Atlantic Meridional Overturning Circulation and δ13C Variability During the Last Interglacial

• Published in: Paleoceanography and paleoclimatology Vol. 35; no. 5
• Main Authors: Kessler, A., Bouttes, N., Roche, D. M., Ninnemann, U. S., Galaasen, E. V., Tjiputra, J.
• Format: Journal Article
• Language: English
• Published: 01.05.2020
• ISSN: 2572-4517; 2572-4525
• DOI: 10.1029/2019PA003818

The Atlantic Meridional Overturning Circulation (AMOC) is thought to be relatively vigorous and stable during Interglacial periods on multimillennial (equilibrium) timescales. However, recent proxy (δ13C benthic) reconstructions suggest that higher frequency variability in deep water circulation may have been common during some interglacial periods, including the Last Interglacial (LIG, 130–115 ka). The origin of these isotope variations and their implications for past AMOC remain poorly understood. Using iLOVECLIM, an Earth system model of intermediate complexity (EMIC) allowing the computation of δ13CDIC and direct comparison to proxy reconstructions, we perform a transient experiment of the LIG (125–115 ka) forced only by boundary conditions of greenhouse gases and orbital forcings. The model simulates large centennial‐scale variations in the interior δ13CDIC of the North Atlantic similar in timescale and amplitude to changes resolved by high‐resolution reconstructions from the LIG. In the model, these variations are caused by changes in the relative influence of North Atlantic Deep Water (NADW) and southern source water (SSW) and are closely linked to large (∼50%) changes in AMOC strength provoked by saline input and associated deep convection areas south of Greenland. We identify regions within the subpolar North Atlantic with different sensitivity and response to changes in preformed δ13CDIC of NADW and to changes in NADW versus SSW influence, which is useful for proxy record interpretation. This could explain the relatively large δ13C gradient (∼0.4%0) observed at ∼3 km water depth in the subpolar North Atlantic at the inception of the last glacial. Key Points Similar variations of bottom water δ13C to that depicted by data reconstructions are simulated in the North Atlantic for the LIG period Changes in AMOC strength may be a key process in distributing δ13C in the ocean interior Magnitude of local bottom water δ13C response depends on position relative to water mass geometry