$00 1009 Ni VAN A \ \__\ e@ & AY o \ \ \ ‘ v\\ 3 v\h Peak Shock Overpressure , psi \ \\\ _ 5 \ WAN \ , ° e ww 100 —%, uw) ra 2 404 Feet 3 z x N 23 ee \ ve <=ere sameeren Va 5 [7 = ° "i ; vn “s° \ \. \ \ — —~— f--- e ° ° 4 | \f a a °\ e + tvy Mie (a 2 307 Feet) - y ° \ — oO Pd vr \ \\ bnamee Theereties! Curve fer ivy Mike 17 Yo iw \ Jangie Surface (5 =~ Free Air Scaled to 2 kt ° po a ee - @ xporimentel Date, Shot — Averoge Theeretical Serve {@: 376 Feet) ~~ ty : A \ \ Shot 6 Woter Surfoce Shst 4 Water Surface @ \ Composite Free Air tkt & © 100 IN oO - 2 NYA — = ° x \ \ Shot 2 Water Surtace @ \ 4 \ \ v & \ 'o >:& = \ \ \ a UNA @ 2349 Feet \ snot tRet ! FoI T Shot 2 Land Surtoce ° a a Limiting Theoretioal Curves Shot 2 @ to 2 = Equivaiont TNT Cherge Radius in Feet | \ lo \\ 10 20. Vertical Distance above GZ , 10° Feet Figure 2.6 Vertical pressure-distance data, Shot 2, with curves derived from NOL theory. | F to 100 1000 Distance from GZ , Feet Figure 2.7 Surface pressure-distance Gaia scaled to 1 kt at sea level.

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