If the West Antarctic Ice Sheet collapses, as many experts believe it will because of global warming, the resulting sea level rise will be significantly higher than is currently projected, a new study published in Science has found.
Already projected to average between 16 and 17 feet around the world, the new figures suggest the rise would likely be almost 21 feet in such places as Washington, D.C. Many coastal areas would be devastated and much of Southern Florida would disappear.
“We aren’t suggesting that a collapse of the West Antarctic Ice Sheet is imminent,” said study author Peter Clark, a professor of geosciences at Oregon State University. “But these findings do suggest that if you are planning for sea level rise, you had better plan a little higher.”
“A study was done more than 30 years ago pointing out this gravitational effect, but for some reason it became virtually ignored,” Clark said. “People forgot about it when developing their sea level projections for the future.”
And aside from incorporating the gravitational effect, the new study adds further wrinkles to the calculation – the weight of the ice forcing down the land mass on which it sits, and also affecting the orientation of the Earth’s spin. When the ice is removed, it appears the underlying land would rebound, and the Earth’s axis of rotation defined by the North and South Pole would actually shift about one-third of a mile, also affecting the sea level at various points.
When these forces are all taken into calculation, the sea level anywhere near Antarctica would actually fall, the report concludes, while many other areas, mostly in the Northern Hemisphere, would go up.
“If this did happen, there would also be many other impacts that go far beyond sea level increase, including much higher rates of coastal erosion, greater damage from major storm events, problems with ground water salinization, and other issues,” Clark explained. “And there could be correlated impacts on other glaciers and ice sheets in coastal areas that could tend to destabilize them as well.”
A significant area of the concern is that much of the base of this huge ice mass actually sits below sea level, forced down to the bedrock by the sheer weight of the ice above it. Its edges flow out into floating ice shelves, including the huge Ross Ice Shelf and Ronne Ice Shelf. This topography makes it “inherently unstable,” Clark said.
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