Evidence for Upwelling of Corrosive "Acidified" Water onto the Continental Shelf¶
Feely. (2008). Evidence for Upwelling of Corrosive "Acidified" Water onto the Continental Shelf. Science.
Cited by¶
1 citation across 1 artifact.
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Domain-specific¶
- Ocean Acidification
- The aragonite saturation horizon (the depth below which seawater is corrosive to aragonite) has shoaled measurably in multiple ocean basins, and in upwelling zones on the US Pacific coast already reaches surface waters during seasonal upwelling events, affecting commercially important shellfish at their most vulnerable larval stages
This sourceShipboard surveys finding aragonite-undersaturated water upwelling onto large portions of the continental shelf of western North America and reaching the surface off northern California.
Supported in partVerified against the publisher's abstract
“We observed seawater that is undersaturated with respect to aragonite upwelling onto large portions of the continental shelf, reaching depths of approximately 40 to 120 meters along most transect lines and all the way to the surface on one transect”
- The aragonite saturation horizon (the depth below which seawater is corrosive to aragonite) has shoaled measurably in multiple ocean basins, and in upwelling zones on the US Pacific coast already reaches surface waters during seasonal upwelling events, affecting commercially important shellfish at their most vulnerable larval stages
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