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1 Introduction The Northwest Atlantic Ocean has been undergoing warming at enhanced rates in the past two decades (e.g., Chen et al., 2020; Forsyth et al., 2015; Loder & Wang, 2015; Pershing et al., 2015). Warming has been observed over the past several decades on the continental shelf and over the continental slope (Seidov et al., 2021) and is associated with larger scale patterns in the North Atlantic (e.g., Gonçalves Neto et al., 2021; Holliday et al., 2020).
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