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Origin and evolution of the sub-Antarctic islands: the Foundation The sub-Antarctic. Papers and Proceedings of the Royal Society of Tasmania, 2007 (Ref: 13527)
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Category 1: Peer-reviewed literature

Sub-Antarctic islands have a diversity of origins in detail but most are volcanic and very young suggesting that they are short-lived and that the distribution would have been very different a few million years ago. They contrast with the common tourist brochure concept of oceanic islands.

Oceanography along East Antarctica (30-80º E) during the BROKE-West survey (CCAMLR Area 58.4.2) in the Austral summer of 2006. Abstracts from the SCAR Open Science Conference, Hobart, 12-14 July 2006., 2006 (Ref: 12606)
Category 3: Abstract

A second East Antarctic Baseline Regional Oceanography Krill and Environment survey, termed BROKE-West, was conducted January 10th – February 25th 2006 and covered … CCAMLR Area 58.4.2 west of the Princess Elizabeth Trough in the Weddell-Enderby Basin.

Reassessing the input-output mass budget of East Antarctica between 50°E and 140°E. Abstracts presented at 'Understanding Sea Level Rise and Variability' - A World Climate Research Programme Workshop and WCRP Contribution to the Global Earth Observation System of Systems, Paris, France, 6-9 June 2006., 2006 (Ref: 12579)
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Category 3: Poster

Accurate assessments of the past and future mass budgets of polar ice sheets are essential to resolving contributions to past sea-level rise and projecting responses to climate change respectively. Both tasks require that ice accumulation and ice flow are each accurately described…

Reassessing the input-output mass budget of East Antarctica between 50°E and 140°E. Abstracts of the SCAR Open Science Conference, Hobart, 12-14 July 2006., 2006 (Ref: 12569)
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Category 3: Abstract

Using satellite altimeter measurements of Antarctic surface elevation changes Davis and … others (Science, 2005) reported that the interior of the East Antarctic ice sheet is thickening … slightly, contributing 0.12 mm/a towards lowering global sea-level.

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