According to a Rutgers University-led study, global sea level rose faster in the 20th century than in any of the 27 previous centuries.
Moreover, without global warming, global sea level would have risen by less than half the observed 20th century increase and might even have fallen.
Sea level change is a naturally occurring process. Since the last glacial maximum, some 18,000 years ago, de-glaciation has taken place and this natural global warming has led to sea-level rise.
For this study, a team led by Andrew Kemp, an assistant professor of earth and ocean sciences at Tufts University, and Benjamin Horton, a professor in Rutgers' Department of Marine and Coastal Sciences, compiled a new database of geological sea-level indicators from marshes, coral atolls and archaeological sites that spanned the last 3,000 years.
Instead, global sea level rose by about 14 centimeters, or 5.5 inches, from 1900 to 2000. That's a substantial increase, especially for vulnerable, low-lying coastal areas.
Global sea-level is estimated using averaged measurements from a worldwide network of coastal tide-gauges or from satellite-borne instruments. Because they represent a worldwide average, neither of these figures has any useful application to coastal management in specific locations, stated Bob Carter, a geologist and environmental scientist.
The 20th century rise was extraordinary in the context of the last three millennia - and the rise over the last two decades has been even faster, said Robert Kopp, the lead author and an associate professor in Rutgers' Department of Earth and Planetary Sciences.
The study, published in Proceedings of the National Academy of Sciences, used a new statistical approach developed over the last two and a half years by Kopp, his postdoctoral associates Carling Hay and Eric Morrow, and Jerry Mitrovica, a professor at Harvard University.
Notably, the study found that global sea level declined by about 8 centimeters from 1000 to 1400, a period when the planet cooled by about 0.2 degrees Celsius.
It is striking that we see this sea-level change associated with this slight global cooling, Kopp said. By comparison, global average temperature today is about 1 degrees Celsius higher than it was in the late 19th century.
Scenarios of future rise depend upon our understanding of the response of sea level to climate changes, Horton said. Accurate estimates of sea-level variability during the past 3,000 years provide a context for such projections.
Kemp said, As geologists, we can reconstruct how sea level changed at a particular site, and progress in the last 10 years has allowed us to do so with ever more detail and resolution. Gathering together and standardizing these reconstructions gave us a chance to look at what they had in common and where they differed, both of which can tell us about the causes of past, present and future sea-level change.
Kopp's collaborators Klaus Bittermann and Stefan Rahmstorf at the Potsdam Institute for Climate Impact Research in Germany used the study's global sea-level reconstruction to calculate how temperatures relate to the rate of sea-level change.
A companion report finds that, without the global warming-induced component of sea-level rise, more than half of the 8,000 coastal nuisance floods observed at studied U.S. tide gauge sites since 1950 would not have occurred. The Climate Central report, led by Benjamin Strauss and co-authored by Kopp, Bittermann, and William Sweet of NOAA, was also published today.
The Kopp-led study also found that it's very likely that global sea level will rise by 1.7 to 4.3 feet in the 21st century if the world continues to rely heavily upon fossil fuels. Phasing out fossil fuels will reduce the very likely rise to between 0.8 and 2.0 feet.