Australia: The Land Where Time Began

A biography of the Australian continent 

Antarctica

  1. Abrupt Change in Atmospheric Co2 During the Last Ice Age
  2. Abyssal Ocean Warming and Salinification Following Weddell Polynyas in GDFL CM2G Coupled Climate Models
  3. Amundsen Sea Shelf Break – Oceanographic Observations
  4. Antarctic Circumpolar Current Transport Across Kerguelen Plateau – Direct Observations
  5. Antarctic Circumpolar Current Transport on the Northern Flank of the Kerguelen Plateau - Direct Observations
  6. Antarctic Climate Change and Environment - Deep-Time, the Geological Dimension
  7. Antarctic Climate Change and Environment - The Holocene
  8. Antarctic Climate Change and Environment - Changes During the Instrumental Period
  9. Antarctic Climate Change and Environment - Next 100 Years
  10. Antarctic Dry Valleys – Formation of Thermokarst in the McMurdo Dry Valleys
  11. Antarctic Sea Ice
  12. Antarctic Sea Ice Expansion - Important role of Ocean Warming and Increased Ice-Shelf Melt
  13. Antarctic Surface Waters - Abrupt Cooling and Sea Ice Expansion in the Southern Ocean, South Atlantic Sector at 5,000 Cal Yr BP
  14. East Antarctic Ice Sheet - Dynamic Behaviour During the Pliocene Warmth
  15. Antarctica - Before and After Gondwana
  16. Antarctica - Borchgrevink Event
  17. Antarctic Bottom Water in the Eastern Weddell Gyre – Remotely induced Warming
  18. Antarctica – Changing Icescapes
  19. Antarctica - Geological History
  20. Antarctic and Greenland Ice Sheets - Acceleration of their Contribution to Sea Level Rise
  21. Antarctica - Role in Global Environment
  22. East Antarctica - Abrupt Climate Warming in the Early Holocene
  23. Antarctica - East Antarctic Ice Sheet
  24. Antarctica - East Antarctica, Major Components
  25. Antarctica - Glacier Tongues
  26. Antarctica - Outlet, Valley and Piedmont Glaciers
  27. Antarctica - Ice Sheets - the glacial setting at the present
  28. Antarctica - Ice Shelves
  29. Antarctica - Ice Flow Sensitivity of Pine Island Glacier to Geothermal Heat Flux
  30. Larsen C Ice Shelf, Basal Crevasses – Implications of meltwater ponding and Hydrofracture
  31. Larsen C Ice Shelf – Marine Ice Formation in a Suture Zone and its Influence on the Dynamics of the Ice Shelf
  32. Larsen C Ice Shelf – Impact on Basal Melting of Tide-Topography Interactions
  33. Larsen C Ice Shelf – In situ Observations of Ocean Circulation Beneath it
  34. Larsen C Ice Shelf – the Structure and Effect of Suture Zones
  35. Antarctica - Palaeozoic Orogenic Events
  36. Antarctica - Precambrian Orogenic Events
  37. Antarctica - Pine Island Glacier, subglacial melt channels & Fracture in Floating Part
  38. Antarctica - Pine Island Glacier, West Antarctica, Rapid Subglacial Erosion
  39. Antarctica - Pine Island Glacier, West Antarctica, Sustained Glacier Retreat
  40. Antarctica - Pine Island Bay, West Antarctica – Ice Cavity Water Export
  41. Antarctica - Pine Island, Thwaites, Smith, and Kohler Glaciers , West Antarctica – Widespread, Rapid Retreat – 1992-2011
  42. Antarctica - Polygonal Ground in the McMurdo Dry Valleys, Antarctica – it’s Relationship to Depth of the Ice Table and Recent Climatic History
  43. Antarctica - Sea Ice
  44. Antarctica - West Antarctica, Major Components
  45. Antarctica - The West Antarctic Ice Sheet - WAIS
  46. Brinicles
  47. East Antarctic Ice Shelf – Meltwater Produced by Interaction between wind and albedo stored in the East Antarctic Ice Sheet
  48. Polar Front Around the Kerguelen Islands – Up-to-Date Determination and Associated Circulation of Surface-Subsurface Waters
  49. Oceanic Ice Shelf Melting – the Effect of Basal Channels
  50. A Rossby Wave Bridge Connecting West Antarctica to the Tropical Atlantic Ocean
  51. Rossby Waves Mediate Impacts on West Antarctic Atmospheric Circulation of Tropical Oceans
  52. Southern Ocean CO2 Sink Saturation Due to Recent Climate Change
  53. Southern Ocean – Factors that Affect the Occurrence in the Atmosphere, and Deposition of, Polychlorinated Biphenyls (BCPs)
  54. Southern Ocean - Upwelling Driven by Wind and the Rise of Atmospheric CO2 During Deglaciation
  55. Southern Ocean Warming Delayed by Circumpolar Upwelling and Equatorwards Transport
  56. Southern Ocean has been slowing Global Warming by Absorbing Carbon, But that Could Change
  57. Totten Ice Shelf – Rapid Basal Melt Driven by Ocean Heat
  58. Totten Glacier, East Antarctica - Ocean Access to a Cavity Beneath it
  59. Totten Glacier – Inland Bed Erosion Indicates Repeated Retreat on a Large Scale

 

 

Sources & Further reading

Author: M. H. Monroe
Email:  admin@austhrutime.com
Last updated 26/02/2017
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                                                                                           Author: M.H.Monroe  Email: admin@austhrutime.com     Sources & Further reading