Future changes in coastal upwelling and biological production in eastern boundary upwelling systems.

Similarly, it can be inferred that a negative trend of UI during the transition month reflects a later onset or an earlier termination.

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Similarly, the CanCS-C, situated at lower latitudes, also demonstrates an increasing trend in upwelling intensity, albeit with a comparatively weaker magnitude (9.1 ± 1.3% per century) compared to the CanCS-P.

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The HCS, located in the South Pacific, exhibits a similar pattern, characterized by a significant increase in upwelling intensity in its poleward region (17.1 ± 2.1% per century) and a decreasing trend of upwelling intensity in its equatorward region (−7.0 ± 1.0% per century).

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