Not exact matches
Washington, which produces farmed oysters, clams and mussels, is particularly vulnerable to acidification, for two reasons: seasonal, wind - driven
upwelling events bring low -
pH waters from the deep ocean towards the shore, and land - based nutrient runoff from farming fuels algal growth, which also lowers
pH.
At
pH 7.1, which is expected to roughly approximate the
pH of
water upwelling on the West Coast with ocean acidification, zoeae survival remained low at 21 percent.
«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.
Inspired by dynamic shifts in
pH due to
upwelling — the movement of nutrient - rich
water toward the ocean surface — the researchers took urchins from the Santa Barbara Channel and brought them into the lab.
Lowest
pH (7.8) and highest pCO2 (658.3 µatm) values measured during a cold -
water intrusion event in the non-
upwelling season were similar to those minimum values reported from
upwelling season (
pH = 7.8, pCO2 = 643.5 µatm), unveiling that natural acidification also occurs sporadically in the non-
upwelling season.
So it is very reasonable to assume that the contribution of human - produced CO2 levels to the
ph change today in
upwelled waters is thus (45 / 120) *.1 or.0375.
«The source of the acidified, low
pH water varies regionally; along the coast resulting from enhanced
upwelling of carbon dioxide rich ocean
waters.»
To attribute her observed dissolution to anthropogenic CO2, Bednarsek argued recent invasions of anthropogenic CO2 into the surface
water had lowered its surface
pH to such an extent, mixing no longer counteracted the low
pH of
upwelled water.
Because oceans contain over 50 times as much CO2 as the atmosphere, surface
pH is more sensitive to changes in the rates of
upwelling of low -
pH, carbon - rich deep
waters.
In Washington and Oregon, oysters farms are in coastal Pacific
waters where
upwelling currents are bringing up cold, deep
water with higher amounts of CO2 and a more acidic
pH. Watch and listen to two oyster farmers from Taylor Shellfish Farms in Washington state talk how about ocean acidification is impacting their young oysters.
Several physical variables and biological processes drive this variability in
pH, including temperature, salinity,
upwelling,
water currents, river runoff, sea ice melt, photosynthesis, respiration, calcification and dissolution.
If the
upwelling on the Pacific coast in 2012 brought up
water that is 30 - 50 years old, then it is very doubtful that the low
pH is due to ACO2.
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).
Upwelling waters are corrosive naturally, but their
pH may decline further over time due to OA.
Organisms living in areas where
upwelling of cool, low
pH water occurs (e.g. Eastern Pacific and Baltic Sea) may be acclimatized / adapted to acidification [31 — 34], whereas those living in areas with strong warming (e.g. Eastern Australia) may be acclimatized / adapted to increased temperature [7,35].