These
people are friggin' optimistic
Arctic
nearly free of summer sea ice during first half
of
21st century
12
April, 2013
For
scientists studying summer sea ice in the Arctic, it’s not a
question of “if” there will be nearly ice-free summers, but
“when.” And two scientists say that “when” is sooner
than many thought — before 2050 and possibly within the next decade
or two.
“Rapid Arctic sea ice loss is probably the most visible indicator of global climate change; it leads to shifts in ecosystems and economic access, and potentially impacts weather throughout the northern hemisphere,” said Overland. “Increased physical understanding of rapid Arctic climate shifts and improved models are needed that give a more detailed picture and timing of what to expect so we can better prepare and adapt to such changes. Early loss of Arctic sea ice gives immediacy to the issue of climate change.”
“There is no one perfect way to predict summer sea ice loss in the Arctic,” said Wang. “So we looked at three approaches that result in widely different dates, but all three suggest nearly sea ice-free summers in the Arctic before the middle of this century.”
Overland
and Wang emphasized that the term “nearly” ice free is important
as some sea ice is expected to remain north of the Canadian
Archipelago and Greenland.
- The “trendsetters” approach uses observed sea ice trends. These data show that the total amount of sea ice decreased rapidly over the previous decade. Using those trends, this approach extrapolates to a nearly sea ice-free Arctic by 2020.
- The “stochasters” approach is based on assuming future multiple, but random in time, large sea ice loss events such as those that occurred in 2007 and 2012. This method estimates it would take several more events to reach a nearly sea ice-free state in the summer. Using the likelihood of such events, this approach suggests a nearly sea ice-free Arctic by about 2030 but with large uncertainty in timing.
The “modelers” approach is based on using the large collection of global climate model results to predict atmosphere, ocean, land, and sea ice conditions over time. These models show the earliest possible loss of sea ice to be around 2040 as greenhouse gas concentrations increase and the Arctic warms. But the median timing of sea ice loss in these models is closer to 2060. There are several reasons to consider that this median timing of sea ice loss in these models may be too slow.
Taken
together, the range among the multiple approaches still suggests that
it is very likely that the timing for future sea ice loss will be
within the first half of the 21st century, with a possibility of
major loss within a decade or two.


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