( nnn. | ' . | ‘ Cox ,&, | | a Meteora legy C Development ; Cirects for 1 Where ~~ ho Eiast near-greend . twé, - a ft: Ae. bursts) ' I (See also Shock t _. + -. _ . } Petpse: where [. rm ! Lo. velecity = | For | Wave wt-303) eC ie oes7 Pp), !) wr CCito42g 7P), BEST AVAILABLE COPY ~ 2 ¢ # shock speed ware veloc Fy of seen a —+— Pp peak Overle ressurag: A = P= ambient air pressure A - * b | Diverg ence. rap idty Pp + f E~ (+ - fpese 2 \ tec one fren ~_e eo RK K ft [sec 22.07 %-K”* The (bbe 4t eq Ko stat. Mm! K = teme c = tas For humidity The ensuing ‘ bors 4; /M?) ase eT degrees Small, correction develagments tan og: Yr" = Sp. ft. ratee % (v8) Rigas covctant Mawel, wrt. Rs gas cous Tt. z) Jbr seynd, stl ys AT om 7gyceme. ee . érature , of veleccty LAT wh f: deussty GS. gH a@Qir ten om Bs embiont kuets k Cverrtees f. res 7 2433 feom =(r Cerrec Tere x t ft . 2.7 38.98 Kk@® \ where 6CO fean 1 Cc ; pse PU/p tt Cc reduces use « Keluim 2 C2 + 273 dry air. ( fomis. ty virtual assume e temperature that ox Cc. 7 i : Cr UL tose whine Cz = irclination A= velosity tos B CSneli's Law) of wind velocity of shock ef wave 3) LLNL . of Soond velocity wu 2 Component B= A vay fyent tm from bearing coms déreae LoviqenT Ls tnte-rsectier afte