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X-WR-CALNAME:Oceans at MIT
X-WR-CALDESC:Striving to understand\, harness and sustain Earth&#039\;s def
 ining frontier.
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DTSTART:20171105T020000
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RDATE:20181104T020000
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UID:3dsmv53iq9qrj9rm821u916qvg@google.com
DTSTAMP:20180503T102215Z
CATEGORIES;LANGUAGE=en-US:MIT Seminar | PAOC Oceanography and Climate Sack 
 Lunch
CONTACT:
DESCRIPTION:Recent observations show that the Southern Ocean is dominating 
 anthropogenic ocean heat uptake. Southern Ocean heat uptake is large becau
 se the strong northward transport of the heat content anomaly limits warmi
 ng of the sea surface temperature in the uptake region. Using results from
  eddy-rich global climate simulations\, I will discuss the processes contr
 olling the northward heat transport away from the uptake region and the co
 nvergence of the heat content anomaly in the midlatitude Southern Ocean. H
 eat budget analyses reveal that different processes dominate to the north 
 and south of the main convergence region. The heat transport northward fro
 m the high-latitude uptake region is driven primarily by passive advection
  of the heat content anomaly by the existing time mean circulation\, with 
 a smaller contribution from enhanced upwelling. The heat anomaly builds up
  in the midlatitudes due to a convergent Ekman transport anomaly\, combine
 d with limited heat transport further northward into the mode waters. To t
 he north of the peak convergence region\, eddy processes drive the warming
  and account for nearly 80% of the northward heat transport anomaly.
DTSTART;TZID=America/New_York:20160525T120000
DTEND;TZID=America/New_York:20160525T125000
LOCATION:54-915
SEQUENCE:0
SUMMARY:SLS – Adele Morrison (Princeton) – Mechanisms of Southern Ocean hea
 t uptake and transport
URL:http://oceans.mit.edu/event/sls-adele-morrison-princeton-mechanisms-of-
 southern-ocean-heat-uptake-and-transport
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