From Baja to BC, it’s shown up near the ocean’s surface sooner than we thought.
Five years ago, many scientists probably thought they’d never see large pools of corrosive water near the ocean’s surface in their lifetimes.
Basic chemistry told them that as the oceans absorbed more carbon dioxide pollution from cars and smokestacks and industrial processes, seawater would become more acidic. Eventually, the oceans could become corrosive enough to kill vulnerable forms of sea life like corals and shellfish and plankton.
But scientists believed the effects of this chemical process — called ocean acidification — would be confined to deep offshore ocean waters for some time. Models projected it would take decades before corrosive waters reached the shallow continental shelf off the Pacific Coast, where an abundance of sea life lives.
Until a group of oceanographers started hunting for it.
“What we found, of course, was that it was everywhere we looked,” said Richard Feely, an oceanographer at the National Oceanic and Atmospheric Administration’s Pacific Marine Environmental Laboratory in Seattle, Washington, who was one of the first to recognize the trouble ahead.
Vancouver Pride 2011
The researchers found surprisingly acidic water — corrosive enough to begin dissolving the shells and skeletal structures of some marine creatures — at relatively shallow depths all along the west coast, from British Columbia to the tip of Baja California. Researchers hadn’t expected to see that extent of ocean acidification until the middle to the end of this century. But in a seasonal process called “upwelling,” summertime winds pushed surface waters offshore and pulled deeper, more acidic water towards the continental shelf, shorelines, and beaches.
Or as one Oregon State University marine ecologist put it: “The future of ocean acidification is already here off the Oregon Coast.”
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Jennifer Langston, The Tyee, 16 June 2011. Full article.
