Galveston
By Alex Kirby
Climate News Network
Each degree Celsius (1.8 degrees Fahrenheit) of global warming may raise world sea levels by more than two meters (6.6 feet), a new scientific study concludes.
Sea-level rise may be slow to show its hand but once it really starts, researchers say, it will keep going for centuries, with baleful effects. For each degree by which the Earth warms, they believe, sea levels will probably rise by over two meters.
Some recent research has suggested that the future rate of sea-level rise may not be as fast as scientists had expected. But a study published in the Proceedings of the National Academy of Sciences, “The multi-millennial sea-level commitment of global warming” (article available in open access on publication: http://www.pnas.org/content/early/recent), paints a different picture.
Today’s greenhouse gas emissions will cause sea levels to rise for centuries to come. “CO2, once emitted by burning fossil fuels, stays an awful long time in the atmosphere”, says Anders Levermann, lead author of the study and research domain co-chair at the Potsdam Institute for Climate Impact Research, Germany. “Consequently, the warming it causes also persists.”
The oceans and ice sheets are slow to respond to warming, simply because of their enormous mass, which is why observed sea-level rise is now measured in millimeters per year. But once they start responding, they are unrelenting.
“The problem is: once heated out of balance, they simply don’t stop”, says Levermann. “We’re confident that our estimate is robust because of the combination of physics and data that we use.”
The study is the first to combine evidence from the Earth’s early climate history with comprehensive computer simulations using physical models of all four major contributors to long-term global sea-level rise.
Correctly estimating future rise
During the 20th century, sea level rose by about 0.2 meters (7.9 inches), and it is projected at the moment to rise by significantly less than two meters by 2100, even under the most far-reaching scenarios considered.
But the researchers say past climate records, which average sea-level and temperature changes over a long time, suggest much higher sea levels during periods of Earth history that were warmer than at present.
For this study the international team used data from sediments from the sea bottom and ancient raised shorelines found on coastlines around the world. All the models are based on fundamental physical laws.
“The Antarctic computer simulations were able to simulate the past five million years of ice history, and the other two ice models were directly calibrated against observational data – which in combination makes the scientists confident that these models are correctly estimating the future evolution of long-term sea-level rise”, says Peter Clark, a paleo-climatologist at Oregon State University and co-author of the study.
While it remains a challenge to simulate rapid ice loss from Greenland and Antarctica, the models are able to capture ice loss that occurs on long time scales where the research team says a lot of the small rapid motion averages out.
If global mean temperature rises by 4 degrees C (7.2 degrees F) compared with pre-industrial times, which in a business-as-usual scenario is projected to happen within less than a century, the Antarctic ice sheet will contribute about 50 percent of sea-level rise over the next two millennia.
“Continuous sea-level rise is something we cannot avoid unless global temperatures go down again. Thus we can be absolutely certain that we need to adapt”
The researchers say that while thermal expansion of the ocean (the way warmer water expands) and melting mountain glaciers are the most important factors causing sea-level change today, the Greenland and Antarctic ice sheets will be the dominant contributors within the next two millennia.
Half of that rise might come from ice loss in Antarctica, which is currently contributing less than 10 percent to global sea-level rise. Greenland will add another 25 percent to the total, while thermal expansion, currently the largest component of sea-level rise, will contribute only about 20 percent. The share from mountain glaciers will decline to less than 5 percent, mostly because many will shrink to a minimum.
“Continuous sea-level rise is something we cannot avoid unless global temperatures go down again”, Levermann says. “Thus we can be absolutely certain that we need to adapt.
“Sea-level rise might be slow on the time scales on which we elect governments, but it is inevitable and therefore highly relevant for almost everything we build along our coastlines, for many generations to come.”
The International Energy Agency said last month that the world was on a path which was likely to result in a temperature increase of between 3.6 degrees C (6.5 degrees F) and 5.3 degrees C (9.5 degrees F). The following week the World Bank said that, without concerted action now, the world could warm by 2 degrees C (3.6 degrees F) within 20 or 30 years, and by 4 degrees C (7.2 degrees F) by the end of the century.
Recent research suggests that even fairly modest sea-level rise is cause for concern, chiefly because of its ability to increase the probable frequency of severe storms and floods.
Earlier this month the World Meteorological Organization published its decadal report, “The Global Climate 2001-2010: a decade of climate extremes.”
It reported that during the decade from 2001 to 2010 “global mean sea levels rose about three millimeters per year, about double the observed 20th century trend of 1.6 mm (0.06 inches) per year. Global sea level averaged over the decade was about 20 cm (0.79 inches) higher than that of 1880.”
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