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CATEGORIES:Rouse Ball Lectures
SUMMARY:Heat Rises: 100 Years of Rayleigh-Bénard Convectio
 n (Rouse Ball Lecture) - Professor Charles Doering
  (University of Michigan)
DTSTART;TZID=Europe/London:20170502T120000
DTEND;TZID=Europe/London:20170502T130000
UID:TALK69953AThttp://talks.cam.ac.uk
URL:http://talks.cam.ac.uk/talk/index/69953
DESCRIPTION:Buoyancy forces result from density variations\, o
 ften due to temperature variations\, in the presen
 ce of gravity. Buoyancy-driven fluid flows shape t
 he weather\, ocean and atmosphere dynamics\, the c
 limate\, and the structure of the earth and stars.
  In 1916 Lord Rayleigh published a paper entitled 
 "On Convection Currents in a Horizontal Layer of F
 luid\, when the Higher Temperature is on the Under
  Side" introducing the minimal mathematical model 
 of buoyancy-driven fluid flow now known as Rayleig
 h-Bénard convection.  For a century this model has
  served as a primary paradigm of complex nonlinear
  dynamics displaying spontaneous symmetry breaking
  and pattern formation\, chaos and turbulence. Her
 e we describe progress and challenges for the anal
 ysis of Rayleigh's model in the strongly nonlinear
  regime of turbulent convection.\n\n_This lecture 
 is intended to be accessible to all\, including un
 dergraduates\, who are very welcome to attend._
LOCATION:Room 3\, Mill Lane Lecture Rooms\, 8 Mill Lane\, C
 ambridge
CONTACT:Christelle Greaves
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