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- Changes in Antarctic permafrost over the past 50 years
- Changes in Antarctic snowfall over the past 50 years
- Changes in sea ice extent through the Holocene
- Changes to the Terrestrial cryosphere over the next 100 years
- Concluding remarks on the pre-instrumental period
- Conclusions on the ice sheet in the instrumental period
- Coupled atmosphere-ocean models
- Deep time
- Deglaciation of the continental shelf, coastal margin and continental interior
- ENSO links and teleconnections to vertebrate life histories and population
- Editors
- Future developments in Antarctic observation
- Glacial interglacial cycles
- Holocene climate change in East Antarctica (EA)
- Holocene climate change in the Antarctic Peninsula (AP)
- Holocene climate change in the Ross Sea region (RS)
- Holocene climate changes
- Ice sheet models
- Impacts of instrumental period climate change on invertebrates
- Impacts of instrumental period climate change on macroalgae
- In-situ ocean observations
- Key points - 2009 version
- Key points - 2013 version
- Long term sea level change in the instrumental period
- Main Page
- Marine and terrestrial pollution
- Marine biological responses to climate change
- Marine biology in the instrumental period
- Marine biology over the next 100 years
- Marine biota of the Antarctic
- 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