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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).
Supporting Information Filename Description 2024JC021543-sup-0001-Supporting Information SI-S01.pdf228.4 KB Supporting Information S1 References , , , & (2018). Up to what extent can we characterize ocean eddies using present-day gridded altimetric products? Journal of Geophysical Research: Oceans, 123(10), 7220–7236. https://doi.org/10.1029/2018jc014140 (2016). On the recent destabilization of the Gulf Stream path downstream of Cape Hatteras. Geophysical Research Letters, 43(18), 9836–9842.
1 Introduction Warm and cold core rings (WCRs and CCRs) are types of mesoscale eddies that are formed by the Gulf Stream. These rings can transport water masses across the Gulf Stream front and westward hundreds of kilometers from their formation site until they dissipate or are reabsorbed by the Gulf Stream. WCRs are well-studied on account of their importance for heat and salt transport and their interactions with other regional flows (Flierl, 1979; Silver et al., 2021).
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