Publications

10777 to 10788 of 13949 results

1. The unknown and the uncertain in Earth system modeling

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2. Oceanographic conditions beneath Ronne Ice Shelf: a comparison between model and field data

   Within the cavity beneath Filchner-Ronne Ice Shelf (FRIS), High Salinity Shelf Water (HSSW) is transformed into Ice Shelf Water (ISW) by a combination of melting and freezing at the ice […]

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3. Measuring the basal melt rate of Antarctic ice shelves using GPS and phase-sensitive radar observations

   Basal melting of Antarctica’s floating ice shelves accounts for between 15 and 35% of the total mass loss from the ice sheet and helps to precondition the shelf waters for […]

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4. Trends in Antarctic terrestrial and limnetic ecosystems: Antarctica as a global indicator

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5. Colonisation processes

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6. Evolution of the Antarctic Peninsula Pacific margin offshore from Adelaide Island since the Late Miocene: an example of a glacial passive margin

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7. Pelagic provinces of the world: A biogeographic classification of the world’s surface pelagic waters

   Off-shelf waters cover 66% of the planet. Growing concerns about the state of natural resources in these waters, and of future threats have led to a growing movement to improve […]

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8. Physiological traits of organisms in a changing environment

   Antarctic ecosystems represent one extreme of the continuum of environmental conditions across the planet. To our eyes, the environment appears harsh but, even though terrestrial biological diversity is restricted, a […]

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9. Forecasting future weather from rocks

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10. Distribution, lithofacies and environmental context of Neogene glacial sequences on James Ross and Vega islands, Antarctic Peninsula

    Considerable controversy exists concerning the stability of the Antarctic Ice Sheet during the Neogene Period. The northern Antarctic Peninsula is in a critical position in this debate as it represents […]

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11. Steep reverse bed slope at the grounding line of the Weddell Sea sector in West Antarctica

    The bed of the West Antarctic Ice Sheet is, in places, more than 1.5 km below sea level1, 2. It has been suggested that a positive ice-loss feedback may occur when […]

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12. Patterns of marine bacterioplankton biodiversity in the surface waters of the Scotia Arc, Southern Ocean

    Spatial patchiness in marine surface bacterioplankton populations was investigated in the Southern Ocean, where the Antarctic Circumpolar Current meets the islands of the Scotia Arc and is subjected to terrestrial […]

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