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Evolution of upwelling systems coupled to the long-term variability in sea surface temperature and Ekman transport
2011
Climate Research (CR)
In the early 1990s it was hypothesized that the global warming process would produce an increase in sea-land temperature gradients and, subsequently, enhance the wind patterns responsible for coastal upwelling. Hence, an increase in the intensity of coastal upwelling was expected in the main upwelling ecosystems around the world. However, recently published analyses of the evolution of coastal upwelling processes have shown contradictory evidence. For this reason, time series of sea-surface
doi:10.3354/cr00989
fatcat:srnq7zvcx5as3nhfq37b2sr35i