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SCIENCE: Disaster Insurance
By Richard A. Posner
No one knows how global warming will unfold, but we
should prepare today as if catastrophe will strike tomorrow. By Richard A. Posner.
The latest report of the Intergovernmental Panel on
Climate Change, issued in February, confirms the scientific consensus that
the emission of carbon dioxide and other greenhouse gases, as a result of
the combustion of fossil fuels such as oil and gas, and other human
activities (such as deforestation by burning), is having significant and on
the whole negative effects, causing global temperatures and sea levels to
rise. In my book Catastrophe: Risk and Response (2004), I considered the evidence to be altogether
convincing that global warming was a serious problem for which human-caused
emissions were the principal cause—and since then, more evidence has
accumulated and the voices of the dissenters are growing weaker. The
global-warming skeptics are beginning to sound like the people who for so
many years, in the face of compelling evidence, denied that cigarette
smoking was harmful to health.
What has changed since I wrote my book is that not
only has the evidence become even more convincing that our activities
(primarily the production of energy) are causing serious harm, but also the
scientists are becoming increasingly pessimistic. It is now thought likely
that by the end of the century, global temperatures will have risen by an
average of 7 degrees Fahrenheit and the sea level will have risen by almost
two feet. Besides inundating low-lying land, turning tropical farms into
desert, and causing tropical diseases to migrate north, global warming is
expected to produce ever more violent weather patterns—typhoons,
cyclones, floods, and so forth.
There is much uncertainty in climate science, and
climate scientists concede that their predictions may be off—and they
may be off in either direction. Far worse consequences are possible than
those thought highly likely by the authors of the report, including a
temperature increase of 12 rather than 7 degrees Fahrenheit, higher sea
levels that could force the migration inland of tens of millions of people
(or more), the deflection of the path of the Gulf Stream, causing
Europe’s climate to become Siberian, and abrupt, catastrophic
sea-level rises due to the Antarctic ice shelf sliding into the ocean. Not
only has the consensus grown stronger among scientists concerning the
harmful anthropogenic (human-caused) character of global warming, but
recent evidence indicates that the global-warming problem is more serious
than scientists thought just a few years ago.
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Global warming is already imposing costs. These will probably increase steadily in the years ahead.
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My own view, argued in the book, is that the risk of
abrupt global warming—a catastrophe that could strike us at any time,
with unknown though presumably low probability—is sufficiently costly
in expected-cost terms (that is, multiplying the cost of the catastrophe by
its probability) to warrant taking costly measures today to reduce
emissions of carbon dioxide and other greenhouse gases. Both the scientists
and the policy makers, however, are focused mostly on the long-term costs
of global warming—costs that will unfold over the remainder of this
century. That focus makes the choice of the discount rate important, and
potentially decisive.
The discount rate is an interest rate used to equate a
future cost or value to a present cost or value. As a simple illustration
(and ignoring complications such as risk aversion), if the interest rate is
5 percent, the present value of $1.05 to be received in a year is $1,
because if you are given $1 today you can invest it and have $1.05 in a
year. Such is financial discounting. But discounting is important even when
financial considerations are not the only ones involved. If you have a very
strong desire to spend money now rather than a year from now, you might
prefer $1 today to $1.50 a year from now.
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Illustration by Taylor Jones for the Hoover Digest.
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These approaches, however, don’t work well when
we ask how much we should spend today to avert costs that global warming
will impose in the year 2107. Suppose we estimated that those costs would
be $1 trillion. At a discount rate of 5 percent, the present-value
equivalent of those costs is only $7.6 billion, for that is the amount
that, invested at 5 percent, would grow to $1 trillion in 100 years. At a
10 percent discount rate, the present value shrinks to $73 million.
So it is possible to argue that, rather than spending
a substantial amount of money today to try to prevent losses from global
warming in the future, we should be setting aside a modest amount of money
every year—$73 million this year to deal with global warming in 2107,
the same amount next year to deal with global warming in 2108, and so on.
Of course, we would also want to pay to prevent the lesser losses from
global warming that we anticipate in earlier years. For example, suppose we
estimate that the loss in the year 2057 will be $100 billion. Then, at the
same 10 percent interest rate, we would want to spend $852 million this
year.
Thus, two effects are being balanced in computing the
present equivalent of future losses from global warming—the larger
loss in the more distant future, and the greater shrinkage of the larger
loss, because of its remoteness from today, by the operation of
discounting. The discounting effect will often dominate, as in the
examples, but this depends critically on the choice of a rate. At an
interest rate of 3 percent, a $1 trillion loss in 2107 has a present value
not of $73 million, or $7.6 billion, but $52 billion. When any of those
figures is added to the present value of losses in intermediate years, the
sum will be formidable.
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Environmental worries aside, if we reduce our consumption of energy
by imposing a heavy energy tax, we gain national security benefits by reducing our dependence on imported oil.
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What would justify a very high discount rate, which
implies that optimal current expenditures to avert the consequences of
global warming are relatively low? Perhaps the march of science will
deliver us from the consequences of global warming long before the end of
the century. Clean fuels for automobiles and electrical plants (where there
is already a clean, though more expensive, substitute for oil or coal:
nuclear power) will be developed; carbon dioxide emissions from electrical
plants may be piped underground; bacteria may be developed to
“eat” atmospheric carbon dioxide. Although these are not
certainties, they are likely, and so provide a good argument for using a
high discount rate, such as 10 percent—and perhaps for considering no
losses after 2107, on the theory that the problem of global warming is
almost certain to be solved by then.
Nevertheless, there are at least three arguments for
incurring hefty current expenditures to reduce carbon dioxide emissions in
the near term. The first is that global warming is already imposing costs,
which will probably increase steadily in the years ahead. Discounting does
not affect those costs very much. They may well be great enough to warrant
remedial action now.
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My own view is that the risk of abrupt global warming—a catastrophe
that could strike us at any time, with unknown though presumably low probability—is sufficiently costly to warrant taking costly measures today.
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The second argument is that there is a small risk of
abrupt, catastrophic global warming at any time, and a small risk of a huge
catastrophe can add up to a very large expected cost. “Any
time” could of course be well into the future, and thus discounting
still has a role, but it is minimized when the focus is on imminent danger.
The third argument is that reducing our consumption of
energy by imposing a heavy energy tax would confer national security
benefits by reducing our dependence on imported oil. Our costly involvement
in the Middle East is due in significant part to our economic interest in
maintaining the flow of oil. It is true that because our own oil is costly
to extract, a heavy energy tax would not cause much if any substitution of
domestic for foreign oil. But that is fine; our oil would remain in the
ground, available for consumption if we decide to take measures abroad,
such as withdrawing from Iraq, that might reduce our oil imports.
Heavy U.S. energy taxes would induce greater
expenditures by industry on developing clean fuels and techniques for
carbon sequestration, might persuade other big emitters like China and
India to follow suit, and by reducing emissions of carbon dioxide slow the
increase in the atmospheric concentration of the gas. Drastic reductions
might actually reduce that concentration, because carbon dioxide does
eventually leach out of the atmosphere, though at a slower rate than it is
built up by emissions.
This essay appeared in the Becker-Posner Blog on
February 4, 2007.
Available from the Hoover Press is Politicizing
Science: The Alchemy of Policymaking, edited by Michael Gough. To
order, call 800.935.2882 or visit www.hooverpress.org.
Judge, U.S. Seventh Circuit Court of Appeals; Author, Breaking the Deadlock.
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