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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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