On a warming Earth, seas inevitably rise, as ice on land melts and makes its way to the ocean. And not only that – the ocean itself swells, because warm water expands. We already know this is happening – according to NASA, seas are currently rising at a rate of 3.5 millimeters per year, which converts to about 1.4 inches per decade.
However, scientists have long expected that the story should be even worse than this. Predictions suggest that seas should not only rise, but that the rise should accelerate, meaning that the annual rate of rise should itself increase over time. That’s because the great ice sheets, Greenland and Antarctica, should lose more and more mass, and the heat in the ocean should also increase.
The problem, or even mystery, is that scientists haven’t seen an unambiguous acceleration of sea level rise in a data record that’s considered the best for observing the problem – the one produced by the TOPEX/Poseidon satellite, which launched in late 1992 and carries an instrument, called a radar altimeter, that gives a very precise measurement of sea level around the globe.
This record actually shows a decrease in the rate of sea level rise from the first decade measured by the satellite (1993 to 2002) to the second one (2003 to 2012). “We’ve been looking at the altimeter records and scratching our heads, and saying, ‘why aren’t we seeing an acceleration in the satellite record?’ We should be,” said John Fasullo, a climate scientist at the National Center for Atmospheric Research in Boulder, Colorado.
The cause? The 1991 eruption of Mount Pinatubo in the Philippines, which filled the planet’s stratosphere with aerosols that reflected sunlight away from the Earth and actually led to a slight sea level fall in ensuing years as the ocean temporarily cooled.
“What we’ve shown is that sea level acceleration is real, and it continues to be going on, it’s ongoing, and we understand why you don’t see it in the short satellite record,” said Fasullo, who conducted the research along with scientists from the University of Colorado in Bolder and Old Dominion University.
The study was performed using a suite of 40 climate change models to determine how the Pinatubo eruption affected seas and the global distribution of water. The scientists estimate as a result that sea level not only fell between 5 and 7 millimeters due to a major ocean cooling event in the eruption’s wake, but then experienced a rebound, or bounce back, of the same magnitude once the influence of the eruption had passed.
This had a major effect on what the satellite record of sea level looks like, because the bounce-back occurred earlier in the record and made the sea level rise then appear extra fast. So the researchers conclude that while no official acceleration trend can be seen in the satellite record now, that’s an artificial consequence of Pinatubo and should be gone over time – barring another Pinatubo-like event.
“Our initial impression of sea level rise was not only influenced by climate change and the rate of change, but the response and the recovery from the eruption itself,” says Fasullo. “Those effects largely have ebbed by now, and once we get a few more years into the altimeter record, we should see a clear acceleration. That’s really the punchline of the article.”
In fact, the researchers also removed the sea level effect of Pinatubo, and found that when they did so they could see sea level rise acceleration happening already.
Another study last year, using a different record of sea level rise – global tide gauges – in addition to satellite data, also found that sea level rise has accelerated in the last 15 years.
One sea level rise expert who was not involved in the new study, Robert Kopp of Rutgers University, praised the work in response to a query from the Post.
The study, Kopp explained by email, found that the Pinatubo eruption would have caused seas to fall “just before the start of the altimetry record, the recovery from which was spread out of the remainder of the 1990s and therefore masked some of the acceleration that would otherwise have been seen in the tide-gauge record between the 1990s and the 2000s. This makes strong physical sense.”
It also aligns better with actual observations from Greenland and Antarctica. Scientists have shown that both of the Earth’s major ice sheets have seen an accelerating rate of ice loss in recent years, which ought to help drive an accelerating rate of sea level as well.
The key question then becomes just how fast the annual rate of sea level rise can actually increase. In one thought experiment recently, former NASA climate scientist James Hansen calculated the consequences if the “doubling time” for ice loss is as fast as 10 years – finding dramatic sea level increases as a result.
“Doubling times of 10, 20 or 40 years yield sea level rise of several meters in 50, 100 or 200 years,” Hansen’s study concluded. However, it is far from clear at this point that ice loss is actually increasing this rapidly.
So far, the U.N.’s Intergovernmental Panel on Climate Change officially estimates that the high-end sea-level rise projection for 2100 is lower than some of these scenarios, closer to about 1 meter (3.3 feet) by that year. But that has recently been challenged by new work estimating that Antarctica alone could add this much to global sea levels by 2100 if high levels of human greenhouse gas emissions continue.
Fasullo says that debate – over precisely how fast acceleration happens, or where that leaves us in 2100 – remains unresolved. For now, he says, at least it’s pretty clear that the acceleration is actually happening as expected.
“Accelerated sea level rise is real, and it’s ongoing, and it’s not something we should doubt based on the altimeter record,” said Fasullo.