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Taenzer, L. L., Chen, K., Plueddemann, A. J., & Gawarkiewicz, G. G. (2025). Seasonal Salinification of the US Northeast Continental Shelf Cold Pool Driven by Imbalance Between Cross-Shelf Fluxes and Vertical Mixing. Journal of Geophyscial Research: Oceans, 130(5), e2024JC021070. https://doi.org/10.1029/2024JC021270

Image provided by Al Plueddemann

 

The annual cycle of US Northeast continental shelf Cold Pool salinity. A linear trend has been fitted to the black‐highlighted data during the stratified season (April–October. (a) Observed salinity change at 67 m depth from the OOI Pioneer Array PMUI mooring. The ±1σ envelope depicts one standard deviation of interannual variability. (b) Salinity change from the NorthEast Shelf and Slope (NESS) model for all waters below the 10°C cold pool temperature threshold along 70.875°W. The cold pool along 70.875°W is fully eroded by September and no mean cold pool salinity can be computed for the rest of the fall. The ±1σ envelope depicts the combined variability across the cold pool volume on a given day and across all eight model years. Note that the Pioneer Array (a) measures Practical salinity (PSU) while the NESS model (b) advects absolute salinity (g/kg).

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