Since the northern Atlantic Ocean is one of the main areas that the AMO is active (meaning that area of the ocean is what warms up) it is hardly surprising that
arctic ice in that region is impacted.
Not exact matches
The findings back up a body of data suggesting that «the effects of global [warming] will be seen first, and will be most pronounced,
in the
arctic region,» says Mark Serreze, an
arctic climatologist at the National Snow and
Ice Data Center
in Boulder, Colorado.
In this new regime, with a complete absence of sea ice and snow in the Northern Hemisphere, with rapid warming of the arctic region due to increased solar absorption, a jump in regional temps will occu
In this new regime, with a complete absence of sea
ice and snow
in the Northern Hemisphere, with rapid warming of the arctic region due to increased solar absorption, a jump in regional temps will occu
in the Northern Hemisphere, with rapid warming of the
arctic region due to increased solar absorption, a jump
in regional temps will occu
in regional temps will occur.
If some suitably huge area of the
arctic is totally free of
ice this summer, could it then be claimed with confidence that this was the first time such a large
region was free of
ice in «x» years, where x is some largeish number like 50,000 or 100,000?
Ice - albedo feedback, he added, could give considerably greater warming
in arctic regions.
But
in polar
regions [within
arctic circle] one is still going to have 6 months per year of darkness and therefore will still have freezing weather, though polar
ice may not form during the winter.
A good point as
arctic regions that are hit with warmer water streams will prevent sea
ice extent while those with colder ones can massivly increase
in volume when the air is cold enough though no growth would be visible from the top down view.
T, his was sho \ vn not only by the rise of temperature at land stations, but also by the clccrease
in the amount of
ice in arctic and probably also
in antarctic
regions and by the rise of sea temperatures.
A long - lived paradigm
in polar oceanography is that
arctic pelagic ecosystems, characterized by short food webs, remain
in a dormant state throughout most of the winter season beneath the sea -
ice cover, which can last 8 — 10 months
in some
regions.
I'm sure there must be a clear signature of this scenario from Eamian
in which the
arctic regions were 5 degrees C warmer than at present, all the
arctic sea
ice was melted and the Greenland
ice cap somewhat reduced.
Below are examples of photos show the strongest and most obvious result of global warming; retreating glaciers, melting
ice and shrinking snow cover occurring
in the
arctic region of the world.
In arctic regions, the acceleration of permafrost thaw and deepening of the seasonal active layer leads to thaw pond formations due to the organic and
ice - rich ground subsiding [1]--[2].
Satellite data and ground observations also indicate that
ice conditions
in the Nares Strait west of Greenland may favor an influx of old high
arctic ice into the
region later
in the season.
Does less
arctic sea
ice results
in enhanced cooling to space
in this
region?
The constant flow of relatively warmer surface water that started
in the mid 60s from the equitorial atlantic produced a net increase
in arctic ice melt, thus a colder southward current
in the E Atlantic, giving the wrong impression of generalised cooling
in the
region.
Much like your arguement above about trends
in arctic ice since 2003, how much traction would I get suggesting that surface temperature trends
in some
region the size of the
arctic showed a negative trend?
Statistics Canada — Average area covered by total (all) sea
ice during summer from 1968 to 2010 for sea
ice regions of
Arctic Domain — EnviroStats — See how clear the trends are
in all of Canada's
arctic regions: down, down, down at something like 7 or 8 percent a decade.