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Summary

Description NOAA provides evidence for upwelling of corrosive "acidified" water onto the Continental Shelf. In the figure above, note the vertical sections of (A) temperature, (B) aragonite saturation, (C) pH, (D) DIC, and (E) pCO2 on transect line 5 off Pt. St. George, California. The potential density surfaces are superimposed on the temperature section. The 26.2 potential density surface delineates the location of the first instance in which the undersaturated water is upwelled from depths of 150 to 200 m onto the shelf and outcropping at the surface near the coast. The red dots represent sample locations
Source http://www.pmel.noaa.gov/pubs/outstand/feel3087/feel3087.shtml
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Licensing

Public domain
This image is in the public domain because it contains materials that originally came from the U.S. National Oceanic and Atmospheric Administration, taken or made as part of an employee's official duties.

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The original description page was here. All following user names refer to en.wikipedia.
Date/Time Dimensions User Comment
2013-12-22 10:14:46 1423× 1974× Jwratner1 ==Summary== source = http://www.pmel.noaa.gov/pubs/outstand/feel3087/feel3087.shtml = {{int:license-header}} == {{PD-USGov-DOC-NOAA}} {{PD-USGov}}

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applies to jurisdiction: United States of America
determination method: work of the federal government of the United States

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current22:44, 22 June 2016Thumbnail for version as of 22:44, 22 June 20161,423 × 1,974 (3.06 MB)FastilyCloneTransferred from en.wikipedia (MTC!)
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