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Cited by 1,450

The DOI matches its Crossref record; 3 of the 3 references it cites were found in a registry or an index.

Evidence for Upwelling of Corrosive "Acidified" Water onto the Continental Shelf

Feely, Richard A., Sabine, Christopher L., Hernandez-Ayon, J. Martin, Ianson, Debby, Hales, Burke·2008·Science

Abstract

The absorption of atmospheric carbon dioxide (CO 2 ) into the ocean lowers the pH of the waters. This so-called ocean acidification could have important consequences for marine ecosystems. To better understand the extent of this ocean acidification in coastal waters, we conducted hydrographic surveys along the continental shelf of western North America from central Canada to northern Mexico. We observed seawater that is undersaturated with respect to aragonite upwelling onto large portions of the continental shelf, reaching depths of ∼40 to 120 meters along most transect lines and all the way to the surface on one transect off northern California. Although seasonal upwelling of the undersaturated waters onto the shelf is a natural phenomenon in this region, the ocean uptake of anthropogenic CO 2 has increased the areal extent of the affected area.

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Crossref · 10.1126/science.1155676

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Metadata

Authors
Feely, R. A., Sabine, C. L., Hernandez-Ayon, J. M., Ianson, D., & Hales, B.
Venue
Science
Published
2008-06-13
Volume
320
Issue
5882
Pages
1490-1492
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W2050103984
Cited by
1,450
References
3
FWCI
51.31
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Evidence for Upwelling of Corrosive "Acidified" Water onto the Continental Shelf. https://app.cochat.ai/papers/10.1126/science.1155676
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Feely, R. A., Sabine, C. L., Hernandez-Ayon, J. M., Ianson, D., & Hales, B. (2008). Evidence for Upwelling of Corrosive "Acidified" Water onto the Continental Shelf. Science. https://doi.org/10.1126/science.1155676

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

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