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SUMMARY:Mantle convection\, plumes and dynamic topography - case studies f
 rom the North Atlantic and West Antarctica [Rescheduled to online] - Dr. B
 ernhard Steinberger\, GFZ Potsdam
DTSTART:20200520T110000Z
DTEND:20200520T120000Z
UID:TALK142018@talks.cam.ac.uk
CONTACT:Camilla Penney
DESCRIPTION:*This seminar will be held online. Details will be sent to the
  Earth Sciences and Bullard mailing lists. If you are not in Earth Science
 s but would like to attend\, please contact the talk organisers.*\n\nMantl
 e convection is the main mode how heat is transported from the deep Earth 
 interior to near its surface\, and mantle plumes are part of this convecti
 on. Dynamic topography is one surface expression of these convective proce
 sses. Here we discuss these features\, focusing on the North Atlantic and 
 West Antarctica\, because topography and (potential) plumes in these regio
 ns are important for determining ocean currents and ice sheet stability. H
 ence they also play an important role in understanding causes and effects 
 of changing climates.
LOCATION:ONLINE - Details to be sent by email
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