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Climatic impacts of fresh water hosing under Last Glacial Maximum conditions: a multi-model study

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Figure

Table 1. Models compared in this analysis.
Table 2. Brief description of the experiments compared in this analysis.
Fig. 1. Summary of AMOC behaviour in the different fresh water hosing simulations. The AMOC is defined as the maximum of the“AMOC relative anomaly”, in %, is defined as 100meridional streamfunction of the North Atlantic circulation in the Northern Hemisphere
Fig. 2. Mean annual surface air temperature response (hosing experiment – reference experiment, in K) to fresh water hosing in the 11 hosingexperiments.
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