Cyclonic Activity persists in Arctic
30
June, 2013
Above image, edited from Naval Research Laboratory, shows that a large area has developed at the center of the Arctic Ocean with very thin ice, at some places down to virtually zero, i.e. open water.
This development is to a large extent caused by persistent cyclonic activity in the Arctic. The Arctic is warming up faster than anywhere else, and this is reducing the temperature difference between the Arctic and lower latitudes. As a result, the polar vortex and jet stream get distorted, resulting in extreme weather. This is graphically illustrated by the animation below, from the California Regional Weather Server.
Note:
this animation is a 2.5 MB file that may take some time to fully
load.
Credit: California Regional Weather Server |
Related
Open Water In Areas Around North Pole - June 22, 2013http://arctic-news.blogspot.com/2013/06/open-water-in-areas-around-north-pole.html
Thin Spots developing in Arctic Sea Ice - June 13, 2013http://arctic-news.blogspot.com/2013/06/thin-spots-developing-in-arctic-sea-ice.html
Polar jet stream appears hugely deformed - December 20, 2012
Changes to Polar Vortex affect mile-deep ocean circulation patterns - September 24, 2012http://arctic-news.blogspot.com/2012/09/changes-to-polar-vortex-affect-mile-deep-ocean-circulation-patterns.html
Diagram of Doom - August 28, 2012
http://arctic-news.blogspot.com/2012/08/diagram-of-doom.html
Opening further Doorways to Doom - August 28, 2012
Opening further Doorways to Doom - August 28, 2012
http://arctic-news.blogspot.com/2012/08/opening-further-doorways-to-doom.html
Huge cyclone batters Arctic sea ice - August 11, 2012
Huge cyclone batters Arctic sea ice - August 11, 2012
Unprecedented
Jet Stream Wave Sparks 120+ Degree Temps in the US Southwest and
Tundra Fires in Extreme Northern Canada.
30
June, 2013
Today,
as temperatures rocketed to above 120 in the US Desert Southwest,
temperatures hit 87 degrees on the shore of the frozen waters of the
Canadian Archipelago. These were the south to north markers of a
heatwave that spanned 3,000 miles from Death Valley, California to
Cambridge Bay in extreme northern Canada.
Beneath
the southern section of this vast and sprawling heat dome, US
communities coped by setting up cooling centers and issuing heat
warnings. But despite this agile preparedness, hospitals in the
hardest hit areas were flooded with cases of heat injury.
In
one instance, an outdoor concert in Las Vegas saw more than 200
persons treated for heat injuries while more than 36 were
hospitalized. Sadly, an elderly man also passed away at one local
hospital after suffering from heat stroke. Temperatures reached an
extraordinarily hot 115 (Fahrenheit) in Sin City.
Elsewhere,
across the region, Palm Springs hit 122, Death Valley hit 125, and
Phoenix hit a scorching 119. Tomorrow is expected to bring another
day of extreme record heat, so area cities and residents are still
under the gun.
Further
north, near 90 degree temperatures stretched all the way to the
frozen shores of Cambridge Bay in extreme northern Canada. There,
some locations on the ice choked waterway experienced 87 degree
temperatures, which is nearly 40 degrees (Fahrenheit) above average
for this time of year.
The
extreme heat sparked numerous tundra fires across Northern Canada,
some of which you can see in the NASA satellite image above. Note the
smoke tails rising from two clusters of fires in the upper center
portion of the image. That ice speckled area of blue to the right is
the, usually frigid, Hudson Bay.
The
heat also set off melt and fracturing of sea ice in Cambridge Bay,
which you can see in the NASA shot below:
Warming
air temperatures typical for this region (high 40s to low 50s)
usually result in a more gradual melt. But hot air temperatures at up
to 55 degrees (Fahrenheit) above freezing tend to have a far more
rapid effect. It is also worth noting the nearly complete lack of
visible snow cover in this extreme northern region.
I’ve
Never Seen A Rossby Wave Like This
The
cause of this 3000 mile swath of heat is an extremely high amplitude
wave in the Jet Stream that stretches from the Western US all the way
up to the Arctic Ocean. This large bulge has allowed a powerful ‘heat
dome’ high pressure system to build up beneath it, concentrating
heat over the vast area affected.
Note
the up-flow of Jet Stream winds rising up the coast of California,
Oregon, Washington and British Columbia then lifting all the way up
to the Arctic Ocean before diving back down through central Hudson
Bay and into the US Midwest, before making another hairpin turn north
again over the Appalachians.
Large
Jet Stream waves of this kind are termed ‘Rossby Waves’ after the
climate scientist who first identified them. They show extreme
north-south and south-north elongation. In the time I’ve been
tracking the extreme changes to the Northern Hemisphere Jet Stream
brought about by human-caused warming, I’ve never seen a Rossby
Wave quite so large as this. Nor have I seen one that is the result
of so many large back and forth meanders. In fact, the entire
Northern Hemisphere Jet is a mess of meanders, cut off upper level
lows and blocking highs.
One
of these upper level lows is expected to bring abnormally heavy rain
with up to 3-5 inches for some parts of the US East Coast over the
next couple of days. So as heat bakes a swath from Death Valley to
the Arctic Ocean, the Eastern US braces for potential flooding.
Similar Jet Stream loops and swirls spawned the European floods this
June, a series of deadly floods that killed hundreds in India and
Tibet, and multiple anomalous Arctic heatwaves occurring throughout
the past month.
Extreme
Jet Streams, like the one displayed above (for late Saturday, June
29), are far more likely to spawn extreme weather events than the
usual, gently wavy Jet Stream that human civilization has been used
to for much of the 20th Century and, probably, for most of the 10,000
year period since the last ice age. But a combination of eroding sea
ice and record or near record low Northern Hemisphere snow cover
contribute to both a slowing of the Jet Stream and in greater
north-south and south-north flows. The result is large wave patterns
in the Jet that tend to get stuck in the same configuration for long
periods. Beneath the swells in the Jet, we get hotter temperatures,
dryer conditions, and the risk of everything from extreme heatwaves
to droughts and fires. In the dips, we get cooler temperatures and
much, much stormier conditions resulting in a range of weather from
extreme winters (Europe during winter/spring 2013), to floods (Europe
summer 2013, India late June 2013), to record rainfall and powerful
thunderstorms (US May-June 2013).
These
are vivid examples of how human-caused climate change can result in
extreme weather.
Heat
Wave to Last For at Least a Week
The
current record heat wave affecting both the US West and a large
section of Canada is expected to last at least until the end of this
week. Slow moderation, though, is expected for some regions after
Sunday. However, the blocking pattern that spawned this particular
heat wave shows little sign of changing position. So hotter, dryer
conditions are expected to remain in place for the foreseeable future
for much of the US South-West.
Meanwhile,
Canada and regions along the Arctic coastline are still likely to see
much warmer than usual conditions as periodic warm air invasions from
the south are likely to continue.
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