Some of the structure off the coast of Chile may also be consistent with
enhanced upwelling, something that was deduced to occur during the 20th century.
«The source of the acidified, low pH water varies regionally; along the coast resulting from
enhanced upwelling of carbon dioxide rich ocean waters.»
It could be
enhanced upwelling of cold water from deep ocean, but could that occur in a way that's doesn't affect ocean fluxes elsewhere doesn't seem obvious.
Not exact matches
Phytoplankton production is
enhanced by strong winds (because they cause
upwelling of nutrients from deeper waters) and diminished by weaker winds, and the scientists found evidence that trade winds were weaker then.
Enhanced north / south blocking patterns in periods of low solar activity
enhance flow in the Peruvian and Californian Currents facilitating increased eastern Pacific
upwelling of cold and nutrient rich water from the deep ocean.
More or less flow in the Peruvian Current
enhances or otherwise
upwelling in the region of the Humboldt Current.
This region of
upwelling propagates across the central Pacific driven by winds and Coriolis forces
enhancing Walker Circulation — which with Hadley Circulation establishes the dominant trade winds in the north and south sub equatorial regions.
Over the last 5000 years intermittent melting and reforming of sea ice in the Marguerite Bay is consistent with
enhanced sensitivity to ENSO forcing and increased
upwelling of CDW; a similar sensitivity to ENSO events has been documented over the most recent decades.
Limited sea ice
enhanced primary productivity that lasted for over 2000 years and was consistent with evidence of increased
upwelling of warm CDW.
The nutrient rich
upwelling enhances biological productivity — remember that this is a hydrological and biological pattern primarily.
The ocean as a whole is warming; however, coastal
upwelling may ultimately be
enhanced by alongshore winds, which strengthen in proportion to the temperature contrast between the oceanic and continental air masses [Sydeman et al., 2014].