As Arctic Ocean Ice Disappears, The Global Climate Impacts Intensify #Auspol

Arctic Ocean sea ice melt as seen from the U.S. Coast Guard icebreaker Cutter Healy.
The top of the world is turning from white to blue in summer as the ice that has long covered the north polar seas melts away. This monumental change is triggering a cascade of effects that will amplify global warming and could destabilize the global climate system. 
BY PETER WADHAMS 
The news last week that summer ice covering the Arctic Ocean was tied for the second-lowest extent on record is a sobering reminder that the planet is swiftly heading toward a largely ice-free Arctic in the warmer months, possibly as early as 2020.


author Peter Wadhams ABOUT THE AUTHOR

Peter Wadhams, professor emeritus of ocean physics at Cambridge University, is a sea ice specialist with 46 years of research on sea ice and ocean processes in the Arctic and Antarctic. In more than 50 expeditions to both polar regions, he has worked from ice camps, icebreakers, and aircraft. He also has traveled six times on Royal Navy submarines under frozen north polar seas to conduct research. His new book is A Farewell to Ice: A Report from the Arctic. 

After that, we can expect the ice-free period in the Arctic basin to expand to three to four months a year, and eventually to five months or more. 

Since my days measuring the thickness of Arctic Ocean ice from British nuclear submarines in the early 1970s, I have witnessed a stunning decline in the sea ice covering the northern polar regions — a more than 50 percent drop in extent in summer, and an even steeper reduction in ice volume. 

Just a few decades ago, ice 10 to 12 feet thick covered the North Pole, with sub-surface ice ridges in some parts of the Arctic extending down to 150 feet. 

Now, that ice is long gone, while the total volume of Arctic sea ice in late summer has declined, according to two estimates, by 75 percent in half a century. 
The great white cap that once covered the top of the world is now turning blue — a change that represents humanity’s most dramatic step in reshaping the face of our planet. And with the steady disappearance of the polar ice cover, we are losing a vast air conditioning system that has helped regulate and stabilize earth’s climate system for thousands of years. 


Few people understand that the Arctic sea ice “death spiral” represents more than just a major ecological upheaval in the world’s Far North. The decline of Arctic sea ice also has profound global climatic effects, or feedbacks, that are already intensifying global warming and have the potential to destabilize the climate system. 

Indeed, we are not far from the moment when the feedbacks themselves will be driving the change every bit as much as our continuing emission of billions of tons of carbon dioxide annually. 

So what are these feedbacks, and how do they interact? The most basic stem from turning the Arctic Ocean from white to blue, which changes the region’s albedo — the amount of solar radiation reflected off a surface. Sea ice, in summer, reflects roughly 50 percent of incoming radiation back into space. Its replacement with open water — which reflects roughly 10 percent of incoming solar radiation — is causing a high albedo-driven warming across the Arctic. 
When covered almost entirely by ice in summer — which the Arctic was for tens of thousands of years — water temperatures there didn’t generally rise above freezing. Now, as the open Arctic Ocean absorbs huge amounts of solar radiation in summer, water temperatures are climbing by several degrees Fahrenheit, with some areas showing increases of 7 degrees F above the long-term average. 
Such changes mean that a system that was once a vast air conditioner has started to turn into a heater. Just how much extra heat are the dark waters of Arctic Ocean in summer adding to the planet? One recent study estimates that it’s equivalent to adding another 25 percent to global greenhouse emissions. 

To appreciate the complexity of these feedbacks and interactions, one need only look at the growing role played by waves and storms in the melting Arctic. 

With more of the Arctic Ocean becoming ice-free in summer, more waves are being generated. 

In summer, this increased wave action breaks up large ice floes into smaller fragments and hastens their melt. Then, in autumn, larger storms fed by open water cause wave-induced mixing of the Arctic Ocean, which brings up heat absorbed during the summer. This warms the water, making it harder for ice to form in the fall. 

I observed this phenomenon last September and October aboard the University of Alaska research vessel Sikuliaq in the western Arctic Ocean. 

After the warm summer of 2015, the advance of winter ice was slow and sporadic, apparently held back by the quantity of heat in the water column. 

Yet another Albedo- related effect with important global climatic repercussions is now unfolding in the Arctic. As ice-free Arctic waters have warmed, in turn warming the air above them, these rising temperatures have spread over land. This is an important factor in the increased melting of snow in Arctic terrestrial regions. Today, in midsummer, the Arctic land area covered by snow has decreased by several million square miles compared to five decades ago. These now-dark lands absorb more heat and further warm the Arctic — and the planet. 
Also, as the tundra and boreal forests heat up, runoff from snowmelt and waterways runs through warmer land, increasing the temperature of the great Arctic rivers such as the Mackenzie in Canada and the Ob, Lena, and Yenisei in Siberia. The warmer waters of these north-flowing rivers discharge into the Arctic basin, injecting more heat into the polar ocean. 
By my calculations, the terrestrial warming in the Arctic is roughly equivalent to a 25 percent boost in global CO2 emissions. 

This, combined with the warming caused by the loss of Arctic sea ice, means that the overall ice/snow albedo effect in the Arctic could add as much as 50 percent to the direct global heating effect of CO2. 

Scientists can debate the potential magnitude of such increases. But there is no doubt that they will be significant — vividly illustrating how the Arctic can become a driver of, rather than just a responder to, global climate change. 

What I am trying to offer in this tale of apparently unremitting gloom is a wake-up call rather than a statement of despair. What is taking place in the Arctic reinforces the conclusion of many scientists that last year’s Paris agreement to limit global warming to 2 degrees C is unrealistic so long as it only involves the reduction of CO2 emissions. As the various Arctic climate feedbacks show, we are fast approaching the stage when climate change will be playing the tune for us while we stand by and watch helplessly, with our reductions in CO2 emissions having no effect in the face of, say, runaway emissions of methane. 
What is needed today is a widespread global campaign to actually remove carbon dioxide from the atmosphere using techniques like direct air capture. In my view, initiatives to devise economically acceptable methods for carbon dioxide removal from the atmosphere should be the most important concern of science and technology. The success of these efforts will mean the difference between the prospect of a positive future for mankind and the certainty of a descent towards climate-driven chaos. 
In my professional lifetime, I have witnessed the transformation of the top of the world from a beautiful ice-bound expanse of wilderness to a region now characterized by warming and melting on all fronts. These changes represent a spiritual impoverishment of the earth, as well as a practical catastrophe for humanity. The time for action has long since passed. 

Press link for more: e360.yale.edu

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