Publications

8821 to 8832 of 14026 results

1. Phase-sensitive FMCW radar system for high-precision Antarctic ice shelf profile monitoring

   Ice shelves fringe much of the Antarctic continent, and, despite being up to 2 km thick, are vulnerable to climate change. Owing to their role in helping to control the […]

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2. A new bathymetric compilation for the South Orkney Islands, Antarctic Peninsula (49°-39°W to 64°-59°S): insights into the glacial development of the continental shelf

   We present a new, high resolution (300 m) bathymetric grid of the continental shelf surrounding the South Orkney Islands, northeast of the Antarctic Peninsula. The new grid, derived from a […]

   Read more of: A new bathymetric compilation for the South Orkney Islands, Antarctic Peninsula (49°-39°W to 64°-59°S): insights into the glacial development of the continental shelf

3. Pristine Antarctica: threats and protection

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4. Prediction of relativistic electron flux at geostationary orbit following storms: Multiple regression analysis

   Many solar wind and magnetosphere parameters correlate with relativistic electron flux following storms. These include relativistic electron flux before the storm, seed electron flux, solar wind velocity and number density […]

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5. Mopsechiniscus franciscae, a new species of a rare genus of Tardigrada from continental Antarctica

   Despite the importance and regular occurrence of tardigrades in the Antarctic terrestrial ecosystem, taxonomic studies of, in particular, continental Antarctica species have advanced very slowly. During a large survey to […]

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6. Simulating the Earth’s radiation belts: internal acceleration and continuous losses to the magnetopause

   In the Earth’s radiation belts the flux of relativistic electrons is highly variable, sometimes changing by orders of magnitude within a few hours. Since energetic electrons can damage satellites it […]

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7. Three-dimensional stochastic modeling of radiation belts in adiabatic invariant coordinates

   A 3-D model for solving the radiation belt diffusion equation in adiabatic invariant coordinates has been developed and tested. The model, named REM (for Radbelt Electron Model), obtains a probabilistic […]

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8. Hydrography and circulation in the Filchner Depression, Weddell Sea, Antarctica

   Cold and dense Ice Shelf Water (ISW) emerging from the Filchner-Ronne Ice Shelf cavity in the southwestern Weddell Sea flows northward through the Filchner Depression to eventually descend the continental […]

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9. Surface energy budget on Larsen and Wilkins ice shelves in the Antarctic Peninsula: results based on reanalyses in 1989-2010

   Ice shelves in the Antarctic Peninsula have significantly disintegrated during recent decades. To better understand the atmospheric contribution in the process, we have analysed the inter-annual variations in radiative and […]

   Read more of: Surface energy budget on Larsen and Wilkins ice shelves in the Antarctic Peninsula: results based on reanalyses in 1989-2010

10. Stable isotopes and Antarctic moss banks: plants and soil microbes respond to recent warming on the Antarctic Peninsula [abstract only]

    The Antarctic Peninsula is one of the most rapidly warming regions on Earth, with air temperature increases of as much as 3°C recorded since the 1950s. However, the longer-term context […]

    Read more of: Stable isotopes and Antarctic moss banks: plants and soil microbes respond to recent warming on the Antarctic Peninsula [abstract only]

11. Radio-echo Sounding of Pine Island Glacier, West Antarctica: Understanding the Past from Observations, Analysis and Modelling of Internal Layering

    Pine Island Glacier is one of the fastest and most dynamic glaciers in West Antarctica. The stability of the glacier may thus have profound impact on the overall stability of […]

    Read more of: Radio-echo Sounding of Pine Island Glacier, West Antarctica: Understanding the Past from Observations, Analysis and Modelling of Internal Layering

12. Conclusions: Present and future of Southern Ocean biogeography

    Read more of: Conclusions: Present and future of Southern Ocean biogeography