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    An interhemispheric mechanism for glacial abrupt climate change

    The last glacial period was punctuated by abrupt climate changes that are widely considered to result from millennial-scale variability of the Atlantic meridional overturning circulation (AMOC). However, the ...

    Rubén Banderas, Jorge Alvarez-Solas, Alexander Robinson, Marisa Montoya in Climate Dynamics (2015)