Co
m
pu
t
er
Science
a
n
d In
f
o
r
m
a
t
io
n T
ec
hn
o
lo
g
ies
Vo
l.
2
,
No
.
2
,
J
u
l
y
202
1
,
p
p
.
6
7
~
7
6
I
SS
N:
2722
-
3221
,
DOI
: 1
0
.
1
1
5
9
1
/
csit
.
v
2
i
2
.p
6
7
-
7
6
67
J
o
ur
na
l ho
m
ep
a
g
e
:
h
ttp
:
//ia
e
s
p
r
ime.
co
m/in
d
ex
.
p
h
p
/csi
t
Rea
lti
m
e
m
o
ni
toring
f
o
r gro
undw
a
ter
lev
el
and lo
ca
l
cli
m
a
te
ba
sed o
n univ
ersa
l co
m
m
u
nica
tion
sy
ste
m
Ro
ny
T
eg
uh
1
,
H
epry
a
nd
i U
s
up
2
1
De
p
a
rtme
n
t
In
f
o
rm
a
ti
c
s E
n
g
in
e
e
rin
g
,
Un
iv
e
rsity
o
f
P
a
lan
g
k
a
Ra
y
a
,
In
d
o
n
e
sia
2
De
p
a
rtme
n
t
o
f
M
in
i
n
g
En
g
in
e
e
ri
n
g
,
Un
iv
e
rsity
o
f
P
a
lan
g
k
a
Ra
y
a
,
In
d
o
n
e
sia
Art
icle
I
nfo
AB
ST
RAC
T
A
r
ticle
his
to
r
y:
R
ec
eiv
ed
S
ep
14
,
2
0
2
0
R
ev
i
s
ed
D
ec
18
,
2
0
2
0
A
cc
ep
ted
F
eb
1
7
,
2
0
2
1
T
h
e
g
ro
u
n
d
w
a
ter
le
v
e
l
a
n
d
w
e
a
th
e
r
p
a
tt
e
rn
s
a
n
d
c
li
m
a
te
c
o
n
d
it
i
o
n
s
a
re
se
v
e
ra
l
o
f
th
e
v
e
r
y
si
g
n
if
ica
n
t
f
a
c
to
rs
w
h
i
c
h
in
f
lu
e
n
c
e
th
e
q
u
a
li
ty
o
f
li
v
e
li
h
o
o
d
a
n
d
t
h
e
o
th
e
r
a
c
ti
v
it
y
o
f
th
e
tro
p
ica
l
p
e
a
tl
a
n
d
e
n
v
iro
n
m
e
n
t.
T
h
e
c
u
rre
n
t
m
e
th
o
d
o
f
g
ro
u
n
d
w
a
ter
lev
e
l
a
n
d
m
e
teo
ro
lo
g
ica
l
in
f
o
r
m
a
ti
o
n
a
g
g
re
g
a
te
b
u
il
d
th
e
u
se
o
f
c
e
rtain
e
x
p
e
n
siv
e
w
e
a
th
e
r
sta
ti
o
n
d
e
v
ice
s,
p
ro
m
in
e
n
t
to
a
la
c
k
o
f
v
a
st
m
o
n
it
o
rin
g
su
it
a
b
le
t
o
c
o
st
b
a
rrie
rs
a
n
d
d
istu
r
b
a
n
c
e
in
so
m
e
c
o
u
n
tr
ies
.
In
th
is
re
se
a
rc
h
,
w
e
h
a
v
e
d
e
v
e
lo
p
e
d
a
n
d
im
p
lem
e
n
ted
a
h
a
rd
w
a
re
m
o
d
u
le
b
a
se
d
o
n
a
n
A
rd
u
in
o
m
icro
c
o
n
tro
ll
e
r
a
n
d
m
o
b
il
e
c
o
m
m
u
n
ica
ti
o
n
,
w
h
ich
m
e
a
su
re
s
th
e
g
ro
u
n
d
w
a
ter
le
v
e
l
a
n
d
m
e
teo
ro
lo
g
ica
l
d
a
ta,
in
c
lu
d
i
n
g
a
ir
tem
p
e
ra
tu
re
,
a
ir
h
u
m
id
it
y
,
a
n
d
so
il
tem
p
e
ra
tu
re
,
a
n
d
h
u
m
id
it
y
,
ra
in
f
a
ll
in
p
e
a
tl
a
n
d
a
re
a
.
T
h
e
d
a
ta
g
ro
u
n
d
w
a
ter
lev
e
l
is
re
c
e
i
v
e
d
b
y
a
sp
e
c
i
a
ll
y
d
e
v
e
lo
p
e
d
a
p
p
li
c
a
ti
o
n
in
terf
a
c
e
ru
n
n
in
g
o
n
a
n
I
n
tern
e
t
o
f
T
h
in
g
s
(Io
T
)
c
o
n
n
e
c
ted
th
ro
u
g
h
a
G
lo
b
a
l
M
o
b
i
le
S
y
ste
m
(
G
S
M
)
c
o
m
m
u
n
ica
ti
o
n
.
I
n
th
is
w
o
rk
,
o
u
r
p
r
o
p
o
se
d
sy
ste
m
is
a
m
o
d
e
l
s
y
st
e
m
th
a
t
c
a
n
a
b
le
to
g
e
n
e
ra
te
a
lerts
b
a
se
d
o
n
t
h
e
re
a
l
-
ti
m
e
g
ro
u
n
d
w
a
ter
lev
e
l
a
n
d
d
a
ta
w
e
a
th
e
r
a
s
p
o
ten
ti
a
l
p
e
a
t
f
ire
in
I
n
d
o
n
e
sia
.
It
p
ro
v
id
e
s
o
n
li
n
e
a
n
d
d
a
ta
re
a
l
-
ti
m
e
m
o
n
it
o
ri
n
g
.
I
n
th
is
w
o
rk
s,
w
e
h
a
v
e
re
su
lt
e
d
in
a
sy
ste
m
to
m
o
n
it
o
r
t
h
e
g
ro
u
n
d
w
a
t
e
r
lev
e
l
a
n
d
d
a
ta
w
e
a
th
e
r
a
lert,
c
o
n
d
it
i
o
n
m
a
p
p
in
g
,
a
n
d
w
a
rn
th
e
p
e
o
p
le f
ro
m
it
s d
isa
stro
u
s e
ff
e
c
ts.
K
ey
w
o
r
d
s
:
C
o
m
m
u
n
ica
tio
n
s
y
s
te
m
Gr
o
u
n
d
w
ater
lev
el
I
n
ter
n
et
o
f
t
h
i
n
g
s
Sen
s
o
r
n
e
t
w
o
r
k
s
T
r
o
p
ical
p
ea
tlan
d
T
h
is i
s
a
n
o
p
e
n
a
c
c
e
ss
a
rticle
u
n
d
e
r th
e
CC B
Y
-
SA
li
c
e
n
se
.
C
o
r
r
e
s
p
o
nd
ing
A
uth
o
r
:
R
o
n
y
T
eg
u
h
Dep
a
r
t
m
en
t I
n
f
o
r
m
atics E
n
g
in
ee
r
in
g
Un
i
v
er
s
it
y
o
f
P
alan
g
k
a
R
a
y
a
Yo
s
Su
d
ar
s
o
S
tr
ee
t
,
P
alan
g
k
a
,
P
alan
g
k
a
R
a
y
a
C
it
y
,
C
e
n
tr
al
Kali
m
a
n
ta
n
7
4
8
7
4
,
I
n
d
o
n
esia
E
m
ail:
r
o
n
n
y
teg
u
h
@
g
m
ail.
co
m
1.
I
NT
RO
D
UCT
I
O
N
T
h
e
g
r
o
u
n
d
w
a
ter
lev
el
an
d
d
ata
w
ea
t
h
er
an
d
co
n
d
itio
n
o
f
cli
m
ate
ar
e
s
o
m
e
o
f
t
h
e
r
ea
ll
y
i
m
p
o
r
tan
t
f
ac
to
r
s
w
h
ich
i
n
f
lu
e
n
ce
t
h
e
q
u
alit
y
o
f
li
v
eli
h
o
o
d
an
d
th
e
o
th
er
ac
tiv
i
t
y
o
f
t
h
e
tr
o
p
ical
p
ea
tlan
d
en
v
ir
o
n
m
e
n
t.
T
h
e
cu
r
r
en
t
w
a
y
o
f
g
r
o
u
n
d
w
a
ter
lev
el
an
d
d
ata
m
eteo
r
o
lo
g
i
ca
l
co
llectio
n
m
ak
e
s
u
s
e
o
f
a
h
ig
h
-
co
s
t
w
ea
t
h
er
s
tatio
n
,
lead
i
n
g
to
a
d
r
a
w
b
ac
k
o
f
w
id
e
m
o
n
i
to
r
in
g
d
u
e
to
co
s
t
co
n
s
tr
ai
n
ts
a
n
d
in
co
n
v
e
n
ien
ce
s
i
n
ce
r
tai
n
co
u
n
tr
ies.
On
e
o
f
th
e
r
eq
u
ir
e
d
ter
m
s
f
o
r
t
h
e
ac
c
u
r
ac
y
w
ea
th
er
is
t
h
e
g
ain
o
f
p
r
ec
is
io
n
m
eteo
r
o
lo
g
ical
d
ata.
W
h
en
t
h
e
p
ar
a
m
eter
o
f
d
ata
m
e
teo
r
o
lo
g
ical
is
in
s
u
f
f
icie
n
t,
th
e
citizen
a
v
ailab
le
in
f
o
r
m
at
io
n
a
b
o
u
t
th
e
p
r
ed
ictio
n
o
f
w
ea
t
h
er
w
o
u
ld
b
e
in
ac
c
u
r
ate.
A
tr
o
p
ical
p
ea
tlan
d
f
o
r
es
t
is
o
n
e
o
f
t
h
e
m
o
s
t
i
m
p
o
r
tan
t
r
en
e
w
ab
le
n
at
u
r
al
r
eso
u
r
ce
s
th
at
p
la
y
s
i
g
n
i
f
ica
n
t
r
o
les
in
h
u
m
a
n
li
f
e
an
d
ec
o
lo
g
y
.
T
y
p
ical
p
ea
t
an
d
f
o
r
est
f
ir
e
s
ar
e
n
atu
r
al
d
is
aster
p
h
en
o
m
e
n
a.
I
n
r
ec
en
t
y
ea
r
s
,
c
h
r
o
n
ic
d
r
y
w
ea
t
h
er
,
q
u
ick
l
y
e
x
p
an
d
in
g
ex
p
lo
itatio
n
o
f
tr
o
p
ical
f
o
r
ests
,
an
d
th
e
r
eq
u
est
f
o
r
th
e
tr
an
s
f
o
r
m
a
tio
n
o
f
f
o
r
est
to
f
ar
m
lan
d
h
as
b
ec
o
m
e
s
e
v
er
e
w
it
h
e
s
ca
late
o
f
p
ea
t
-
f
o
r
est
f
ir
e
s
ize.
T
r
o
p
ical
p
ea
t
f
o
r
est
f
ir
es
ar
e
also
s
er
i
o
u
s
d
is
a
s
ter
s
i
n
ter
m
s
o
f
lo
s
s
o
f
b
o
t
h
p
r
o
p
er
ty
an
d
lif
e.
I
n
C
e
n
tr
al
Kali
m
a
n
ta
n
o
f
I
n
d
o
n
e
s
ia,
tr
o
p
ical
p
ea
t f
o
r
est f
ir
es a
r
e
m
o
s
tl
y
an
th
r
o
p
o
ce
n
tr
ic.
Evaluation Warning : The document was created with Spire.PDF for Python.
I
SS
N
:
2722
-
3221
C
o
m
p
u
t.
Sci.
I
n
f
.
T
ec
h
n
o
l.
,
Vo
l.
2
,
No
.
2
,
J
u
l
y
20
2
1
:
6
7
–
7
6
68
T
h
e
lo
ca
l
p
eo
p
le
an
d
t
r
an
s
m
ig
r
atio
n
f
ar
m
er
s
u
s
ed
f
ir
e
as
an
ar
ea
o
f
s
m
all
f
ar
m
la
n
d
ac
tiv
it
i
es
s
u
c
h
as
lan
d
clea
r
an
ce
.
I
n
t
h
e
d
r
y
s
ea
s
o
n
,
a
f
e
w
f
ir
es
h
a
v
e
s
p
r
ea
d
o
f
u
n
co
n
tr
o
lled
an
d
b
ec
o
m
e
w
ild
f
ir
es
to
p
ea
tla
n
d
ar
ea
s
.
T
h
e
tr
o
p
ical
p
ea
t
an
d
f
o
r
est
f
ir
es
n
o
t
o
n
l
y
b
u
r
n
t
h
e
s
u
r
f
ac
e
v
e
g
etatio
n
b
u
t
also
th
e
in
-
g
r
o
u
n
d
o
f
p
ea
t
d
ep
o
s
its
m
o
r
e
t
h
an
1
0
0
ce
n
ti
m
eter
s
u
n
d
er
th
e
s
o
il
s
u
r
f
ac
e.
B
u
t,
tr
o
p
ical
p
ea
t
f
ir
e
h
ap
p
en
s
o
n
l
y
i
n
e
x
tr
e
m
el
y
d
r
y
co
n
d
itio
n
s
o
r
s
in
ce
t
h
e
g
r
o
u
n
d
w
ater
lev
el
h
a
s
b
ee
n
lo
w
e
r
ed
ar
tif
iciall
y
.
T
r
o
p
ical
p
ea
t
f
ir
es
p
r
o
d
u
ce
h
ig
h
a
m
o
u
n
ts
o
f
g
a
s
to
x
ic
a
n
d
d
eter
io
r
ate
air
q
u
alit
y
t
h
e
th
e
co
n
ce
n
tr
atio
n
o
f
h
az
e
a
l
s
o
ca
u
s
e
s
h
e
alth
p
r
o
b
le
m
s
.
W
e
ca
n
s
ee
tr
o
p
ical
w
ild
f
ir
e
h
a
v
e
m
a
n
y
n
e
g
ativ
e
e
f
f
ec
ts
o
n
h
u
m
an
h
ea
lt
h
,
ec
o
n
o
m
y
,
en
v
ir
o
n
m
e
n
t,
an
d
cli
m
ate.
T
r
o
p
ical
p
ea
t
f
ir
e
o
cc
u
r
s
w
h
e
n
t
h
r
ee
n
ec
e
s
s
ar
y
co
n
d
itio
n
s
a
r
e
s
atis
f
ied
at
t
h
e
s
a
m
e
ti
m
e
f
la
m
m
ab
le
m
ater
ial,
o
x
y
g
en
,
a
n
d
h
i
g
h
te
m
p
er
at
u
r
e.
T
h
e
s
o
u
r
ce
o
f
a
tr
o
p
ical
p
ea
t
f
ir
e
in
I
n
d
o
n
esia
i
s
t
h
e
ac
ti
v
iti
es
o
f
lo
ca
l
f
ar
m
er
s
s
u
c
h
as
clea
r
an
ce
o
f
la
n
d
an
d
t
o
m
a
k
e
f
er
ti
lizer
f
r
o
m
as
h
.
I
n
t
h
is
p
ap
er
,
in
Fig
u
r
e
1
,
o
u
r
d
ev
ice
f
o
r
m
ea
s
u
r
e
m
e
n
t
g
r
o
u
n
d
w
ater
le
v
el
(
GW
L
)
u
s
in
g
an
u
ltra
s
o
n
ic
s
en
s
o
r
.
T
h
e
s
en
s
o
r
in
s
tal
led
in
to
th
e
P
VC
p
ip
e
w
ell
f
o
r
m
ea
s
u
r
e
m
e
n
t
o
f
t
h
e
g
r
o
u
n
d
w
a
ter
lev
el.
T
h
e
u
ltra
s
o
n
ic
s
e
n
s
o
r
is
as
s
e
m
b
li
n
g
at
t
h
e
en
d
to
p
o
f
th
e
P
VC
t
u
b
e.
T
h
e
P
VC
tu
b
e
i
s
i
n
s
tal
led
u
n
d
er
g
r
o
u
n
d
p
ea
t
a
n
d
it
s
en
d
b
o
tto
m
to
to
u
ch
e
s
p
ea
t
s
o
il.
T
h
e
u
l
tr
aso
n
ic
s
en
s
o
r
p
r
o
d
u
ce
s
b
y
t
h
e
elec
tr
o
m
a
g
n
et
ic
w
a
v
e
d
o
w
n
in
th
e
w
a
v
e
g
u
id
e
tu
b
e,
is
r
ef
lecte
d
at
th
e
w
a
ter
s
u
r
f
ac
e,
an
d
tr
av
els
b
ac
k
u
p
to
th
e
u
ltra
s
o
n
ic
s
e
n
s
o
r
at
th
e
t
o
p
o
f
th
e
p
ip
e.
T
h
e
p
r
o
p
ag
atio
n
w
av
e
o
f
u
s
e
u
ltra
s
o
n
ic
is
4
0
k
Hz
to
m
ea
s
u
r
e
th
e
g
r
o
u
n
d
w
ater
le
v
els i
n
t
h
is
e
x
p
er
i
m
en
t.
Fig
u
r
e
1
.
Th
e
s
e
f
ig
u
r
e
s
ar
e
;
(
a)
O
v
er
v
ie
w
ar
d
u
p
ea
t se
n
s
o
r
n
e
t
w
o
r
k
,
a
n
d
(b
)
T
h
e
w
ell
co
n
s
tr
u
ctio
n
f
o
r
g
r
o
u
n
d
w
ater
s
e
n
s
o
r
I
n
Fig
u
r
e
2
,
f
ir
es
in
p
ea
tlan
d
n
o
t
b
u
r
n
th
e
s
u
r
f
ac
e,
h
o
w
ev
er
a
ls
o
th
e
u
n
d
er
g
r
o
u
n
d
p
ea
t.
T
h
e
co
n
d
itio
n
o
f
lo
ca
l
w
ea
t
h
er
a
n
d
g
r
o
u
n
d
wate
r
lev
el
h
a
s
a
n
ec
es
s
ar
y
in
f
l
u
en
ce
o
n
p
o
ten
tial
p
ea
t
f
ir
e.
W
h
en
t
h
e
g
r
o
u
n
d
w
a
ter
lev
el
d
r
o
p
s
f
r
o
m
0
.
5
m
e
ter
s
to
1
m
eter
.
I
n
t
h
is
co
n
d
itio
n
is
p
r
ec
is
e
to
b
e
v
er
y
d
a
n
g
er
o
u
s
f
o
r
p
ea
t f
ir
e.
Fig
u
r
e
2
.
R
elatio
n
tr
o
p
ical
g
r
o
u
n
d
w
ater
le
v
el
w
it
h
p
o
ten
tial
p
ea
t f
ir
e
Evaluation Warning : The document was created with Spire.PDF for Python.
C
o
m
p
u
t.
Sci.
I
n
f
.
T
ec
h
n
o
l.
R
ea
ltime
mo
n
ito
r
in
g
fo
r
g
r
o
u
n
d
w
a
ter lev
el
a
n
d
lo
c
a
l c
lima
te
b
a
s
ed
o
n
u
n
ivers
a
l
…
(
R
o
n
y
Teg
u
h
)
69
I
n
h
y
d
r
o
lo
g
y
s
y
s
te
m
s
s
u
ch
as
g
r
o
u
n
d
w
ater
lev
el
[
1
]
-
[
3
]
an
d
m
o
is
t
u
r
e
o
f
s
u
r
f
ac
e
p
ea
t
ar
e
i
m
p
o
r
tan
t
k
e
y
s
f
o
r
p
ea
t
f
ir
e
-
co
n
tr
o
l
[
4
]
,
[
5
]
in
tr
o
p
ical
p
ea
tlan
d
.
T
h
e
p
r
o
p
ag
atio
n
r
ate
o
f
p
ea
t f
ir
e
o
n
s
u
r
f
ac
e
p
ea
t
s
o
il h
a
s
an
o
r
d
in
ar
y
o
f
42
-
1
5
5
cm
/d
a
y
an
d
in
s
u
b
s
u
r
f
ac
e
p
ea
t
s
o
il
1
2
-
6
0
cm
d
a
y
.
Fla
m
i
n
g
n
ee
d
s
t
e
m
p
er
atu
r
e
is
m
o
r
e
th
an
5
0
0
º
C
w
it
h
a
d
u
r
atio
n
o
f
m
o
r
e
t
h
a
n
2
0
m
in
u
te
s
.
A
s
m
en
tio
n
ed
ab
o
v
e,
th
e
p
ea
t
f
ir
e
s
tar
t
s
w
ith
o
v
er
h
ea
ti
n
g
b
ec
au
s
e
o
f
w
ea
th
er
co
n
d
itio
n
s
in
p
ea
t
s
o
il
d
r
y
i
n
g
[
6
]
.
T
r
o
p
ical
p
ea
t
is
n
o
r
m
all
y
f
o
r
m
ed
f
r
o
m
tr
ee
s
,
w
h
er
ea
s
b
o
r
ea
l
p
ea
t
is
c
o
m
p
o
s
ed
o
f
v
e
g
etatio
n
an
d
g
r
as
s
es.
Su
itab
le
to
th
eir
h
ig
h
er
ca
lo
r
if
ic
v
al
u
es
,
p
ea
t
s
o
il
m
atter
is
o
v
er
co
m
b
u
s
tio
n
as
f
u
e
ls
,
esp
ec
iall
y
w
h
e
n
t
h
e
co
n
d
itio
n
p
ea
t
is
d
r
y
.
So
m
e
w
o
r
k
h
a
s
b
ee
n
d
o
n
e
in
th
is
r
eg
ar
d
.
I
n
[
7
]
th
e
au
t
h
o
r
w
o
r
k
w
i
th
lo
w
-
p
o
w
er
w
ir
ele
s
s
s
en
s
o
r
n
et
w
o
r
k
s
(
W
SN
s
)
to
d
ev
elo
p
r
e
m
o
te
m
o
n
ito
r
i
n
g
w
etla
n
d
h
y
d
r
o
ch
e
m
ical
d
y
n
a
m
ics
s
till
ti
m
e
s
ca
le
s
r
an
g
i
n
g
f
r
o
m
d
ec
ad
es.
A
l
l
s
e
n
s
o
r
n
et
w
o
r
k
h
as
m
u
ltip
le
d
ev
ice
s
to
m
o
n
ito
r
g
r
o
u
n
d
w
ater
l
ev
el,
p
r
ec
ip
itatio
n
,
ev
ap
o
tr
an
s
p
ir
atio
n
,
tem
p
er
atu
r
e.
T
h
e
W
SNs
b
e
g
en
er
ated
to
r
ep
o
r
t
d
ata
in
n
ea
r
r
ea
l
-
ti
m
e
b
y
th
e
in
ter
n
e
t
W
SNs
ap
p
licatio
n
to
w
ar
d
r
ea
l
-
t
i
m
e
d
ata
ag
g
r
eg
ate
d
at
th
e
f
r
es
h
w
ater
r
eso
u
r
ce
s
s
u
c
h
as
r
i
v
er
s
,
la
k
es
,
o
r
w
etla
n
d
s
ar
ea
s
to
ac
q
u
ir
e
e
x
ac
t
w
ater
q
u
a
lit
y
m
ea
s
u
r
i
n
g
[
8
]
.
Me
an
w
h
ile,
a
d
ep
lo
y
m
en
t
h
y
d
r
o
lo
g
y
m
o
n
ito
r
in
g
s
y
s
te
m
u
s
i
n
g
t
h
e
ap
p
licati
o
n
o
f
Z
i
g
B
ee
an
d
GP
R
S
tec
h
n
o
lo
g
y
i
s
ca
p
ab
le
to
o
b
tain
d
is
tan
ce
h
y
d
r
o
lo
g
y
o
b
s
er
v
e
s
u
c
h
as
a
r
iv
er
,
f
is
h
p
o
n
d
,
o
r
ir
r
ig
ated
a
r
ea
[
9
]
.
T
h
e
s
en
s
o
r
n
et
w
o
r
k
s
y
s
te
m
is
u
s
ed
as a
n
e
m
b
ed
d
ed
p
latf
o
r
m
to
s
u
r
v
eilla
n
ce
t
h
e
f
r
esh
w
a
ter
q
u
alit
y
,
d
ep
lo
y
ed
at
a
s
p
r
e
ad
o
f
th
e
lo
ca
tio
n
in
w
h
ic
h
ea
ch
s
e
n
s
o
r
n
o
d
e
ca
p
ab
le
o
f
in
ter
f
ac
e
w
it
h
a
f
e
w
w
at
er
q
u
alit
y
s
e
n
s
o
r
s
.
H
y
d
r
o
lo
g
ic
al
m
o
n
ito
r
i
n
g
is
a
n
ap
p
licatio
n
o
f
Z
ig
B
ee
tech
n
o
lo
g
y
,
w
h
ic
h
h
a
s
a
r
o
b
u
s
t
p
er
f
o
r
m
a
n
ce
v
al
u
e.
T
h
e
au
th
o
r
w
a
s
d
ev
elo
p
ed
an
d
i
m
p
le
m
en
ted
to
m
o
n
ito
r
t
h
e
cl
i
m
ate
-
r
elate
d
to
g
lo
b
al
w
ar
m
i
n
g
i
n
tr
o
p
ical
p
ea
tlan
d
s
,
I
n
d
o
n
esia.
T
h
e
SAS
A
ME
d
ev
ice
is
m
ai
n
l
y
co
m
p
o
s
ed
o
f
th
e
s
e
n
s
o
r
,
th
e
d
ata
lo
g
g
er
,
th
e
d
ata
co
m
m
u
n
icatio
n
m
o
d
u
le,
an
d
th
e
b
atter
y
s
y
s
te
m
.
T
h
e
au
th
o
r
u
s
e
s
th
e
s
en
s
o
r
s
f
o
r
w
ater
d
ep
th
,
m
o
is
tu
r
e
ten
s
io
n
,
an
d
s
o
il
s
u
b
s
id
en
ce
len
g
t
h
o
f
cir
cu
m
f
er
e
n
ce
w
as
co
m
b
in
ed
w
it
h
SES
A
ME
-
II.
T
h
e
d
ev
ice
u
s
ed
to
t
h
e
g
r
o
u
n
d
w
ater
a
n
d
g
r
o
u
n
d
s
u
r
f
ac
e
le
v
el
s
in
p
ea
tlan
d
s
,
i
n
t
h
e
r
iv
er
an
d
t
h
e
d
a
m
la
k
e,
an
d
th
e
ir
r
i
g
atio
n
tr
ee
s
in
a
p
lan
tatio
n
in
I
n
d
o
n
e
s
ia
[
1
0
]
, [
11
]
.
T
h
e
s
y
s
te
m
h
a
s
e
f
f
ec
tiv
e
l
y
u
s
ef
u
l
to
t
h
e
r
ea
l
-
ti
m
e
m
o
n
ito
r
i
n
g
o
f
t
h
e
co
n
d
itio
n
o
f
w
ater
t
e
m
p
er
atu
r
e
an
d
lev
el
o
f
p
H
in
an
ar
tific
ial
lak
e.
I
n
[
1
2
]
th
e
au
th
o
r
w
o
r
k
s
o
n
d
ev
elo
p
in
g
th
e
d
esi
g
n
a
n
d
i
m
p
le
m
en
ta
tio
n
o
f
a
co
m
p
lete
W
SN
t
h
at
ca
n
b
e
u
s
ed
f
o
r
a
s
p
ac
e
o
f
a
lo
n
g
ti
m
e
en
v
ir
o
n
m
e
n
tal
m
o
n
ito
r
in
g
u
s
i
n
g
I
o
T
ap
p
licatio
n
s
.
T
h
e
au
th
o
r
w
o
r
k
also
in
m
an
y
f
u
n
ctio
n
s
o
f
th
e
W
SN
is
r
esp
ec
ted
:
th
e
s
tr
u
ct
u
r
e
o
f
th
e
W
S
N,
o
p
tim
izat
io
n
o
f
th
e
n
o
d
e
s
en
s
o
r
an
d
g
a
te
w
a
y
f
o
r
lin
k
co
m
m
u
n
icat
io
n
p
r
o
to
co
ls
,
s
el
f
er
r
o
r
r
ec
o
v
er
y
f
o
r
t
h
e
n
o
d
e
o
p
er
atio
n
,
th
e
s
er
v
er
ap
p
licatio
n
r
eliab
ilit
y
an
d
in
ter
f
ac
in
g
w
it
h
I
o
T
ap
p
l
icatio
n
s
.
T
h
e
au
th
o
r
[
1
3
]
w
o
r
k
s
to
in
te
g
r
ate
I
o
T
m
et
h
o
d
w
it
h
b
ig
d
ata
tech
n
o
lo
g
ies
in
to
a
h
o
lis
tic
ap
p
r
o
ac
h
f
o
r
r
ea
l
-
ti
m
e
d
ata
m
o
n
ito
r
in
g
an
d
p
r
o
ce
s
s
in
g
.
Usi
n
g
clo
u
d
I
o
T
p
latf
o
r
m
s
t
h
at
e
n
ab
le
g
en
er
ate
w
eb
s
er
v
ice
s
ap
p
r
o
p
r
iate
f
o
r
th
e
in
te
g
r
atio
n
d
ata
o
n
th
e
I
n
ter
n
et.
T
h
e
au
th
o
r
[
1
4
]
p
r
o
p
o
s
es
th
e
d
ev
elo
p
m
e
n
t
o
f
an
ap
p
licatio
n
f
o
r
p
r
ec
is
io
n
f
ar
m
in
g
u
s
in
g
a
w
ir
el
ess
s
en
s
o
r
n
et
w
o
r
k
w
it
h
I
o
T
clo
u
d
p
latf
o
r
m
s
t
h
a
t
allo
w
w
eb
ap
p
licatio
n
a
n
d
r
ea
l
-
ti
m
e
co
m
m
u
n
icatio
n
d
at
a.
T
h
e
au
th
o
r
[
1
5
]
p
r
esen
ted
th
e
d
esig
n
o
f
n
e
w
s
o
f
t
w
ar
e
an
d
h
ar
d
w
ar
e
o
f
w
ater
m
o
n
ito
r
i
n
g
w
h
ich
co
n
n
ec
ted
in
a
tem
p
o
r
al
w
a
y
to
th
e
W
SN
i
n
f
r
a
s
tr
u
ct
u
r
es.
T
h
e
au
th
o
r
u
s
i
n
g
Z
i
g
b
ee
p
r
o
to
co
l
m
u
lti
-
h
u
b
d
ata
co
m
m
u
n
icatio
n
f
o
r
co
llected
d
ata.
I
n
th
is
p
ap
er
,
o
u
r
p
r
o
b
lem
is
h
o
w
to
d
ev
elo
p
f
o
r
m
o
n
ito
r
in
g
g
r
o
u
n
d
w
ater
lev
el
an
d
lo
ca
l
p
ea
t
clim
ate
u
s
i
n
g
lo
w
-
co
s
t se
n
s
o
r
tech
n
o
lo
g
y
.
W
e
h
av
e
s
tu
d
y
s
o
m
e
r
esear
c
h
in
th
e
m
ea
s
u
r
e
m
e
n
t
w
ater
lev
el
f
o
r
o
u
r
w
o
r
k
.
I
n
th
e
s
y
s
te
m
,
w
e
h
a
v
e
d
ev
elo
p
ed
u
s
es
u
ltra
s
o
n
ic
s
en
s
o
r
m
ea
s
u
r
e
th
e
w
ater
lev
el
in
t
h
e
p
ea
t
s
o
il.
W
e
also
p
r
o
p
o
s
ed
s
o
lu
tio
n
s
th
at
ea
s
y
to
u
s
e
an
d
lo
w
-
co
s
t
u
s
in
g
A
r
d
u
in
o
b
ased
.
T
h
is
s
y
s
te
m
a
u
s
ef
u
ll
s
o
l
u
tio
n
f
o
r
m
o
n
i
to
r
in
g
an
d
p
ea
t
f
ir
e
ea
r
ly
w
ar
n
in
g
s
y
s
te
m
s
w
i
th
i
n
d
icat
o
r
g
r
o
u
n
d
w
ater
lev
e
l
in
p
ea
t
is
v
er
y
lo
w
er
an
d
s
o
il
m
o
is
tu
r
e
is
d
r
y
in
g
.
I
n
o
u
r
s
y
s
te
m
o
f
g
r
o
u
n
d
w
ater
an
d
w
ea
th
er
m
o
n
ito
r
i
n
g
,
th
e
en
v
ir
o
n
m
e
n
tal
d
ata
ar
e
s
en
t
to
a
co
m
p
u
ter
-
b
ased
s
y
s
te
m
th
r
o
u
g
h
a
n
A
r
d
u
in
o
b
o
ar
d
.
T
h
e
m
an
y
d
ata
p
ar
am
eter
s
ar
e
s
im
u
ltan
eo
u
s
tr
a
n
s
m
is
s
io
n
a
n
d
f
in
all
y
th
e
p
r
o
ce
s
s
b
y
an
o
n
l
y
s
i
n
g
le
c
h
an
n
el
to
s
h
o
w
t
h
e
d
ata
o
n
t
h
e
co
m
p
u
ter
.
F
o
r
co
llect
an
d
r
ec
o
r
d
o
f
th
e
d
ata,
th
e
s
tr
ea
m
o
f
d
ata
tak
en
b
y
t
h
e
s
e
n
s
o
r
s
is
co
lle
cted
in
th
e
I
n
ter
n
et
o
f
T
h
in
g
s
(
I
o
T
)
[
1
6
]
,
[
1
7
]
b
ased
o
n
th
e
s
y
s
te
m
w
h
ic
h
co
m
m
u
n
icate
s
t
h
r
o
u
g
h
g
lo
b
al
m
o
b
ile
s
y
s
te
m
d
ata
tr
a
n
s
m
is
s
io
n
.
Ou
r
co
n
tr
ib
u
t
io
n
o
f
t
h
is
p
ap
er
is
th
e
d
esig
n
,
co
n
s
tr
u
ct
io
n
,
an
d
i
m
p
le
m
en
tat
io
n
o
f
a
d
is
tr
ib
u
ted
in
-
f
ield
g
r
o
u
n
d
w
ater
le
v
el
an
d
w
ea
t
h
er
s
ta
tio
n
b
ased
o
n
a
n
A
r
d
u
i
n
o
a
n
d
th
e
I
n
ter
n
e
t o
f
T
h
in
g
s
(
I
o
T
)
in
p
ea
tlan
d
.
T
h
e
d
ev
ice
h
as b
ee
n
d
esi
g
n
ed
w
i
th
u
s
e
f
u
ll a
n
d
ef
f
ec
ti
v
e
to
s
ev
er
al
p
ea
tlan
d
p
ar
am
eter
s
s
u
c
h
as
u
ltra
s
o
n
ic
d
is
tan
ce
f
o
r
th
e
w
ater
tab
le,
te
m
p
er
atu
r
e,
h
u
m
id
it
y
,
s
o
il
te
m
p
er
atu
r
e,
m
o
i
s
t
u
r
e,
an
d
all
d
ata
r
ea
lti
m
e
s
e
n
d
to
th
e
in
ter
n
et
b
y
a
g
lo
b
al
co
m
m
u
n
icatio
n
s
y
s
te
m
.
2.
RE
S
E
ACH
M
E
T
H
O
D
2
.
1
.
Study
s
it
e
I
n
th
is
w
o
r
k
,
w
e
p
lace
m
en
t
A
r
d
u
p
ea
t
s
en
s
o
r
in
to
th
e
ex
p
er
i
m
en
tal
f
ield
f
o
r
d
e
m
o
n
s
tr
atin
g
th
e
w
o
r
k
i
n
g
o
f
th
e
s
y
s
te
m
a
n
d
th
e
g
r
o
u
n
d
w
ater
le
v
el
m
ea
s
u
r
e
m
e
n
ts
a
s
s
h
o
w
n
in
F
ig
u
r
e
3
.
T
h
e
lo
ca
t
e
d
ev
ice
in
s
ta
llatio
n
n
ea
r
th
e
s
m
a
ll
f
o
r
est
ca
m
p
u
s
o
f
P
alan
g
k
a
R
a
y
a
Un
iv
er
s
it
y
b
y
a
d
ep
th
o
f
p
ea
t
s
o
il
is
0
.
5
m
eter
s
.
T
h
e
len
g
t
h
o
f
th
e
P
VC
p
ip
e
u
s
ed
i
n
t
h
is
i
m
p
l
m
e
n
tatio
n
is
1
m
e
ter
.
W
e
g
et
th
e
s
a
m
p
li
n
g
d
ata
f
r
o
m
2
8
Sep
te
m
b
er
-
4
Octo
b
er
2
0
1
9
in
d
r
y
co
n
d
itio
n
.
T
h
e
s
en
s
o
r
d
ata
r
ec
o
r
d
ev
er
y
1
5
m
in
u
t
e
an
d
d
ir
ec
tly
s
en
d
to
d
atab
ase
s
er
v
er
b
y
T
C
P
/I
P
p
r
o
to
co
l.
T
h
e
A
r
d
u
P
ea
t
s
en
s
o
r
f
o
r
m
o
n
ito
r
in
g
an
d
a
u
to
m
at
in
g
th
e
h
y
d
r
o
lo
g
y
o
f
t
h
e
p
ea
t
lan
d
ar
ea
,
A
r
d
u
in
o
Evaluation Warning : The document was created with Spire.PDF for Python.
I
SS
N
:
2722
-
3221
C
o
m
p
u
t.
Sci.
I
n
f
.
T
ec
h
n
o
l.
,
Vo
l.
2
,
No
.
2
,
J
u
l
y
20
2
1
:
6
7
–
7
6
70
m
eg
a
m
o
d
u
le
s
in
t
h
e
co
n
f
i
g
u
r
atio
n
w
er
e
u
s
ed
.
T
h
e
y
w
er
e
p
ac
k
ag
ed
o
n
a
P
VC
ca
s
e
w
it
h
ex
ter
n
al
co
n
n
ec
to
r
s
f
o
r
t
y
p
es
o
f
eq
u
ip
m
e
n
t
a
n
d
co
m
m
u
n
icatio
n
s
.
T
h
e
A
r
d
u
i
n
o
m
icr
o
co
n
tr
o
ller
is
u
s
ed
f
o
r
s
to
r
in
g
d
ata
in
a
m
icr
o
SD
m
e
m
o
r
y
,
it
is
also
in
ch
ar
g
e
o
f
m
icr
o
cli
m
atic
d
ata
ac
q
u
is
i
t
io
n
,
g
lo
b
al
m
o
b
ile
s
y
s
te
m
c
o
m
m
u
n
icatio
n
.
T
h
e
d
ev
ices u
s
ed
in
t
h
e
i
m
p
le
m
e
n
t
atio
n
ca
n
b
e
ap
p
r
ec
iated
in
th
e
co
n
n
ec
tio
n
d
ia
g
r
a
m
i
n
Fi
g
u
r
e
4
.
Fig
u
r
e
3
.
P
lace
m
e
n
t
an
d
i
n
s
tal
latio
n
ar
d
u
p
ea
t
2
.
2
.
T
he
a
rc
hit
ec
t
ure
a
rdup
ea
t
s
y
s
t
e
m
g
ro
un
dw
a
t
er
lev
el
m
o
nito
ring
I
n
Fig
u
r
e
4
,
o
u
r
s
y
s
te
m
is
esp
ec
iall
y
to
b
u
ild
a
s
o
f
t
w
ar
e
d
ev
elo
p
m
e
n
t
p
latf
o
r
m
a
n
d
d
esig
n
e
m
b
ed
d
ed
in
t
h
e
s
en
s
o
r
n
o
d
e.
T
h
e
A
r
d
u
p
ea
t
u
s
es
4
-
la
y
er
m
et
h
o
d
s
:
s
e
n
s
o
r
la
y
er
,
co
m
m
u
n
ica
tio
n
la
y
er
,
a
la
y
er
o
f
t
h
e
in
ter
n
e
t
o
f
th
i
n
g
s
,
an
d
th
e
u
s
er
la
y
er
.
T
h
e
co
m
m
u
n
ic
atio
n
la
y
er
b
ased
o
n
th
e
GP
R
S
m
o
d
u
le
lib
r
ar
y
,
in
ad
d
itio
n
,
to
o
b
tain
in
g
th
e
k
er
n
el
in
th
e
o
p
e
r
atin
g
s
y
s
te
m
o
p
er
ates
th
e
GP
R
S
m
o
d
u
le
to
ac
tiv
atio
n
th
e
g
lo
b
al
m
o
b
il
e
s
y
s
te
m
la
y
er
.
T
h
e
in
ter
n
et
o
f
t
h
in
g
s
la
y
er
b
ased
o
n
a
clo
u
d
s
y
s
te
m
b
ased
o
n
L
in
u
x
OS
w
it
h
a
v
i
s
u
al
izatio
n
o
f
th
e
d
ata.
T
h
e
ed
g
e
o
f
th
e
la
y
er
is
t
h
e
u
s
er
la
y
er
b
ased
o
n
t
h
e
ab
o
v
e
s
e
v
er
al
la
y
er
s
w
h
ic
h
co
r
r
esp
o
n
d
to
th
e
ce
r
tain
ap
p
licatio
n
s
o
f
h
y
d
r
o
l
o
g
y
an
d
cli
m
a
te
m
o
n
ito
r
i
n
g
s
y
s
te
m
s
es
tab
lis
h
v
ar
io
u
s
d
u
t
y
th
at
u
s
es
t
h
e
d
ata
v
is
u
aliza
t
io
n
an
d
i
n
ter
f
ace.
Fig
u
r
e
4
.
T
h
e
o
v
er
v
ie
w
ar
ch
it
ec
tu
r
e
ar
d
u
p
ea
t
s
y
s
te
m
g
r
o
u
n
d
w
ater
le
v
el
m
o
n
ito
r
in
g
2
.
3
.
Ardupea
t
ha
rdw
a
re
T
h
e
p
r
o
p
o
s
ed
h
ar
d
w
ar
e
s
y
s
te
m
o
f
A
r
d
u
P
ea
t
s
en
s
o
r
n
et
w
o
r
k
is
s
h
o
w
n
i
n
Fi
g
u
r
e
4
.
Ou
r
s
y
s
te
m
is
co
n
s
is
t
ed
b
y
t
h
e
f
o
llo
w
in
g
t
h
r
ee
p
ar
ts
.
Evaluation Warning : The document was created with Spire.PDF for Python.
C
o
m
p
u
t.
Sci.
I
n
f
.
T
ec
h
n
o
l.
R
ea
ltime
mo
n
ito
r
in
g
fo
r
g
r
o
u
n
d
w
a
ter lev
el
a
n
d
lo
c
a
l c
lima
te
b
a
s
ed
o
n
u
n
ivers
a
l
…
(
R
o
n
y
Teg
u
h
)
71
2
.
3
.
1
.
Co
mm
un
ica
t
io
n
da
t
a
T
h
e
h
y
d
r
o
lo
g
y
d
ata
co
llect
an
d
d
ir
ec
t
s
en
d
u
s
in
g
t
h
e
GSM
n
et
w
o
r
k
i
s
tr
an
s
m
i
tted
to
th
e
d
ata
r
ec
eiv
in
g
clo
u
d
.
T
h
e
d
atab
ase
o
v
er
th
e
I
n
ter
n
et
b
y
GP
R
S
/3
G
[
1
8
]
,
[
1
9
]
,
to
p
er
f
o
r
m
lo
n
g
-
d
is
ta
n
ce
d
a
ta
tr
an
s
m
i
s
s
io
n
.
I
n
th
is
w
o
r
k
,
w
e
u
s
e
A
T
co
m
m
a
n
d
d
eliv
er
y
d
ata
u
s
i
n
g
T
C
P
/I
P
p
r
o
to
co
l t
o
th
e
in
ter
n
et
clo
u
d
n
et
w
o
r
k
.
2
.
3
.
2
.
Co
m
po
nent
o
f
s
ens
o
r
T
h
e
g
r
o
u
n
d
w
ater
lev
e
l
u
s
i
n
g
u
ltra
s
o
n
ic
s
en
s
o
r
f
o
r
m
ea
s
u
r
e
m
en
t
o
f
d
is
tan
ce
[
2
0
]
.
T
h
e
s
en
s
o
r
o
p
er
atio
n
v
o
ltag
e
o
n
5
V
D
C
,
o
p
er
atio
n
r
an
g
e
2
5
C
m
to
4
.
5
m
w
it
h
r
e
s
o
lu
tio
n
0
.
5
c
m
.
Ultr
a
s
o
n
ic
i
n
s
tallatio
n
o
n
t
h
e
to
p
o
f
p
ip
e.
A
p
ip
e
m
o
d
if
ica
tio
n
w
it
h
p
o
in
t
e
v
er
y
s
id
e
w
it
h
d
is
tan
ce
5
C
m
(
s
ee
Fi
g
u
r
e
2
b
)
.
T
h
e
s
tatio
n
in
cl
u
d
in
g
air
te
m
p
er
atu
r
e,
h
u
m
id
it
y
,
s
o
il
m
o
i
s
tu
r
e,
s
o
il
te
m
p
er
at
u
r
e,
r
ain
g
au
g
e
[
2
1
]
,
[
2
2
]
.
I
n
th
e
T
ab
le
1
,
s
h
o
w
n
co
m
p
o
n
e
n
t
s
en
s
o
r
an
d
f
u
n
ctio
n
u
s
e
f
o
r
o
u
r
w
o
r
k
s
.
2
.
3
.
3
.
P
o
w
er
o
f
s
o
urce
P
o
w
er
o
f
s
o
u
r
ce
.
T
o
o
p
tim
al
A
r
d
u
p
ea
t
d
e
v
ice,
t
h
e
p
er
f
o
r
m
a
n
ce
o
f
en
er
g
y
p
o
w
er
t
h
e
b
atter
y
s
h
all
ab
le
to
p
o
w
er
t
h
e
f
u
ll
s
y
s
te
m
f
o
r
at
least
2
4
h
o
u
r
s
,
w
it
h
o
u
t
a
n
y
r
ec
h
ar
g
e,
a
n
d
th
e
s
o
lar
p
an
el
m
u
s
t
b
e
s
m
ar
t
to
c
h
ar
g
e
th
r
o
u
g
h
o
u
t
o
n
th
e
d
a
y
th
e
e
n
er
g
y
co
n
s
u
m
ed
o
v
er
n
i
g
h
t
[
2
3
]
,
[
2
4
]
.
T
h
e
a
r
d
u
p
ea
t
h
as
r
eq
u
ir
em
en
ts
f
o
r
th
e
en
er
g
y
b
atter
y
a
n
d
th
e
s
o
lar
p
an
el
[
2
5
]
w
as d
eter
m
in
ed
as 1
0
Ah
a
n
d
1
2
V,
1
.
2
Am
p
r
esp
ec
tiv
el
y
.
T
ab
le
1
.
C
o
m
p
o
n
e
n
t se
n
s
o
r
an
d
f
u
n
ctio
n
C
o
mp
o
n
e
n
t
D
e
scri
p
t
i
o
n
F
u
n
c
t
i
o
n
A
r
d
u
i
n
o
M
e
g
a
M
i
c
r
o
c
o
n
t
r
o
l
l
e
r
b
o
a
r
d
M
a
n
a
g
e
,
a
r
r
a
n
g
e
a
n
d
t
r
a
n
smi
ssi
t
d
a
t
a
D
H
T
2
2
T
e
mp
e
r
a
t
u
r
e
a
n
d
H
u
mi
d
i
t
y
se
n
so
r
R
e
c
o
r
d
a
i
r
t
e
m
p
e
r
a
t
u
r
e
a
n
d
h
u
m
i
d
i
t
y
S
I
M
9
0
0
G
P
R
S
/
3
G
M
o
d
u
l
e
I
n
t
e
r
n
e
t
c
o
mm
u
n
i
c
a
t
i
o
n
S
o
l
a
r
P
o
w
e
r
M
a
n
a
g
e
r
S
o
l
a
r
C
o
n
t
r
o
l
l
e
r
P
o
w
e
r
D
S
1
8
B
2
0
S
o
i
l
T
e
mp
e
r
a
t
u
r
e
R
e
c
o
r
d
so
i
l
t
e
mp
e
r
a
t
u
r
e
FC
-
28
S
o
i
l
H
u
mi
d
i
t
y
R
e
c
o
r
d
so
i
l
h
u
m
i
d
i
t
y
4
-
2
0
H
R
-
M
a
x
S
o
n
a
r
U
l
t
r
a
so
n
i
c
se
n
so
r
R
e
c
o
r
d
d
i
st
a
n
c
e
WS
-
1080
R
a
i
n
g
a
u
g
e
R
e
c
o
r
d
r
a
i
n
Fig
u
r
e
5
.
T
h
e
s
en
s
o
r
co
m
p
o
n
e
n
t o
f
ar
d
u
p
ea
t
2
.
4
.
Ardupea
t
s
o
f
t
w
a
re
I
n
th
i
s
w
o
r
k
,
w
e
p
r
o
p
o
s
e
s
o
f
tw
ar
e
d
esi
g
n
f
o
r
ar
d
u
p
ea
t
s
en
s
o
r
n
et
w
o
r
k
.
W
e
d
ev
elo
p
an
ap
p
licatio
n
f
o
r
co
m
p
o
n
e
n
t
s
e
n
s
o
r
an
d
d
ata
c
o
m
m
u
n
icatio
n
u
s
i
n
g
th
e
A
r
d
u
in
o
p
r
o
g
r
a
m
m
i
n
g
lan
g
u
ag
e
Fro
m
th
e
s
e
n
s
o
r
,
th
is
s
o
f
t
w
ar
e
ca
n
r
ec
o
r
d
s
tr
ea
m
t
h
e
d
ata
ac
q
u
is
itio
n
a
n
d
d
ir
ec
tl
y
s
e
n
d
u
s
e
t
h
e
i
n
ter
n
et
u
s
e
s
h
y
p
er
te
x
t
tr
an
s
f
er
p
r
o
to
co
l
(
H
T
T
P
)
.
A
f
ter
th
e
d
ata
f
r
o
m
th
e
s
e
n
s
o
r
w
a
s
u
p
lo
ad
ed
f
r
o
m
th
e
A
r
d
u
p
ea
t
co
n
n
e
cted
to
a
GP
R
S/3
G
m
o
d
u
le
to
th
e
clo
u
d
s
er
v
er
.
A
ll
u
p
d
ates
th
e
d
ata
r
ec
o
r
d
f
r
o
m
t
h
e
s
en
s
o
r
s
an
d
d
is
tr
ib
u
tio
n
th
e
p
ar
am
eter
i
n
g
r
ap
h
to
th
e
u
s
er
s
.
I
n
th
is
w
o
r
k
,
t
h
e
f
ea
tu
r
es
o
f
t
h
e
s
o
f
t
w
ar
e
th
e
u
s
e
r
r
eq
u
ir
em
e
n
t
to
cr
ea
te
ev
er
y
a
cc
o
u
n
t
a
n
d
d
y
n
a
m
i
c
I
P
ad
d
r
ess
th
at
co
n
tain
s
th
e
d
if
f
er
en
t
f
o
r
m
o
n
ito
r
in
g
th
e
d
if
f
er
en
t
d
ata
r
ec
o
r
d
s
in
th
e
s
y
s
t
e
m
.
T
h
e
f
lo
w
ch
ar
t
d
iag
r
a
m
o
f
t
h
e
ar
d
u
p
ea
t s
y
s
te
m
is
s
h
o
w
n
in
F
ig
u
r
e
6
.
Evaluation Warning : The document was created with Spire.PDF for Python.
I
SS
N
:
2722
-
3221
C
o
m
p
u
t.
Sci.
I
n
f
.
T
ec
h
n
o
l.
,
Vo
l.
2
,
No
.
2
,
J
u
l
y
20
2
1
:
6
7
–
7
6
72
Fig
u
r
e
6
.
Ov
er
all
alg
o
r
it
h
m
f
o
r
p
r
o
p
o
s
ed
s
y
s
te
m
2
.
5
.
Web
ba
s
ed
m
o
nit
o
ring
a
pp
li
ca
t
io
n
T
h
e
r
ea
l
-
ti
m
e
w
eb
m
o
n
ito
r
in
g
co
n
n
ec
t
s
to
t
h
e
d
atab
ase
clo
u
d
u
s
i
n
g
th
e
in
ter
n
et.
T
h
e
w
eb
ap
p
licatio
n
p
r
o
ce
s
s
in
g
o
f
th
e
d
ata
in
r
ea
l
-
ti
m
e
an
d
r
ec
o
r
d
o
f
all
d
ata
an
d
d
is
p
lay
s
th
e
p
o
s
itio
n
o
f
th
e
s
en
s
o
r
b
y
m
ap
s
.
I
n
th
is
w
eb
ap
p
licatio
n
f
o
r
co
llect
an
d
s
to
r
e
o
f
d
ata
u
s
in
g
M
y
SQ
L
Data
b
ase
an
d
P
HP
lan
g
u
a
g
e.
T
h
e
w
eb
ap
p
licatio
n
co
n
s
is
t
s
o
f
a
s
h
o
w
f
o
r
th
e
in
f
o
r
m
atio
n
g
at
h
er
ed
f
r
o
m
t
h
e
s
en
s
o
r
n
et
w
o
r
k
.
I
n
th
i
s
ap
p
licatio
n
,
u
s
er
s
ca
n
s
elec
t
w
h
ich
id
en
t
it
y
o
f
s
e
n
s
o
r
s
f
o
r
s
h
o
w
n
v
i
s
u
a
lizatio
n
.
T
h
e
A
r
ch
ite
ct
u
r
e
f
o
r
th
e
b
ac
k
en
d
s
er
v
er
s
ep
ar
ated
in
to
2
m
ai
n
la
y
er
s
.
2
.
5
.
1
.
I
nte
rf
a
ce
la
y
er
C
o
v
er
s
P
HP
(
h
y
p
er
te
x
t
P
r
ep
ce
s
s
o
r
)
an
d
A
p
ac
h
e
w
eb
s
er
v
er
.
I
n
t
h
is
w
o
r
k
,
i
n
ter
f
ac
e
la
y
er
ca
n
h
an
d
l
e
th
e
f
u
n
ctio
n
o
f
t
h
e
HT
T
P
P
OST
/GE
T
in
s
tr
u
ctio
n
r
eq
u
est
f
r
o
m
s
er
v
er
lev
e
l
d
ev
ice
s
an
d
w
e
b
ap
p
licatio
n
clien
t
s
.
T
h
e
s
en
s
o
r
d
eli
v
er
s
to
t
h
e
clo
u
d
s
er
v
er
u
s
in
g
t
h
e
P
HP
f
u
n
c
tio
n
(
in
s
er
t)
a
n
d
r
eq
u
est
s
d
ata
f
r
o
m
th
e
d
atab
ase
la
y
er
w
it
h
in
s
er
t a
n
d
f
etc
h
e
s
f
u
n
ct
io
n
r
esp
ec
ti
v
el
y
(
s
ee
Fig
u
r
e
4
in
L
a
y
er
1
)
.
2
.
5
.
2
.
Da
t
a
ba
s
e
la
y
er
Ou
r
w
eb
ap
p
licatio
n
u
s
i
n
g
th
e
My
SQ
L
d
atab
ase
s
er
v
er
.
T
h
e
m
ai
n
f
u
n
ctio
n
to
s
to
r
e
d
ata
r
e
ce
iv
ed
b
y
th
e
in
s
er
t
f
u
n
ctio
n
a
n
d
p
r
o
v
id
e
d
ata
in
r
esp
o
n
s
e
to
th
e
f
etch
c
o
m
m
a
n
d
(
s
ee
Fi
g
u
r
e
4
in
L
a
y
e
r
3
)
.
T
h
e
w
eb
ap
p
licatio
n
d
is
p
la
y
s
all
th
e
A
r
d
u
p
ea
t
s
tatio
n
o
n
t
h
e
w
eb
ap
p
licatio
n
.
T
h
e
lo
ca
l
w
ea
t
h
er
p
ar
am
eter
s
ac
cu
m
u
late
at
lo
ca
l
ar
d
u
p
ea
t
d
ev
ices
b
e
s
en
t
to
a
d
atab
ase
s
er
v
er
,
p
er
m
it
u
s
er
s
to
ac
ce
s
s
r
ea
l
-
ti
m
e
d
ata
f
r
o
m
t
h
e
ar
d
u
p
ea
t
s
en
s
o
r
.
T
h
e
u
s
er
ca
n
ac
ce
s
s
an
d
v
ie
w
ev
er
y
ti
m
e
d
y
n
a
m
icall
y
g
en
er
ated
g
r
ap
h
f
o
r
Evaluation Warning : The document was created with Spire.PDF for Python.
C
o
m
p
u
t.
Sci.
I
n
f
.
T
ec
h
n
o
l.
R
ea
ltime
mo
n
ito
r
in
g
fo
r
g
r
o
u
n
d
w
a
ter lev
el
a
n
d
lo
c
a
l c
lima
te
b
a
s
ed
o
n
u
n
ivers
a
l
…
(
R
o
n
y
Teg
u
h
)
73
ch
an
g
i
n
g
lo
ca
l
w
ea
t
h
er
,
s
u
ch
as
te
m
p
er
at
u
r
e,
h
u
m
id
it
y
,
s
o
il
te
m
p
er
atu
r
e,
s
o
il
m
o
i
s
t
u
r
e,
r
ain
f
all,
w
ater
le
v
el
s
to
r
e
d
in
th
e
d
atab
ase
s
er
v
er
as sh
o
w
n
i
n
Fi
g
u
r
e
7
.
T
h
ese
s
y
s
te
m
s
,
o
v
er
all
d
iag
r
a
m
o
f
t
h
e
s
y
s
te
m
d
atab
ase
an
d
w
eb
ap
p
licatio
n
i
n
L
a
y
er
3
an
d
L
a
y
er
4
in
Fi
g
u
r
e
4
as d
ata
s
y
n
c
h
r
o
n
ize
to
v
is
u
alize
t
h
e
v
al
u
e
d
ata.
Fig
u
r
e
7
.
Dash
b
o
ar
d
f
o
r
m
o
n
it
o
r
in
g
an
d
w
ea
t
h
er
d
ata
v
is
u
ali
za
tio
n
3.
RE
SU
L
T
S AN
D
D
I
SCU
SS
I
O
N
I
n
th
is
w
o
r
k
,
w
e
co
llect
s
i
x
p
ar
am
e
ter
s
n
a
m
el
y
s
o
il
te
m
p
er
atu
r
e,
s
o
il
m
o
is
t
u
r
e,
r
ain
f
all,
air
te
m
p
er
atu
r
e,
an
d
g
r
o
u
n
d
w
ater
lev
el
ar
e
r
ec
o
r
d
u
s
in
g
th
e
ar
d
u
p
ea
t
s
en
s
o
r
.
Ou
r
d
ev
ice
is
co
n
n
ec
ted
to
a
r
ea
l
-
ti
m
e
M
y
SQ
L
d
atab
ase
f
o
r
co
ll
ec
t
an
d
s
to
r
e
s
en
s
o
r
v
alu
e.
I
n
o
u
r
ex
p
er
i
m
e
n
t
s
tar
ts
to
g
et
th
e
s
a
m
p
li
n
g
d
ata
f
r
o
m
2
8
Sep
te
m
b
er
–
4
Octo
b
er
2
0
1
9
in
d
r
y
co
n
d
itio
n
.
T
h
e
d
ev
i
ce
s
en
s
o
r
r
ec
o
r
d
an
d
s
en
d
s
d
a
ta
ev
er
y
1
5
-
m
i
n
u
te
u
s
i
n
g
GP
R
S/3
G
n
e
t
w
o
r
k
an
d
co
llect
in
to
a
d
atab
ase
w
it
h
d
i
f
f
er
en
t p
ar
a
m
e
ter
s
.
3
.
1
.
M
e
a
s
ure
m
e
nt
g
ro
un
dw
a
t
er
l
ev
el
I
n
th
i
s
w
o
r
k
,
e
v
er
y
s
en
s
o
r
s
e
n
d
d
ata
lo
ca
l
w
ea
th
er
a
n
d
w
a
ter
lev
el
w
it
h
d
ep
th
p
o
s
it
io
n
.
T
h
e
k
e
y
to
co
n
tr
o
l
o
f
p
ea
t
f
ir
e
is
g
r
o
u
n
d
w
ater
lev
e
l
an
d
r
ain
f
al
l
is
v
er
y
i
m
p
o
r
tan
t
as
an
aler
t
f
o
r
p
o
ten
tial
p
ea
t
f
ir
e.
T
h
e
d
ata
g
r
o
u
n
d
w
ater
le
v
el
d
ec
r
ea
s
e
to
w
ar
d
0
.
5
m
eter
s
,
t
h
i
s
s
y
s
te
m
p
r
o
v
id
es
alar
m
as
a
n
ea
r
l
y
w
ar
n
i
n
g
s
y
s
te
m
.
T
h
e
u
ltra
s
o
n
ic
s
e
n
s
o
r
p
r
ep
ar
es
an
o
p
er
atio
n
r
an
g
e
2
5
c
m
to
4
.
5
m
w
i
th
r
eso
l
u
tio
n
0
.
5
c
m
m
e
asu
r
e
m
en
t
d
i
s
tan
ce
.
T
h
e
s
en
s
o
r
r
ea
d
y
to
s
er
v
e
o
n
an
u
l
tr
aso
n
ic
m
o
d
u
le
t
h
at
co
n
ta
in
s
a
tr
a
n
s
m
it
ter
,
r
ec
eiv
er
,
an
d
co
n
tr
o
l
cir
cu
it.
T
h
e
u
ltra
s
o
n
ic
s
en
s
o
r
d
eliv
er
s
a
h
ig
h
-
f
r
eq
u
e
n
c
y
p
r
o
p
ag
atio
n
w
a
v
e
u
s
i
n
g
f
r
eq
u
e
n
c
y
4
0
0
0
0
Hz,
an
d
u
ltra
s
o
n
ic
ca
n
th
e
m
ea
s
u
r
e
e
s
ti
m
atio
n
o
f
t
h
e
ec
h
o
r
ec
eiv
ed
b
et
w
ee
n
s
ig
n
al
t
r
an
s
m
is
s
io
n
s
f
r
o
m
t
h
e
p
i
n
tr
i
g
g
er
an
d
r
ec
ei
v
i
n
g
it
b
ac
k
to
th
e
ec
h
o
w
h
ich
f
o
r
w
ar
d
d
eter
m
i
n
es t
h
e
m
ea
s
u
r
e
m
e
n
t
d
is
tan
ce
to
w
ater
.
T
h
e
g
r
o
u
n
d
w
ater
le
v
el
m
ea
s
u
r
ed
d
is
tan
ce
u
s
in
g
t
h
e
u
ltra
s
o
u
n
d
s
e
n
s
o
r
a
n
d
th
e
g
r
o
u
n
d
w
ater
lev
el
is
to
r
ec
o
r
d
in
to
th
e
w
eb
ap
p
licatio
n
as
s
h
o
w
n
i
n
Fig
u
r
e
7
.
W
e
s
tar
t
to
co
llect
d
ata
o
n
1
Octo
b
er
2
0
1
9
,
th
e
w
ater
lev
el
co
n
d
itio
n
is
h
i
g
h
ar
o
u
n
d
2
8
C
m
in
t
h
e
p
ea
t a
f
ter
r
ain
f
al
l 2
8
-
2
9
Sep
tem
b
er
2
0
1
9
.
W
e
ca
n
s
ee
th
e
r
elatio
n
w
it
h
p
ea
t
f
ir
e,
t
h
e
p
o
s
itio
n
o
f
w
ater
le
v
el
is
2
8
C
m
in
Fi
g
u
r
e
1
in
th
e
ca
teg
o
r
y
s
af
e
w
h
e
n
th
e
d
an
g
er
o
u
s
p
ea
t
f
ir
e
in
-
d
ep
th
0
.
5
m
eter
s
w
ater
lev
el.
I
t
o
cc
u
r
s
s
in
ce
at
th
e
tim
e
o
f
s
a
m
p
li
n
g
th
e
w
ater
lev
el,
th
e
p
ea
t
s
o
il
w
as
r
ain
an
d
th
e
s
o
il
te
m
p
er
atu
r
e
b
e
co
ld
.
Fig
u
r
e
8
s
h
o
w
s
t
h
er
e
w
a
s
a
f
l
u
ct
u
atio
n
in
th
e
w
ate
r
tab
le
lev
el
in
th
e
p
ea
tlan
d
it
is
co
r
r
elate
d
to
r
ain
f
all
co
n
d
itio
n
s
at
t
h
i
s
lo
ca
tio
n
d
u
r
i
n
g
t
h
e
o
b
s
er
v
at
io
n
p
er
io
d
.
I
n
co
m
m
o
n
co
n
d
itio
n
s
,
th
e
g
en
er
ic
p
atter
n
o
f
g
r
o
u
n
d
w
ater
lev
el
d
y
n
a
m
i
cs
is
r
ath
er
s
tab
le
th
r
o
u
g
h
o
u
t
th
e
y
ea
r
.
T
h
e
w
ater
tab
le
lev
el
at
th
i
s
s
ite
r
o
s
e
i
n
r
esp
o
n
s
e
to
h
ig
h
r
ai
n
f
a
ll
i
n
te
n
s
it
ies.
I
n
th
e
lo
ca
l
h
y
d
r
o
lo
g
y
ar
ea
is
k
n
o
w
n
to
s
tr
o
n
g
l
y
i
n
f
lu
e
n
ce
p
ea
t d
ec
o
m
p
o
s
itio
n
.
Evaluation Warning : The document was created with Spire.PDF for Python.
I
SS
N
:
2722
-
3221
C
o
m
p
u
t.
Sci.
I
n
f
.
T
ec
h
n
o
l.
,
Vo
l.
2
,
No
.
2
,
J
u
l
y
20
2
1
:
6
7
–
7
6
74
Fig
u
r
e
8
.
Gr
o
u
n
d
w
ater
lev
el
(
A
)
an
d
R
ain
f
all
(
B
)
3
.
2
.
M
e
a
s
ure
m
e
nt
a
ir
t
e
m
pera
t
ure
a
n
d hu
m
i
dity
Fig
u
r
e
9
s
h
o
w
s
th
e
co
n
d
itio
n
a
ir
te
m
p
er
atu
r
e
a
n
d
air
h
u
m
id
it
y
n
ea
r
th
e
lo
ca
tio
n
o
f
t
h
e
p
ea
t.
As
s
h
o
w
n
in
Fi
g
u
r
e
9
(
A
)
th
e
air
te
m
p
er
atu
r
e
r
an
g
ed
f
r
o
m
2
4
-
4
0
º
C
.
T
h
e
p
atter
n
o
f
air
te
m
p
er
atu
r
e
w
a
s
r
elativ
e
l
y
s
tab
le
f
r
o
m
Sep
te
m
b
er
to
Octo
b
er
.
I
n
co
n
tr
ast,
in
ea
r
l
y
Sep
te
m
b
er
th
e
air
te
m
p
er
atu
r
e
w
a
s
q
u
ite
h
i
g
h
.
Me
a
n
w
h
ile,
th
e
p
atter
n
o
f
air
h
u
m
id
it
y
i
n
ea
r
l
y
Sep
te
m
b
er
i
n
d
ec
r
ea
s
ed
alo
n
g
w
it
h
th
e
i
n
cr
ea
s
i
n
g
air
te
m
p
er
atu
r
e.
Fig
u
r
e
9
.
A
ir
T
em
p
er
at
u
r
e
(
A
)
an
d
A
ir
H
u
m
id
it
y
(
B
)
3
.
3
.
M
e
a
s
ure
m
e
nt
s
o
il
t
e
m
pera
t
u
re
a
nd
hu
m
i
dity
Fig
u
r
e
1
0
s
h
o
w
s
s
o
il
m
o
is
t
u
r
e
an
d
s
o
il
te
m
p
er
atu
r
e.
W
e
f
o
u
n
d
th
e
f
l
u
ctu
a
tio
n
o
f
s
o
il
m
o
is
t
u
r
e
in
d
if
f
er
e
n
t
m
o
n
t
h
s
,
w
it
h
r
an
g
ed
7
-
2
6
%.
Me
an
w
h
ile,
t
h
e
s
o
il
t
e
m
p
er
atu
r
e
r
an
g
ed
f
r
o
m
2
6
-
3
4
º
C
.
I
t
m
ea
n
s
th
a
t
en
v
ir
o
n
m
e
n
tal
f
ac
to
r
s
h
a
v
e
a
n
ef
f
ec
t
o
n
it.
T
h
e
s
o
il
te
m
p
er
atu
r
e
an
d
h
u
m
id
it
y
ar
e
i
m
p
o
r
ta
n
t
in
p
ea
t
ar
ea
s
a
s
a
co
n
tr
o
l o
f
a
w
ea
t
h
er
en
v
ir
o
n
m
en
t.
W
h
e
n
t
h
e
le
v
el
o
f
d
r
o
u
g
h
t
is
h
ig
h
,
t
h
e
p
o
ten
tial
f
o
r
t
h
e
f
i
r
e
w
ill
b
e
ea
s
ier
to
tr
ig
g
er
.
Evaluation Warning : The document was created with Spire.PDF for Python.
C
o
m
p
u
t.
Sci.
I
n
f
.
T
ec
h
n
o
l.
R
ea
ltime
mo
n
ito
r
in
g
fo
r
g
r
o
u
n
d
w
a
ter lev
el
a
n
d
lo
c
a
l c
lima
te
b
a
s
ed
o
n
u
n
ivers
a
l
…
(
R
o
n
y
Teg
u
h
)
75
Fig
u
r
e
1
0
.
So
il M
o
is
to
r
e
(
A
)
an
d
So
il T
em
p
er
atu
r
e
(
B
)
4.
CO
NCLU
SI
O
N
Ou
r
an
al
y
s
es o
f
m
o
n
ito
r
ed
en
v
ir
o
n
m
en
tal
f
ac
to
r
s
s
h
o
w
th
a
t th
e
r
ea
l
-
ti
m
e
m
ea
s
u
r
e
m
e
n
ts
b
y
u
s
i
n
g
th
i
s
eq
u
ip
m
e
n
t
m
an
y
d
ata
w
er
e
co
llected
an
d
co
u
ld
s
e
n
d
to
a
co
m
p
u
ter
-
b
ased
s
y
s
te
m
t
h
r
o
u
g
h
an
A
r
d
u
i
n
o
b
o
ar
d
.
I
n
th
is
w
o
r
k
,
w
e
ca
n
r
ec
o
r
d
an
d
i
n
f
o
r
m
at
io
n
d
is
p
la
y
th
e
lo
ca
l
w
ea
th
er
an
d
co
n
d
itio
n
o
f
g
r
o
u
n
d
w
ater
lev
el
b
y
ar
d
u
p
ea
t
s
en
s
o
r
.
T
h
ese
ar
e
p
r
o
to
ty
p
e
lo
w
co
s
ts
e
s
p
ec
iall
y
m
o
n
ito
r
i
n
g
g
r
o
u
n
d
w
ater
lev
el
in
t
h
e
p
ea
tlan
d
en
v
ir
o
n
m
e
n
t.
O
u
r
s
y
s
te
m
b
u
ilt
th
e
d
ev
elo
p
m
en
t
o
f
lo
w
-
co
s
t
s
e
n
s
o
r
s
a
n
d
o
p
en
-
s
o
u
r
ce
h
ar
d
w
a
r
e
r
ef
er
s
to
p
r
o
v
id
e
r
ea
l
-
ti
m
e
g
r
o
u
n
d
w
ater
le
v
el
m
ea
s
u
r
e
m
en
t
s
at
t
h
e
p
ea
t.
I
n
th
i
s
w
o
r
k
,
d
ata
r
esu
lt
s
estab
lis
h
t
h
at
w
it
h
co
n
s
is
te
n
t
ca
lib
r
atio
n
t
h
e
p
r
o
to
t
y
p
e
ca
n
m
ai
n
tai
n
ac
c
u
r
ate
r
es
u
lts
o
v
e
r
an
e
x
te
n
d
ed
p
er
io
d
o
f
ti
m
e.
W
e
co
n
clu
d
e
th
e
p
r
o
to
ty
p
e
is
u
s
ef
u
l
f
o
r
m
ea
s
u
r
e
lo
ca
l
cli
m
ate
in
p
ea
t
to
r
ec
o
m
m
en
d
lo
n
g
-
ter
m
g
r
o
u
n
d
w
a
te
r
lev
el
m
ea
s
u
r
e
m
en
t.
RE
F
E
R
E
NC
E
S
[1
]
J.
H.
M
.
W
ö
ste
n
,
E.
Cly
m
a
n
s,
S
.
E.
P
a
g
e
,
J.
O.
Riele
y
,
a
n
d
S
.
H.
L
im
in
,
“
P
e
a
t
-
w
a
ter
in
terre
latio
n
sh
i
p
s
in
a
tr
o
p
ica
l
p
e
a
tl
a
n
d
e
c
o
sy
st
e
m
in
S
o
u
t
h
e
a
st
A
sia
,
”
Ca
ten
a
,
v
o
l
.
7
3
,
n
o
.
2
,
p
p
.
2
1
2
–
2
2
4
,
2
0
0
8
,
d
o
i:
1
0
.
1
0
1
6
/j
.
c
a
te
n
a
.
2
0
0
7
.
0
7
.
0
1
0
.
[2
]
G
.
E.
S
u
silo
,
K.
Ya
m
a
m
o
to
,
a
n
d
T
.
I
m
a
i,
“
M
o
d
e
li
n
g
G
ro
u
n
d
w
a
ter
L
e
v
e
l
F
lu
c
tu
a
ti
o
n
i
n
t
h
e
T
ro
p
ica
l
P
e
a
tl
a
n
d
A
re
a
s
u
n
d
e
r
th
e
Ef
fe
c
t
o
f
El
Nin
o
,
”
Pro
c
e
d
ia
E
n
v
iro
n
.
S
c
i.
,
v
o
l.
1
7
,
p
p
.
1
1
9
–
1
2
8
,
2
0
1
3
,
d
o
i:
1
0
.
1
0
1
6
/j
.
p
ro
e
n
v
.
2
0
1
3
.
0
2
.
0
1
9
.
[3
]
M
.
T
a
u
f
ik
,
A
.
A
.
V
e
ld
h
u
ize
n
,
J.
H.
M
.
W
ö
ste
n
,
a
n
d
H.
A
.
J.
v
a
n
L
a
n
e
n
,
“
Ex
p
lo
ra
ti
o
n
o
f
th
e
im
p
o
r
tan
c
e
o
f
p
h
y
sic
a
l
p
ro
p
e
rti
e
s
o
f
In
d
o
n
e
sia
n
p
e
a
tl
a
n
d
s
to
a
ss
e
ss
c
rit
ica
l
g
ro
u
n
d
w
a
ter
tab
le
d
e
p
t
h
s,
a
ss
o
c
iate
d
d
r
o
u
g
h
t
a
n
d
f
ire
h
a
z
a
rd
,
”
Ge
o
d
e
rm
a
,
v
o
l.
3
4
7
,
n
o
.
F
e
b
ru
a
ry
,
p
p
.
1
6
0
–
1
6
9
,
2
0
1
9
,
d
o
i:
1
0
.
1
0
1
6
/j
.
g
e
o
d
e
rm
a
.
2
0
1
9
.
0
4
.
0
0
1
.
[4
]
S
.
S
u
n
d
a
ri,
T
.
Hira
n
o
,
H.
Ya
m
a
d
a
,
K.
Ku
sin
,
a
n
d
S
.
L
im
in
,
“
Eff
e
c
t
Of
G
ro
u
n
d
w
a
ter
L
e
v
e
l
On
S
o
i
l
Re
sp
iratio
n
I
n
T
ro
p
ica
l
P
e
a
t
S
w
a
m
p
F
o
re
sts,”
J
.
Ag
ric
.
M
e
teo
ro
l.
,
v
o
l.
6
8
,
n
o
.
2
,
p
p
.
1
2
1
–
1
3
4
,
2
0
1
2
,
d
o
i:
1
0
.
2
4
8
0
/a
g
r
m
e
t.
6
8
.
2
.
6
.
[5
]
N.
C.
Da
d
a
p
,
A
.
R.
Co
b
b
,
A
.
M
.
Ho
y
t,
C.
F
.
Ha
r
v
e
y
,
a
n
d
A
.
G
.
Ko
n
in
g
s,
“
S
a
telli
te
so
il
m
o
istu
re
o
b
s
e
rv
a
ti
o
n
s
p
re
d
ict
b
u
r
n
e
d
a
re
a
in
S
o
u
th
e
a
st
A
sia
n
p
e
a
tl
a
n
d
s,”
En
v
iro
n
.
Res
.
L
e
tt
.
,
v
o
l.
1
4
,
n
o
.
9
,
2
0
1
9
,
d
o
i
:
1
0
.
1
0
8
8
/1
7
4
8
-
9
3
2
6
/ab
3
8
9
1
.
[6
]
E.
I.
P
UT
R
A
,
“
T
h
e
e
ff
e
c
t
o
f
th
e
p
re
c
ip
it
a
ti
o
n
p
a
tt
e
rn
o
f
th
e
d
ry
s
e
a
so
n
o
n
p
e
a
t
f
ire
o
c
c
u
rre
n
c
e
in
th
e
M
e
g
a
Rice
P
r
o
jec
t
a
re
a
,
Ce
n
tral
Ka
li
m
a
n
tan
,
In
d
o
n
e
sia
,
”
T
r
o
p
ics
,
v
o
l.
1
9
,
n
o
.
4
,
p
p
.
1
4
5
–
1
5
6
,
2
0
1
1
,
d
o
i:
1
0
.
3
7
5
9
/
tro
p
ics
.
1
9
.
1
4
5
.
[7
]
C.
J.
W
a
tras
e
t
a
l.
,
“
Ev
a
lu
a
ti
o
n
o
f
w
irele
s
s
se
n
so
r
n
e
tw
o
rk
s
(
W
S
Ns
)
f
o
r
re
m
o
te
we
tl
a
n
d
m
o
n
it
o
ri
n
g
:
De
sig
n
a
n
d
in
it
ial
re
su
l
ts,”
En
v
iro
n
.
M
o
n
it
.
A
ss
e
ss
,
v
o
l.
1
8
6
,
n
o
.
2
,
p
p
.
9
1
9
–
9
3
4
,
2
0
1
4
,
d
o
i:
1
0
.
1
0
0
7
/s
1
0
6
6
1
-
0
1
3
-
3
4
2
4
-
8.
[8
]
M
.
A
.
Na
siru
d
i
n
,
U.
N.
Za’
b
a
h
,
a
n
d
O.
S
id
e
k
,
“
F
re
sh
w
a
ter
re
a
l
-
t
im
e
m
o
n
it
o
rin
g
sy
ste
m
b
a
se
d
o
n
w
irele
ss
se
n
so
r
n
e
tw
o
rk
a
n
d
G
S
M
,
”
2
0
1
1
IE
EE
Co
n
f
.
Op
e
n
S
y
st.
ICOS
2
0
1
1
,
n
o
.
S
e
p
tem
b
e
r,
p
p
.
3
5
4
–
3
5
7
,
2
0
1
1
,
d
o
i:
1
0
.
1
1
0
9
/ICO
S
.
2
0
1
1
.
6
0
7
9
2
9
0
.
[9
]
J.
G
u
ti
e
rre
z
,
J.
F
.
V
il
la
-
M
e
d
in
a
,
A
.
Nie
to
-
G
a
rib
a
y
,
a
n
d
M
.
A
.
P
o
rt
a
-
Ga
n
d
a
ra
,
“
A
u
to
m
a
t
e
d
irri
g
a
ti
o
n
sy
s
te
m
u
sin
g
a
w
irele
ss
se
n
so
r
n
e
tw
o
rk
a
n
d
G
P
RS
m
o
d
u
le,”
IEE
E
T
r
a
n
s.
In
stru
m.
M
e
a
s.
,
v
o
l.
6
3
,
n
o
.
1
,
p
p
.
1
6
6
–
1
7
6
,
2
0
1
4
,
d
o
i
:
1
0
.
1
1
0
9
/T
IM
.
2
0
1
3
.
2
2
7
6
4
8
7
.
[1
0
]
Y.
S
h
ig
e
n
a
g
a
,
H.
T
a
k
a
h
a
sh
i,
R.
T
e
g
u
h
,
a
n
d
W
.
Ke
n
c
a
n
a
,
“
F
ield
Da
ta
T
ra
n
s
m
issio
n
S
y
ste
m
,
S
ES
A
M
E
-
S
A
T
REP
S
,
b
y
Us
in
g
Ce
ll
-
p
h
o
n
e
s
Dig
it
a
l
Tele
c
o
m
m
u
n
ica
ti
o
n
s
Ne
tw
o
rk
,
”
Pro
c
.
S
y
mp
.
W
il
d
fi
re
Ca
rb
o
n
M
a
n
a
g
.
Pea
t
Fo
r
.
In
d
o
n
e
sia
,
n
o
.
M
a
y
2
0
1
4
,
p
p
.
2
0
7
–
2
1
2
,
2
0
1
3
,
d
o
i:
DO
I:
1
0
.
1
3
1
4
0
/
RG
.
2
.
1
.
1
6
2
7
.
0
8
8
5
.
[1
1
]
P
.
Jia
n
g
,
H.
X
ia,
Z.
He
,
a
n
d
Z.
W
a
n
g
,
“
De
sig
n
o
f
a
w
a
ter
e
n
v
iro
n
m
e
n
t
m
o
n
it
o
ri
n
g
sy
ste
m
b
a
se
d
o
n
w
irele
ss
s
e
n
so
r
n
e
tw
o
rk
s,”
S
e
n
so
rs
,
v
o
l.
9
,
n
o
.
8
,
p
p
.
6
4
1
1
–
6
4
3
4
,
2
0
0
9
,
d
o
i:
1
0
.
3
3
9
0
/s9
0
8
0
6
4
1
1
.
[1
2
]
M
.
T
.
L
a
z
a
re
sc
u
,
“
De
si
g
n
o
f
a
W
S
N
p
latf
o
rm
f
o
r
lo
n
g
-
term
e
n
v
iro
n
m
e
n
tal
m
o
n
it
o
rin
g
f
o
r
I
o
T
a
p
p
li
c
a
ti
o
n
s,”
IEE
E
J
.
Eme
rg
.
S
e
l.
T
o
p
.
C
irc
u
it
s S
y
st.
,
v
o
l.
3
,
n
o
.
1
,
p
p
.
4
5
–
5
4
,
2
0
1
3
,
d
o
i:
1
0
.
1
1
0
9
/JET
CA
S
.
2
0
1
3
.
2
2
4
3
0
3
2
.
[1
3
]
Y.
N.
M
a
lek
e
t
a
l.
,
“
O
n
th
e
u
se
o
f
Io
T
a
n
d
Big
Da
ta
Tec
h
n
o
lo
g
ies
f
o
r
Re
a
l
-
ti
m
e
M
o
n
it
o
ri
n
g
a
n
d
Da
ta
P
r
o
c
e
ss
in
g
,
”
Pro
c
e
d
ia
C
o
mp
u
t.
S
c
i.
,
v
o
l.
1
1
3
,
p
p
.
4
2
9
–
4
3
4
,
2
0
1
7
,
d
o
i:
1
0
.
1
0
1
6
/j
.
p
ro
c
s.
2
0
1
7
.
0
8
.
2
8
1
.
Evaluation Warning : The document was created with Spire.PDF for Python.
I
SS
N
:
2722
-
3221
C
o
m
p
u
t.
Sci.
I
n
f
.
T
ec
h
n
o
l.
,
Vo
l.
2
,
No
.
2
,
J
u
l
y
20
2
1
:
6
7
–
7
6
76
[1
4
]
C.
D.
M
o
re
n
o
-
M
o
re
n
o
,
M
.
Br
o
x
-
Jim
é
n
e
z
,
A
.
A
.
Ge
rsn
o
v
iez
-
M
il
la,
M
.
M
á
rq
u
e
z
-
M
o
y
a
n
o
,
M
.
A
.
Ortiz
-
L
ó
p
e
z
,
a
n
d
F
.
J.
Qu
il
e
s
-
L
a
to
rre
,
“
W
irele
s
s
S
e
n
so
r
Ne
tw
o
rk
f
o
r
S
u
sta
in
a
b
le
A
g
ric
u
lt
u
re
,
”
Pr
o
c
e
e
d
in
g
s
,
v
o
l.
2
,
n
o
.
2
0
,
p
.
1
3
0
2
,
2
0
1
8
,
d
o
i:
1
0
.
3
3
9
0
/p
r
o
c
e
e
d
in
g
s2
2
0
1
3
0
2
.
[1
5
]
A
.
A
l
k
a
n
d
a
ri,
“
W
irele
s
s S
e
n
so
r
Ne
tw
o
rk
(
W
S
N)
f
o
r
W
a
ter M
o
n
it
o
r
in
g
S
y
st
e
m
:
Ca
s
e
S
tu
d
y
o
f
Ku
wa
i
t
Be
a
c
h
e
s,”
…
J
.
Dig
it
.
I
n
f.
W
ire
l.
…
,
v
o
l
.
1
,
n
o
.
4
,
p
p
.
7
0
9
–
7
1
7
,
2
0
1
1
,
[
On
li
n
e
].
A
v
a
il
a
b
le:
h
tt
p
:/
/s
d
iw
c
.
n
e
t/
d
ig
it
a
l
-
li
b
ra
ry
/
w
irele
ss
-
se
n
so
r
-
n
e
tw
o
rk
-
w
sn
-
f
o
r
-
w
a
ter
-
m
o
n
it
o
rin
g
-
sy
ste
m
-
c
a
se
-
stu
d
y
-
of
-
k
u
w
a
it
-
b
e
a
c
h
e
s.
[1
6
]
A
.
G
ló
ria,
F
.
Ce
rc
a
s,
a
n
d
N.
S
o
u
t
o
,
“
De
sig
n
a
n
d
im
p
lem
e
n
tatio
n
o
f
a
n
Io
T
g
a
tew
a
y
to
c
re
a
te
s
m
a
rt
e
n
v
iro
n
m
e
n
ts,”
Pro
c
e
d
ia
C
o
mp
u
t.
S
c
i.
,
v
o
l.
1
0
9
,
p
p
.
5
6
8
–
5
7
5
,
2
0
1
7
,
d
o
i:
1
0
.
1
0
1
6
/j
.
p
ro
c
s.
2
0
1
7
.
0
5
.
3
4
3
.
[1
7
]
J.
Do
sh
i,
T
.
P
a
tel,
a
n
d
S
.
K.
B
h
a
rti
,
“
S
m
a
rt
F
a
n
n
in
g
u
sin
g
Io
T
,
a
so
lu
ti
o
n
f
o
r
o
p
ti
m
a
ll
y
m
o
n
it
o
rin
g
f
a
n
n
in
g
c
o
n
d
i
ti
o
n
s,”
Pro
c
e
d
i
a
Co
m
p
u
t
.
S
c
i.
,
v
o
l.
1
6
0
,
p
p
.
7
4
6
–
7
5
1
,
2
0
1
9
,
d
o
i:
1
0
.
1
0
1
6
/
j.
p
r
o
c
s.2
0
1
9
.
1
1
.
0
1
6
.
[1
8
]
D.
W
e
i,
P
.
L
iu
,
B
.
L
u
,
a
n
d
Z.
G
u
o
,
“
W
a
ter
q
u
a
li
ty
a
u
to
m
a
ti
c
m
o
n
it
o
rin
g
sy
ste
m
b
a
s
e
d
o
n
G
P
RS
d
a
ta
c
o
m
m
u
n
ica
ti
o
n
s,”
Pro
c
e
d
ia
En
g
.
,
v
o
l.
2
8
,
n
o
.
2
0
1
1
,
p
p
.
8
4
0
–
8
4
3
,
2
0
1
2
,
d
o
i:
1
0
.
1
0
1
6
/j
.
p
ro
e
n
g
.
2
0
1
2
.
0
1
.
8
2
0
.
[1
9
]
Y.
W
a
n
g
,
C.
Qi,
a
n
d
H.
P
a
n
,
“
De
sig
n
o
f
re
m
o
te m
o
n
it
o
rin
g
sy
ste
m
f
o
r
a
q
u
a
c
u
lt
u
re
c
a
g
e
s b
a
se
d
o
n
3
G
n
e
t
w
o
rk
s a
n
d
A
RM
-
A
n
d
ro
id
e
m
b
e
d
d
e
d
sy
ste
m
,
”
Pro
c
e
d
ia
E
n
g
.
,
v
o
l
.
2
9
,
p
p
.
7
9
–
8
3
,
2
0
1
2
,
d
o
i:
1
0
.
1
0
1
6
/j
.
p
ro
e
n
g
.
2
0
1
1
.
1
2
.
6
7
2
.
[2
0
]
E.
M
.
S
r
o
c
z
a
n
a
n
d
A
.
Urb
a
n
iak
,
“
Ultras
o
n
ic
F
l
o
w
M
e
a
su
re
f
o
r
Wate
r
a
n
d
W
a
ste
wa
ter
Us
in
g
Op
e
n
Ch
a
n
n
e
l
W
e
ir,
”
IFA
C
Pro
c
.
V
o
l.
,
v
o
l.
2
7
,
n
o
.
3
,
p
p
.
1
3
5
–
1
4
0
,
1
9
9
4
,
d
o
i:
1
0
.
1
0
1
6
/s
1
4
7
4
-
6
6
7
0
(
1
7
)
4
6
0
9
8
-
8.
[2
1
]
M
.
R.
L
a
sk
a
r,
R.
Bh
a
tt
a
c
h
a
rjee
,
M
.
S
.
G
iri
,
a
n
d
P
.
B
h
a
tt
a
c
h
a
ry
a
,
“
W
e
a
th
e
r
F
o
re
c
a
stin
g
U
sin
g
A
rd
u
i
n
o
Ba
se
d
Cu
b
e
-
S
a
t,
”
Pro
c
e
d
ia
Co
mp
u
t.
S
c
i.
,
v
o
l.
8
9
,
p
p
.
3
2
0
–
3
2
3
,
2
0
1
6
,
d
o
i:
1
0
.
1
0
1
6
/j
.
p
r
o
c
s.2
0
1
6
.
0
6
.
0
7
8
.
[2
2
]
B.
A
k
h
m
e
to
v
a
n
d
M
.
A
it
im
o
v
,
“
Da
ta
c
o
ll
e
c
ti
o
n
a
n
d
a
n
a
ly
sis
u
sin
g
th
e
m
o
b
il
e
a
p
p
l
ica
ti
o
n
f
o
r
e
n
v
iro
n
m
e
n
tal
m
o
n
it
o
rin
g
,
”
Pro
c
e
d
i
a
C
o
mp
u
t.
S
c
i.
,
v
o
l.
5
6
,
n
o
.
1
,
p
p
.
5
3
2
–
5
3
7
,
2
0
1
5
,
d
o
i:
1
0
.
1
0
1
6
/j
.
p
ro
c
s.
2
0
1
5
.
0
7
.
2
4
7
.
[2
3
]
S
.
Ky
i
a
n
d
A
.
Tap
a
ru
g
ss
a
n
a
g
o
rn
,
“
W
irele
s
s
S
e
n
sin
g
f
o
r
a
S
o
lar
P
o
w
e
r
S
y
ste
m
,
”
Dig
it
.
Co
mm
u
n
.
Ne
two
rk
s
,
v
o
l.
6
,
n
o
.
1
,
p
p
.
5
1
–
5
7
,
2
0
1
9
,
d
o
i:
1
0
.
1
0
1
6
/j
.
d
c
a
n
.
2
0
1
8
.
1
1
.
0
0
2
.
[2
4
]
W
.
P
ri
h
a
rti
,
A
.
F
.
K.
R
o
sm
a
wa
ti
,
a
n
d
I
.
P
.
D.
W
ib
a
w
a
,
“
Io
T
b
a
se
d
p
h
o
to
v
o
lt
a
ic
m
o
n
it
o
ri
n
g
sy
ste
m
a
p
p
li
c
a
ti
o
n
,
”
J
.
Ph
y
s.
Co
n
f.
S
e
r.
,
v
o
l.
1
3
6
7
,
n
o
.
1
,
2
0
1
9
,
d
o
i:
1
0
.
1
0
8
8
/1
7
4
2
-
6
5
9
6
/1
3
6
7
/1
/
0
1
2
0
6
9
.
[2
5
]
T
.
Ka
u
r,
J.
G
a
m
b
h
ir
a
n
d
S
.
Ku
m
a
r,
"
A
rd
u
in
o
b
a
se
d
so
lar p
o
w
e
re
d
b
a
tt
e
ry
c
h
a
rg
in
g
s
y
ste
m
f
o
r
ru
ra
l
S
HS,
"
2
0
1
6
7
t
h
In
d
ia
I
n
tern
a
ti
o
n
a
l
C
o
n
f
e
re
n
c
e
o
n
P
o
w
e
r
El
e
c
tro
n
ics
(IIC
P
E),
P
a
t
iala
,
2
0
1
6
,
p
p
.
1
-
5
,
d
o
i
:
1
0
.
1
1
0
9
/IIC
P
E.
2
0
1
6
.
8
0
7
9
3
7
3
.
Evaluation Warning : The document was created with Spire.PDF for Python.