Toronto Star

Pacific Ocean may rise higher than expected, California says

Ocean Protection Council says waters off San Francisco could rise by up to 3 metres

- ELLEN KNICKMEYER THE ASSOCIATED PRESS

SAN FRANCISCO— New climate-change findings mean the Pacific Ocean off California may rise higher, and storms and high tides hit harder, than previously thought, officials said.

The state’s Ocean Protection Council on Wednesday revised upward its prediction­s for how much the waters off California will rise as the climate warms. The forecast helps agencies in the most populous state in the U.S. plan for climate change as rising water seeps toward low-lying airports, highways and communitie­s, especially in the San Francisco Bay Area.

Discoverie­s that ice sheets are melting increasing­ly fast in Antarctica, which holds nearly 90 per cent of the world’s ice, largely spurred the change. As fossil-fuel emissions warm the Earth’s atmosphere, melting Antarctic ice is expected to raise the water off California’s 1,770 kilo- metres of coastline even more than for the world as a whole.

“Emerging science is showing us a lot more than even five years ago,” council deputy director Jenn Eckerle said Thursday.

Gov. Jerry Brown has mandated that state agencies take climate change into account in planning and budgeting.

In the best-case scenario, waters in the vulnerable San Francisco Bay, for example, likely would rise between one-third of a metre and three-quarters of a metre by the end of this century, the ocean council said.

However, that’s only if the world cracks down on climate-changing fossil-fuel emissions far more than it is now.

The worst-case scenario entails an even faster melting of Antarctic ice, which could raise ocean levels off California a devastatin­g three metres by the end of this century, the state says. That’s at least 30 times faster than the rate over the past 100 years.

Scientists say rising water from climate change already is playing a role in extreme winters such as this past one in California.

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