Macro-Scale Patterns in Upwelling/Downwelling Activity at North American West Coast.

PLoS One · 2016 · PMC5125649 · PMID 27893826

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a positive trendno p-value reported

For example, it can be observed a positive trend of MAF-3 during 1986–2007, changing amplitude about ~1000m 3 /s/100 m coastline at each station: in the northern station (39°N) the Ekman transport reached its highest value (1614m 3 /s/100 m coastline ) in 1999, meanwhile in the south (24°N) the peak value (1542 m 3 /s/100 m coastline ) was reached in 2007, eight years later ( Fig 4 ).

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