For a number of years now, climate change skeptics have argued that there’s a key part of the Earth’s climate system that upends our expectations about global warming, and that is showing trends that actually cut in the opposite direction.
Scientists don’t fully understand why Antarctic sea ice is growing — suggested explanations have posited more glacial melt dumping cold fresh water into the surrounding seas, or the way the Antarctic ozone hole has changed the circulation of winds around the continent. In a new study in Nature Geoscience, though, researchers with the National Center for Atmospheric Research (NCAR) in Boulder, Colo., along with colleagues from the University of Washington in Seattle and Australia, suggest that the phenomenon is simply the result of natural variability of the climate system — driven, in this case, by changes in the tropical Pacific Ocean that reverberate globally.
“When you get changes in [sea surface temperatures] in some areas of the tropics, you affect precipitation, that affects the amount of energy released in the atmosphere,” said Gerald Meehl, the study’s lead author and a climate scientist with NCAR. “That starts affecting, through this kind of chain reaction process, circulation at great distances away.”
The new study confirms that the ice floating around Antarctica has been expanding — indeed, the expansion has accelerated since around the turn of the century. But that’s also around the time that a cycle dubbed the “Interdecadal Pacific Oscillation,” or IPO, shifted into a negative phase, which is characterized by ocean surface cooling in the tropical Pacific, and particularly its eastern part around the equator.
This is the same phenomenon that, scientists such as Meehl believe, helped fuel a global warming “slowdown” or “hiatus” during the 2000s (see also here). Heat was in effect buried deep below the surface of the Pacific Ocean, rather than bursting forth and influencing the globe, during this period.
But what’s new in the latest study is the suggestion that this negative IPO phase had consequences that stretched all the way to the Southern Ocean waters surrounding Antarctica — and that this, in turn, explains why most climate models didn’t predict the observed growth of Antarctic sea ice.
Most of the state-of-the-art climate change model simulations run to help support the 2013 report of the United Nations’ Intergovernmental Panel on Climate Change did not capture the growth of Antarctic sea ice that has occurred of late. Rather, the average of these models suggested that this ice should decline. This shows that skeptics who have cited the growing ice are raising a serious concern — this anomaly really does cry out for an explanation.
But the new study finds that in the small minority of climate change simulations that do happen to correctly capture these natural changes in the Pacific, and the global warming “slowdown” to boot, there is also growth in Antarctic sea ice. These are the models, it appears, that happened to get the role of natural variability in the Pacific right — or more specifically, to get the timing right for a phase shift in this ocean.
Out of “262 realizations of 2oth century climate, 10 of those got this observed slowdown of global warming happening at about the same time as in the observations, at the same magnitude,” Meehl said. “And for those 10, there was the negative phase of the IPO, and it also has the signature of Antarctic sea ice.”
But how could a naturally occurring climate wobble in the tropical Pacific Ocean translate into more Antarctic sea ice?
Here, the research suggests the key factor is how the state of that ocean in turn influences an Antarctic atmospheric phenomenon called the Amundsen Sea Low, a low-pressure region off the Antarctic coast that lies more or less directly south of the tropical Pacific.
This low-pressure region deepens (or sees its pressure drop even further) in negative IPO conditions, the study finds, which drive cooler seas in the eastern tropical Pacific. As this shift reverberates across the globe, it in turn means that down in Antarctica, winds increase in force around the area of low pressure at the center of the Amundsen Sea Low (winds blow inward toward regions of lower pressure). These stronger winds, in turn, push sea ice outward and away from the Antarctic continent, which leaves room for more ice to form in the gaps that are created — and increases the extent of sea ice overall.
“The dramatic decrease in Arctic sea ice, which currently exceeds model predictions and could exhibit a record or near-record low this year, is fairly straightforward to understand in terms of the unprecedented warming in the Arctic,” Michael Mann, a climate researcher at Penn State University, said in an email in response to Meehl’s study.
“By contrast, Antarctic sea ice is more complicated. It is dominated by what we refer to as ‘dynamical effects,’ especially the strength and position of the westerly winds over the southern ocean. Those dynamical effects are governed to a large extent by natural, internal climate variability, and it is unsurprising that the very modest increase in Antarctic sea ice in recent decades can be explained in terms of them.”
Granted, the precise causes behind the recent growth in Antarctic sea ice probably will be debated for some time. After all, there is much that scientists still don’t understand about this enormous but exceedingly remote region. Recent research continues to make new discoveries about why ice floating atop the southern ocean behaves in the way it does, for instance, and even about how it helps drive the circulation of ocean waters in the region, and therefore, around the world.
As for the future, Meehl says he thinks that the IPO has now turned back, and doesn’t think Antarctic sea ice will keep expanding in the same way. Notably, the ice did not continue its streak of breaking records in 2015. “Averaged over the next 5 to 10 years, if this is all correct, this increase in Antarctic sea ice extent would stop growing, maybe start shrinking a little bit,” he said.
For now, though, the new research suggests that two phenomena that have furnished some of the most popular arguments among climate change skeptics and doubters in the past several years — growing Antarctic sea ice, and a global warming slowdown or “hiatus” during the 2000s — can perhaps both be chalked up to simple natural climate variability, superimposed on top of a global warming trend.
And if that’s right, it means that despite heated debate over both of these matters, neither manages to dent — at all — the main message about ongoing global warming.
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