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DTSTAMP:20260515T071724Z
SUMMARY:The reduced state of the Atlantic Meridional Overturning Circulatio
 n
DESCRIPTION: \nThe Atlantic Meridional Overturning Circulation (AMOC) is r
 esponsible for a variable and climatically important northward transport o
 f heat. Using data from an array of instruments that span the Atlantic at 
 26°N\, we show that the AMOC has been in a state of reduced overturning s
 ince 2008 as compared to 2004–2008. This change of AMOC state is concurr
 ent with other changes in the North Atlantic such as a northward shift and
  broadening of the Gulf Stream and altered patterns of heat content and se
 a surface temperature. These changes resemble the response to a declining 
 AMOC predicted by coupled climate models. Concurrent changes in air-sea fl
 uxes close to the western boundary reveal that the changes in ocean heat t
 ransport and sea surface temperature have altered the pattern of ocean-atm
 osphere heat exchange over the North Atlantic.\nSmeed\, D. A.\, Josey\, S.
  A.\, Beaulieu\, C.\, Johns\, W. E.\, Moat\, B. I.\, Frajka-Williams\, E.\
 , et al. (2018). The North Atlantic Ocean Is in a state of reduced overtur
 ning. Geophysical Research Letters\, 370(1962)\, 1228–1533. http://doi.o
 rg/10.1002/2017GL076350
URL:https://www.imperial.ac.uk/events/97033/the-reduced-state-of-the-atlant
 ic-meridional-overturning-circulation/
DTSTART;TZID=Europe/London:20190430T113000
DTEND;TZID=Europe/London:20190430T123000
LOCATION:United Kingdom
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DTSTART:20190430T113000
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