ECOSCIENCE AFTER NUCLEAR WAR
Atomic affects on the environment.
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STAFF PHOTOS
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Paul Ehrlich (Bing Professor of Population Studies and
Professor of Biological Sciences, Stanford University) and
Anne Ehrlich (Senior Research Associate, Department of
Biological Sciences, Stanford) are familiar names to
ecologists and environmentalists everywhere. But while most
folks are aware of the Ehrlichs' popular writing in the
areas of ecology and overpopulation (most of us for
instance - have read Paul's book The Population Bomb),
few people have any idea of how deeply the Ehrlichs are
involved in ecological research (the type that tends to be
published only in technical journals and college texts).
That's why we're pleased to present this regular semi
technical column by these well-known authors/
ecologists/educators.
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by Anne and Paul Ehrlich
Recent studies indicate that our previous evaluation of the
ecological impact of nuclear war (in MOTHER NO. 71) was
probably much too optimistic! Put simply, the
potential effects of the production of huge amounts of
smoke and dust (resulting from a nuclear attack), upon
which we speculated in our earlier column, have now been
subjected to the scrutiny of atmospheric scientists. And
the results of that research are frightening.
The most thorough of these studies owes its inspiration, in
part, to a catastrophe that occurred long before Homo
sapiens arrived on the scene. About 65 million years
ago, at the transition between the Cretaceous and Tertiary
geological periods (it's called the KT boundary), a number
of groups of unspectacular microscopic marine creatures
went extinct quite suddenly. Furthermore, the last of the
dinosaurs accompanied them into oblivion.
The cause of the K-T extinctions-as well as the actual
speed with which they took place remains rather
controversial. One recent hypothesis suggests that they
were the consequence of a thick cloud of dust that was
thrown into the atmosphere by the impact of a gigantic
meteor. A good bit of interesting geological evidence
supports this theory, too, and it-in turn-has stimulated
scientific consideration of the potential climatic (and
other) effects of suddenly introducing massive amounts of
particulate matter into the atmosphere.
A COMPLICATED SYSTEM
Of course, evaluating the effects of such a hypothetical
event is far from simple, partly because the workings of
the atmosphere are not yet completely understood. In
particular, predicting the results of relatively minor
atmospheric changes is often impossible. However, the
effects of major changes can sometimes be more
readily calculated (for example, the primary differences
between winter and summer are easily forecast).
Today, projections produced by computers are made with
models that are very simplified, compared with actual
weather systems, and carry uncertainties about the effects
of even large-scale disturbances. Nonetheless, such
projections can provide valuable insights into the
climatic results of atmospheric changes.
Once the investigation of massive particulate injections
into the atmosphere was stimulated by interest in the K-T
extinctions, it was a logical step to apply computer
analysis to the meteorological consequences of an atomic
war. This is precisely what a small group of physical
scientists did. A draft paper based on their work was
subjected to the scrutiny of a conference of leaders in
that field this past April, and the results were then
immediately presented to a group of distinguished
biologists. Both meetings were closed to the public in
order to prevent the premature release of tentative
conclusions.
The authors of the paper on atmospheric effects-R.P. Turco,
O.B. Toon, T. Ackerman, J.B. Pollack, and the well-known
astronomer Carl Sagan-gave the document the lugubrious
(and, unfortunately, appropriate) acronym TTAPS. The TTAPS
conclusions can be summarized briefly: If a nuclear
exchange exploded as little as 100 megatons (about 1% of
the combined megatonnage contained in U.S. and Soviet
strategic arsenals), it could produce sufficient dust
and smoke to prevent 99% or more of the sunlight from
reaching the Earth's surface for weeks!
We do want to emphasize the word "could", because of the
many variables involved. While as little as 100 megatons
-if distributed over cities in a manner that would maximize
soot producing fires might produce such a
catastrophe, a larger war that expended 5,000 to 10,000
megatons would be far more likely to bring about a
worldwide "blackout". Yet even in a larger war, the size
and altitude of the explosions could produce a variety of
effects. High-yield ground bursts-used to dig out the
enemy's missile silos-would inject vast amounts of dust
into the upper atmosphere (the stratosphere), and
smaller air bursts used against cities and troops-would
ignite huge, widespread fires, injecting soot into the
lower layer of air (the troposphere).
The characteristics of these two layers are very different.
The troposphere is relatively well mixed vertically, and
particles in it usually settle out rather rapidly. The
stratosphere, in contrast, is quite stable, and particles
tend to remain in it for a long time. But the presence of
huge quantities of dust and soot could change those
characteristics, possibly even destroying the division
between troposphere and stratosphere!
The degree to which atmospheric effects would spread from
the Northern to the Southern Hemisphere would be determined
by the geographic placement of the nuclear bursts and by
what happened to the structure of the atmosphere. A final
uncertainty is that the simple TTAPS model doesn't include
the effects of atmospheric motions. Nevertheless, despite
its built-in uncertainties, the study's basic findings have
recently been supported by a more complex, dynamic model
run by Dr. Stephen H. Schneider's group at the National
Center for Atmospheric Research.
A GAME WITH NO WINNERS
Basically, then, TTAPS and related studies can't tell us
precisely what will happen in an atomic war . . . but they
can tell us what consequences can't be ruled out.
Such "worst case scenarios" are vitally important to
decision makers (and to the rest of us!) . . . and the
TTAPS description of the possible effects of a war fought
largely in the Northern Hemisphere is enough to make any
sane strategist forget all about "winning" a nuclear
battle.
The blocking of incoming solar radiation would produce
severe climatic disturbances, the most important of which
would be a pronounced surface cooling of the globe . . .
especially in the continental regions of the Northern
Hemisphere. In a matter of weeks, the average temperature
could drop to far below freezing and remain very low for
months. (The Schneider group's model also shows that in
three weeks much of this land area would be plunged into
below-freezing weather ... even in the month of July!) And
the TTAPS study predicts that, for as long as a year after
the war, temperatures might remain subnormal. At worst, the
planet's entire surface would be dusky or dark at noon . .
. and most land areas would be in the grip of temperatures
well below the freezing point.
The biologists who were consulted were unanimous in their
opinion that any war that caused widespread cooling and
darkness would have no less than a catastrophic impact on
natural and agricultural ecosystems. (Again, however, the
precise nature of the consequences would depend on such
unknowns as the season in which the war broke out and the
degree to which atmospheric changes spread southward.) The
combination of freezing cold with light levels too low to
permit photosynthesis would destroy most of Earth's growing
vegetation . . . upon which all animals, including people,
are completely dependent. Much of the flora, especially in
temperate zones, would eventually regenerate from seeds and
roots, but by then most of the animals would be beyond
saving. Standing crops in the Northern Hemisphere that
survived fires would be destroyed by the freezing
temperatures and lack of sunlight.
As all the streams, rivers, and lakes froze, water would
become scarce. Low light levels would reduce the
productivity of the ocean, too. And all of these disasters
would occur in combination with the presence of toxic smog
over the entire Northern Hemisphere . . . higher levels of
radiation than previously forecast . .. and a variety of
other assaults on both people and ecosystems (many of which
we discussed in our earlier column).
DOWN THE PATHOF THE
DINOSAURS
If you put all this information together, just what have
you got? Well, you have a rather clear idea that-after a
nuclear warcivilization would have almost no chance of
surviving in the Northern Hemisphere. The vast majority of
its inhabitants would be dead . . . and those not killed
outright by blast, fire, and lethal radiation would quickly
succumb to exposure, thirst, starvation, disease, or
radiation sickness in the freezing, smoggy darkness.
You can also see the likelihood of an epidemic of sudden
extinctions of nonhuman organisms even more
dramatic than the one that occurred at the K-T boundary.
Finally, you may now have the chilling suspicion that
humankind itself might be pushed rapidly down the path to
oblivion once trod by the dinosaurs.
The basic results of the TTAPS study and the
conclusions of the biologists are summarized in two
manuscripts recently submitted to Science
magazine. A more detailed discussion of post-war
ecological effects can be found in Paul's chapter in
The Counterfeit Ark: Crisis Relocation for Nuclear War
edited by Jennifer Leaning and Langley Keyes. The book
is available in paperback for $11.95 postpaid and in
hardcover for $28.00 postpaid from Ballinger Publishing
Company (Dept. TMEN, P.O. Box 281, Harvard Square,
Cambridge, Massachusetts 02138).
The Ehrlich's work is supported in part by a grant from
the Koret Foundation of San Francisco.