The scientific community is investing considerable effort in organizing our current knowledge of the physical and biogeochemical properties of sea ice, exploring poorly understood sea ice processes, and forecasting future changes of the sea ice cover.
In this session, organizers invite contributions regarding all aspects of sea ice science and sea ice-climate interactions. Oral presentations and posters on snow and sea ice thermodynamics and dynamics, sea ice-atmosphere and sea ice-ocean interactions, sea ice biological and chemical processes, and sea ice models will be welcome.
Abstract Submission Deadline for all Sessions: Monday, 18 January 2010.
To submit an abstract, you will need to log in or create an account at:
https://administrator.copernicus.org/authentication.php
For further information, please go to:
http://meetingorganizer.copernicus.org/EGU2010/session/1890
Or contact:
Daniel Feltham
Email: dlf@cpom.ucl.ac.uk
Session Announcement and Call for Abstracts CR9.1: Sea Ice and Sea Ice-Climate Interactions European Geosciences Union General Assembly 2010
Mon, Jan 11, 2010
Organizers of Session CR9.1, "Sea Ice and Sea Ice-Climate Interactions,"
announce a call for abstracts.
The year 2008 was another very low sea ice year in the Arctic. Some climate models now predict that summer arctic sea ice might altogether disappear in about 30 or 40 years. While the effects of a shrinking sea ice cover on global climate, ocean circulation, and marine biology are expected to be quite significant, they are very difficult to evaluate because of our incomplete understanding of the polar climate components and our limited ability to model them.
announce a call for abstracts.
The year 2008 was another very low sea ice year in the Arctic. Some climate models now predict that summer arctic sea ice might altogether disappear in about 30 or 40 years. While the effects of a shrinking sea ice cover on global climate, ocean circulation, and marine biology are expected to be quite significant, they are very difficult to evaluate because of our incomplete understanding of the polar climate components and our limited ability to model them.