File:Comparison of modeled and reconstructed ocean circulation and climate changes.png

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Ivanovic RF; Gregoire LJ; Burke A; Wickert AD; Valdes PJ; Ng HC; Robinson LF; McManus JF; Mitrovica JX; Lee L; Dentith JE (2018) Acceleration of northern ice sheet melt induces AMOC slowdown and northern cooling in simulations of the early last deglaciation, Paleoceanography and Paleoclimatology. doi: 10.1029/2017PA003308

Comparison of modeled and reconstructed ocean circulation and climate changes. (a) Ice sheet meltwater fluxes from the drainage network model (global mean sea level rise: GMSLR), as in Figure 1. (b) Simulated maximum Atlantic Meridional Overturning Circulation (AMOC) and an AMOC transport proxy record from compiled North Atlantic 231Pa/230Th activity ratio (Ng et al., 2018); note that the 231Pa/230Th axis has been scaled to the amplitude of the simulated AMOC anomaly. (c) North Atlantic sea surface temperature (SST) from the Iberian Margin (SU81‐18; Bard et al., 2000). (d) Subtropical North Atlantic SST (MD95‐2037; Calvo et al., 2001). (e) SST north of the subtropics (IODP Hole 306‐U1313B; Naafs et al., 2013). (f) Surface air temperature (SAT) over Greenland (Buizert et al., 2014), including precipitation‐weighted model SAT (“p‐wgt”; see discussion in section 3). Climate anomalies (b)–(f) are from the 19.145–18.145 ka mean, using 100‐year annual running means for the model data.

The underlying data is available as 3 discrete datasets from the Research Data Leeds Repository:

Ivanovic, Ruza and Gregoire, Lauren and Wickert, Andrew and Mitrovica, Jerry (2018) Climate model data presented in 'Acceleration of northern ice sheet melt induces AMOC slowdown and northern cooling in simulations of the early last deglaciation'. University of Leeds. [Dataset] https://doi.org/10.5518/400
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institution QS:P195,Q24568958
Source https://doi.org/10.5518/400
Author Ivanovic, Ruza and Gregoire, Lauren and Wickert, Andrew and Mitrovica, Jerry

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