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ec
ti
v
it
y
[
2
0
]
,
FS
O
s
y
s
te
m
s
ar
e
o
f
ten
u
tili
ze
d
as
th
e
lo
ca
l
ar
ea
n
et
w
o
r
k
s
(
L
AN)
lin
k
b
etw
ee
n
b
u
ild
in
g
s
o
r
as
th
e
la
s
t
-
m
ile
co
m
m
u
n
icati
o
n
s
co
n
n
ec
tio
n
.
Fig
u
r
e
1
illu
s
tr
ates
s
o
m
e
o
f
t
h
e
F
SO
co
m
m
u
n
icat
io
n
s
y
s
te
m
ap
p
licatio
n
s
f
o
r
ter
r
estrial
n
et
w
o
r
k
s
to
estab
li
s
h
L
OS
co
n
n
e
ctio
n
b
et
w
ee
n
t
w
o
tr
an
s
ce
i
v
er
s
o
v
er
at
m
o
s
p
h
er
i
c
ch
an
n
el.
L
i
n
k
av
a
ilab
ilit
y
f
o
r
ca
r
r
ier
-
class
ap
p
licatio
n
s
i
n
telec
o
m
m
u
n
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io
n
s
is
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s
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al
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y
e
x
p
ec
ted
to
b
e
9
9
.
9
9
9
%.
I
n
co
m
p
ar
is
o
n
,
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9
%
lin
k
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ailab
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it
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icie
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ter
p
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-
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s
s
L
AN
ap
p
licatio
n
s
[
2
1
]
.
Fig
u
r
e
1
.
Dep
lo
y
m
e
n
t o
f
F
SO
lin
k
s
U
s
in
g
l
o
c
al
m
et
e
o
r
o
l
o
g
i
c
a
l
d
at
a
i
s
c
r
u
c
ia
l
f
o
r
a
n
a
c
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r
at
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p
r
e
d
i
c
t
i
o
n
o
f
F
S
O
l
in
k
a
v
ai
l
a
b
i
l
i
ty
.
On
e
im
p
o
r
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an
t
f
a
c
t
o
r
t
o
c
o
n
s
i
d
e
r
w
h
en
p
r
e
d
i
ct
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g
atm
o
s
p
h
e
r
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t
te
n
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a
ti
o
n
d
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e
t
o
h
a
ze
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is
i
b
i
l
i
ty
w
h
i
ch
is
r
el
a
t
e
d
to
p
a
r
t
i
c
l
e
s
i
z
e
d
is
t
r
i
b
u
ti
o
n
[
2
2
]
.
FS
O
av
a
il
a
b
i
l
ity
in
t
r
o
p
i
c
a
l
w
e
a
th
e
r
c
o
n
d
i
t
i
o
n
s
c
an
b
e
r
e
a
l
is
t
ic
a
lly
as
s
e
s
s
e
d
b
y
u
s
in
g
m
e
asu
r
e
d
v
i
s
i
b
i
li
ty
d
a
t
a
in
t
r
o
p
i
c
a
l
cl
im
a
t
e
s
u
ch
as
M
al
ay
s
i
a
.
B
a
s
e
d
o
n
o
u
r
s
tu
d
y
o
f
th
e
c
o
l
lec
t
e
d
d
a
t
a
,
Ma
l
ay
s
i
a
h
as
an
a
v
e
r
a
g
e
v
i
s
i
b
i
l
ity
o
f
9
k
m
.
T
h
is
s
tu
d
y
c
o
m
p
u
t
es
av
a
il
a
b
i
l
ity
u
s
in
g
th
e
FS
O
s
y
s
t
em
’
s
l
in
k
b
u
d
g
e
t
a
n
d
m
e
asu
r
e
d
v
i
s
i
b
i
li
ty
d
a
t
a
.
T
o
p
r
e
d
i
c
t
a
tm
o
s
p
h
e
r
i
c
a
tt
en
u
a
t
i
o
n
d
u
e
t
o
h
a
z
e
,
em
p
i
r
i
c
al
m
o
d
e
ls
a
r
e
u
s
e
d
b
a
s
e
d
o
n
m
e
asu
r
e
d
v
i
s
i
b
i
l
ity
d
a
t
a
.
W
e
in
s
p
e
c
t
h
o
w
h
a
z
e
at
t
en
u
a
ti
o
n
a
f
f
e
c
t
s
F
SO
l
in
k
av
a
il
a
b
i
li
ty
b
y
ex
am
in
in
g
th
e
r
an
g
es
o
f
tw
o
ty
p
i
c
al
l
as
e
r
b
e
a
m
w
a
v
e
le
n
g
t
h
s
em
p
l
o
y
e
d
in
FS
O
s
y
s
t
em
s
th
a
t
a
r
e
c
o
m
m
o
n
ly
u
t
il
i
z
e
d
in
b
u
s
i
n
e
s
s
a
p
p
l
i
c
a
t
i
o
n
s
.
T
h
e
m
ax
im
u
m
o
p
e
r
a
t
i
o
n
a
l
r
an
g
e
f
o
r
F
SO
s
y
s
t
em
s
u
n
d
e
r
v
a
r
i
o
u
s
av
ai
l
a
b
il
i
ty
c
o
n
d
i
t
i
o
n
s
i
s
s
u
g
g
e
s
t
e
d
i
n
t
h
i
s
p
a
p
e
r
.
A
d
d
i
t
i
o
n
a
lly
,
i
t
p
r
o
v
i
d
es
s
u
g
g
e
s
t
i
o
n
s
t
o
t
e
le
c
o
m
m
u
n
i
c
at
i
o
n
s
e
r
v
ic
e
s
p
r
o
v
i
d
e
r
s
r
e
g
a
r
d
in
g
a
ch
ie
v
a
b
l
e
a
v
a
il
a
b
i
li
ty
in
d
i
ca
t
o
r
s
t
h
a
t
m
ay
b
e
c
o
n
s
i
d
e
r
e
d
f
o
r
s
e
tt
in
g
in
FS
O
l
in
k
s
as
a
la
s
t
-
m
il
e
o
p
ti
o
n
.
2.
H
A
Z
E
-
I
NDUC
E
D
AT
T
E
NU
AT
I
O
N
Dif
f
er
en
t
s
u
s
p
en
d
ed
p
ar
ticles
ar
e
en
co
u
n
ter
ed
b
y
th
e
F
S
O
s
ig
n
al
as
it
p
r
o
p
ag
ates
t
h
r
o
u
g
h
t
h
e
at
m
o
s
p
h
er
e
i
n
cl
u
d
in
g
ae
r
o
s
o
l
p
ar
ticles
an
d
g
ase
s
m
o
lec
u
les.
De
g
r
ad
atio
n
r
es
u
lt
s
f
r
o
m
t
h
ese
p
ar
ticle
s
’
in
ter
ac
tio
n
s
w
ith
t
h
e
o
p
tical
s
ig
n
al.
T
h
e
m
a
in
ca
u
s
es
o
f
t
h
e
FS
O
s
i
g
n
al
’
s
atten
u
atio
n
ar
e
s
ca
tter
in
g
an
d
ab
s
o
r
p
tio
n
in
t
h
e
at
m
o
s
p
h
er
i
c
ch
an
n
el.
T
h
e
ab
s
o
r
p
tio
n
i
s
d
ep
en
d
en
t
o
n
t
h
e
w
a
v
ele
n
g
t
h
t
h
at
i
s
u
t
ilized
to
tr
an
s
m
it
d
ata,
a
n
d
it
is
g
e
n
er
al
l
y
v
er
y
s
m
al
l
an
d
i
n
s
ig
n
i
f
ica
n
t
in
t
h
e
o
p
er
atin
g
w
a
v
elen
g
t
h
r
an
g
e
o
f
F
SO
li
n
k
s
.
Scatter
in
g
is
w
a
v
ele
n
g
th
-
d
ep
en
d
en
t
(
λ
)
an
d
I
t
is
d
i
v
id
ed
in
to
th
r
ee
ca
te
g
o
r
ies
ac
c
o
r
d
in
g
to
th
e
s
ize
o
f
air
p
ar
ticles
(
r
)
:
i
)
n
o
n
-
s
e
lecti
v
e
s
ca
tter
in
g
(
r
>>
λ
)
;
ii
)
Mie
s
ca
tte
r
in
g
(
r
≈
λ
)
;
an
d
iii
)
R
a
y
lei
g
h
s
c
atter
in
g
(
r
<<
λ
)
.
T
h
e
ab
s
o
r
p
tio
n
an
d
s
ca
tter
i
n
g
o
f
i
n
f
r
ar
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li
g
h
t
b
y
at
m
o
s
p
h
er
ic
g
as
m
o
lecu
les
a
n
d
ae
r
o
s
o
ls
p
r
o
d
u
ce
s
at
m
o
s
p
h
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ic
atten
u
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n
.
U
s
in
g
t
h
e
ex
p
o
n
e
n
tial B
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r
-
L
a
m
b
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t la
w
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at
m
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ca
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1
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2
3
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1
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w
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p
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atten
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n
co
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f
icien
t
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o
f
len
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.
Mie
s
ca
tter
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g
is
p
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o
v
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R
ay
lei
g
h
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s
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f
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p
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s
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m
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wav
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p
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[
2
4
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w
h
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h
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s
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d
is
tr
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t
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n
o
f
t
h
e
s
ca
tt
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in
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p
ar
ticle
s
.
T
h
e
v
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o
f
is
d
er
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ex
p
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en
tall
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f
o
r
h
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,
m
o
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lo
w
v
is
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il
it
y
a
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g
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as
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.
Evaluation Warning : The document was created with Spire.PDF for Python.
T
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elec
o
m
m
u
n
C
o
m
p
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l
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P
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ma
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ce
a
n
a
lysi
s
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r
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G
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3.
F
RE
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SP
ACE O
P
T
I
CA
L
L
I
NK
M
ARG
I
N
A
li
n
k
p
o
w
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b
u
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g
et
an
al
y
s
i
s
i
s
a
cr
u
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task
f
o
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an
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f
ic
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t
co
m
m
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s
y
s
te
m
d
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g
n
er
to
cr
ea
te
a
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co
m
m
u
n
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n
s
y
s
t
e
m
.
T
h
is
a
n
al
y
s
is
co
n
s
id
er
s
al
l
r
ec
o
g
n
ized
p
o
w
er
lo
s
s
s
o
u
r
ce
s
in
t
h
e
tr
a
n
s
m
itted
p
o
w
er
.
Haz
e
-
i
n
d
u
ce
d
atte
n
u
a
tio
n
is
co
n
s
id
er
ed
in
t
h
is
i
n
v
esti
g
a
tio
n
’
s
li
n
k
b
u
d
g
e
tin
g
p
r
o
ce
d
u
r
e.
T
h
e
lin
k
m
ar
g
i
n
is
th
e
d
if
f
er
en
ce
b
et
wee
n
th
e
p
o
w
er
r
ec
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ed
an
d
th
e
s
en
s
iti
v
it
y
o
f
th
e
r
ec
eiv
er
.
T
h
e
r
eq
u
ir
e
m
e
n
t
f
o
r
lin
k
av
ai
lab
ilit
y
s
i
g
n
if
ie
s
t
h
at
th
e
li
n
k
w
ill
o
p
er
ate
o
n
l
y
i
f
t
h
e
lin
k
m
ar
g
i
n
d
o
es
n
o
t
ex
ce
ed
a
d
ef
in
ed
r
ec
eiv
er
s
en
s
iti
v
it
y
.
I
n
cr
ea
s
i
n
g
at
m
o
s
p
h
er
ic
atte
n
u
at
io
n
d
u
e
to
r
ed
u
ce
d
v
is
ib
ilit
y
lead
s
to
a
r
ed
u
ctio
n
in
o
p
tical
r
ec
eiv
e
d
p
o
w
er
.
T
h
is
d
ec
r
ea
s
e
in
r
ec
eiv
ed
o
p
tical
p
o
w
er
f
alli
n
g
b
elo
w
th
e
r
ec
eiv
er
s
e
n
s
it
iv
i
t
y
th
r
e
s
h
o
ld
co
u
ld
r
esu
lt
i
n
an
FS
O
l
in
k
o
u
ta
g
e.
T
h
e
lin
k
m
ar
g
i
n
is
d
e
f
i
n
ed
as
(
4
)
:
(
)
=
+
|
|
−
−
−
(
4
)
w
h
er
e
is
t
h
e
tr
an
s
m
itted
p
o
w
e
r
in
d
B
m
,
|
|
is
th
e
ab
s
o
l
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te
v
alu
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r
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eiv
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it
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n
d
B
m
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co
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p
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s
es,
is
th
e
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m
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tr
ic
lo
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d
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h
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ic
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v
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(
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2
5
]
:
=
20
(
)
(
5
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w
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O
li
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k
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D
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t,
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m
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A
d
m
in
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tr
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(
NOAA
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[
2
6
]
,
NOAA
ag
e
n
c
y
p
l
ay
s
a
v
ital
r
o
le
in
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o
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at
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cc
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ased
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k
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RE
SU
L
T
S AN
D
D
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a
p
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m
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a
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p
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b
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(
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C
alcu
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Evaluation Warning : The document was created with Spire.PDF for Python.
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6
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d
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Evaluation Warning : The document was created with Spire.PDF for Python.
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.
Evaluation Warning : The document was created with Spire.PDF for Python.