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SUMMARY:Arctic atlantification vs Atlantic Arctification - Professor Yueng
 -Djern Lenn\, Bangor University
DTSTART:20260512T110000Z
DTEND:20260512T120000Z
UID:TALK246771@talks.cam.ac.uk
CONTACT:Carrie Soderman
DESCRIPTION:<p><span style="color: rgb(0\, 0\, 0)\;">Northwards heat trans
 port from the North Atlantic has been a key driver of climate change in th
 e Arctic Ocean and its marginal seas in a process now commonly known as At
 lantification.  Characteristics of Atlantification in the eastern Arctic i
 nclude weaker upper ocean stratification\, enhanced sea ice melt and warme
 r SSTs.  Some observations point towards these characteristics spreading i
 nto the western Arctic\, perhaps ’spicing’ up the Beaufort gyre.  At t
 he same time\, this excess oceanic heat from the Atlantic inflow to the Ar
 ctic is thought to be contributing to increase freshwater export to the No
 rth Atlantic.  That freshwater\, in combination with Greenland glacier bas
 al melt driven by recirculating Atlantic water\,  is simultaneously changi
 ng the North Atlantic stratification potentially pushing the upper ocean t
 owards salinity stratification- an Arctification.   We present observation
 s that track the changes in stratification in the Beaufort gyre and North 
 Atlantic sites of deep water convection over nearly 3 decades and discuss 
 the relative progress of Atlantification and Arctification.</span></p>
LOCATION:Department of Earth Sciences\, Tilley Lecture Theatre
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