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SUMMARY:Mantle convection\, plumes and dynamic topography - case studies f
 rom the North Atlantic and West Antarctica - Dr. Bernhard Steinberger
DTSTART:20200520T110000Z
DTEND:20200520T120000Z
UID:TALK142015@talks.cam.ac.uk
CONTACT:Camilla Penney
DESCRIPTION:Mantle convection is the main mode how heat is transported fro
 m the deep Earth interior to near its surface\, and mantle plumes are part
  of this convection. Dynamic topography is one surface expression of these
  convective processes. Here we discuss these features\, focusing on the No
 rth Atlantic and West Antarctica\, because topography and (potential) plum
 es in these regions are important for determining ocean currents and ice s
 heet stability. Hence they also play an important role in understanding ca
 uses and effects of changing climates.
LOCATION:ONLINE - Details to be sent by email
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