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Polar Jet Stream Wrecked By Climate Change Fuels Unprecedented Wildfires Over Canada and Siberia
18
July, 2014
This
year, the warm air invasion started early. A high amplitude ridge in
the Jet Stream stretching for thousands of miles over the temperate
Pacific and on up into Alaska and the Chukchi Sea slowly drifted
eastward. Reinforced by a powerful bank of blocking high pressure
systems over the northeastern Pacific, this ridge settled over
Canada’s Northwest Territory in a zone from the Mackenzie Delta and
over a broad region east and south. From mid June onward,
temperatures in the 70s, 80s and even low 90s dominated sections of
this Arctic region.
The
heat built and built, drying the shallow soil zone over the thawing
permafrost creating a tinder-dry bed layer waiting for the lightning
strikes that were bound to follow in the abnormal Arctic heat.
By
late June, major fire complexes had erupted over the region. Through
early and mid July, these massive systems expanded even as the
anomalous heat dome tightened its grip. Today, the fires in
Northwestern Canada have reached a horrific intensity and one, the
Birch Complex fire, alone has now consumed more than a quarter of a
million acres.
According
to reports from Canada’s Interagency Fire Center, total
acres burned to date are more than six times that of a typical year.
A rate of burning that, according to a recent scientific study, is
unprecedented not just for this century, but for any period in
Canada’s basement forest record over the last 10,000 years.
(Thunderstorm?
No. Smoke from a major volcanic eruption injecting ash into the
stratosphere? No. The upper frame shot is an aerial photo taken of
the Birch Creek Fire Complex on July 14, 2014 from a distance of
about 30 miles away. It is just one of the massive fires now raging
in the Northwest Territory region of Canada. A closer picture, taken
from a few miles out, reveals the flaming base of a massive smoke
plume. Image source: NWT
Fire Facebook.)
From
helicopter and airplane, the volume of smoke pouring out of these
massive tundra and boreal forest fires is amazing, appearing to mimic
major thunderstorm complexes or volcanic eruptions. Closer shots
reveal towering walls of flame casting billows of smoke thousands of
feet into the air above.
The
smoke from these fires, now numbering in excess of 186 separate
blazes, is becoming entrained in the weakening circumpolar Jet
Stream. The steely gray billows now trail in a massive cloud of
heat-trapping black carbon that stretches more than 2000 miles south
and east. Its southern-most reaches have left residents of the
northwestern and north-central US smelling smoke for weeks, now.
Meanwhile, the cloud’s eastern-most reaches approach Baffin Bay and
the increasingly vulnerable ice sheets of Greenland.
(Satellite
shot of smoke from massive fire complexes over Canada spreading
eastward. Black carbon and related CO2 emissions from forest fires
can serve as a powerful amplifying feedback to already dangerous
human-caused climate change. Image source:NASA/LANCE-MODIS.)
Across
the Arctic, Siberia Also Burns
As
media attention focuses on the admittedly horrific fires of
unprecedented magnitude raging over Canada, a second region of less
well covered but possibly even more extensive blazes burns on the
other side of the Arctic Ocean throughout the boreal forest and
tundra zones of Central Siberia in Russia.
There,
record heat that settled in during winter time never left, remaining
in place throughout summer and peaking in the range of 80-90 degree
Arctic temperatures over the past couple of weeks. Over the last
seven days, massive fires have erupted which, from the satellite
vantage, appear about as energetic as the very intense blazes that
ripped through Siberia during the record summer fire year of 2012. It
is a set of extreme conditions we’ve been warning could break out
ever since March and April when intense early season fires ripped
through the Lake Baikal and Southern Yedoma regions.
Now,
what appears to be more than 200 fires are belching out very thick
plumes of smoke stretching for more than 2000 miles over
North-Central Siberia and on into the recently ice-free zone of the
Laptev Sea:
(Massive
sea of smoke and fire stretching from Lake Baikal and northeast over
Central Siberia and on into the Arctic Ocean. Image
source: NASA/LANCE-MODIS.)
As
with the other set of fires in Canada, the smoke from these massive
blazes is entraining in the Jet Stream and stretching across Arctic
regions. An ominous blanket of steely gray for the roof of the world
and yet one more potential amplifying heat feedback the Arctic
certainly does not need.
Potential
Amplifying Feedbacks in Context
During
recent years, scientists have been concerned by what appears to be an
increased waviness and northward retreat of the northern hemisphere
Jet Stream. This retreat and proliferation of ridge and trough
patterns is thought to be a result of a combined loss of snow and sea
ice coverage over the past century and increasing over the past few
decades. In 2012, sea ice coverage fell to as low as 55% below 1979
levels with volume dropping as low as 80% below previous values. Over
the past seven years, not one day has seen sea ice at average levels
for the late 20th Century in the north.
Meanwhile,
northern polar temperatures have risen very rapidly under the rapidly
rising human greenhouse gas heat forcing, increasing by 0.5 C per
decade or about double the global average. It is this combination of
conditions that set the stage for fixed ridges over both Russia and
Canada creating extreme risk for extraordinary fires.
(Weak
and wavy polar jet stream on July 17, 2014 shows fixed ridges over
the Northwest Territory, Central and Eastern Siberia, Northern Europe
and the adjacent North Atlantic and Arctic. Image source: Earth
Nullschool.
Data Source: NOAA
GFS and
various.)
Should
both the current sets of fires continue to rage under anomalous high
amplitude jet stream waves setting off extreme heat in these Arctic
regions, it is possible that large clouds of heat absorbing black
carbon could ring the Arctic in a kind of hot halo. The dark smoke
particles in the atmosphere would trap more heat locally even as they
rained down to cover both sea ice and ice sheets. With the Canadian
fires, deposition and snow darkening are a likely result, especially
along the western regions of the Greenland Ice Sheet — zones that
have already seen a multiplication of melt ponds and increasing
glacial destabilization over recent years.
Recent
scientific studies have also highlighted the possibility that
human-caused climate change is increasing high amplitude jet stream
ridge patterns that are transporting more and more heat into Arctic
tundra and boreal forest regions.
These regions are more vulnerable
to fires due to the fact that trees in boreal forest have uniform
characteristics that favor burning and tend to rapidly ignite and
spread once the upper branches become involved. The unfrozen soil
features a narrow basement layer above tundra which dries more
rapidly than the soils of more temperate areas, providing tinder fuel
to aid in the initial ignition by lightning strike. Thawing, deeper
tundra, when dried, is a meters-deep pile of fuel that has
accumulated for thousands of years — a kind of peat-like layer that
can smolder and re-ignite fires that burn over very long periods. It
is this volatile and expanding basement zone that is cause for
serious concern and greatly increases the potential fire hazard for
thousands of miles of thawing tundra going forward.
Overall,
both boreal forest and thawing tundra provide an extraordinary
potential fuel for very large fire complexes as the Arctic continues
to warm under the human greenhouse gas forcing. And though climate
models are in general agreement that the frequency of fires in tundra
regions will increase, doubling or more by the end of this century,
it is uncertain how extensive and explosive such an increase would be
given the high volume of fuel available. Direct and large-scale
burning of these stores, which in tundra alone house about 1,500
gigatons of carbon, could provide a major climate and Earth System
response to the already powerful human heat forcing.
Though
the science at this point is uncertain, we observe very large and
unprecedented fire outbreaks with increasing frequency:
“I think it’s really important for us to take advantage of studying these big disturbance events,” noted Dr. Jill Johnstone in recent interview. “Because, if we can say anything, we can say that we think they’re going to be more common.”
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