The
Point Everyone Is Missing About The Return Of The ‘Polar Vortex’
14
July, 2014
It
will be unseasonably chilly in the eastern part of the United States
this week, due to a peculiar weather pattern that’s causing deep
waves in the jet stream. One of those big waves is bringing cool air
down from the northeast Pacific and the Arctic. This will cause
nighttime temperatures to be, on average, in the 50s or 60s on
Tuesday and Wednesday.
So
is it the polar vortex, or isn’t it? That’s been the big
debate
among meteorologists and news outlets. But according to at least one
scientist, that debate misses a more important point about the
unusual weather pattern sweeping the United States — that it’s
causing extreme weather in other parts of the country.
“We’ve
got this cool air coming down over the eastern half of the country,
and that’s gonna just be kind of nice,” said Jennifer Francis, an
atmospheric scientist and research professor at Rutgers University’s
Institute of Marine and Coastal Sciences. “But along the east
coast, we’re looking at storms and floods. On the west coast, we’re
looking at heat and fires. And it’s all part of this jet stream
pattern.”
The
jet stream is set to make a huge dip into the eastern U.S. this week.
CREDIT:
ACCUWEATHER
A
particularly wavy jet stream is what is causing the so-called “polar
vortex,” or cold air from the Arctic, to travel down to the United
States, Francis said. The dramatic and unusual southward swoop, shown
in the map on the right, allows air from the cold north to travel
south. The same thing happened this past January, when a dramatic
southward swing of the jet stream brought increased cold air to an
already-freezing region. That was big news, extreme weather-wise.
Now,
the “polar vortex” is making for fairly mild weather. But at the
same time, that same wavy jet stream is swinging northward in the
western United States, bringing increased
heat
to an already-dry
and wildfire-stricken
region. Extreme weather-wise, Francis says, this is a bigger deal.
“They’re
going to be suffering out there,” she said. “That part of the
story is more important in a way because they’re already dealing
with such a drought that this is just going make the drought and the
fires and everything much worse, while in the east it’s just going
to be a nice couple of cool days to break up the hot summer.”
As
the jet stream dips upward following its southward travels, the east
coast will also see some more newsworthy weather, Francis said.
“That’s where it’s really stormy,” she said “You see storms
and flooding on the east side of those southward dips.”
Weather
forecasts are predicting
thunderstorms and flash flooding up the East Coast this week, from
Atlanta
to New
York.
This
particularly wavy jet stream has been largely
attributed
to Japan’s typhoon Neoguri, the immense energy of which likely
caused a swift acceleration of the North Pacific jet stream. Francis
says to think of it like taking a jump rope and giving it a whip with
your hand — except the jump rope is the jet stream, and your hand
is a typhoon. The whip, intensified by your strength, travels along
the rope with a ripple effect.
In
addition to being powered by storms, though, the jet streams
movements may be impacted by a warming Arctic. Francis’ research
suggests that as the Arctic warms due to climate change, less drastic
changes in temperatures occur between northern and southern climates.
This leads to weakened west-to-east winds, and ultimately, a wavier
jet stream.
“Our
research suggests that these kinds of patterns where the jet stream
is taking these big northward and southward swings is going to become
more frequent in the future, at least partly related to the fact that
the Arctic is warming so fast,” she said. “We can’t say that
this particular example is related to the Arctic. That being said,
the Arctic is very warm right now, and so it could be contributing to
making this pattern more wavy than it would have been otherwise.”
Francis’
research on Arctic warming being connected to a wavier jet stream is
still disputed. Dr. Kevin E. Trenberth, a distinguished senior
climate scientist at the National Center for Atmospheric Research,
told ClimateProgress in January that he was still skeptical of the
connection. “[It] shows a correlation, but correlation is not
causation,” he said
at the time. In a recently published update
on the linkage between Arctic warming and its impact on jet stream
patterns, The National Research Council was optimistic about the
connection, but noted it was still too early to draw concrete
conclusions.
The
weather the U.S. is experiencing now is the result of a similar
offshoot of the Arctic jet stream that brought down the colder
temperatures in January, though this week’s weather will include a
good deal of northeast Pacific air, rather than just Arctic. As for
whether both instances should really be called the “polar vortex,”
Francis says no, saying it’s a mischaracterization of the term.
Really, she said, the polar vortex refers to the whole Arctic jet
stream taken together, not the actual cold air inside of it.
Some
still feel comfortable using the term, though, since the flow of air
that’s coming down is — at least partially — coming from the
Arctic. Jason Samenow has a piece
in the Washington Post
defending the term, detailing three graphs that he says prove this
week’s weather patterns are a “textbook case of polar vortex
influence on mid-latitude weather.”
“In
my view, discussing the polar vortex’s significant role in
mid-latitude cold air outbreaks is a great way to engage the public
in the intriguing dynamics of meteorology,” Samenow wrote. “Some
critics are being too literal about its definition and/or burying
their heads in the sand, blinding themselves from a fascinating
weather reality.”
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