Showing posts with label Arctic's melting trend. Show all posts
Showing posts with label Arctic's melting trend. Show all posts

Monday, 6 May 2013

Arctic Ocean 'acidifying rapidly'


Arctic Ocean 'acidifying rapidly'

Saunders Island and Wolstenholme Fjord with Kap Atholl in the background is shown in this picture taken during an Operation IceBridge survey flight in April 2013

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The Arctic seas are being made rapidly more acidic by carbon-dioxide emissions, according to a new report.
Scientists from Norway's Center for International Climate and Environmental Research monitored widespread changes in ocean chemistry in the region.
They say even if CO2 emissions stopped now, it would take tens of thousands of years for Arctic Ocean chemistry to revert to pre-industrial levels.
Many creatures, including commercially valuable fish, could be affected.
They forecast major changes in the marine ecosystem, but say there is huge uncertainty over what those changes will be.
It is well known that CO2 warms the planet, but less well-known that it also makes the alkaline seas more acidic when it is absorbed from the air.

The Arctic

arctic volcano
  • The Arctic region contains a vast ice-covered ocean roughly centred on the Earth's geographic North Pole
  • The Sun doesn't rise at all on the shortest day of the year within the Arctic Circle
  • Humans have inhabited the Arctic region for thousands of years, and the current population is four million
  • Geologists estimate the Arctic may hold up to 25% of the world's remaining oil and natural gas
Absorption is particularly fast in cold water so the Arctic is especially susceptible, and the recent decreases in summer sea ice have exposed more sea surface to atmospheric CO2.
The Arctic's vulnerability is exacerbated by increasing flows of freshwater from rivers and melting land ice, as freshwater is less effective at chemically neutralising the acidifying effects of CO2.
The researchers say the Nordic Seas are acidifying over a wide range of depths - most quickly in surface waters and more slowly in deep waters.
The report’s chairman, Richard Bellerby from the Norwegian Institute for Water Research, told BBC News that they had mapped a mosaic of different levels of pH across the region, with the scale of change largely determined by the local intake of freshwater.
“Large rivers flow into the Arctic, which has an enormous catchment for its size,” he said.
“There’s slow mixing so in effect we get a sort of freshwater lens on the top of the sea in some places, and freshwater lowers the concentration of ions that buffers pH change. The sea ice has been a lid on the Arctic, so the loss of ice is allowing fast uptake of CO2.”
This is being made worse, he said, by organic carbon running off the land – a secondary effect of regional warming.
“Continued rapid change is a certainty,” he said.
“We have already passed critical thresholds. Even if we stop emissions now, acidification will last tens of thousands of years. It is a very big experiment.”
The research team monitored decreases in seawater pH of about 0.02 per decade since the late 1960s in the Iceland and Barents seas.
Chemical effects related to acidification have also been encountered in surface waters of the Bering Strait and the Canada Basin of the central Arctic Ocean.
Scientists estimate that the average acidity of surface ocean waters worldwide is now about 30% higher than before the Industrial Revolution.
The researchers say there is likely to be major change to the Arctic marine ecosystem as a result. Some key prey species like sea butterflies may be harmed. Other species may thrive. Adult fish look likely to be fairly resilient but the development of fish eggs might be harmed. It is too soon to tell.

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Saturday, 3 December 2011

Arctic's melting trend

Pause in Arctic's melting trend

Walrus 
Walrus have been seen on Alaska's north coast in unusual numbers
This summer's melt of Arctic sea ice has not been as profound as in the last two years, scientists said as the ice began its annual Autumn recovery.
At its smallest extent this summer, on 12 September, the ice covered 5.10 million sq km (1.97 million sq miles).
This was larger than the minima seen in the last two years, and leaves 2007's record low of 4.1 million sq km (1.6 million sq miles) intact.
But scientists note the long-term trend is still downwards.
They note that at this year's minimum, the ice covered 24% less ocean than for the 1979-2000 average.
The analysis is compiled from satellite readings at the US National Snow and Ice Data Center (NSIDC) in Boulder, Colorado.
Colder front
Among the reasons for the less drastic melt are that Arctic temperatures have been cooler this year than last, researchers said, and that winds have helped disperse sea ice across the region.


Arctic ice in retreat

1999   yet.
"We had cloudier conditions and low pressure zones in late summer that probably helped keep temperatures down," he told BBC News.
"It's something we need to look at in more detail.
"But it certainly wasn't as warm as 2007, which was in the order of 2-3C warmer than the average in a lot of places."
The question now, he said, was whether 2007 turns out to be a "high-melt blip", or whether 2009 turns out to be a "low-melt blip" - which will not become evident until next summer at the earliest.
What continues to have scientists worried is that a significant proportion of the cover consists of young, thin ice formed in a single winter.
This is much more prone to melting than the older, thicker ice that dominated in years gone by.
"If we get another warm year, anything like 2007, then the ice is really  going to go," said Dr Meier.
"And the chances are that at some point in the next few years we are going to get a warm one."
White heat
In recent decades, the Arctic region has been warming about twice as fast as the average for the Earth's surface.
Recently, scientists specialising in reconstructing past temperatures released data showing that the current decade is the warmest in the Arctic for at least 2,000 years.
Melting ice is a "positive feedback" mechanism driving temperature rise faster. Whereas white ice reflects sunlight back into space, dark water absorbs it, leading to faster warming.
The NSIDC team cautions that this is a preliminary analysis and that further melt is possible, though unlikely, this year.
Next month they will publish a full analysis including more details of how temperatures, currents and winds affected the sea ice this summer.

windy weston plus