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Interactive comment on “Disentangling the effect of ocean temperatures and isotopic content on the oxygen – isotope signals in the North Atlantic Ocean during Heinrich Event 1 using a global climate model” by Marianne Bügelmayer-Blaschek

This study analyses three simulations of Heinrich Event 1 with an isotope-enabled model of intermediate complexity. Time series of simulated d18O seawater and calculated d18O calcite (based on simulated d18O seawater and simulated seawater temperatures) are then analysed and loosely compared to four sediment cores. The three different simulations differ in the length of the iceberg calving episode and have different impacts on the Atlantic Overturning Motion. The authors conclude that the duration of the simulated Heinrich event causes a strong and non-linear response in the AMOC.