For every 1 degree C we warm the Planet we will see 7% more moisture in the Atmosphere
Kevin Hester
7
June, 2016
For
every 1 degree C we increase the temperature on the planet we see 7%
more moisture in the atmosphere. We are heading to and beyond
the IPCC worst
case scenario of 6C minimum which will generate another 40% of
moisture in the air.
This will lead to a greater number of flooding
events and increased number of lightning strikes and Tornadoes.
This is an enormous amount of energy and associated warming as water vapour is in itself a green house gas.
“The
impact of climate change may be worse than previously thought, a new
study suggests”: “As
world leaders hold climate talks in Paris, research shows that land
surface temperatures may rise by an average of almost 8C by 2100, if
significant efforts are not made to counteract climate change.”
Personally
I disagree with the suggestion that it will take until the magic 2100
for our locked in 8C temperature rise. Factor in the myriad of
feedback loops and we could be there in a few decades,not that humans
will survive that long to bare witness.
Such
a rise would have a devastating impact on life on Earth: ‘Climate
Outlook May be Worse than Feared.’
“The
amount of water vapor in the atmosphere exists in direct
relation to the temperature. If you increase the temperature, more
water evaporates and becomes vapor, and vice versa. So when something
else causes a temperature increase (such as extra CO2 from
fossil fuels), more water evaporates. Then, since water vapor is
a green house gas, this additional water vapor causes the
temperature to go up even further—a positive feedback.”
How much does water vapor
amplify CO2 warming? Studies show that water vapor feed
backroughly doubles the amount of warming caused by CO2. So if
there is a 1°C change caused byCO2, the water vapor will cause the
temperature to go up another 1°C. When other feedbackloops are
included, the total
warming from a potential 1°C change caused by CO2 is, in
reality, as much as 3°C.
“A
warmer atmosphere can hold more moisture, and globally water vapour
increases by 7% for every degree centigrade of warming.”
Thunderstruck: Lightning Will Increase With Warming
13
November, 2014
While
severe weather like hurricanes and tornadoes typically only hit
particular areas of the globe, lightning can strike anywhere. And it
does, a lot. A bolt of lightning flashes through the sky and hits the
ground somewhere around the world about 100
times every second.
That’s 8 million lightning strikes in a single day — yes, you
read that right: just one day.
Now,
a new study finds that lightning strikes will become even more
frequent as the planet warms, at least in the continental U.S.
For
years scientists have been exploring how the steady warming of the
planet might be impacting severe weather, though most of the
attention has been placed on hazards like hurricanesand heavy
downpours.
And while those events are major killers, lightning is also a
significant hazard. So far this year, 25
people have been killed by
lightning strikes in the U.S., and lightning is the trigger for more
than half of U.S. wildfires,
putting pressure on human infrastructure as well as natural
ecosystems.
But
so far, relatively scant attention has been paid to how lightning
might change as the planet’s temperature rises with
the accumulation
of greenhouse gases in
the atmosphere. And the studies that have been done to date estimate
the increase in lightning to be anywhere from 5 to 100 percent per
degree Celsius rise — a strikingly wide range.
The
new study, detailed in the Nov. 13 issue of the
journal Science,
has found a relatively simple way to use other atmospheric factors to
predict changes in lightning rates. The findings suggest that
lighting rates will increase 12 percent per every degree Celsius
(about 2°F) rise in global temperatures. That comes to a 50 percent
increase by the end of the century.
‘Beautiful’ Lightning Data
Study
author David Romps, who studies atmospheric dynamics at
the University
of California, Berkeley,
didn’t set out to study the effect of warming on lightning, but
instead was trying to use lightning to “understand something about
how, when, where, and why convection pops up over the United States,”
he told Climate Central. (Convection is the process that drives
thunderstorms.)
It
just so happens that there is what Romps calls a “really beautiful”
lightning dataset from the National
Lightning Detection Network,
which records when and where each of the approximately 20 million
flashes of cloud-to-ground lightning occurs over the U.S. each year.
Somewhere
during the process of exploring his initial question, Romps started
to wonder if other atmospheric variables could be used to predict
lightning rates. In science, “it’s rare that you end up doing
what you think you’re going to do,” he said.
The
particular variables he looked at can be used as measures of storm
convection, the idea being that more vigorous convection is linked to
more lightning. They include how heavy the rain in a storm is and how
much energy is available in the atmosphere to fuel the storm’s
convection.
Measurements
at individual weather stations suggested these factors could say
something about lightning rates, but they were fairly isolated. While
he was skeptical, it was enough for Romps to start digging deeper
into the data.
To
start, Romps made some simple maps: One showed lightning strike data
over the continental U.S. from 2011. The other combined precipitation
and convection energy data for the same year (the only one for which
data for all three variables was available). The two maps showed a
surprising similarity, with much of the area with the most lightning
also the area where the other two factors were high.
Lightning
flashes (bottom right) compared to other atmospheric variables that
could be used to help predict changes in lightning rates.Click
image to enlarge. Credit:
Romps, et al./Science
A
graph that compared lightning with the other two factors over time
was even more shocking, with the peaks and valleys of all three
matching strikingly closely. Romps was, well, thunderstruck.
“That’s
basically when my jaw hit the floor,” Romps said. “That’s when
we knew we were really on to something.”
Romps
said that match shows that using precipitation and storm energy data
was “a much more robust method for predicting lightning” than
other studies have previously used.
Lightning in a Warmer World
It’s
also fortuitous because the latest batch of climate models from the
most recent assessment of theIntergovernmental
Panel on Climate Change are
the first to include those two factors, meaning Romps and his
colleagues could use that model data to make a prediction of the
changes to lightning rates in a warmer future.
Running
the data, the team found that lightning would be expected to increase
by about 12 percent per degree Celsius of warming (give or take 5
percent), with about a 50 percent rise over the 21st century. Using
the 20 million-strike average, that would mean some 30 million
lightning strikes per year over the continental U.S. by 2100.
The
results make physical sense given that both heavy precipitation and
storm energy are related to the amount of water vapor available in
the atmosphere and one of the main accepted results of a warming
atmosphere is also a moister one. Essentially, more moisture suggests
more vigorous thunderstorms and so more lightning.
Colin
Price, an atmospheric scientist at Tel
Aviv University and
one of the few people to look at the issue of warming and lightning,
said that the results of the study were in broad agreement with ones
he published for
the whole globe in 1994, “so I am happy to see this study supports
our earlier work.”
Price,
who was not involved in the new study, said that it was “not
surprising” that factors investigated in this study could say
something about lightning rates. “But I am sure there are many
other indices and parameters that may be just as good in predicting
lightning. And the proxies will very likely vary with region and
season,” he said in an email.
That
variation is something the new study didn’t look at, since it
examined only the continental U.S. “We don’t know how that
increase is distributed over the seasons or geographically,” Romps
said, adding that tackling those questions are the next step in his
research.
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