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magazine / jf10
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January/February 2010 issue |
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INTERNATIONAL POLAR YEAR
In springtime, something strange happens in the Arctic atmosphere. Canadian scientists follow the chemical clues. Photo: Spencer Brown
Mercury mystery: Scientists with the OASIS project work to unlock the Arctic’s heavy metal mystery
Hot water: Investigate global warming’s impact on marine wildlife and Ocean currents part 1 and part 2
Finding the flow: Watch animations of Arctic currents
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What is IPY?

International Polar Year (IPY) 2007-08 is a collaborative international effort to research the polar regions. Discover its key issues. Read more »
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Community research station

At the Kluane Lake Research Station, what’s happening in the Arctic is a family affair. Read more »
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Are the Inuit Healthy?

A mass health checkup of the Inuit attempts to set right a terrifying legacy left by the C.D. Howe. Read more »
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The Arctic mercury mystery

Scientists rush to unlock why Mercury taints the Arctic air and what this means for the planet. Read more »
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A Canadian scientist in Norway

Does sending a geography student to Norway offer the answer to fostering Arctic scientists of the future?
Read more »
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The Future of Arctic Research

After the glut of International Polar Year funding evaporates, what does the future hold for Arctic exploration?
Read more »
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Multimedia
Discover videos, interactive features and photo essays mapping the issues, science and communities behind the International Polar Year.
View now »
Mercury is a Roman god, a lifeless planet, a former singer with Queen and a mystery enfolded in the fog of the
coldest, most isolated coves of Canada.
Up in the Arctic, when the spring sun finally deigns to rise after abandoning the land for months, something unusual
occurs. Compounds of the chemical element mercury — the furtive quicksilver that takes our temperature and lights
our offices — suddenly vanish from the sky.
| With its high salt content, first-year sea ice, as opposed to
the permanent ice pack, may hold the key to the mystery of
the missing mercury. In a warming Arctic, young ice abounds. |
One moment, the air is tainted with mercury and flush with highly reactive low-level ozone, and the next instant,
it is devoid of the two compounds. Like baseball, blackflies and income tax, this happens every spring. No one understands
why mercury disappears or how it reassembles in the lower atmosphere when the weary sun sets in fall.
A leading Canadian scientist investigating the phenomenon, Jan Bottenheim of Environment Canada, calls it
“amazing and mind-boggling,” and he has been poking around the mystery for more than 20 years.
If mercury were not a known and powerful neurotoxin, capable of seriously damaging the human nervous system,
and if ozone were not a greenhouse gas and the instigator of chemical reactions with many human-caused pollutants,
this subject might be merely academic. But when mercury vanishes from the air at Arctic sunrise, it has to go somewhere:
onto the ice, onto the snow, into the sea, into the fish, into the seals and, perhaps, into the bodies of the
people of Canada’s North. So there is an urgency to the search for answers.
That search is the main focus of the Ocean-Atmosphere-Sea Ice-Snowpack (OASIS) project, one of the studies
under the International Polar Year umbrella. OASIS, which runs to 2011, sends intrepid scientists from Canada, Europe
and the United States to the Arctic’s most desolate coastlines and out onto the open seas. There, they deploy remotelymonitored
sleds, floating sampling stations, ship-based experiments and their own sense of wonder.
In 2008, OASIS-Canada scientists spent three months on the Canadian Coast Guard icebreaker CCGS Amundsen
taking measurements, collected data from an ozone monitor aboard a French sailboat named Tara, which was left to drift
with the Arctic currents, and launched the first of three planned high-tech buoys in the Beaufort Sea. No longer
confined to taking measurements from shore, the researchers are now able to study bodies of water and ice from Alaska to
Quebec and from Hudson Bay to the North Pole.
Their recording instruments are some the hardiest ever designed. Several have cute nicknames, such as a sled known
as OOTI, for Out On The Ice, that relays data on atmospheric mercury via a wireless communications link. The
floating ozone gauges are known as O-buoys.
If the recording instruments are hardy, so, too, are the researchers who venture north. OASIS-Canada investigator
and atmospheric mercury specialist Alexandra (Sandy) Steffen has worked at Canadian Forces Station Alert 21
times. In her more comfortable office at the Toronto headquarters of Environment Canada, Steffen describes the
research base at Alert, 800 kilometres from the North Pole, as “a beautiful lab to study. It’s spectacular. My sister lived
in Africa, and she had what she called mal d’Afrique. I have mal d’Arctique.”
At a computer station in the Toronto laboratory, Steffen shows off a graph of the suspect compounds’ mercurial rise
and fall. It is a cardiogram of jagged peaks and plunging valleys that looks like the pulse of a beating world — a
wealth of hard-won information from across the Arctic that has a story to tell.
That story began more than 20 years ago. The depletion of ozone in the atmosphere over the Arctic was first reported
in scientific journals in 1986 by Bottenheim and his colleagues at Environment Canada, based on their observations
at Alert. In 1998, Environment Canada’s William Schroeder reported his discovery that mercury depletion
occurs simultaneously with ozone depletion.
Over the years, the Canadian scientists developed a greater understanding of the chemistry behind these occurrences.
They now know, for example, that when ozone reacts with sea salt on frozen surfaces such as ice and snow, a form of
bromine atom is produced. Bromine reacts with ozone and mercury in different ways.
“The reaction of bromine atoms with ozone leads to the destruction of ozone molecules, so ozone effectively disappears,”
explains Bottenheim. “The reaction between bromine atoms and mercury does not lead to the destruction of
mercury but, instead, leads to the production of a new molecule that includes the mercury and bromine atoms.” The
chemical identity and properties change, but the mercury is not destroyed. Rather, it disappears, possibly migrating
from the atmosphere to the snowpack and ocean. “There are liable to be other consequences we haven’t even scratched
yet,” Bottenheim says.
For reasons that still puzzle Bottenheim, these phenomena are observed only in the spring. He speculates that
first-year ice, as opposed to the permanent ice pack, is a particularly effective type of ice surface to drive the depletion
chemistry. For one thing, “young” sea ice cover is more concentrated in sea salt, the source of bromine. For
another, first-year ice features plenty of open leads that refreeze, which can then result in the promotion of frost flowers, whose ice crystals are thought to “scavenge”
chemicals from the atmosphere.
If it is true that first-year ice is responsible for the chemical train of events, then mercury levels in the North
may rise with the warming of the Arctic Ocean. Changes in the Arctic ecosystem drive climate changes elsewhere on
Earth, which explains the urgency to understand where the mercury goes when spring arrives.
So the work of OASIS continues, even in the early winter, when mercury and ozone re-form in the Arctic
atmosphere, waiting for the pulse of virgin sunshine that will banish the lightless skies.
A frequent contributor to the magazine, Allen Abel lives near Washington, D.C. Photographer Spencer Brown is based in
San Francisco.
Related content and resources:
Photo Club
Read a one-on-one interview with photographer Fritz Mueller and view a gallery of his photos.
The Canadian Atlas Online
A great source of information on International Polar Year in Canada, from its origins to the latest research findings.
Interactive IPY Map
An interactive map that locates, describes and illustrates more than 50 IPY projects across Canada’s North.
| Comments on this article | Leave a comment | Your post really informative.It will be a growing area to watch this year. Like you say, comments keep the conversation going.They also provide additional insight to the readers and the bloggers. Comments offer a different perspective and put a "face" to the readership.Orange County Web Design
I am glad to read this post, its an interesting one. I am always searching for quality posts and articles and this is what I found here, I hope you will be adding more in future. Thanks
I wish I was a scientist, because I believe in what these are doing and I wish I could participate in determining the facts in this issue. There is a lot of science that I think most people are particularly unaware of and it's important the information get out. I envy the writer's ability to cover this story. The best I can do is bug my MP to get some traction on the issue. Good luck writer and scientists all. The north is Canada and we shouldn't forget about it.
Nice to read an article on another promising young Labradorian! Good Luck, Robert!!
Not really a cause for rejoicing. Dozens of reports indicate this ice is thin and that the Arctic has changed in a disastrous way. http://www.cbc.ca/technology/story/2009/02/21/arctic-ice.html
http://www.metronews.ca/ottawa/canada/article/414964melt-season-for-canadian-arctic-sea-ice-outpacing-global-average-study
http://www.guardian.co.uk/environment/2009/jan/25/melting-arctic-north-pole-explorers
http://www.guardian.co.uk/environment/2007/sep/05/climatechange.sciencenews
http://www.nytimes.com/2007/10/02/science/earth/02arct.html
I was fortunate enough to do some research at KLRS with the University of Ottawa and let me tell you, Andy and the gang really make you feel at home. I wish you all the best with renovations and I hope to one day go back to the station to show my children how wonderful it is.
It's good to know that polar ice is increasing again: "A report from the US National Snow and Ice Data Center in Colorado finds that Arctic summer sea ice has increased by 409,000 square miles, or 26 per cent, since 2007."
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