Mainstream
media is slowly coming round
Loss
of Arctic ice leads to drought in California
BY
JOHN LINDSEY
18
January, 2014
In
the 1990s, U.S. Navy submarines reported a shocking loss of thickness
in Arctic sea ice. Over the past decade, satellite altimetry readings
confirmed this.
In
the summer of 2012, the level of ice in the Arctic Ocean dropped to
its lowest on record, according to the National
Snow and Ice Data Center.
To make matters worse, this ice melt came faster than earlier climate
models had predicted.
From
year to year, the amount of ice continues to change, some years
higher and some years lower. Nevertheless, the long-term trend
indicates a dramatic and startling loss of sea ice.
The
loss of this ice in the Arctic is a direct result of warming
temperatures there. In fact, average temperatures have increased at
about two to three times faster relative to the midlatitudes. This
enhanced amount of warming in the high northern latitudes is referred
to as Arctic Amplification.
It’s
interesting to note that some climatologists and scientist suspect
that this condition could be the culprit behind the big and
persistent ridge of high pressure over California that has produced
unprecedented dry conditions and record-breaking temperatures
throughout the state.
For
example, just this past Thursday, Cal Poly, home of climatology for
San Luis Obispo, reported
an all-time January maximum temperature
of 89 degrees, breaking the old monthly record of 88
degrees set back in 1976. San Luis Obispo County Regional Airport
reached 91 degrees.
On
the other hand, a seemingly everlasting trough of low pressure has
plagued the eastern part of the country with bone-chilling cold and
endless rain and snow.
So
how could warmer temperatures over the Arctic affect the country’s
weather pattern?
Jennifer
Francis of Rutgers University gave a persuasive presentation,
“Wacky
Weather and the Disappearing Arctic Sea Ice: Are They
Connected?”
at the Weather and Climate Summit in Breckenridge, Colo., last year.
Her
hypothesis is that Arctic Amplification is producing more persistent
and stronger ridges of high pressure and deeper and longer-lasting
troughs of low pressure as the amplitude of the polar jet stream
increases.
The
jet stream is typically a tubular ribbon of high-speed winds flowing
in wavelike patterns for thousands of miles from west to east some
18,000 to 40,000 feet up.
Most
of the time, the peak or the northern part of the wave pattern
indicates ridges of high pressure and fair weather, while the trough
or southern part of the wave is associated with low pressure and
unsettled conditions.
The
amplitude, or the distance between the peaks and troughs of these
waves, can stretch for hundreds of miles from Baja California
northward to Washington state. Typically, the higher-amplitude wave
pattern changes at a slower rate, meaning that both drought events
and rain events will last longer in a particular area.
As
the Arctic continues to warm, the thickness of the atmosphere over
that region will continue to reach higher in altitude, like a hot air
balloon. On average, half of the atmosphere’s weight lies between
the Earth’s surface and an altitude of about 18,000 feet.
Meteorologists
determine the thickness of the atmosphere by analyzing 500-millibar
upper-level charts. In other words, this chart will tell you how high
the pressure is 3 or 4 miles above the Earth’s surface.
The
atmosphere is at its thickest near the equator and gradually narrows
toward the poles.
Francis
theorizes that as the polar regions become warmer and the atmosphere
thickens, the downward slope between the equator and the poles will
lessen. This condition may result in greater amplitude of the wave of
the jet stream.
Consequently,
droughts could become more prolonged and precipitation events,
especially combined with ever-increasing amounts of water vapor that
a warmer atmosphere can hold, could produce floods.
If
you would like to learn more about climate change and how to deal
with it, the group Lifelong Learners of the Central Coast is offering
a series of courses in March at the PG&E Energy Education Center.
Please visit http://www.lifelearnerscc.org
to sign up.
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