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401
Gravity‐Derived Antarctic Crustal Thickness Based on the Gauss‐FFT Method
Published 2022-08-01“…We compare the relationship between the Moho and Curie interfaces and find that the uppermost mantle is magnetized in some areas of East Antarctica, which may indicate preserved Precambrian cratonic roots.…”
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402
Snow accumulation variability derived from radar and firn core data along a 600 km transect in Adelie Land, East Antarctic plateau
Published 2012-11-01“…In the framework of the TASTE-IDEA (Trans-Antarctic Scientific Traverses Expeditions – Ice Divide of East Antarctica) program, an International Polar Year project, continuous ground penetrating radar (GPR) measurements were carried out during a traverse in Adelie Land (East Antarctica) during the 2008–2009 austral summer between the Italian–French Dome C (DC) polar plateau site and French Dumont D'Urville (DdU) coastal station. …”
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403
Change and variability in East antarctic sea ice seasonality, 1979/80-2009/10.
Published 2013-01-01“…The pattern of change in sea ice seasonality off East Antarctica comprises mixed signals on regional to local scales, with pockets of strongly positive and negative trends occurring in near juxtaposition in certain regions e.g., Prydz Bay. …”
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404
Summary of Glaciological Studies in Mizuho Plateau (Special Issue of the Proceedings of the First Symposium on Antarctic Meteorology and Glaciology)
Published 1979-10-01“…A summary report of the traverse glaciology proiect accomplished by the Japanese Antarctic Research Expedition in 1969-1975 was published in 1978 under the title of "Glaciological Studies in Mizuho Plateau, East Antarctica, 1969- 1975" as a special issue of Memoirs of National Institute of Polar Research, No 7 This paper outlines the abovementioned summary report…”
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405
A Steam-Operated Drill Used by the 14th Japanese Antarctic Research Expedition (1972-1974)
Published 1975-08-01“…HODGE was used to measure 10m snow temperature at Mizuho Plateau, East Antarctica, in 1973/74. The average drilling time for firn was 22 min (depth 10m, diameter 3cm, firn temperature about -20℃).…”
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406
Estimation of present-day glacial isostatic adjustment, ice mass change and elastic vertical crustal deformation over the Antarctic ice sheet
Published 2017-08-01“…The inferred GIA shows that the strongest uplift is found in the Amundsen Sea Embayment (ASE) sector and subsidence mostly occurs in Adelie Terre and the East Antarctica inland. The total GIA-related mass change estimates for the entire AIS, West Antarctica Ice Sheet (WAIS), East Antarctica Ice Sheet (EAIS), and Antarctic Peninsula Ice Sheet (APIS) are 43 ± 38, 53 ± 24, −23 ± 29 and 13 ± 6 Gt a−1, respectively. …”
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407
ANTASed – An Updated Sediment Model for Antarctica
Published 2021-08-01“…West Antarctica has wide sedimentary basins: the Ross basin (thickness 2–6 km), the Filchner-Ronne basin (2–12 km) with continuations into East Antarctica, the Bentley Subglacial Trench and the Byrd basin (2–4 km). …”
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408
Sea-level response to melting of Antarctic ice shelves on multi-centennial timescales with the fast Elementary Thermomechanical Ice Sheet model (f.ETISh v1.0)
Published 2017-08-01“…Coulomb friction in the grounding-line transition zone leads to significantly higher mass loss in both West and East Antarctica on centennial timescales, leading to 1.5 m sea-level rise after 500 years for a limited melt scenario of 10 m a<sup>−1</sup> under freely floating ice shelves, up to 6 m for a 50 m a<sup>−1</sup> scenario. …”
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409
Magnetotelluric investigation of lithospheric electrical structure beneath the Dharwar Craton in south India: Evidence for mantle suture and plume-continental interaction
Published 2019-09-01“…A west-verging moderately conductive feature imaged beneath EGMB lithosphere is interpreted as the remnant of the Proterozoic collision process between the Indian land mass and East Antarctica. Thin (∼120 km) lithosphere is seen below the EGMB, which form the exterior margin of the India shield subsequent to its separation from East Antarctica through rifting and opening of the Indian Ocean in the Cretaceous. …”
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410
An Assessment of ERA5 Reanalysis for Antarctic Near-Surface Air Temperature
Published 2021-02-01“…The performance of ERA5 shows regional differences, and the correlations are high in West Antarctica and low in East Antarctica. Compared with ERA5, ERA-Interim has a slightly higher linear relationship with observations in the Antarctic Peninsula. …”
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411
Upper crustal structure of Soya Coast, Antarctica, revealed by explosion seismology
Published 1981-01-01“…A surface thin layer with a P-wave velocity of 4-5km/s was derived from the traveltime analysis for the first time in East Antarctica by explosion seismology.…”
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412
Bare ice fields developed in the inland part of the Antarctic ice sheet
Published 1997-03-01“…Observations of a bare ice field were carried out at Seal Rock in the Sor Rondane area, East Antarctica. A large sublimation rate, 200 to 280mm/a, was observed on the bare ice field. …”
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413
Ice mass loss sensitivity to the Antarctic ice sheet basal thermal state
Published 2022-09-01“…This study uses ice sheet modeling experiments to show that thawing portions of the Antarctic ice sheet bed can increase century-scale mass loss, particularly in the Wilkes and Enderby Land regions of East Antarctica.…”
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414
A newly developed snow vehicle (SM100S) for Antarctica V. Result of general performance tests
Published 1992-11-01“…This paper describes the results of the fundamental and the general performance tests for a newly developed snow vehicle, which will be used for the deep ice coring project at Dome Fuji, East Antarctica. The result of the tests showed that the vehicle generally satisfied the expected performance and the purpose of the systems design, but was partially unsatisfactory in its structure. …”
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415
Evaluation of the geoid based on the SEASAT altimetry data at sea around Antarctica
Published 1982-09-01“…However, some significant features such as geoid depressions at the Ross Sea and the Weddell Sea or the regional geoid upheavals over the Indian Ocean off East Antarctica have been clearly displayed.…”
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416
ICE FLOW VELOCITY MAPPING IN GREENLAND USING HISTORICAL IMAGES FROM 1960s TO 1980s: SCHEME DESIGN
Published 2022-05-01“…We proposed three methods, including parallax decomposition, grid-based NCC image matching, feature and gird-based image matching with constraints for estimation of surface velocity in East Antarctica based on ARGON KH-5 and LANDSAT imagery, and a systematic compilation method for the ice surface velocity in East Antarctica from the 1960s to 1980s. …”
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417
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418
Spatial link between Adélie penguin foraging effort and krill swarm abundance and distribution
Published 2023-01-01“…Our work substantially improves understanding of penguin-krill dynamics in East Antarctica and provides a greater level of nuance regarding the utility of Adélie penguins as indicator species under CCAMLR’s Ecosystem Monitoring Programme (CEMP). …”
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419
Large-scale population assessment informs conservation management for seabirds in Antarctica and the Southern Ocean: A case study of Adélie penguins
Published 2017-01-01“…The 16 Antarctic Specially Protected Areas currently designated in East Antarctica offer protection to breeding populations close to stations in four of six regional populations. …”
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420
A synoptic bridge linking sea salt aerosol concentrations in East Antarctic snowfall to Australian rainfall
Published 2022-08-01“…Rainfall in subtropical Australia and sea salt deposited in snowfall at the Law Dome ice core site in East Antarctica are linked through a synoptic weather pattern that bridges the two regions, according to a synoptic typing data analysis.…”
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