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- Marine picoplankton response to climate change
- Meteorological and ozone observing in the Antarctic
- Modelling of the ACC and polar gyres
- Models of the physical and biological environment of the Antarctic
- Near-shore marine disturbances over the next 100 years
- Observations, data accuracy and tools
- Observations for studies of environmental change in the Antarctic
- Observations of Antarctic permafrost
- Observations of marine biology
- Observations of terrestrial biology
- Observations of the ice sheet
- Ocean change over the next 100 years
- Ocean models of the Southern Ocean
- Pathways of research in cold-adapted organisms and climate change
- Precipitation changes over the 21st century
- Prospects for marine invasions by non-indigenous species
- Recommendations
- Regional climate models
- Regional patterns of holocene climate change in Antarctica
- Ross Sea shelf waters in the instrumental period
- Satellite observations of the Southern Ocean
- Sea ice biological and physical modeling
- Sea ice change over the 21st century
- Sea ice ecosystems in the instrumental period
- Sea ice observations
- Sea ice over the last million years
- Sea level observations
- Small-scale processes in the Southern Ocean
- Temperature changes in the instrumental period
- Temperature changes over the 21st century
- Terrestrial biological responses to climate change
- Terrestrial biology in the instrumental period
- Terrestrial biology over the next 100 years
- Terrestrial biota of the Antarctic
- The Amundsen and Bellingshausen seas in the instrumental period
- The Antarctic Peninsula cryosphere in the instrumental period
- The Antarctic cryosphere
- The Antarctic environment in the global system
- The Antarctic marine ecosystem in the year 2100
- The Australian sector in the instrumental period
- The East Antarctic cryosphere in the instrumental period
- The Greenhouse world - from the breakup of Gondwana to 34 million years ago
- The Holocene
- The IPCC fourth assessment report
- The Icehouse world - the last 34 million years
- The Southern Ocean carbon cycle response to future climate change
- The Southern Ocean carbon cycle response to historical climate change
- The Southern Ocean in the instrumental period
- The Weddell Sea sector in the instrumental period
- The West Antarctic cryosphere in the instrumental period