of MeHg in the marine food web. However, the influence of the upwelling of Circumpolar Deep Water (CDW), the most voluminous water mass in the Southern Ocean, on the MeHg cycle in the surrounding oceans and marine biota of Antarctica remains unclear. Here, we study the mercury (Hg) isotopes in an ornithogenic sedimentary profile strongly influenced by penguin activity on Ross Island, Antarctica. Results indicate that penguin guano is the primary source of Hg in the sediments, and the mass-independent isotope fractionation of Hg (represented by Δ199Hg) can provide insights on the source of marine MeHg accumulated by penguin. The Δ199Hg in the sediments shows a significant decrease at ∼1550 CE, which is primarily attributed to the enhanced upwelling of CDW that brought more MeHg with lower Δ199Hg from the deeper seawater to the upper ocean. We estimate that the contribution of MeHg from the deeper seawater may reach more than 38% in order to explain the decline in Δ199Hg at ∼1550 CE. Moreover, we found that the intensified upwelling may have increased the MeHg exposure for marine organisms, highlighting the importance of CDW upwelling on the MeHg cycle in Antarctic coastal ecosystems.
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Affiliation(s)
- Hongwei Liu
- Department of Environmental Science and Engineering, Anhui Key Laboratory of Polar Environment and Global Change, University of Science and Technology of China, Hefei, Anhui 230026, China
| | - Wang Zheng
- Institute of Surface-Earth System Science, School of Earth System Science, Tianjin University, Tianjin 300072, China
- School of Earth and Space Exploration, Arizona State University, Tempe, Arizona 85287, United States
| | - Yuesong Gao
- Department of Environmental Science and Engineering, Anhui Key Laboratory of Polar Environment and Global Change, University of Science and Technology of China, Hefei, Anhui 230026, China
| | - Lianjiao Yang
- Department of Environmental Science and Engineering, Anhui Key Laboratory of Polar Environment and Global Change, University of Science and Technology of China, Hefei, Anhui 230026, China
| | - Fange Yue
- Department of Environmental Science and Engineering, Anhui Key Laboratory of Polar Environment and Global Change, University of Science and Technology of China, Hefei, Anhui 230026, China
| | - Tao Huang
- School of Resources and Environmental Engineering, Anhui University, Hefei, Anhui 230601, China
| | - Zhouqing Xie
- Department of Environmental Science and Engineering, Anhui Key Laboratory of Polar Environment and Global Change, University of Science and Technology of China, Hefei, Anhui 230026, China
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Volcanic Fluxes Over the Last Millennium as Recorded in the Gv7 Ice Core (Northern Victoria Land, Antarctica). GEOSCIENCES 2020. [DOI: 10.3390/geosciences10010038] [Citation(s) in RCA: 8] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 11/16/2022]
Abstract
Major explosive volcanic eruptions may significantly alter the global atmosphere for about 2–3 years. During that period, volcanic products (mainly H2SO4) with high residence time, stored in the stratosphere or, for shorter times, in the troposphere are gradually deposited onto polar ice caps. Antarctic snow may thus record acidic signals providing a history of past volcanic events. The high resolution sulphate concentration profile along a 197 m long ice core drilled at GV7 (Northern Victoria land) was obtained by Ion Chromatography on around 3500 discrete samples. The relatively high accumulation rate (241 ± 13 mm we yr −1) and the 5-cm sampling resolution allowed a preliminary counted age scale. The obtained stratigraphy covers roughly the last millennium and 24 major volcanic eruptions were identified, dated, and tentatively ascribed to a source volcano. The deposition flux of volcanic sulphate was calculated for each signature and the results were compared with data from other Antarctic ice cores at regional and continental scale. Our results show that the regional variability is of the same order of magnitude as the continental one.
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Lenaerts JTM, Medley B, van den Broeke MR, Wouters B. Observing and Modeling Ice Sheet Surface Mass Balance. REVIEWS OF GEOPHYSICS (WASHINGTON, D.C. : 1985) 2019; 57:376-420. [PMID: 31598609 PMCID: PMC6774314 DOI: 10.1029/2018rg000622] [Citation(s) in RCA: 5] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Subscribe] [Scholar Register] [Received: 11/13/2018] [Revised: 03/17/2019] [Accepted: 03/19/2019] [Indexed: 06/10/2023]
Abstract
Surface mass balance (SMB) provides mass input to the surface of the Antarctic and Greenland Ice Sheets and therefore comprises an important control on ice sheet mass balance and resulting contribution to global sea level change. As ice sheet SMB varies highly across multiple scales of space (meters to hundreds of kilometers) and time (hourly to decadal), it is notoriously challenging to observe and represent in models. In addition, SMB consists of multiple components, all of which depend on complex interactions between the atmosphere and the snow/ice surface, large-scale atmospheric circulation and ocean conditions, and ice sheet topography. In this review, we present the state-of-the-art knowledge and recent advances in ice sheet SMB observations and models, highlight current shortcomings, and propose future directions. Novel observational methods allow mapping SMB across larger areas, longer time periods, and/or at very high (subdaily) temporal frequency. As a recent observational breakthrough, cosmic ray counters provide direct estimates of SMB, circumventing the need for accurate snow density observations upon which many other techniques rely. Regional atmospheric climate models have drastically improved their simulation of ice sheet SMB in the last decade, thanks to the inclusion or improved representation of essential processes (e.g., clouds, blowing snow, and snow albedo), and by enhancing horizontal resolution (5-30 km). Future modeling efforts are required in improving Earth system models to match regional atmospheric climate model performance in simulating ice sheet SMB, and in reinforcing the efforts in developing statistical and dynamic downscaling to represent smaller-scale SMB processes.
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Affiliation(s)
- Jan T. M. Lenaerts
- Department of Atmospheric and Oceanic SciencesUniversity of Colorado BoulderBoulderCOUSA
| | - Brooke Medley
- Cryospheric Sciences LaboratoryNASA GSFCGoddardMDUSA
| | | | - Bert Wouters
- Institute for Marine and Atmospheric ResearchUtrecht UniversityUtrechtThe Netherlands
- Faculty of Civil Engineering and GeosciencesDelft University of TechnologyDelftThe Netherlands
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Caiazzo L, Baccolo G, Barbante C, Becagli S, Bertò M, Ciardini V, Crotti I, Delmonte B, Dreossi G, Frezzotti M, Gabrieli J, Giardi F, Han Y, Hong SB, Hur SD, Hwang H, Kang JH, Narcisi B, Proposito M, Scarchilli C, Selmo E, Severi M, Spolaor A, Stenni B, Traversi R, Udisti R. Prominent features in isotopic, chemical and dust stratigraphies from coastal East Antarctic ice sheet (Eastern Wilkes Land). CHEMOSPHERE 2017; 176:273-287. [PMID: 28273535 DOI: 10.1016/j.chemosphere.2017.02.115] [Citation(s) in RCA: 4] [Impact Index Per Article: 0.6] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 10/10/2016] [Revised: 02/17/2017] [Accepted: 02/22/2017] [Indexed: 06/06/2023]
Abstract
In this work we present the isotopic, chemical and dust stratigraphies of two snow pits sampled in 2013/14 at GV7 (coastal East Antarctica: 70°41' S - 158°51' E, 1950 m a.s.l.). A large number of chemical species are measured aiming to study their potentiality as environmental changes markers. Seasonal cluster backward trajectories analysis was performed and compared with chemical marker stratigraphies. Sea spray aerosol is delivered to the sampling site together with snow precipitation especially in autumn-winter by air masses arising from Western Pacific Ocean sector. Dust show maximum concentration in spring when the air masses arising from Ross Sea sector mobilize mineral dust from ice-free areas of the Transantarctic mountains. The clear seasonal pattern of sulfur oxidized compounds allows the dating of the snow-pit and the calculation of the mean accumulation rate, which is 242 ± 71 mm w.e. for the period 2008-2013. Methanesulfonic acid and NO3- do not show any concentration decreasing trend as depth increases, also considering a 12 m firn core record. Therefore these two compounds are not affected by post-depositional processes at this site and can be considered reliable markers for past environmental changes reconstruction. The rBC snow-pit record shows the highest values in summer 2012 likely related to large biomass burning even occurred in Australia in this summer. The undisturbed accumulation rate for this site is demonstrated by the agreement between the chemical stratigraphies and the annual accumulation rate of the two snow-pits analysed in Italian and Korean laboratories.
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Affiliation(s)
- L Caiazzo
- Dept. of Chemistry "Ugo Schiff", University of Florence, Via della Lastruccia, 3, 50019 Sesto F.no (Florence), Italy
| | - G Baccolo
- DISAT-University Milano-Bicocca, Piazza della Scienza, 1, 20126 Milano, Italy; University of Siena, Earth Science Department, Via Laterino, 8, 53100 Siena, Italy
| | - C Barbante
- Institute for the Dynamics of Environmental Processes-CNR, Via Torino, 155, 30172 Venice-Mestre, Italy; DAIS, Ca' Foscari University of Venice, Via Torino, 155, Venice-Mestre, Italy
| | - S Becagli
- Dept. of Chemistry "Ugo Schiff", University of Florence, Via della Lastruccia, 3, 50019 Sesto F.no (Florence), Italy.
| | - M Bertò
- DAIS, Ca' Foscari University of Venice, Via Torino, 155, Venice-Mestre, Italy
| | - V Ciardini
- Laboratory for Earth Observations and Analyses, ENEA - C.R. Casaccia, I-00123 Rome, Italy
| | - I Crotti
- DISAT-University Milano-Bicocca, Piazza della Scienza, 1, 20126 Milano, Italy
| | - B Delmonte
- DISAT-University Milano-Bicocca, Piazza della Scienza, 1, 20126 Milano, Italy
| | - G Dreossi
- DAIS, Ca' Foscari University of Venice, Via Torino, 155, Venice-Mestre, Italy
| | - M Frezzotti
- Laboratory for Earth Observations and Analyses, ENEA - C.R. Casaccia, I-00123 Rome, Italy
| | - J Gabrieli
- DAIS, Ca' Foscari University of Venice, Via Torino, 155, Venice-Mestre, Italy
| | - F Giardi
- Dept. of Chemistry "Ugo Schiff", University of Florence, Via della Lastruccia, 3, 50019 Sesto F.no (Florence), Italy
| | - Y Han
- Korea Polar Research Institute (KOPRI), 26 Songdomirearo, Yeonsu-gu, Incheon 21990, Republic of Korea
| | - S-B Hong
- Korea Polar Research Institute (KOPRI), 26 Songdomirearo, Yeonsu-gu, Incheon 21990, Republic of Korea
| | - S D Hur
- Korea Polar Research Institute (KOPRI), 26 Songdomirearo, Yeonsu-gu, Incheon 21990, Republic of Korea
| | - H Hwang
- Korea Polar Research Institute (KOPRI), 26 Songdomirearo, Yeonsu-gu, Incheon 21990, Republic of Korea
| | - J-H Kang
- Korea Polar Research Institute (KOPRI), 26 Songdomirearo, Yeonsu-gu, Incheon 21990, Republic of Korea
| | - B Narcisi
- Laboratory for Earth Observations and Analyses, ENEA - C.R. Casaccia, I-00123 Rome, Italy
| | - M Proposito
- Laboratory for Earth Observations and Analyses, ENEA - C.R. Casaccia, I-00123 Rome, Italy
| | - C Scarchilli
- Laboratory for Earth Observations and Analyses, ENEA - C.R. Casaccia, I-00123 Rome, Italy
| | - E Selmo
- Department of Chemistry, Life Sciences and Environmental Sustainability, University of Parma, Parco Area delle Scienze, 11/A, Parma, Italy
| | - M Severi
- Dept. of Chemistry "Ugo Schiff", University of Florence, Via della Lastruccia, 3, 50019 Sesto F.no (Florence), Italy
| | - A Spolaor
- Institute for the Dynamics of Environmental Processes-CNR, Via Torino, 155, 30172 Venice-Mestre, Italy; DAIS, Ca' Foscari University of Venice, Via Torino, 155, Venice-Mestre, Italy
| | - B Stenni
- DAIS, Ca' Foscari University of Venice, Via Torino, 155, Venice-Mestre, Italy
| | - R Traversi
- Dept. of Chemistry "Ugo Schiff", University of Florence, Via della Lastruccia, 3, 50019 Sesto F.no (Florence), Italy
| | - R Udisti
- Dept. of Chemistry "Ugo Schiff", University of Florence, Via della Lastruccia, 3, 50019 Sesto F.no (Florence), Italy; ISAC CNR, Via Gobetti 101, 40129, Bologna, Italy
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Severi M, Becagli S, Caiazzo L, Ciardini V, Colizza E, Giardi F, Mezgec K, Scarchilli C, Stenni B, Thomas ER, Traversi R, Udisti R. Sea salt sodium record from Talos Dome (East Antarctica) as a potential proxy of the Antarctic past sea ice extent. CHEMOSPHERE 2017; 177:266-274. [PMID: 28314231 DOI: 10.1016/j.chemosphere.2017.03.025] [Citation(s) in RCA: 3] [Impact Index Per Article: 0.4] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 10/07/2016] [Revised: 02/17/2017] [Accepted: 03/07/2017] [Indexed: 06/06/2023]
Abstract
Antarctic sea ice has shown an increasing trend in recent decades, but with strong regional differences from one sector to another of the Southern Ocean. The Ross Sea and the Indian sectors have seen an increase in sea ice during the satellite era (1979 onwards). Here we present a record of ssNa+ flux in the Talos Dome region during a 25-year period spanning from 1979 to 2003, showing that this marker could be used as a potential proxy for reconstructing the sea ice extent in the Ross Sea and Western Pacific Ocean at least for recent decades. After finding a positive relationship between the maxima in sea ice extent for a 25-year period, we used this relationship in the TALDICE record in order to reconstruct the sea ice conditions over the 20th century. Our tentative reconstruction highlighted a decline in the sea ice extent (SIE) starting in the 1950s and pointed out a higher variability of SIE starting from the 1960s and that the largest sea ice extents of the last century occurred during the 1990s.
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Affiliation(s)
- M Severi
- University of Florence, Chemistry Dept. "Ugo Schiff", Via della Lastruccia, 3, 50019, Sesto Fiorentino, FI, Italy.
| | - S Becagli
- University of Florence, Chemistry Dept. "Ugo Schiff", Via della Lastruccia, 3, 50019, Sesto Fiorentino, FI, Italy
| | - L Caiazzo
- University of Florence, Chemistry Dept. "Ugo Schiff", Via della Lastruccia, 3, 50019, Sesto Fiorentino, FI, Italy
| | - V Ciardini
- Laboratory for Earth Observations and Analyses, ENEA, Rome, Italy
| | - E Colizza
- Department of Mathematics and Geosciences, University of Trieste, Trieste, Italy
| | - F Giardi
- University of Florence, Chemistry Dept. "Ugo Schiff", Via della Lastruccia, 3, 50019, Sesto Fiorentino, FI, Italy
| | - K Mezgec
- Department of Mathematics and Geosciences, University of Trieste, Trieste, Italy
| | - C Scarchilli
- Laboratory for Earth Observations and Analyses, ENEA, Rome, Italy
| | - B Stenni
- Department of Environmental Sciences, Informatics and Statistics, "Ca' Foscari" University of Venice, Italy
| | | | - R Traversi
- University of Florence, Chemistry Dept. "Ugo Schiff", Via della Lastruccia, 3, 50019, Sesto Fiorentino, FI, Italy
| | - R Udisti
- University of Florence, Chemistry Dept. "Ugo Schiff", Via della Lastruccia, 3, 50019, Sesto Fiorentino, FI, Italy; ISAC CNR, Via Gobetti 101, 40129, Bologna, Italy
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Caiazzo L, Becagli S, Frosini D, Giardi F, Severi M, Traversi R, Udisti R. Spatial and temporal variability of snow chemical composition and accumulation rate at Talos Dome site (East Antarctica). THE SCIENCE OF THE TOTAL ENVIRONMENT 2016; 550:418-430. [PMID: 26849319 DOI: 10.1016/j.scitotenv.2016.01.087] [Citation(s) in RCA: 3] [Impact Index Per Article: 0.4] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 10/16/2015] [Revised: 01/13/2016] [Accepted: 01/14/2016] [Indexed: 06/05/2023]
Abstract
Five snow pits and five firn cores were sampled during the 2003-2004 Italian Antarctic Campaign at Talos Dome (East Antarctica), where a deep ice core (TALDICE, TALos Dome Ice CorE, 1650m depth) was drilled in 2005-2008 and analyzed for ionic content. Particular attention is spent in applying decontamination procedures to the firn cores, as core sections were stored for approximately 10years before analysis. By considering the snow pit samples to be unperturbed, the comparison with firn core samples from the same location shows that ammonium, nitrate and MSA are affected by storage post-depositional losses. All the other measured ions are confirmed to be irreversibly deposited in the snow layer. The removal of the most external layers (few centimeters) from the firn core sections is proved to be an effective decontamination procedure. High-resolution profiles of seasonal markers (nitrate, sulfate and MSA) allow a reliable stratigraphic dating and a seasonal characterization of the samples. The calculated mean accumulation-rate values range from 70 to 85mmw.e.year(-1), in the period 2003-1973 with small differences between two sectors: 70-74mmw.e.year(-1) in the NNE sector (spanning 2003-1996years) and 81-92mmw.e.year(-1) in the SSW sector (spanning 2003-1980years). This evidence is interpreted as a coupled effect of wind-driven redistribution processes in accumulation/ablation areas. Statistical treatment applied to the concentration values of the snow pits and firn cores samples collected in different points reveals a larger temporal variability than spatial one both in terms of concentration of chemical markers and annual accumulation. The low spatial variability of the accumulation rate and chemical composition measured in the five sites demonstrates that the TALDICE ice core paleo-environmental and paleo-climatic stratigraphies can be considered as reliably representative for the Talos Dome area.
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Affiliation(s)
- Laura Caiazzo
- Department of Chemistry "Ugo Schiff", Via della Lastruccia 3, I-50019, Sesto F.no (Florence), Italy
| | - Silvia Becagli
- Department of Chemistry "Ugo Schiff", Via della Lastruccia 3, I-50019, Sesto F.no (Florence), Italy
| | - Daniele Frosini
- Department of Chemistry "Ugo Schiff", Via della Lastruccia 3, I-50019, Sesto F.no (Florence), Italy
| | - Fabio Giardi
- Department of Chemistry "Ugo Schiff", Via della Lastruccia 3, I-50019, Sesto F.no (Florence), Italy
| | - Mirko Severi
- Department of Chemistry "Ugo Schiff", Via della Lastruccia 3, I-50019, Sesto F.no (Florence), Italy
| | - Rita Traversi
- Department of Chemistry "Ugo Schiff", Via della Lastruccia 3, I-50019, Sesto F.no (Florence), Italy.
| | - Roberto Udisti
- Department of Chemistry "Ugo Schiff", Via della Lastruccia 3, I-50019, Sesto F.no (Florence), Italy
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Schlosser E, Anschütz H, Divine D, Martma T, Sinisalo A, Altnau S, Isaksson E. Recent climate tendencies on an East Antarctic ice shelf inferred from a shallow firn core network. JOURNAL OF GEOPHYSICAL RESEARCH. ATMOSPHERES : JGR 2014; 119:6549-6562. [PMID: 25821663 PMCID: PMC4370759 DOI: 10.1002/2013jd020818] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Subscribe] [Scholar Register] [Received: 09/03/2013] [Accepted: 05/20/2014] [Indexed: 06/04/2023]
Abstract
UNLABELLED Nearly three decades of stable isotope ratios and surface mass balance (SMB) data from eight shallow firn cores retrieved at Fimbul Ice Shelf, East Antarctica, in the Austral summers 2009-2011 have been investigated. An additional longer core drilled in 2000/2001 extends the series back to the early eighteenth century. Isotope ratios and SMB from the stacked record of all cores were also related to instrumental temperature data from Neumayer Station on Ekström Ice Shelf. Since the second half of the twentieth century, the SMB shows a statistically significant negative trend, whereas the δ18O of the cores shows a significant positive trend. No trend is found in air temperature at the nearest suitable weather station, Neumayer (available since 1981). This does not correspond to the statistically significant positive trend in Southern Annular Mode (SAM) index, which is usually associated with a cooling of East Antarctica. SAM index and SMB are negatively correlated, which might be explained by a decrease in meridional exchange of energy and moisture leading to lower precipitation amounts. Future monitoring of climate change on the sensitive Antarctic ice shelves is necessary to assess its consequences for sea level change. KEY POINTS Mass balance and stable oxygen isotope ratios from shallow firn coresDecreasing trend in surface mass balance, no trend in stable isotopesNegative correlation between SAM and SMB.
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Affiliation(s)
- E Schlosser
- Institute of Meteorology and Geophysics, University of Innsbruck Innsbruck, Austria
| | | | - D Divine
- Norwegian Polar Institute, Fram Centre Tromsø, Norway
| | - T Martma
- Institute of Geology, Tallinn University of Technology Tallinn, Estonia
| | - A Sinisalo
- Department of Geosciences, University of Oslo Oslo, Norway
| | - S Altnau
- Institute of Meteorology and Geophysics, University of Innsbruck Innsbruck, Austria
| | - E Isaksson
- Norwegian Polar Institute, Fram Centre Tromsø, Norway
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Frezzotti M, Orombelli G. Glaciers and ice sheets: current status and trends. RENDICONTI LINCEI 2013. [DOI: 10.1007/s12210-013-0255-z] [Citation(s) in RCA: 5] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 11/28/2022]
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Lenaerts JTM, van den Broeke MR, Déry SJ, van Meijgaard E, van de Berg WJ, Palm SP, Sanz Rodrigo J. Modeling drifting snow in Antarctica with a regional climate model: 1. Methods and model evaluation. ACTA ACUST UNITED AC 2012. [DOI: 10.1029/2011jd016145] [Citation(s) in RCA: 71] [Impact Index Per Article: 5.9] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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Lenaerts JTM, van den Broeke MR. Modeling drifting snow in Antarctica with a regional climate model: 2. Results. ACTA ACUST UNITED AC 2012. [DOI: 10.1029/2010jd015419] [Citation(s) in RCA: 31] [Impact Index Per Article: 2.6] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/10/2022]
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Anschütz H, Sinisalo A, Isaksson E, McConnell JR, Hamran SE, Bisiaux MM, Pasteris D, Neumann TA, Winther JG. Variation of accumulation rates over the last eight centuries on the East Antarctic Plateau derived from volcanic signals in ice cores. ACTA ACUST UNITED AC 2011. [DOI: 10.1029/2011jd015753] [Citation(s) in RCA: 27] [Impact Index Per Article: 2.1] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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Anschütz H, Müller K, Isaksson E, McConnell JR, Fischer H, Miller H, Albert M, Winther JG. Revisiting sites of the South Pole Queen Maud Land Traverses in East Antarctica: Accumulation data from shallow firn cores. ACTA ACUST UNITED AC 2009. [DOI: 10.1029/2009jd012204] [Citation(s) in RCA: 22] [Impact Index Per Article: 1.5] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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