(
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