Publications

2137 to 2148 of 14011 results

1. Commercial fishery disturbance of the global ocean biological carbon sink

   Plankton drive a major sink of carbon across the global oceans. Dead plankton, their faeces and the faeces of plankton feeders, form a huge rain of carbon sinking to the […]

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2. Vision transformers and techniques for improving solar wind speed forecasts using solar EUV images

   Extreme-ultraviolet images taken by the Atmospheric Imaging Assembly make it possible to use deep vision techniques in the prediction of solar wind speed – a difficult, high-impact, and unsolved problem. […]

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3. Supervised classification of slush and ponded water on Antarctic ice shelves using Landsat 8 imagery

   Surface meltwater is becoming increasingly widespread on Antarctic ice shelves. It is stored within surface ponds and streams, or within firn pore spaces, which may saturate to form slush. Slush […]

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4. Summer variability of the atmospheric NO2 :  NO ratio at Dome C on the East Antarctic Plateau

   Previous Antarctic summer campaigns have shown unexpectedly high levels of oxidants in the lower atmosphere of the continental plateau and at coastal regions, with atmospheric hydroxyl radical (OH) concentrations up […]

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5. Landfast ice controls on turbulence in Antarctic coastal seas

   Knowledge of the ocean surface layer beneath Antarctic landfast ice is sparse. In this article surface layer turbulent and fine structure are quantified with and without landfast ice in the […]

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6. Antarctic Ice Sheet changes since the Last Glacial Maximum

   Technological advances in the study and dating of both land and marine glacial geologic features, combined with both glaciological and post-glacial isostatic rebound modelling, have developed knowledge and understanding of […]

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7. Antarctic environmental change and ice sheet evolution through the Miocene to Pliocene – a perspective from the Ross Sea and George V to Wilkes Land Coasts

   The Miocene to Pliocene (Neogene) occurred between 23.04 and 2.58 million years ago and includes intervals of peak global warmth where Earth’s average surface temperature was up to 8℃ warmer […]

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8. The Eocene-Oligocene boundary climate transition: an Antarctic perspective

   Antarctica underwent a complex evolution over the course of the Cenozoic, which influenced the history of the Earth’s climate system. The Eocene-Oligocene boundary is a divide of this history when […]

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9. Cenozoic history of Antarctic glaciation and climate from onshore and offshore studies

   The past three decades have seen a sustained and coordinated effort to refine the seismic stratigraphic framework of the Antarctic margin that has underpinned the development of numerous geological drilling […]

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10. Past Antarctic ice sheet dynamics (PAIS) and implications for future sea-level change

    The legacy of the Scientific Committee on Antarctic Research’s (SCAR) PAIS strategic research programme includes not only breakthrough scientific discoveries, but it is also the story of a long-standing deep […]

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11. Radar observations of winds, waves and tides in the mesosphere and lower thermosphere over South Georgia island (54° S, 36° W) and comparison with WACCM simulations

    The mesosphere and lower thermosphere (MLT) is a dynamic layer of the earth’s atmosphere. This region marks the interface at which neutral atmosphere dynamics begin to influence the ionosphere and […]

    Read more of: Radar observations of winds, waves and tides in the mesosphere and lower thermosphere over South Georgia island (54° S, 36° W) and comparison with WACCM simulations

12. Under pressure: Nanoplastics as a further stressor for sub-Antarctic pteropods already tackling ocean acidification [Short communication]

    In the Southern Ocean (SO), plastic debris has already been found in waters and sediments. Nanoplastics (

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