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Octo
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.
T
h
is
m
ed
ian
SI
h
a
s
g
i
v
en
a
n
i
n
s
ig
h
t
th
at
th
i
s
v
al
u
e
w
ill
n
o
t
w
o
r
k
w
it
h
th
e
e
x
is
tin
g
NO
C
T
p
r
o
ce
d
u
r
e.
Ho
w
e
v
er
,
it is
v
er
y
i
m
p
o
r
tan
t to
f
o
llo
w
as c
l
o
s
e
as p
o
s
s
ib
le
w
it
h
th
e
e
x
i
s
tin
g
NO
C
T
p
r
o
ce
d
u
r
e
f
o
r
f
u
r
t
h
er
co
m
p
ar
i
s
o
n
in
t
h
e
f
u
t
u
r
e.
D
u
e
to
t
h
i
s
ar
g
u
m
e
n
t,
a
s
t
u
d
y
w
ill
b
e
co
n
d
u
cted
in
estab
li
s
h
i
n
g
an
SR
E
f
o
r
NOCT
test
in
g
w
it
h
d
ed
icate
d
ap
p
r
o
ac
h
f
o
r
tr
o
p
ical
r
eg
io
n
.
I
n
o
r
d
er
t
o
ach
iev
e
t
h
i
s
,
m
ed
ia
n
v
al
u
es o
f
a
m
b
ien
t p
ar
a
m
eter
s
o
f
S
R
E
will b
e
d
eter
m
i
n
ed
an
d
ev
al
u
ate
d
.
2
.
RE
SE
ARCH
M
E
T
H
O
D
T
h
e
m
et
h
o
d
o
lo
g
y
ap
p
lied
i
n
th
i
s
s
tu
d
y
w
a
s
ai
m
i
n
g
to
e
s
tab
lis
h
an
S
R
E
f
o
r
NOCT
t
esti
n
g
th
at
r
ep
r
esen
t
tr
o
p
ical
Ma
la
y
s
ia
co
n
d
itio
n
b
y
f
o
llo
w
i
n
g
a
s
clo
s
e
as
p
o
s
s
ib
le
to
th
e
p
r
esen
t
i
n
te
r
n
atio
n
al
s
tan
d
ar
d
s
p
r
o
ce
d
u
r
es
an
d
m
ec
h
a
n
is
m
[
3
]
,
[
4
]
.
I
n
o
r
d
e
r
to
d
o
th
is
,
t
h
e
m
et
h
o
d
o
lo
g
y
h
as
to
b
e
o
f
tr
o
p
ical
ap
p
r
o
ac
h
co
n
s
is
tin
g
f
ield
test
i
n
g
,
s
u
f
f
ici
en
t d
ata
co
llectio
n
an
d
a
n
al
y
ti
ca
l
m
et
h
o
d
.
T
h
e
f
ield
test
in
g
co
n
d
u
cted
is
r
ef
er
r
in
g
to
th
e
o
u
td
o
o
r
m
o
d
u
le
test
i
n
g
o
f
NOCT
th
at
co
m
p
lies
w
i
th
th
e
r
eq
u
ir
e
m
e
n
t
o
f
i
n
ter
n
atio
n
al
s
ta
n
d
ar
d
s
in
th
e
asp
ec
ts
o
f
ex
p
er
i
m
e
n
tal
s
et
u
p
,
d
ata
lo
g
g
i
n
g
an
d
s
en
s
o
r
s
ac
cu
r
ac
y
as
r
ep
o
r
ted
in
th
e
p
r
eli
m
i
n
ar
y
s
tu
d
y
[
7
]
.
T
h
er
e
is
n
o
ch
an
g
es
m
ad
e
in
ter
m
s
o
f
t
h
ese
th
r
ee
asp
ec
ts
a
s
co
m
p
ar
ed
to
t
h
e
p
r
eli
m
in
ar
y
s
t
u
d
y
r
ep
o
r
ted
ea
r
lier
ex
ce
p
t
th
at
th
e
d
ata
co
llectio
n
h
a
s
b
ee
n
ex
ten
d
ed
f
o
r
an
o
th
er
s
i
x
m
o
n
t
h
s
[
7
]
.
I
n
o
t
h
er
w
o
r
d
s
,
t
h
e
a
m
o
u
n
t
o
f
d
ata
h
as
in
cr
ea
s
ed
b
y
5
0
%
a
n
d
th
e
d
ata
w
ill
r
ep
r
esen
t
a
cli
m
ate
p
r
o
f
ile
f
o
r
ea
ch
m
o
n
th
i
n
a
y
ea
r
.
T
h
e
ad
d
itio
n
o
f
an
o
th
er
s
i
x
m
o
n
th
s
d
ata
o
f
f
i
v
e
m
i
n
u
tes
lo
g
g
i
n
g
in
ter
v
a
l
w
ill
f
o
r
m
a
co
m
p
lete
o
n
e
-
y
ea
r
c
y
cle
o
f
d
ata
co
llec
tio
n
r
ep
r
esen
ted
b
y
1
2
m
o
n
th
s
o
f
Feb
r
u
ar
y
2
0
1
7
u
n
t
il J
an
u
ar
y
2
0
1
8
.
T
h
e
ex
p
er
i
m
en
tal
s
e
tu
p
f
o
r
N
OC
T
test
in
g
o
f
m
o
n
o
cr
y
s
talli
n
e,
p
o
l
y
cr
y
s
talli
n
e
a
n
d
C
I
S
th
in
f
il
m
P
V
m
o
d
u
les
;
w
as
b
u
ilt
a
n
d
o
p
er
ated
u
n
d
er
E
n
er
g
y
a
n
d
E
n
v
ir
o
n
m
e
n
t
Fie
ld
L
ab
(
E
E
F
L
)
,
Un
iv
er
s
iti
T
ek
n
o
lo
g
i
MA
R
A
(
UiT
M)
,
Sh
a
h
A
l
a
m
(
L
at:
3
.
0
7
o
N,
L
o
n
g
:
1
0
1
.
4
9
o
E
)
.
T
h
e
NOCT
test
in
g
s
et
u
p
a
s
s
h
o
w
n
i
n
Fig
u
r
e
1
w
a
s
co
n
d
u
cted
in
tr
o
p
ical
Ma
la
y
s
ia.
T
h
e
ch
o
s
e
n
tilt
a
n
g
le
w
as
5
°,
w
h
ic
h
is
a
n
o
p
ti
m
u
m
t
ilt
an
g
le
f
o
r
o
p
tim
u
m
ab
s
o
r
p
tio
n
o
f
s
o
lar
ir
r
ad
ian
ce
an
d
n
a
tu
r
al
c
lea
n
in
g
b
y
r
ai
n
w
ater
a
s
o
b
s
er
v
ed
th
r
o
u
g
h
o
u
t
t
h
e
s
tu
d
y
[
1
1
]
.
B
esid
e
f
ield
te
s
ti
n
g
,
th
e
a
n
al
y
tical
m
et
h
o
d
ap
p
lied
w
er
e
d
iv
id
ed
in
to
f
o
u
r
co
n
s
ec
u
ti
v
e
s
eg
m
e
n
ts
:
Seg
m
en
t
1
w
a
s
o
n
e
-
y
ea
r
s
t
atis
tical
an
al
y
s
is
o
f
SI,
A
T
,
R
H,
W
S,
w
i
n
d
d
ir
ec
tio
n
(
W
D)
,
an
d
m
o
d
u
le
te
m
p
er
atu
r
e
(
MT
)
o
f
th
r
ee
P
V
ce
ll
tech
n
o
lo
g
ie
s
(
MT
_
Mo
n
o
,
MT
_
P
o
ly
a
n
d
MT
_
T
F);.
T
h
is
s
eg
m
e
n
t
ai
m
i
n
g
to
g
iv
e
o
v
er
all
y
ea
r
l
y
p
ict
u
r
e
o
f
th
e
r
ea
l
cli
m
ate
o
f
tr
o
p
ical
Ma
la
y
s
ia
w
it
h
t
h
e
co
r
r
esp
o
n
d
in
g
MT
at
o
p
en
cir
cu
it
co
n
d
itio
n
a
n
d
d
eter
m
i
n
e
t
h
e
p
r
eli
m
i
n
ar
y
y
ea
r
l
y
m
e
d
ian
v
al
u
e
s
o
f
ea
c
h
p
ar
a
m
ete
r
s
b
ased
o
n
t
h
e
d
ata
co
llectio
n
.
Se
g
m
e
n
t
2
w
as
m
o
n
th
l
y
s
tati
s
tical
a
n
al
y
s
i
s
o
f
S
I
an
d
A
T
,
w
h
ich
ar
e
th
e
t
w
o
d
esig
n
ated
a
m
b
ie
n
t
p
ar
am
eter
s
r
ated
in
S
R
E
b
esid
es
W
S.
I
t
w
a
s
d
o
n
e
to
m
a
g
n
if
y
ea
c
h
m
o
n
t
h
b
eh
a
v
io
u
r
in
ter
m
s
o
f
v
al
u
es
o
f
SI
an
d
A
T
an
d
f
u
r
t
h
er
co
n
f
ir
m
w
h
et
h
er
t
h
ese
p
ar
a
m
e
ter
s
b
eh
av
e
co
n
s
is
te
n
tl
y
w
it
h
t
h
e
y
ea
r
l
y
m
ed
ian
v
a
lu
e
s
o
f
SI
an
d
A
T
o
b
s
er
v
ed
in
Se
g
m
e
n
t
1
.
Nev
er
t
h
eles
s
,
R
H
i
s
an
o
t
h
er
a
m
b
ie
n
t
p
ar
a
m
eter
w
h
ich
th
e
b
eh
a
v
io
u
r
n
ee
d
to
b
e
lo
o
k
ed
in
to
in
th
e
co
n
te
x
t
o
f
tr
o
p
ical
Ma
la
y
s
ia.
T
h
is
i
s
b
ec
au
s
e
m
o
n
t
h
l
y
R
H
i
s
an
o
t
h
er
co
r
r
esp
o
n
d
in
g
p
ar
am
eter
t
h
at
n
ee
d
to
b
e
ev
a
l
u
ated
in
th
is
s
eg
m
e
n
t
d
u
e
to
t
h
e
h
y
p
o
th
e
s
is
th
a
t
it
w
i
ll
h
av
e
a
r
elatio
n
s
h
ip
w
it
h
th
e
m
o
n
t
h
l
y
tr
e
n
d
o
f
SI.
Se
g
m
en
t
3
w
ill
s
h
o
w
t
h
e
SI
a
n
d
A
T
m
o
n
t
h
l
y
tr
e
n
d
an
al
y
s
is
i
n
b
ar
ch
ar
t
f
o
r
m
.
T
h
ese
w
il
l
allo
w
to
ev
a
lu
ate
w
h
eth
e
r
th
e
m
ed
ia
n
A
T
an
d
SI
ar
e
s
u
i
tab
le
to
b
e
u
s
ed
as
SR
E
f
o
r
NOCT
test
i
n
g
.
T
h
e
f
i
n
al
s
eg
m
e
n
t
w
as
p
lo
tti
n
g
g
r
ap
h
s
o
f
te
m
p
er
atu
r
e
d
if
f
er
e
n
ce
b
et
w
ee
n
MT
an
d
A
T
as
a
f
u
n
ctio
n
o
f
SI.
A
r
eg
r
ess
io
n
eq
u
atio
n
f
r
o
m
th
i
s
g
r
ap
h
w
i
ll
b
e
u
s
ed
to
later
f
in
alis
ed
t
h
e
SI
an
d
A
T
o
f
th
e
SR
E
th
at
w
i
ll
s
u
it
tr
o
p
ical
Ma
la
y
s
ia.
T
h
e
p
er
ce
n
tag
e
er
r
o
r
w
as
also
ca
lc
u
lated
as
p
er
f
o
r
m
a
n
ce
in
d
ice
s
o
f
t
h
e
ch
o
s
en
p
ar
a
m
eter
f
o
r
th
e
p
r
o
p
o
s
ed
SR
E
.
Evaluation Warning : The document was created with Spire.PDF for Python.
I
n
d
o
n
esia
n
J
E
lec
E
n
g
&
C
o
m
p
Sci
I
SS
N:
2502
-
4752
E
s
ta
b
lis
h
men
t o
f S
ta
n
d
a
r
d
R
ef
eren
ce
E
n
viro
n
men
t fo
r
P
h
o
t
o
vo
lta
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N
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(
M.M.M.
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a
n
ifa
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)
435
Fig
u
r
e
1
.
E
x
p
er
i
m
en
tal
s
ite
v
i
e
w
a
n
d
NOCT
T
esti
n
g
Set
u
p
Diag
r
a
m
3
.
RE
SUL
T
S
A
ND
DI
SC
USSI
O
N
3
.
1
.
O
ne
-
y
ea
r
s
t
a
t
is
t
ica
l a
na
ly
s
is
o
f
SI
,
AT
,
RH
,
WS,
WD
,
M
T
_
M
o
no
,
M
T
_
P
o
ly
a
nd
M
T
_
T
F
Statis
t
ical
an
a
l
y
s
is
w
a
s
co
n
d
u
cted
o
n
1
2
m
o
n
t
h
s
d
ata
co
n
s
is
tin
g
o
f
ap
p
r
o
x
i
m
atel
y
4
8
0
0
0
s
et
o
f
d
ata.
T
h
is
an
al
y
s
is
w
a
s
co
n
d
u
cted
to
co
m
e
o
u
t
w
i
th
a
y
ea
r
p
atter
n
o
f
t
h
e
cli
m
ate
p
r
o
f
ile
i
n
e
x
ten
s
io
n
to
t
h
e
p
r
eli
m
in
ar
y
w
o
r
k
co
n
d
u
c
ted
f
o
r
s
ix
m
o
n
th
s
o
f
t
h
e
s
a
m
e
p
r
o
j
ec
t
r
ep
o
r
ted
ea
r
lier
[
7
]
.
T
h
e
s
tatis
t
ical
a
n
al
y
s
i
s
tab
u
lated
in
T
ab
le
1
c
o
m
p
r
is
e
s
o
f
eig
h
t
p
ar
a
m
eter
s
n
a
m
el
y
SI,
A
T
,
R
H,
W
S,
W
D,
M
T
_
Mo
n
o
,
MT
_
Po
ly
a
n
d
MT
_
T
F.
T
h
e
s
tatis
t
ical
i
n
d
ice
s
en
co
m
p
ass
m
ea
n
,
s
ta
n
d
ar
d
er
r
o
r
o
f
m
ea
n
,
m
ed
ia
n
,
m
o
d
e,
s
tan
d
ar
d
d
ev
iatio
n
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s
k
e
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s
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s
ta
n
d
ar
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er
r
o
r
o
f
s
k
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r
an
g
e,
m
i
n
i
m
u
m
a
n
d
m
a
x
i
m
u
m
.
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v
al
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ati
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g
th
e
s
e
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ar
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ill
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cid
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at
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r
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f
t
h
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t
w
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NO
C
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test
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p
r
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r
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ill
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h
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h
e
m
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al
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r
t
y
p
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eteo
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g
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p
ar
am
eter
s
o
f
SI,
A
T
,
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H
an
d
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S
in
th
is
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tu
d
y
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er
e
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/
m
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3
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0
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d
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9
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p
ar
t
f
r
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th
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h
e
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D
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as 1
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a
s
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et
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t a
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d
s
o
u
th
d
ir
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tio
n
.
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h
e
m
ea
n
P
V
m
o
d
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le
te
m
p
er
at
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r
e
r
ec
o
r
d
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d
f
o
r
t
h
e
th
r
ee
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ell
tech
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9
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7
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4
0
.
2
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an
d
4
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1
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r
e
s
p
ec
tiv
el
y
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T
h
ese
r
esu
lts
g
i
v
e
a
s
i
g
n
if
ica
n
t
in
d
icat
io
n
to
r
ev
i
s
e
t
h
e
S
R
E
u
s
ed
i
n
NOCT
test
in
g
p
r
o
ce
d
u
r
es
f
o
r
tr
o
p
ical
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eg
io
n
,
w
h
ic
h
p
r
o
v
en
to
h
a
v
e
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er
SI
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d
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ig
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er
A
T
w
ith
co
r
r
esp
o
n
d
in
g
h
i
g
h
er
R
H
[
7
]
,
[
9
]
.
H
o
w
ev
er
,
f
u
r
th
er
r
ev
i
s
io
n
m
ad
e
in
t
h
is
s
tu
d
y
w
i
ll
b
e
s
teer
ed
to
b
e
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cl
o
s
e
as p
o
s
s
ib
le
to
th
e
p
r
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t p
r
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ce
d
u
r
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s
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e
n
tio
n
ed
in
i
n
ter
n
a
tio
n
al
s
ta
n
d
ar
d
[
3
]
.
T
ab
le
1
.
On
e
y
ea
r
s
ta
tis
tica
l a
n
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s
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s
f
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r
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T
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o
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ly
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T
F
SI
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RH
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M
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r
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8
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i
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m
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m
2
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4
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1
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2
.
M
o
nthly
Sta
t
is
t
ica
l A
na
ly
s
is
o
f
SI
,
AT
a
nd
RH
T
h
er
e
ar
e
th
r
ee
a
m
b
ien
t
p
ar
am
eter
s
in
v
o
l
v
e
f
r
o
m
to
tal
f
i
v
e
p
ar
a
m
eter
s
as
ad
d
r
ess
ed
in
i
n
ter
n
atio
n
al
s
tan
d
ar
d
s
.
T
h
e
th
r
ee
a
m
b
ie
n
t
p
ar
am
eter
s
ar
e
SI,
A
T
an
d
W
S.
B
ased
o
n
th
e
d
ef
i
n
itio
n
o
f
SR
E
,
th
e
SI,
A
T
an
d
W
S
to
b
e
ch
o
s
e
n
as
S
R
E
in
NOCT
test
i
n
g
ar
e
th
e
m
ed
ia
n
v
al
u
es
[
8
]
.
T
h
e
s
tati
s
tical
a
n
a
l
y
s
i
s
a
s
p
r
esen
ted
i
n
T
ab
le
1
s
h
o
w
ed
t
h
at
t
h
e
m
ed
ian
f
o
r
SI
w
a
s
(
2
2
8
±
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0
)
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/
m
2
,
t
h
e
m
ed
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n
f
o
r
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a
s
(
3
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.
3
9
±
0
.
2
1
)
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d
th
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m
ed
ian
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r
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as
(
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8
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±
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1
1
)
m
/
s
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h
e
W
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m
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r
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w
e
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e
m
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n
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o
f
2
2
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2
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d
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T
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f
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h
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t
d
if
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er
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t
th
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f
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h
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co
r
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s
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,
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r
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.
Evaluation Warning : The document was created with Spire.PDF for Python.
I
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4752
I
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n
J
E
lec
E
n
g
&
C
o
m
p
Sci,
Vo
l
.
1
2
,
No
.
1
,
Octo
b
er
201
8
:
4
3
3
–
440
436
Sin
ce
t
h
e
r
esu
lt
s
o
f
a
y
ea
r
an
al
y
s
i
s
is
an
ex
te
n
s
io
n
o
f
th
e
p
r
ev
io
u
s
w
o
r
k
o
f
s
ix
m
o
n
t
h
s
an
al
y
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s
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co
m
p
ar
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n
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s
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n
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ch
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n
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t
h
e
m
ed
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n
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ar
tic
u
lar
l
y
th
e
t
h
r
ee
a
m
b
ien
t
p
ar
am
eter
o
f
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A
T
an
d
W
S.
Fro
m
th
e
p
r
ev
io
u
s
s
ix
m
o
n
t
h
s
an
al
y
s
i
s
,
th
e
m
ed
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n
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9
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ea
n
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le
t
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e
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A
T
w
a
s
(
3
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±
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2
1
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[
7
]
.
T
h
e
d
i
f
f
er
en
ce
s
o
cc
u
r
r
ed
d
u
e
to
t
h
e
ad
d
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n
o
f
a
n
o
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e
r
s
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m
o
n
th
s
d
ata
co
n
s
is
tin
g
f
r
o
m
Au
g
u
s
t
2
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7
to
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an
2
0
1
8
in
t
h
e
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n
e
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r
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al
y
s
is
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t
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s
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k
n
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n
P
en
in
s
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lar
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f
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ased
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th
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en
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m
e
n
t
w
a
s
5
%.
T
ab
le
2
.
Mo
n
th
l
y
s
ta
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s
o
f
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T
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d
R
H
M
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t
h
P
a
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M
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n
M
a
x
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SD
Jan
SI
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8
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3
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5
5
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2
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0
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8
2
2
2
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6
1
3
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2
8
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7
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6
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6
2
1
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9
9
0
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0
3
8
3
.
0
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6
0
4
RH
7
9
.
6
7
9
.
6
6
5
1
0
0
4
9
.
4
0
.
0
3
8
1
3
.
1
6
2
7
F
e
b
SI
2
6
1
3
3
5
1
2
2
6
2
0
.
0
4
3
2
8
2
.
4
5
4
AT
3
0
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8
3
0
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1
8
3
5
.
9
2
3
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5
9
0
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0
4
3
2
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5
8
7
7
7
RH
6
6
.
6
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3
.
M
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T
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Fig
u
r
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2
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o
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S
I
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ed
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1
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Evaluation Warning : The document was created with Spire.PDF for Python.
I
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4752
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s
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437
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ate
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NOCT
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[
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8
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[
1
3
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.
I
t
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k
n
o
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th
a
t
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at
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is
8
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/m
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ated
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T
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as
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tated
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ter
n
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ta
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m
[
3
]
.
T
h
u
s
,
m
a
k
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g
t
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m
e
d
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m
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o
v
e
m
a
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t b
e
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as S
R
E
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g
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tco
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h
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ed
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d
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o
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ical
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r
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ate
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h
is
ap
p
r
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llo
w
s
th
e
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ated
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o
f
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/m
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,
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S
o
f
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m
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u
t
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r
o
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o
s
ed
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ew
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T
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atin
g
f
o
r
SR
E
to
s
u
it tr
o
p
ical
r
eg
io
n
.
Fig
u
r
e
2
.
Mo
n
th
l
y
SI
tr
en
d
Fig
u
r
e
3
.
Mo
n
th
l
y
A
T
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en
d
3.
4
.
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a
T
a
s
f
un
ct
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n o
f
S
I
T
h
e
n
e
w
A
T
r
atin
g
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a
s
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eter
m
i
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y
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lo
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g
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r
ap
h
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o
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t
e
m
p
er
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d
i
f
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n
ce
(
d
elta
T
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b
etw
ee
n
MT
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d
A
T
,
as
a
f
u
n
ct
io
n
o
f
SI.
Sin
ce
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h
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t
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,
th
r
ee
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i
m
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lar
g
r
ap
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w
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e
p
lo
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as
s
h
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n
in
Fi
g
u
r
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4
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Fig
u
r
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5
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d
Fig
u
r
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6
r
esp
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.
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ac
h
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g
r
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Eq
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3
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,
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r
esp
o
n
d
in
g
A
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at
SI
o
f
8
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W
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ter
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m
in
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th
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v
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s
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tech
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o
lo
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ies ar
e
s
h
o
w
n
:
(
)
(
)
Evaluation Warning : The document was created with Spire.PDF for Python.
I
SS
N
:
2
5
0
2
-
4752
I
n
d
o
n
esia
n
J
E
lec
E
n
g
&
C
o
m
p
Sci,
Vo
l
.
1
2
,
No
.
1
,
Octo
b
er
201
8
:
4
3
3
–
440
438
(
)
C
alcu
latio
n
i
n
d
eter
m
i
n
i
n
g
AT
at
SI
o
f
8
0
0
W
/m
2
:
M
o
no
cr
y
s
t
a
llin
e
P
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ly
cr
y
s
t
a
llin
e
T
hin
F
il
m
(
CIS
)
(
)
W
h
er
e;
MT
-
AT
SI
⁄
A
T
=
MT
–
,
(
at
⁄
,
MT
=
5
4
.
3
3
1
2
7
)
A
T
=
3
1
.
0
8
°C
(
)
W
h
er
e;
MT
-
AT
SI
⁄
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T
=
MT
–
,
(
at
⁄
,
MT
=
5
5
.
7
3
0
7
3
)
A
T
=
3
1
.
1
5
°C
(
)
W
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e
;
MT
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T
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(
at
⁄
,
MT
=
5
9
.
6
1
7
0
9
)
A
T
=
3
0
.
9
2
°C
Fro
m
t
h
e
ab
o
v
e
ca
lc
u
latio
n
s
,
th
e
A
T
f
o
r
m
o
n
o
cr
y
s
talli
n
e,
p
o
ly
cr
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tal
lin
e
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d
C
I
S
t
h
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n
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il
m
w
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e
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1
.
0
8
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3
1
.
1
5
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d
3
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9
2
°
C
r
esp
ec
tiv
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y
.
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h
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r
ee
v
a
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ar
e
o
b
v
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l
y
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n
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is
te
n
t
w
it
h
i
n
3
1
°C
.
T
h
u
s
,
th
e
p
r
o
p
o
s
ed
A
T
f
o
r
S
R
E
i
n
NOCT
test
i
n
g
at
t
h
i
s
s
tag
e
o
f
an
al
y
s
i
s
i
s
3
1
°C
in
r
elatio
n
t
o
8
0
0
W
/m
2
o
f
SI.
T
h
ese
v
alu
e
s
o
f
A
T
an
d
SI
ar
e
s
ig
n
i
f
ican
tl
y
d
i
f
f
er
en
t
f
r
o
m
t
h
e
ea
r
lier
f
i
n
d
in
g
o
f
t
h
is
s
tu
d
y
in
s
ec
tio
n
3
.
2
th
at
ad
d
r
ess
ed
th
e
m
ed
ian
v
al
u
es o
f
A
T
o
f
3
0
°C
co
r
r
esp
o
n
d
in
g
to
SI
o
f
2
2
8
W
/m
2
.
Ho
w
e
v
er
,
ele
m
e
n
t
o
f
co
m
p
ar
i
s
o
n
is
es
s
en
tial
to
v
er
i
f
y
t
h
e
ac
cu
r
ac
y
o
f
t
h
e
ch
o
s
e
n
A
T
an
d
SI
th
at
w
il
l
b
e
u
s
ed
in
t
h
e
NO
C
T
d
eter
m
i
n
atio
n
i
n
tr
o
p
ical
cli
m
ate.
T
h
e
co
m
p
ar
is
o
n
w
ill
b
e
m
ad
e
b
et
w
ee
n
th
e
f
i
n
d
in
g
in
s
ec
tio
n
3
.
2
d
esig
n
ated
as
„
R
ev
i
s
ed
1
`
(
A
T
=
3
0
°
C
an
d
SI=
2
2
8
W
/m
2
)
an
d
t
h
e
o
u
tco
m
e
o
f
th
is
r
ec
en
t
f
i
n
d
in
g
d
esi
g
n
ated
as
„
R
ev
i
s
ed
2
`
(
A
T
=
3
1
°C
an
d
SI=
8
0
0
W
/m
2
)
.
I
n
o
r
d
er
to
d
o
th
is
,
th
e
N
OC
T
o
f
ea
ch
f
i
n
d
in
g
a
n
d
t
h
e
p
er
ce
n
t
ag
e
er
r
o
r
(
as
co
m
p
ar
ed
to
t
h
e
ac
tu
al
m
ea
s
u
r
ed
d
ata)
w
ill
b
e
d
eter
m
i
n
ed
i
n
d
er
iv
in
g
to
an
ac
cu
r
ate
NO
C
T
in
tr
o
p
ical
r
eg
io
n
.
T
h
e
NOCT
v
al
u
es
w
er
e
d
ete
r
m
in
ed
b
y
d
ata
f
i
ltra
tio
n
o
f
g
r
ea
ter
t
h
an
4
0
0
W
/
m
2
a
s
ali
g
n
ed
w
it
h
NOCT
te
s
ti
n
g
P
r
o
ce
d
u
r
e
1
0
.
5
.
3
in
i
n
ter
n
at
io
n
al
s
ta
n
d
ar
d
[
3
]
.
T
h
is
is
a
ls
o
to
a
v
o
id
er
r
o
r
s
d
u
e
to
P
V
m
o
d
u
le
‟
s
th
er
m
a
l
m
ass
t
h
at
m
i
g
h
t
b
e
at
tr
ib
u
ted
b
y
clo
u
d
s
i
n
ter
m
itte
n
t
an
d
o
th
er
a
m
b
ie
n
t
f
l
u
ctu
a
tio
n
f
ac
to
r
s
[
6
]
.
B
ased
o
n
T
ab
le
3
,
4
an
d
5
,
th
e
N
OC
T
v
alu
es
f
o
r
„
R
e
v
is
ed
1
`
o
f
m
o
n
o
cr
y
s
talli
n
e,
p
o
l
y
cr
y
s
tall
in
e
an
d
th
i
n
f
il
m
w
er
e
4
1
.
9
°C
,
4
2
.
1
°C
an
d
4
4
.
4
°C
r
esp
ec
tiv
el
y
.
Me
a
n
w
h
ile,
th
e
NOCT
v
al
u
es
f
o
r
„
R
ev
is
ed
2
`
o
f
m
o
n
o
cr
y
s
tall
in
e,
p
o
ly
cr
y
s
tall
in
e
a
n
d
th
in
f
il
m
w
er
e
5
3
.
°C
,
5
4
.
°C
a
n
d
5
8
.
°C
co
r
r
esp
o
n
d
in
g
l
y
.
I
n
s
u
m
m
a
r
y
,
t
h
e
NO
C
T
v
alu
e
s
f
o
r
all
t
h
e
t
h
r
ee
tech
n
o
lo
g
ie
s
ar
e
s
ig
n
i
f
ica
n
tl
y
h
ig
h
er
u
s
i
n
g
„
R
e
v
i
s
ed
2
`
ap
p
r
o
ac
h
as
co
m
p
ar
ed
to
„
R
e
v
is
ed
1
`
ap
p
r
o
ac
h
.
Su
b
s
eq
u
en
tl
y
,
th
e
p
er
ce
n
tag
e
er
r
o
r
im
p
r
o
v
ed
b
y
2
1
%
to
2
3
%
f
o
r
th
e
th
r
ee
P
V
m
o
d
u
le
tech
n
o
lo
g
ies
w
h
en
„
R
e
v
is
ed
2
`
ap
p
r
o
ac
h
w
as
i
m
p
le
m
e
n
t
ed
.
T
h
u
s
,
t
h
e
„
R
ev
i
s
ed
2
`
S
R
E
h
as
m
u
c
h
lo
w
er
p
er
ce
n
tag
e
er
r
o
r
as c
o
m
p
ar
ed
to
„
R
e
v
is
ed
1
`
SR
E
.
Fig
u
r
e
4
.
Delta
T
v
s
SI
f
o
r
Mo
n
o
cr
y
s
tal
lin
e
T
h
e
s
u
m
m
ar
y
o
f
th
e
p
ar
a
m
e
te
r
s
f
o
r
th
e
p
r
ese
n
t
S
R
E
as
co
m
p
ar
ed
to
p
r
o
p
o
s
ed
SR
E
(
f
r
o
m
t
h
is
s
t
u
d
y
)
is
s
h
o
w
n
i
n
T
ab
le
6
.
Fro
m
t
h
e
f
i
v
e
p
ar
a
m
e
ter
s
,
o
n
l
y
t
w
o
p
ar
a
m
eter
s
w
er
e
ch
a
n
g
ed
th
a
t
ar
e
tilt
a
n
g
le
a
n
d
A
T
.
T
h
e
tilt
an
g
le
f
o
llo
w
s
lo
ca
l la
t
itu
d
e
o
f
t
h
e
ch
o
s
e
n
s
ite
a
n
d
AT
o
f
3
1
°C
as d
eter
m
in
ed
i
n
th
is
s
t
u
d
y
[
1
1
]
.
Evaluation Warning : The document was created with Spire.PDF for Python.
I
n
d
o
n
esia
n
J
E
lec
E
n
g
&
C
o
m
p
Sci
I
SS
N:
2502
-
4752
E
s
ta
b
lis
h
men
t o
f S
ta
n
d
a
r
d
R
ef
eren
ce
E
n
viro
n
men
t fo
r
P
h
o
t
o
vo
lta
ic
N
o
min
a
l…
(
M.M.M.
H
a
n
ifa
h
)
439
Fig
u
r
e
5
.
Delta
T
v
s
SI
f
o
r
P
o
l
y
cr
y
s
talli
n
e
Fig
u
r
e
6
.
Delta
T
v
s
SI
f
o
r
T
h
i
n
f
i
l
m
T
ab
le
3
.
SI
SR
E
P
o
in
t
T
est Su
m
m
ar
y
(
ab
o
v
e
4
0
0
W
/m
2
r
an
g
e)
Fo
r
Mo
n
o
P
a
ra
m
e
ter
NO
CT
v
a
lu
e
(°
C)
P
e
rc
e
n
tag
e
e
rro
r
(%
)
2
2
8
W
/m
2
S
I,
3
0
°
C
AT
(Re
v
i
se
d
1
)
4
1
.
8
9
9
2
9
.
6
5
8
0
0
W
/m
2
S
I,
3
2
°
C
AT
(Re
v
i
se
d
2
)
5
3
.
3
4
5
8.
92
T
ab
le
4
.
SI
SR
E
P
o
in
t
T
est Su
m
m
ar
y
(
ab
o
v
e
4
0
0
W
/m
2
r
an
g
e)
Fo
r
Po
ly
P
a
ra
m
e
ter
NO
CT
v
a
lu
e
(°
C)
P
e
rc
e
n
tag
e
e
rro
r
(%
)
2
2
8
W
/m
2
S
I,
3
0
°
C
AT
(Re
v
i
se
d
1
)
4
2
.
1
3
5
2
8
.
3
2
8
0
0
W
/m
2
S
I,
3
2
°
C
AT
(Re
v
i
se
d
2
)
5
4
.
6
4
8
8
.
6
6
T
ab
le
5
.
SI
SR
E
P
o
in
t
T
est Su
m
m
ar
y
(
ab
o
v
e
4
0
0
W
/m
2
r
an
g
e)
Fo
r
T
h
in
Fil
m
P
a
ra
m
e
ter
NO
CT
v
a
lu
e
(°
C)
P
e
rc
e
n
tag
e
e
rro
r
(%
)
2
2
8
W
/m
2
S
I,
3
0
°
C
AT
(Re
v
i
se
d
1
)
4
4
.
4
1
2
3
2
.
2
0
8
0
0
W
/m
2
S
I,
3
2
°
C
AT
(Re
v
i
se
d
2
)
5
8
.
3
1
6
9
.
0
3
T
ab
le
6
.
C
o
m
p
ar
is
o
n
o
f
P
r
esen
t S
R
E
an
d
P
r
o
p
o
s
ed
SR
E
P
a
ra
m
e
ter
P
re
se
n
t
S
RE
P
r
o
p
o
se
d
S
R
E
Re
m
a
rk
T
il
t
A
n
g
le
45°
L
o
c
a
l
latit
u
d
e
Ch
a
n
g
e
d
SI
8
0
0
W
/m
2
8
0
0
W
/m
2
Re
m
a
in
u
n
c
h
a
n
g
e
d
AT
2
0
°
C
3
1
°
C
Ch
a
n
g
e
d
WS
1
m
/s
1
m
/s
Re
m
a
in
u
n
c
h
a
n
g
e
d
El
e
c
tri
c
a
l
L
o
a
d
Nil
(Op
e
n
c
ircu
i
t)
Nil
(Op
e
n
c
ircu
i
t)
Re
m
a
in
u
n
c
h
a
n
g
e
d
4
.
Co
nclus
io
n
I
n
estab
li
s
h
i
n
g
t
h
e
S
R
E
a
m
b
ien
t
p
ar
a
m
e
ter
s
f
o
r
r
ep
r
esen
t
in
g
tr
o
p
ical
cli
m
ate
r
eg
io
n
,
a
o
n
e
-
y
ea
r
s
tatis
t
ical
an
a
l
y
s
is
a
n
d
d
etails
m
o
n
t
h
l
y
s
ta
tis
tica
l a
n
al
y
s
is
o
f
f
i
v
e
m
in
u
tes d
ata
lo
g
g
in
g
i
n
te
r
v
al
o
f
SI,
A
T
,
R
H,
W
S,
W
D
an
d
MT
w
er
e
d
ete
r
m
in
ed
.
Fro
m
t
h
e
o
u
tco
m
e
o
f
t
h
e
s
tatis
t
ical
a
n
a
l
y
s
is
,
r
eg
r
ess
io
n
an
al
y
s
is
a
n
d
p
er
ce
n
tag
e
er
r
o
r
an
al
y
s
i
s
ex
e
cu
ted
u
s
i
n
g
d
ed
icate
d
ap
p
r
o
a
ch
to
s
u
it
tr
o
p
ical
r
eg
io
n
;
t
h
e
r
ev
is
ed
a
m
b
ien
t
Evaluation Warning : The document was created with Spire.PDF for Python.
I
SS
N
:
2
5
0
2
-
4752
I
n
d
o
n
esia
n
J
E
lec
E
n
g
&
C
o
m
p
Sci,
Vo
l
.
1
2
,
No
.
1
,
Octo
b
er
201
8
:
4
3
3
–
440
440
p
ar
am
eter
o
f
SR
E
w
as
d
eter
m
in
ed
.
T
h
e
r
ev
i
s
ed
a
m
b
ie
n
t
p
ar
a
m
eter
i
s
o
n
l
y
A
T
,
w
h
ic
h
i
s
3
1
°C
co
m
p
ar
ed
to
cu
r
r
en
t
A
T
w
h
ich
i
s
at
2
0
°
C
.
T
h
is
also
m
ea
n
s
t
h
at
t
h
e
r
e
m
ain
i
n
g
t
w
o
a
m
b
ien
t
p
ar
a
m
eter
s
,
w
h
ich
ar
e
SI
a
n
d
W
S
r
e
m
ai
n
t
h
e
s
a
m
e
a
s
s
tated
in
i
n
ter
n
atio
n
al
s
ta
n
d
ar
d
.
T
h
e
r
ef
o
r
e,
th
e
p
r
o
p
o
s
ed
a
m
b
ie
n
t
p
ar
am
eter
s
o
f
S
R
E
f
o
r
tr
o
p
ical
r
eg
io
n
ar
e
SI
o
f
8
0
0
W
/m
2
,
A
T
o
f
3
1
°C
a
n
d
W
S
o
f
1
m
/s
.
T
h
e
n
e
w
p
r
o
p
o
s
ed
A
T
r
atin
g
o
f
SR
E
f
o
r
NOCT
test
in
g
i
s
s
i
g
n
i
f
ica
n
t
to
b
en
ef
it
all
P
V
test
in
g
f
ac
ilit
ies
i
n
tr
o
p
ical
r
eg
io
n
in
d
er
iv
in
g
to
w
ar
d
s
a
m
o
r
e
ac
c
u
r
ate
NOCT
v
al
u
es.
Ac
k
no
w
ledg
e
m
e
nt
T
h
e
au
th
o
r
s
ex
p
r
ess
g
r
ea
tes
t
g
r
atitu
d
e
to
Un
iv
er
s
iti
T
ek
n
o
lo
g
i
MA
R
A
(
UiT
M)
f
o
r
f
u
n
d
in
g
th
i
s
r
esear
ch
u
n
d
er
r
esear
ch
g
r
an
t o
f
6
0
0
-
I
R
MI
/M
y
R
A
5
/3
/B
E
ST
A
R
I
(
0
1
7
/2
0
1
7
)
.
Ref
er
ence
s
[1
]
M
.
Ko
tt
e
k
,
J.
G
ries
e
r,
C.
Be
c
k
,
B.
Ru
d
o
lf
,
a
n
d
F
.
R
u
b
e
l,
“
W
o
rld
m
a
p
o
f
th
e
Kö
p
p
e
n
-
G
e
ig
e
r
c
li
m
a
te
c
las
si
f
ica
ti
o
n
u
p
d
a
te
d
,
”
M
e
teo
ro
l.
Z
e
it
sc
h
rift
,
v
o
l.
1
5
,
n
o
.
3
,
p
p
.
2
5
9
–
2
6
3
,
2
0
0
6
.
[2
]
S
EDA
,
“
S
e
d
a
P
o
rtal,
”
S
EDA
M
a
l
a
y
sia
,
2
0
1
7
.
.
[3
]
IEC6
1
2
1
5
,
Cry
sta
ll
i
n
e
S
il
ico
n
T
e
rr
e
stria
l
Ph
o
t
o
v
o
lt
a
ic
(
PV
)
M
o
d
u
les
–
De
sig
n
Qu
a
li
fi
c
a
ti
o
n
a
n
d
T
y
p
e
Ap
p
ro
v
a
l
(
IEC
6
1
2
1
5
:2
0
0
5
,
IDT)
.
M
a
lay
sia
,
De
p
a
rm
e
n
t
Of
S
tan
d
a
rd
s,
2
0
0
6
.
[4
]
IEC6
1
6
4
6
,
T
h
in
-
fi
lm
T
e
rr
e
stria
l
Ph
o
to
v
o
lt
a
ic
(
PV
)
M
o
d
u
les
D
e
sig
n
-
Qu
a
li
fi
c
a
ti
o
n
a
n
d
T
y
p
e
Ap
p
ro
v
a
l.
(
Fi
rs
t
Rev
isio
n
)(
IEC
6
1
6
4
6
:2
0
0
8
,
IDT)
.
M
a
la
y
sia
,
De
p
a
r
m
e
n
t
O
f
S
tan
d
a
r
d
s,
2
0
1
0
.
[5
]
A
.
M
o
h
a
m
e
d
a
n
d
T
.
Kh
a
ti
b
,
“
Co
rre
latio
n
f
o
r
e
stim
a
ti
n
g
so
lar
c
e
ll
tem
p
e
r
a
tu
re
b
a
se
d
o
n
a
tro
p
ica
l
f
ield
o
p
e
ra
ti
o
n
o
f
a
p
h
o
to
v
o
lt
a
ic sy
ste
m
,
”
2
0
1
4
I
EE
E
PE
S
T
&
D Co
n
f.
Ex
p
o
.
,
p
p
.
1
–
5
,
2
0
1
4
.
[6
]
M
.
Ko
e
h
l,
M
.
He
c
k
,
S
.
W
ies
m
e
ier,
a
n
d
J.
W
irt
h
,
“
M
o
d
e
li
n
g
o
f
t
h
e
n
o
m
in
a
l
o
p
e
ra
ti
n
g
c
e
ll
tem
p
e
ra
tu
re
b
a
se
d
o
n
o
u
t
d
o
o
r
w
e
a
th
e
rin
g
,
”
S
o
l.
En
e
rg
y
M
a
ter
.
S
o
l.
Ce
ll
s
,
v
o
l.
9
5
,
n
o
.
7
,
p
p
.
1
6
3
8
–
1
6
4
6
,
2
0
1
1
.
[7
]
M
.
M
.
M
.
Ha
n
if
a
h
,
Zai
n
u
d
d
i
n
,
a
n
d
M
.
Z.
H
u
ss
in
,
“
Ev
a
lu
a
ti
o
n
o
f
sta
n
d
a
rd
re
f
e
re
n
c
e
e
n
v
iro
n
m
e
n
t
f
o
r
p
h
o
t
o
v
o
lt
a
ic
n
o
m
in
a
l
o
p
e
ra
ti
n
g
c
e
ll
t
e
m
p
e
ra
tu
re
tes
ti
n
g
in
M
a
la
y
sia
,
”
In
d
o
n
e
s.
J
.
El
e
c
tr.
En
g
.
Co
mp
u
t.
S
c
i.
,
v
o
l.
8
,
n
o
.
1
,
p
p
.
245
–
2
5
2
,
2
0
1
7
.
[8
]
J.
W
.
S
tu
lt
z
,
“
T
h
e
rm
a
l
&
Oth
e
r
Te
sts o
f
P
h
o
t
o
v
o
lt
a
ic m
o
d
u
les
p
e
rf
o
rm
e
d
in
n
a
tu
ra
l
su
n
li
g
h
t
.
”
1
9
7
9
.
[9
]
Z.
Ye
,
A
.
No
b
re
,
T
.
R
e
in
d
l,
J.
L
u
th
e
r,
a
n
d
C
.
Re
ise
,
“
On
P
V
m
o
d
u
le
te
m
p
e
ra
tu
re
s
in
tro
p
ica
l
re
g
io
n
s,”
S
o
l.
En
e
rg
y
,
v
o
l.
8
8
,
p
p
.
8
0
–
8
7
,
2
0
1
3
.
[1
0
]
J.
Y.
Ye
,
K.
Di
n
g
,
T
.
Re
in
d
l,
a
n
d
A
.
G
.
A
b
e
rle,
“
Ou
td
o
o
r
P
V
m
o
d
u
le
p
e
rf
o
rm
a
n
c
e
u
n
d
e
r
f
lu
c
t
u
a
ti
n
g
irrad
ia
n
c
e
c
o
n
d
i
ti
o
n
s in
tro
p
ica
l
c
li
m
a
tes
,
”
E
n
e
rg
y
Pro
c
e
d
i
a
,
v
o
l.
3
3
,
p
p
.
2
3
8
–
2
4
7
,
2
0
1
3
.
[1
1
]
M
.
Z.
Ja
c
o
b
so
n
a
n
d
V
.
Ja
d
h
a
v
,
“
W
o
rld
e
sti
m
a
tes
o
f
P
V
o
p
ti
m
a
l
ti
l
t
a
n
g
les
a
n
d
ra
ti
o
s
o
f
su
n
li
g
h
t
in
c
id
e
n
t
u
p
o
n
ti
lt
e
d
a
n
d
trac
k
e
d
P
V
p
a
n
e
ls
re
lativ
e
to
h
o
rizo
n
tal
p
a
n
e
ls,
”
S
o
l.
En
e
rg
y
,
v
o
l.
1
6
9
,
n
o
.
De
c
e
m
b
e
r
2
0
1
7
,
p
p
.
5
5
–
6
6
,
2
0
1
8
.
[1
2
]
IEC6
1
8
5
3
-
1
,
In
ter
n
a
ti
o
n
a
l
S
ta
n
d
a
rd
:
P
h
o
t
o
v
o
lt
a
ic
(
PV
)
mo
d
u
le
p
e
rfo
rm
a
n
c
e
tes
ti
n
g
a
n
d
e
n
e
rg
y
ra
ti
n
g
–
Pa
rt
1
:
Irr
a
d
ia
n
c
e
a
n
d
tem
p
e
ra
tu
re
p
e
rf
o
rm
a
n
c
e
me
a
su
re
me
n
ts
a
n
d
p
o
we
r
ra
ti
n
g
,
n
o
.
A
p
ril
.
2
0
1
1
.
[1
3
]
J
.
W
.
S
tu
lt
z
,
“
T
h
e
rm
a
l
a
n
d
Oth
e
r
T
e
sts o
f
P
h
o
t
o
v
o
lt
a
ic M
o
d
u
les
P
e
rf
o
r
m
e
d
in
Na
tu
ra
l
S
u
n
l
ig
h
t,
”
1
9
7
8
.
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