The mid-Pliocene warm period (3.264–3.025 Ma) is the most recent geological period in
which the atmospheric CO 2 concentration was approximately equal to the concentration we
measure today (ca. 400 ppm). Sea surface temperature (SST) proxies indicate above-
average warming over the North Atlantic in the mid-Pliocene with respect to the pre-
industrial period, which may be linked to an intensified Atlantic Meridional Overturning
Circulation (AMOC). Earlier results from the Pliocene Model Intercomparison Project Phase …

Unraveling the mechanisms and implications of a stronger mid-Pliocene Atlantic Meridional
Overturning Circulation (AMOC) in PlioMIP2 | CiNii Research … Unraveling the
mechanisms and implications of a stronger mid-Pliocene Atlantic Meridional Overturning
Circulation (AMOC) in PlioMIP2 … タイトル Unraveling the mechanisms and implications of
a stronger mid-Pliocene Atlantic Meridional Overturning Circulation (AMOC) in PlioMIP2 …