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POLICYFORUM<br />
762<br />
The OST regime has potenti<strong>al</strong>ly more<br />
fl exibility than CTBT in supporting nontreaty<br />
applications of monitoring. Existing OST<br />
monitoring platforms have been successfully<br />
used, for example, in support of humanitarian<br />
relief after the 2005 hurricanes Katrina<br />
and Rita in the United States and the 12 January<br />
2010 earthquake in Haiti ( 12). Moreover,<br />
Russia has expressed support for this concept<br />
( 13), so there may be opportunities for<br />
fi elding new technologies in aircraft-based<br />
monitoring ( 11) and for at least bilater<strong>al</strong> (and<br />
ultimately multilater<strong>al</strong>) engagement through<br />
nontreaty monitoring.<br />
A case in point is the characterization and<br />
tracking of dust in the atmosphere, which<br />
faces ch<strong>al</strong>lenges similar to those of glob<strong>al</strong><br />
radionuclide monitoring. Lofted across continents<br />
and oceans, dust has an important infl uence<br />
on climate because it can both absorb<br />
and refl ect sunlight, and its distribution is a<br />
symptom of glob<strong>al</strong> atmospheric conditions<br />
( 14– 18). Microorganisms are <strong>al</strong>so transported<br />
<strong>al</strong>ong with the dust, so that public<br />
he<strong>al</strong>th is affected over intercontinent<strong>al</strong> distances<br />
( 19– 21). Despite its signifi cance for<br />
environment and he<strong>al</strong>th (from agriculture<br />
and climate to pollution and disease), little is<br />
known about the nature of dust in the troposphere.<br />
Much could be learned from physic<strong>al</strong><br />
collections made possible by complementary<br />
surface- and aircraft-based platforms.<br />
More gener<strong>al</strong>ly, collection of gases and<br />
aerosols both at and above ground level can<br />
greatly improve atmospheric-transport models,<br />
which have applications ranging from<br />
medium- and long-term weather forecasting<br />
to tracking radioactive plumes caused<br />
by human activity. Examples of success<br />
include a study using the distribution of krypton-85<br />
to constrain atmospheric transport<br />
times b<strong>et</strong>ween northern and southern hemispheres<br />
( 22). Similarly, the Glob<strong>al</strong> N<strong>et</strong>work<br />
of Isotopes in Precipitation, operated jointly<br />
by the Internation<strong>al</strong> Atomic Energy Agency<br />
and World M<strong>et</strong>eorologic<strong>al</strong> Organization, provides<br />
data that have led to improved quantifi -<br />
cation of sources and transformation of water<br />
in the atmosphere, as well as b<strong>et</strong>ter predictions<br />
of precipitation ( 23).<br />
Aircraft can measure vertic<strong>al</strong> profi les of<br />
constituents in the atmosphere much b<strong>et</strong>ter<br />
than satellites, providing data cruci<strong>al</strong> for<br />
identifying sources and sinks (e.g., for CO 2<br />
and other greenhouse gases). For example,<br />
“Civil Aircraft for the Regular Investigation<br />
of the Atmosphere Based on an Instrument<br />
Container” (www.caraabic-atmospheric.<br />
org) uses an instrumented passenger airliner<br />
to monitor gases and aerosols and has<br />
proven to be inv<strong>al</strong>uable for tracking volcanic<br />
clouds, air pollution, and much more.<br />
Similarly, the High-performance Instrumented<br />
Airborne Platform for Environment<strong>al</strong><br />
Research (HIAPER) Pole-to-Pole Observations<br />
Project used a Gulfstream V research<br />
plane (see the photo) to document concentrations<br />
of CO 2, CH 4, and many other gases from<br />
sea level up to 47,000 fe<strong>et</strong>, with unique science<br />
r<strong>et</strong>urn from hundreds of profi les <strong>al</strong>ong<br />
the Pacifi c ( 24). But only fi ve pole-to-pole<br />
transects have been compl<strong>et</strong>ed to date. This<br />
fl ight design can serve either treaty or environment<strong>al</strong><br />
monitoring objectives.<br />
Collecting and an<strong>al</strong>yzing gas and particulate<br />
data are essenti<strong>al</strong> for improving atmospheric<br />
transport models and greatly advance<br />
the ability to characterize the atmosphere to<br />
distances of hundreds and even thousands<br />
of kilom<strong>et</strong>ers from a fl ight path or a groundbased<br />
station. That is, the information can<br />
help in monitoring neighboring countries, as<br />
well as the country being overfl own ( 25).<br />
Fin<strong>al</strong>ly, airborne LIDAR (Light D<strong>et</strong>ection<br />
and Ranging, the laser-based an<strong>al</strong>og of<br />
RADAR) can play an important role in monitoring<br />
forest carbon stocks ( 26). This is v<strong>al</strong>uable<br />
for such efforts as the United Nations<br />
Reducing Emissions from Deforestation<br />
and Forest Degradation program, as well as<br />
broader applications.<br />
We have touched on a few examples to<br />
illustrate rich opportunities for scientific<br />
advancement and internation<strong>al</strong> cooperation<br />
that would be offered by implementing far<br />
more extensive aircraft- and ground-based<br />
environment<strong>al</strong> monitoring around the globe.<br />
Recommendations<br />
In some sense, nontreaty applications should<br />
be viewed as one of the ultimate long-term<br />
objectives of an arms-control monitoring<br />
regime. Without such applications, monitoring<br />
may not be sustainable. With such applications,<br />
however, monitoring can be enhanced<br />
through implementation of new technologies,<br />
engagement of more participants and—more<br />
gener<strong>al</strong>ly—through improvements in transparency<br />
among nations.<br />
Specifi c<strong>al</strong>ly, our recommendations are (i)<br />
to acknowledge the opportunities offered by<br />
nontreaty applications of monitoring capabilities<br />
that origin<strong>al</strong>ly derive from arms-control<br />
regimes; (ii) to develop and implement concr<strong>et</strong>e,<br />
re<strong>al</strong>istic plans to pursue those opportunities,<br />
requiring input from many disciplines<br />
and countries; and (iii) for the United States<br />
and willing partners to take leadership in promoting<br />
nontreaty applications of monitoring,<br />
starting with bilater<strong>al</strong> projects.<br />
A key aspect to implementation of nontreaty<br />
monitoring is to defi ne approaches that<br />
15 FEBRUARY 2013 VOL 339 SCIENCE www.sciencemag.org<br />
Published by AAAS<br />
are fl exible, clear, and mutu<strong>al</strong>ly acceptable to<br />
<strong>al</strong>l parties concerned. There is opportunity not<br />
only for applying existing capabilities to new<br />
circumstances, but <strong>al</strong>so in developing new<br />
technologies for glob<strong>al</strong> environment<strong>al</strong> monitoring<br />
that can serve the broader mandate of<br />
improving transparency and enhancing confi -<br />
dence. The idea is to create a win-win scenario<br />
whereby the monitoring capability is viewed<br />
as benefi ci<strong>al</strong> to <strong>al</strong>l, perhaps even fi rst and foremost<br />
of benefi t to the country being studied.<br />
References and Notes<br />
1. Adopted by the UN Gener<strong>al</strong> Assembly in 1996, the CTBT<br />
has not y<strong>et</strong> entered into force. Of 337 planned IMS facilities,<br />
274 have thus far been certifi ed. See ( 3).<br />
2. U.S. Ambassador Paul Nitze defi ned ”effective verifi cation”<br />
in 1988 as: “if the other side moves beyond the<br />
limits of the treaty in any militarily signifi cant way,<br />
we would be able to d<strong>et</strong>ect such violations in time to<br />
respond effectively and thereby deny the other side the<br />
benefi t of the violation.”<br />
3. CTBTO Preparatory Commission, www.ctbto.org/<br />
verifi cation-regime/.<br />
4. O. Dahlman <strong>et</strong> <strong>al</strong>., D<strong>et</strong>ect and D<strong>et</strong>er: Can Countries Verify<br />
the Nuclear Test Ban? (Springer, New York, 2011).<br />
5. A. Stohl <strong>et</strong> <strong>al</strong>., Atmos. Chem. Phys. Discuss. 11, 28319<br />
(2011).<br />
6. Capacity Development Initiative, www.ctbto.org.<br />
7. There is considerable variability in this growth: see ( 4, 6).<br />
8. D<strong>et</strong>ails on implementation, cost, <strong>et</strong>c., are complicated<br />
by differences among monitoring technologies (e.g.,<br />
seismic versus radionuclide) and the associated research<br />
communities.<br />
9. A sm<strong>al</strong>l fraction of attempted overfl ights are not successful<br />
due to weather or mechanic<strong>al</strong> problems.<br />
10. Organization for Security and Co-operation in Europe,<br />
Open Skies Treaty Observation Flights, From Entry-<br />
Into-Force to December 2011 [Open Skies Consultative<br />
Commission (OSCC), Vienna, 2012]; www.osce.org/<br />
secr<strong>et</strong>ariat/68315/.<br />
11. S. D. Drell, C. W. Stubbs, Arms Control Today 41(6), 15<br />
(2011).<br />
12. M. B<strong>et</strong>ts, D. Spence, presentation at 2nd Open Skies<br />
Review Conference, Vienna, Austria, 7 to 9 June 2010<br />
(OSCC, Vienna, 2010); www.osce.org/secr<strong>et</strong>ariat/68251.<br />
13. S. Federyakov, presentation at 2nd Open Skies Review<br />
Conference, Vienna, Austria, 7 to 9 June 2010 (OSCC,<br />
Vienna, 2010); www.osce.org/secr<strong>et</strong>ariat/68573.<br />
14. J. M. Prospero <strong>et</strong> <strong>al</strong>., Rev. Geophys. 40, 1002 (2002).<br />
15. D. M. Cwiertny, M. A. Young, V. H. Grassian, Annu. Rev.<br />
Phys. Chem. 59, 27 (2008).<br />
16. K. A. Prather, C. D. Hatch, V. H. Grassian, Annu. Rev.<br />
An<strong>al</strong>. Chem. 1, 485 (2008).<br />
17. M. Pósfai, P. R. Buseck, Annu. Rev. Earth Plan<strong>et</strong>. Sci. 38,<br />
17 (2010).<br />
18. S. A. Strode, L. E. Ott, S. Pawson, T. W. Bowyer,<br />
J. Geophys. Res. 117, (D9), D09302 (2012).<br />
19. D. W. Griffi n, Clin. Microbiol. Rev. 20, 459 (2007).<br />
20. S. Ravi <strong>et</strong> <strong>al</strong>., Rev. Geophys. 49, RG3001 (2011).<br />
21. C. E. Morris <strong>et</strong> <strong>al</strong>., Biogeosciences 8, 17 (2011).<br />
22. D. J. Jacob <strong>et</strong> <strong>al</strong>., J. Geophys. Res. 92, (D6), 6614 (1987).<br />
23. Glob<strong>al</strong> N<strong>et</strong>work of Isotopes in Precipitation, www-naweb.<br />
iaea.org/napc/ih/IHS_resources_gnip.html.<br />
24. S. Wofsy <strong>et</strong> <strong>al</strong>., Philos. Trans. R. Soc. London Ser. A<br />
369, 2073 (2011).<br />
25. This can have practic<strong>al</strong> implications in that a friendly neighboring<br />
state may more readily authorize overfl ights.<br />
26. Forest Carbon and Credent form partnership on LiDAR<br />
technology, http://forest-carbon.org/media/forestcarbon-credent-lidar-partnership.<br />
Acknowledgments: We thank S. D. Drell, J. E. Goodby, G.<br />
P. Shultz, and C. W. Stubbs for helpful discussions. Views<br />
presented here are the authors’ and do not necessarily refl ect<br />
those of the U.S. government.<br />
10.1126/science.1228731<br />
on February 14, 2013<br />
www.sciencemag.org<br />
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