O.K. - from the Oceanographer in our midst:
Nice to see you're interested in this climate stuff too. The short
answer is yes, we're in a bit of a fix, but the $64 dollar question is
how bad is it actually going to be. My research relates somewhat to
this question, specifically in terms of how oceans and land ecosytems
are exchanging and will exchange carbon dioxide (CO2) with the
atmosphere. But I am more interested in trying to figure out ways to
mitigate climate change (or "manage the risk of potential climate
change" depending on whether you believe its definitely happening), for
example by exploring how oceans and land ecosystems might be managed to
take up more CO2.
I've written a few emails along these lines before, so with a bit of
cutting and pasting I think I can send you a huge information dump, then
you can let me know if anything didn't make sense and/or what else you'd
like to know more about. . . .
First, a few basics, then some finer points.
1) Atmospheric CO2 concentrations have gone up from 280 parts per
million (ppm) to 380 ppm since the industrial revolution. No credible
scientist disputes that this is a direct result of fossil-fuel
combustion - the isotopic signatures (ratios of carbon with 14, 13, or
12 neutrons) of the new CO2 matches fossil fuels and in fact the
atmospheric increase is only 1/3 of the amount of CO2 that we have
emitted into the atmosphere during that time. Nevertheless, you will
occasionally hear folks from the oil lobby dispute even this fundamental
point. Based on ice core measurements, we know that this number has not
been higher than 280 for at least the past 500,000 years. It oscillated
between 200 ppm during ice ages ("glacial periods") and 280 ppm during
non ice ages ("interglacial periods") over this time, and
emissions/uptake projections in the absence of deliberate reductions
show it reaching 700 to 1000 ppm by the end of this century.
2) Atmospheric CO2 absorbs heat (infrared radiation) that would
otherwise escape to space. The world would be much colder and we likely
wouldn't be here if there were no CO2 in the atmosphere. Water vapor,
which varies around a few percent in concentration, is also responsible
for warming the Earth through this mechanism. The other major
atmospheric gases such as oxygen, nitrogen, and argon do not absorb in
the infra red. Other minor gases, such as methane and
chlorofluorocarbons do absorb infra red and are also relevant for
climate change, but increasing CO2 is the dominant concern.
3) Now, because CO2 absorbs heat and we are increasing it in the
atmosphere, it is going to get warmer. This is also indisputable. What
no one can say for sure, and what leaves room for strong convictions on
both sides of the argument, is whether it is only going to get a few
degrees Fahrenheit warmer, which might be somewhat manageable, or
whether it is going to get 20 F warmer which would have catastrophic
impacts all over the world. This is where supercomputer models come in
(actually you get the same answer on the back of an envelope but simple
calculations aren't defensible because they neglect potentially
important processes). The same models that can now predict the weather
very well for a couple days (and still show some skill out to 10 days or
so), can also be used to predict the climate. The difference between
weather and climate is a somewhat subtle concept - the models couldn't
tell you that there will be a high of 95 in New York on August 1 of this
year (the weather), but they can tell you what the average high
temperature in August in New York is (the climate). All sophisticated
climate models, of which there are probably 30 around the world, predict
that the globally averaged surface temperature will increase by 3 to 10
degrees F over the next 100 years.
4) These models account for myriad processes in the atmosphere and the
oceans and take months to run on the world's fastest computers, yet they
are still vastly crude compared to the real world they attempt to
simulate. Because of this, they have many uncertainties and may in fact
be missing important feedbacks in the climate system would make them
inaccurate. For example, clouds both trap heat and reflect sunlight so
whether it gets cloudier and specifically what type of clouds increase
(high or low) could either work to accelerate or decelerate warming.
There are a very few outspoken but credible scientists, who point out
the shortcomings of current models and argue that climate change
warnings are overstated. One important point: though the current models
are far from perfect, nobody has a computer model that predicts it is
not going to get significantly warmer. Also, it is just as likely that
processes the models have left out would make the predictions worse, not
better.
5) It has gotten warmer. Past temperature records are tricky to
interpret, but the best combination of thermometer data, perma-frost
bore holes, and tree-ring proxies indicate about a 1.5 F warming over
the past 100 years (you may have heard of a recent controversy over how
the graphical presentation of this data was exaggerating the sharpness
of this trend, but the overall numbers are still the same). This
relatively small temperature trend can not be assigned unequivocably to
human influence because it's possible the Earth is simply recovering
from the "little Ice Age" which cooled global temperatures and froze the
Thames in winter for much of the 1700's. However, the observed
temperature increase lines up very well with the computer model
projections of what the human influence on temperature should be to this
point.
6) Predicted and observed warmings are much greater at high latitudes.
Because of feedbacks between evaporation, clouds, radiation and
temperature, the tropics are basically already as warm as they can get.
On the other hand, high latitude regions which are much colder and also
reflect a lot of the sun's energy back to space from white snow and ice
that could convert to darker more absorbent land and ocean with warming,
have a much greater potential for warming. The same models which say
the global average temperature will increase 3-10 F predict that
temperatures over Alaska, Northern Canada, and Siberia will increase by
up to 20 F. This is a big number. In fact, many changes have already
occurred at high latitudes that may be warnings of things to come.
Glaciers are in retreat, permafrost is melting, and spring and fall come
earlier and later by several weeks. I recently read that adult polar
bears now weigh 30% less than they used to, because the amount of time
they can walk around on the ice picking off seals has been greatly reduced.
7) Abrupt climate change is a related concern you've probably heard
about. We know from ice cores that during glacial periods, the global
climate repeatedly warmed and cooled by as much as 15 F over a decade.
It is not clear whether such an abrupt change can happen during an
interglacial, but one scenario that's been discussed is that fresh water
entering the North Atlantic from melting of snow and ice could reduce
the density of the surface water enough to shut off or divert the Gulf
Stream, which is currently responsible for keeping Northern Europe much
warmer than it would otherwise be (e.g. everyone from Sweden would move
to New York and I would win the aforementioned wager). I'm not
particularly concerned about this possibility because I know a lot about
the limitations of the ocean models used in these projections, and even
if it did happen these regional effects would ultimately be washed out
by the larger global temperature trend. I did enjoy The Day After
Tomorrow despite the numerous physical impossibilities it was based on.
Then again, I'm a big Waterworld fan. Don't ever let a few facts get in
the way of a good story.
8) So, how bad could it be? I think sea-level is worth thinking about.
The climate models I've been referring to all predict around 50 cm to 1
m of sea-level rise over the next 100 years. This would make storm
surges and beach erosion worse in the U.S. but would otherwise probably
be manageable. For folks on island nations like the Maldives, whose
average elevation is only a meter or two above sea level, this probably
means everyone will have to move to India. However, these projections
are based almost entirely on thermal expansion of sea water. The ice
dynamics models just aren't good enough to make reliable projections
about the influence warming temperatures on polar ice and of potentially
melting ice on sea level. Yet, the possibilities are a bit scary. Ice
that is already floating, like the Rhode Island sized chunks of
Antarctica that have broken off the past few years, do not change
sea-level when they melt (just as melting ice cubes don't raise the
level of your drink). It's the grounded ice on Greenland and Antarctica
that is of most concern. The Florida Keys were formed as coral reefs
(underwater) during the last interglacial period 100,000 years ago, so
we know that sea-level has been much higher, and the only plausible
explanation for this is that then Greenland Ice Sheet was melted then.
Until very recently, people assumed that it would take 10,000 years to
melt Greenland and that we shouldn't be worried about it. However,
recent studies have revealed that it is currently melting at an alarming
rate and that it may have melted rapidly (over several hundred years) in
the past. I recently saw a talk by famous climatologist named Richard
Alley, where he showed a map of what the U.S. would look like if
Greenland melted (Florida is half gone) and if both Greenland and the
West Antarctic Ice Sheet melted (all of Florida is gone). While these
possibilities are currently considered unlikely in the next 100 years,
they are considered possible (see managing risk diatribe below).
9) Another interesting view on climate change comes from the perspective
of endangered species conservation. Ecologists have mapped out 20 or so
"hot spots" around the globe where biodiversity is high and a number of
threatened species are concentrated, and conservation efforts tend to
focus on these specific regions. The catch is that in the past, before
humans built superhighways, cities, and fenced ranches and farms,
animals would simply migrate with natural climate shifts (animals in
Africa have shifted their ranges by thousands of miles north and south
over thousands of years). Now, if climates shift, and all of those
species' ideal conditions shift 1000 miles north or south, they will be
unable move with them. Some climatologists have consequently suggested
that ecologists should worry more about global climate than local
conditions.
10) What should we do about it? First, I think we need to reject the
skeptics demand for "proof" that significant climate change is
inevitable before taking action, and start managing it like any other
risk. For example, we spend billions of dollars a year managing the
risk that a terrorist will attempt to smuggle a nuclear bomb into the
U.S. without any proof that such an event will actually occur. The
potential impacts on our nation's economy, infrastructure, and natural
resources from climate change are also very significant, but up to now
it has been treated as if because of the scientific uncertainty, doing
nothing about it was the best option. Instead I feel that at a minimum
we should be engaging the international community to establish
frameworks for negotiating emission reductions in the future if/when we
become more certain about the likelihood of negative impacts, and
actually participating in the initial attempts at such reductions (e.g.
ratifying the Kyoto Protocol). I'm not an economist, but I have seen
reports that the argument of dire effects on our economy under Kyoto
were flawed, and I think the argument that India and China should have
been included is a cop-out. India and China are certainly projected to
be major contributors to the CO2 problem, but we are by far the cause of
it up to now. Of the 6 billion tons of carbon as CO2 that humans emit
to the atmosphere each year through fossil-fuel burning, the U.S. is
responsible for almost 2 billion and of the total integrated emissions
up to now we are responsible for an even larger fraction. Also, we
should be investing heavily in alternative energy sources and improved
fuel efficiency technology through government provided incentives. Wind
energy is now financially competitive with coal, yet we are still
building massive coal-burning power plants. Also, if the mpg
regulations for SUVs were the same as cars, we would save more fuel than
is in the the hotly contested Artic National Wildlife Refuge. I'm not a
fan of hydroelectric because I like rafting and fishing, and I'm not a
fan of "nuculer" because I think it's irresponsible until we figure out
what to do with the waste. We should also be investing in research into
carbon sequestration, for example by removing CO2 from power plant smoke
stacks and piping it to the bottom of the ocean, or managing
agricultural systems and forests to store more carbon in soils (and I
have some somewhat far-fetched ideas about how to get more CO2 into the
Southern Ocean that I'm hoping to do some research on). But at the end
of the day, when you add up all our emissions and all the potential ways
to reduce them, there is still a huge mismatch and I'm afraid nothing
short of a global carbon tax will ever slow them down. Even if we
managed to stop emitting any CO2 today (an impossibility), that which we
have already emitted would result in elevated atmospheric concentrations
for another few hundred years. Even if we managed to stop increasing
our emissions and just held them level (a more realistic possibility),
the CO2 concentration would continue to climb steadily for the next
several hundred years. So there are no easy answers. For comparison,
the ozone hole problem is easier to address because CFCs can be
replaced, and industrial pollution is easier to address because the
pollutants are by-products that can be eliminated. In contrast, CO2 is
the inevitable result of burning fossil fuels (oxidation of carbon is
what produces the energy). People have suggested various geoengineering
approaches to control global climate, for example giant mirrors in space
or giant gates controlling water flowing out of the Mediterranean, but
these seem incredibly costly and more likely to do unexpected harm than
their planned good. Nevertheless, I am optimistic that technological
developments will contribute in many ways to mitigating the problem.
So, I think the physical world will be a very different place in 50
years, but I'm also not convinced the global political situation is any
more stable so it's hard to argue that it should take priority over
other items on the national agenda. I'd be interested to hear your
perspective, especially as someone who has a better idea of how big
deals actually get made. If in 10 years, events are such that everyone
in the U.S. is completely convinced that climate change is a serious
threat, how will our political and industrial leaders respond? If I do
figure out how to get CO2 out of the atmosphere, how do I make my
billion? Just for reference, carbon emission credits are already
trading on various exchanges, and are one way countries can meet their
obligations under Kyoto (e.g. instead of reducing their own emissions
France could pay Russia to reduce theirs). It is anticipated that in
the future, CO2 sequestered in forest soils or in the oceans could also
be traded. I haven't checked in awhile, but the going rate was
something like $3 dollars per ton of CO2. The current uncertainty on
how much CO2 forests in the U.S. are taking up is around 500 billion
tons, and our Kyoto emission reduction obligation would have been
several hundred billion tons. So if we do enter into something like
Kyoto and have to buy credits to meet our obligations, a trillion dollar
industry may be created overnight.
If you want to do some further reading, I can recommend the Summary for
Policymakers and the Technical Summary of the Intergovernmental Panel on
Climate Change's Third Assessment Report Scientific Basis Volume
(http://www.grida.no/climate/ipcc_tar/). This is a bit dated (2001),
but the next one won't come out until next year. Also, the
International Geosphere-Biosphere Programme's Past Global Changes
Report: Environmental Variability and Climate Change
(http://130.92.227.18/4DAction/4DLK_SearchProdType/work) is also a good
read. I also just came across this web page, which looks like a good
perspective: http://www.aip.org/history/climate/index.html. You also
have a great resource there in Palisades. The folks at LDEO really know
what they're talking about. I'm sure they have some "public" lectures
that would be interesting, but you might have more fun sitting in on
technical seminars (which are also open to the public) and just seeing
how long you can hang on. Wally Broecker is a famous and charismatic
geochemist / climatologist there who you should keep an eye out for. He
recently got linked up with Gary Comer (I think the founder of Bass) who
as a result is now funding a number of researchers in my field as well
as investing in a company that is trying to develop a device to actively
remove CO2 out of air.
My guess is that this was more information than you were looking for, so
if your heads gone blurry, just remember that A) we're screwed, B) I get
a cameo in your first film, and C) you'd better come visit me in
Colorado while we still have trees and snow.
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