Modeling analysis reveals shoreward shifting of subtropical western boundary currents under ocean warming, indicating climate-driven changes in regional coastal heat transport.
Western boundary currents flow along the western edge of subtropical oceans, transporting heat polewards, and are integral in the climate system. Using high-resolution models, this work shows that western boundary currents will shift shorewards as a result of increased stratification driven by climate change.
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Yang et al. (2025) studied this question.
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