On Fri, 10 Aug 2007, Eric Swanson wrote: > As the sea-ice extent declines, it's thickness also decreases. I > think it's likely that the thickness will decline so much that there > will be the chance of a mechanical failure, even before the extent > could actually reaches zero. The result could look much like the > breakup of the Larson B ice shelf along the Antarctic Peninsula, which > was sudden and spectacular .
This is unlikely. Sea ice has essentially no strength in tension anyway. -W. William M Connolley | [EMAIL PROTECTED] | http://www.antarctica.ac.uk/met/wmc/ Climate Modeller, British Antarctic Survey | 07985 935400 -- This message (and any attachments) is for the recipient only. NERC is subject to the Freedom of Information Act 2000 and the contents of this email and any reply you make may be disclosed by NERC unless it is exempt from release under the Act. Any material supplied to NERC may be stored in an electronic records management system. --~--~---------~--~----~------------~-------~--~----~ You received this message because you are subscribed to the Google Groups Global Change ("globalchange") newsgroup. Global Change is a public, moderated venue for discussion of science, technology, economics and policy dimensions of global environmental change. Posts will be admitted to the list if and only if any moderator finds the submission to be constructive and/or interesting, on topic, and not gratuitously rude. To post to this group, send email to [email protected] To unsubscribe from this group, send email to [EMAIL PROTECTED] For more options, visit this group at http://groups.google.com/group/globalchange -~----------~----~----~----~------~----~------~--~---
