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NASA Scientific and Technical Aerospace Reports

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20040073763 Georgia Tech Research Inst., Atlanta, GA<br />

Mitigation of Atmospheric Effects on Imaging Systems<br />

Gimmestad, Gary G.; Belen’kii, Mikhail S.; Mar. 31, 2004; 27 pp.; In English; Original contains color illustrations<br />

Contract(s)/Grant(s): DAAD19-00-1-0503<br />

Report No.(s): AD-A422695; ARO-40432.1-C1; No Copyright; Avail: CASI; A03, Hardcopy<br />

Atmospheric effects such as refractive turbulence <strong>and</strong> aerosol obscuration can seriously degrade the performance of<br />

military optical systems. A complete underst<strong>and</strong>ing of these effects is therefore essential for optimizing the design of such<br />

systems, <strong>and</strong> it is also necessary for developing mitigation techniques. The project described here was a three- year theoretical<br />

<strong>and</strong> experimental investigation to develop <strong>and</strong> validate a physical underst<strong>and</strong>ing of several atmospheric effects that are<br />

important for current <strong>and</strong> future Army optical systems. a) An investigation of turbulence-induced waviness in images of edges,<br />

<strong>and</strong> techniques for its mitigation. b) An investigation of the degradation of optical images by atmospheric turbulence <strong>and</strong> a<br />

validation of the predicted dependence of the atmospheric Modulation Transfer Function (MTF) on the inner scale of<br />

turbulence.<br />

DTIC<br />

Atmospheric Effects; Atmospheric Refraction; Images; Imaging Techniques; Optical Equipment; Optical Radar; Refractivity<br />

20040073817 Science Applications International Corp., San Diego, CA<br />

Analysis <strong>and</strong> Simulation of Cavity-Decoupled Chemical Explosions<br />

Stevens, J. L.; Rimer, N.; Xu, H.; Murphy, J. R.; Barker, B. W.; Baily, E.; Oct. 24, 2003; 48 pp.; In English; Original contains<br />

color illustrations<br />

Contract(s)/Grant(s): DTRA01-01-C-0069; Proj-DTRA<br />

Report No.(s): AD-A422856; SAIC-03/2050; AFRL-VS-HA-TR-2004-1030; No Copyright; Avail: CASI; A03, Hardcopy<br />

We analyze data from two sets of decoupled chemical explosions. NORSAR has obtained data from seven decoupled<br />

chemical explosions conducted from 1987-2002 in Alvdalen, Sweden, recorded both in he near field <strong>and</strong> on regional seismic<br />

stations NORES, HAGFORS, <strong>and</strong> NORSAR. The explosions were conducted in three granite chambers at a depth of<br />

approximately 100 meters in chambers with volumes of 200, 300 <strong>and</strong> 1000 m <strong>and</strong> yields ranging from 2500 kg to 10,000 kg.<br />

The smallest explosion in the largest chamber is almost fully decoupled while the other explosions are partially coupled,<br />

overdriven by up to a factor of 25. The data show that decoupling remains fairly constant for overdrive up to about a factor<br />

of 10, then decreases rapidly at higher yields. 1D <strong>and</strong> 3D simulations of these explosions are performed to model the data.<br />

IDG has digitized a set of surface seismic data recorded from a series of Soviet high-explosive cavity decoupling tests<br />

conducted in a mine in Kirghizia in the summer of 1960.<br />

DTIC<br />

Cavities; Chemical Explosions; Explosions; Simulation<br />

20040073820 Science Applications International Corp., San Diego, CA<br />

Improved Focal Depth Determination for Use in Seismic Monitoring of the Underground Nuclear Explosions<br />

Murphy, J. R.; Barker, B. W.; Marshall, M. E.; Rodi, W. L.; Nov. 19, 2003; 60 pp.; In English<br />

Contract(s)/Grant(s): DTRA01-01-C-0056; Proj-DTRA<br />

Report No.(s): AD-A422863; AFRL-VS-HA-TR-2004-1031; No Copyright; Avail: CASI; A04, Hardcopy<br />

Seismic event location remains as one of the most important discriminants for separating natural tectonic <strong>and</strong> explosive<br />

events. For example, it has been estimated that approximately 8O%of known global earthquakes have focal depths greater than<br />

50 km or are located more than 25 km at sea. Since underwater nuclear explosions can be confidently identified to very low<br />

yields using hydroacoustic data, it follows that the vast majority of earthquakes can potentially be identified on the basis of<br />

location alone. This is an important observation since global monitoring of underground nuclear testing may require the<br />

screening of tens of thous<strong>and</strong>s of seismic events per year <strong>and</strong>, in order to perform this function efficiently, it will be necessary<br />

to have simple <strong>and</strong> robust discriminants available which can be used to eliminate the vast majority of these events from more<br />

detailed consideration. However, in order to be useful for such discrimination purposes, the uncertainties associated with<br />

seismic locations must be well defined <strong>and</strong> reliable <strong>and</strong> this has proved to be difficult to accomplish.<br />

DTIC<br />

Depth Measurement; Nuclear Explosions; Seismology; Underground Explosions<br />

145

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