EGU General Assembly 2008
Session Programme Meeting Programme Personal Programme Search
 
Quick Search
Programme Groups
Union Symposia
Interdivision Sessions
Educational Symposia
Atmospheric Sciences
Biogeosciences
Climate: Past, Present, Future
Cryospheric Sciences
Earth & Space Science Informatics
Energy, Resources & the Environment
Geochemistry, Mineralogy, Petrology & Volcanology
Geodesy
Geodynamics
Geomorphology
Geosciences Instrumentation & Data Systems
Hydrological Sciences
Isotopes in Geosciences: Instrumentation and Applications
Magnetism, Palaeomagnetism, Rock Physics & Geomaterials
Natural Hazards
Nonlinear Processes in Geophysics
Ocean Sciences
Planetary & Solar System Sciences
Seismology
Soil System Sciences
Solar-Terrestrial Sciences
Stratigraphy, Sedimentology & Palaeontology
Tectonics & Structural Geology
Medal Lectures
Great Debates in Geosciences
Short Courses
Keynote Lectures
Townhall Meetings
Division Business Meetings
Editorial Board Meetings
Union Meetings
Splinter Meetings
  Information - OS10 Variability in the Southern Ocean

Event Information
Southern Ocean physical processes influence the hemispheric and global climate, rate and pattern of sea-level rise, distribution of nutrients and productivity of marine ecosystems, and ocean uptake and storage of carbon dioxide. Recent studies document the variability of the Southern Ocean environment and its impact on regional climate and marine organisms. Southern Ocean water masses contributing to the meridional overturning circulation (MOC) are changing in response to climate change. Climate models predict that the Southern Ocean overturning circulation will slow down as a result of global warming, causing a decrease in the amount of carbon dioxide absorbed by the ocean and a positive feedback on climate change. However, our understanding of how the circulation and water masses of the Southern Ocean vary in time and the impact of such variability on regional ecosystems, the fringing ice sheet, and the global climate remains incomplete, largely due to the lack of appropriate observations. The Southern Ocean is remote and the environment is hostile. Therefore, historical data are scarce and hypotheses regarding the impact of Southern Ocean processes on climate are difficult to validate. However, new tools (e.g. autonomous floats, animal mounted oceanographic sensors, new and more accurate satellite sensors, improved numerical models) and additional measurements from the last decade now allow to investigate changes in the Southern Ocean and to describe and understand the processes responsible for the variability.

We welcome contributions using data and/or models about:
- Variability of Southern Ocean/ACC structure on time-scales from months to
decades.
- Variability of the coupled ocean-atmosphere-sea ice system in the Southern
Ocean.
- Variability of the cross-shelf exchange with consequences for water mass
formation and ice shelf basal melting.
- Variability of upper ocean currents and stratification and their impact on
marine biogeochemical and ecological systems.
- Physical controls on biological productivity and export of biological matter
to the deep ocean.
- Variations in animal distributions and behaviour related to environmental
variability.
- Ocean observations to test and guide refinement of climate models in the
Southern Ocean.
- Hindcasts from a data-assimilating ocean model to infer the statistics of
variability and to diagnose the physical processes responsible for Southern
Ocean variability.
- Connection between the Southern Ocean climate variability and large-scale
climate indices, such as ENSO, SAM, Indian Ocean dipole modes etc.

Preliminary List of Solicited Speakers

Co-Sponsorship

General Statement
The information contained hereafter has been compiled and uploaded by the Session Organizers via the "Organizer Session Form". The Session Organizers have therefore the sole responsibility that this information is true and accurate at the date of publication, and the conference organizer cannot accept any legal responsibility for any errors or omissions that may be made, and he makes no warranty, expressed or implied, with regard to the material published.



Back to Session Programme

 
 
 
 


©2002-2008 Copernicus Systems + Technology GmbH