«Areas of greatest vulnerability will likely be where deep waters, naturally low in pH, meet acidified surface waters,» such as areas of
coastal upwelling along the West Coast and in estuary environments such Hood Canal, the new study predicts.
Not exact matches
These include eastern boundary current
upwelling systems such as those off the U.S. west coast
along coastal California, Oregon and Washington, deep - sea and subsurface oxygen minimum zones, and
coastal waters that are already experiencing excess nutrient levels (eutrophication) and low dissolved oxygen (hypoxia) due to human - driven nutrient pollution from land - based activities.
increased CO -LCB- sub 2 -RCB- by using ocean models that include realistic processes such as horizontal heat transport, vertical mixing due to convection and small - scale processes, and
upwelling along coastal regions and the equator.
Accordingly,
upwelling of waters acidified by anthropogenic CO2 has led to a further decrease in surface pH, as reported in the eastern Pacific Ocean
along the west coast of North America, from central Canada to northern Mexico, where shoaling of the layer of seawater undersaturated with aragonite increased the frequency and magnitude of
coastal acidification associated with
upwelling events (Feely et al. 2008, 2010).