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BEGIN:VEVENT
DTSTAMP:20210916T132449Z
LOCATION:Jean Calvin
DTSTART;TZID=Europe/Stockholm:20210706T123000
DTEND;TZID=Europe/Stockholm:20210706T130000
UID:submissions.pasc-conference.org_PASC21_sess109_msa316@linklings.com
SUMMARY:The Quasi-Biennial Oscillation – from the km-Scale of Deep Convect
 ion to a Global Scale Wind Oscillation in the Stratosphere
DESCRIPTION:Minisymposium\n\nThe Quasi-Biennial Oscillation – from the km-
 Scale of Deep Convection to a Global Scale Wind Oscillation in the Stratos
 phere\n\nGiorgetta\n\nThe quasi-biennial oscillation is observed in the zo
 nal wind in the equatorial stratosphere where alternatively westerly and e
 asterly winds are generated in the upper stratosphere, then propagate down
 wards until the tropopause is reached. A full cycle lasts a bit more than 
 2 years. These global scale jets are driven by waves triggered by tropical
  cloud systems. The challenge we have is to understand how this phenomenon
  will change in a warmer climate. To address this question the QUBICC proj
 ect aims in a first step at global km-scale resolved simulations using the
  ICON model. In this experiment we try for a first time to simulate the dr
 iving mechanism explicitly. Owing to the size of the problem the model was
  ported to GPU for application on "Piz Daint".\n\nDomain: CS and Math, Cli
 mate and Weather, Physics
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