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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:9g2sb4helvoome98emc9t6fva8@google.com
DTSTAMP:20180503T102130Z
CATEGORIES;LANGUAGE=en-US:MIT Seminar | PAOC Oceanography and Climate Sack 
 Lunch
CONTACT:
DESCRIPTION:I will present a suite of records from a 950 m-depth sediment c
 ore from the western North Atlantic\, a site influenced by Antarctic Inter
 mediate Water (AAIW) in the modern ocean. The data suggest that northern s
 ourced waters dominated the water mass mixture during the LGM\, and that A
 AIW was shallower than ~850m. A d18O decrease early in Heinrich Stadial 1 
 (HS1) is attributed to the incorporation of deglacial meltwater into the n
 orthern sourced waters that continued to influence the site. Two interpret
 ations for the mid-to-late HS1 data will be discussed\, having opposite im
 plications for the vigor of the Atlantic Meridional Overturning Circulatio
 n (AMOC) during this interval. After HS1\, the data conform to the consens
 us view of AMOC variability – increased AAIW presence during the Bolling-A
 llerod and the Holocene\, when the AMOC was strong\, and reduced AAIW pres
 ence during the Younger Dryas when the AMOC was weak.
DTSTART;TZID=America/New_York:20151118T120000
DTEND;TZID=America/New_York:20151118T130000
LOCATION:54-915
SEQUENCE:0
SUMMARY:SLS – Delia Oppo (WHOI) – Deglacial Atlantic circulation:evidence f
 rom multiproxy records from shallow western north Atlantic sediment cores
URL:http://oceans.mit.edu/event/sls-delia-oppo-whoi-deglacial-atlantic-circ
 ulationevidence-from-multiproxy-records-from-shallow-western-north-atlanti
 c-sediment-cores
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