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X-WR-CALNAME:Oceans at MIT
X-WR-CALDESC:Striving to understand\, harness and sustain Earth&#039\;s def
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DTSTART:20171105T020000
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UID:0ut5p5eqm7gvf41qhg299rrvf4@google.com
DTSTAMP:20180503T091752Z
CATEGORIES;LANGUAGE=en-US:MIT Seminar | PAOC Oceanography and Climate Sack 
 Lunch
CONTACT:
DESCRIPTION:Eddies in the ocean move westwards. Those shed by western bound
 ary currents must then interact with shelf-slope topography at the western
  boundary.\n\nThis simple picture is complicated by the presence of other 
 eddies and mean flows\, but satellite observations show that many western 
 boundary continental shelves are affected by mesoscale eddies translating 
 near the shelfbreak. In this SST image\, a Gulf Stream Warm Core Ring (ant
 icyclone) transports cold fresh shelf water offshore across the Mid-Atlant
 ic Bight shelfbreak. Using idealized numerical simulations\, I address thr
 ee questions:\n\n1. Does the eddy always get to the shelfbreak\, or can sl
 oping topography stop an eddy from crossing it?\n2. What is the magnitude 
 of offshore transport driven by these eddies?\n3. What is the effect of th
 e eddy on the shelf's flow field?
DTSTART;TZID=America/New_York:20160316T120000
DTEND;TZID=America/New_York:20160316T130000
LOCATION:54-915
SEQUENCE:0
SUMMARY:SLS- Deepak Cherian (MIT/WHOI) – Eddy vs. shelf-slope topography
URL:http://oceans.mit.edu/event/sls-deepak-cherian-mitwhoi-eddy-vs-shelf-sl
 ope-topography
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