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description The past decades have been associated with substantial losses of sea ice over both hemispheres. Existing climate models are currently unable to accurately forecast these changes, in part due
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, ocean-ice interactions and Southern Hemisphere climate dynamics The current list of specific PhD projects and supervisors is updated regularly on our website; applicants are encouraged to browse these and
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, and the presence of additional Northern Hemisphere ice sheets for the Last Glacial Maximum). Their realism can be evaluated using existing and newly acquired records from the AMACLIM project. Particular
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