Extended Data Fig. 2: Ocean response to Dansgaard-Oeschger cycle and Heinrich event.
From: Earth system response to Heinrich events explained by a bipolar convection seesaw
Differences in simulated variables during non-Heinrich Stadial (nHS) relative to Interstadial (IS) (left), Heinrich Stadial (HS) before convection onset relative to non-Heinrich Stadial (middle) and Heinrich Stadial after the onset of convection relative to Heinrich Stadial before convection onset (right) for a–c zonally averaged ocean potential temperature, d–f radiocarbon ventilation age, g–i oxygen concentration and j–l dissolved inorganic carbon. All fields are shown separately for the Atlantic Ocean and the Indo-Pacific Oceans, with the Southern Ocean sectors included.
