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VERSION:2.0
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BEGIN:VEVENT
DTSTAMP:20261011T141203Z
UID:https://www.shh.mpg.de/events/37197/2393678
DTSTART:20240409T130000Z
DTEND:20240409T143000Z
CLASS:PUBLIC
CREATED:20240320T105100Z
DESCRIPTION: The evolution of the Antarctic Ice Sheet is of vital importanc
 e given the coastal and societal implications of ice loss\, with a potenti
 al to raise sea level by up to 58 m if melted entirely. However\, future i
 ce-sheet trajectories remain highly uncertain. In fact\, current estimates
  range from a slight mass gain to a mass loss of the Antarctic Ice Sheet b
 y the end of this century. What is more\, due to ice-sheet inertia and pot
 entially self-sustained mass loss when exceeding critical thresholds or ti
 pping points\, the bulk of sea-level rise is expected to arise beyond the 
 end of this century as sea-level commitment. Here\, we systematically asse
 ss this long-term committed sea-level contribution from the Antarctic Ice 
 Sheet in response to warming projected over the next centuries under lower
 - and higher-emission pathways\, as well as the reversibility of the commi
 tted large-scale ice-sheet changes when reducing warming to relatively col
 der climate conditions.\nSpeaker: Ann Kristin Klose
LAST-MODIFIED:20240422T074907Z
LOCATION:MPI of Geoanthropology\, Room: Villa V14
ORGANIZER;CN=Department Evolutionary Earth System Science:mailto:rennoffice
 @gea.mpg.de
SUMMARY:Long-term sea-level commitment and reversibility of ice loss from A
 ntarctica
URL;VALUE=URI:https://www.shh.mpg.de/events/37197/2393678
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