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Related Pages
Related Symbols
StandardOceanData
GeoElevationData
Quantity
Entity
GeoPosition
Related Categories
Geography
Data Science
Salinity of Seawater at Different Depths
Visualize deviations from the standard average value
Example Notebook
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Use
S
t
a
n
d
a
r
d
O
c
e
a
n
D
a
t
a
to compute an array of values of salinity anomaly along the 180
°
E meridian for depths ranging from 0 to 6000 meters, assuming a constant temperature of 15
°
C:
I
n
[
1
]
:
=
a
n
o
m
a
l
y
=
T
a
b
l
e
[
{
l
a
t
,
Q
u
a
n
t
i
t
y
[
-
d
,
"
M
e
t
e
r
s
"
]
,
S
t
a
n
d
a
r
d
O
c
e
a
n
D
a
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[
"
P
o
s
i
t
i
o
n
"
G
e
o
P
o
s
i
t
i
o
n
[
{
l
a
t
,
1
8
0
}
]
,
"
P
r
e
s
s
u
r
e
"
Q
u
a
n
t
i
t
y
[
d
,
"
D
e
c
i
b
a
r
s
"
]
,
"
T
e
m
p
e
r
a
t
u
r
e
"
Q
u
a
n
t
i
t
y
[
1
5
,
"
D
e
g
r
e
e
s
C
e
l
s
i
u
s
"
]
,
"
A
b
s
o
l
u
t
e
S
a
l
i
n
i
t
y
A
n
o
m
a
l
y
"
]
}
,
{
l
a
t
,
-
8
5
,
6
5
,
5
}
,
{
d
,
0
,
6
0
0
0
,
5
0
}
]
;
Display the data. The highest deviations from the standard average value of 35.2 g/kg are found for larger latitudes:
I
n
[
2
]
:
=
a
n
o
m
a
l
y
P
l
o
t
=
L
i
s
t
D
e
n
s
i
t
y
P
l
o
t
[
F
l
a
t
t
e
n
[
a
n
o
m
a
l
y
,
1
]
,
C
o
l
o
r
F
u
n
c
t
i
o
n
"
T
e
m
p
e
r
a
t
u
r
e
M
a
p
"
,
F
r
a
m
e
L
a
b
e
l
{
"
l
a
t
i
t
u
d
e
"
,
"
e
l
e
v
a
t
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o
n
"
}
,
P
l
o
t
L
e
g
e
n
d
s
A
u
t
o
m
a
t
i
c
,
I
m
a
g
e
S
i
z
e
M
e
d
i
u
m
]
O
u
t
[
2
]
=
Next use
G
e
o
E
l
e
v
a
t
i
o
n
D
a
t
a
to obtain an elevation profile of the sea floor along the same meridian:
I
n
[
3
]
:
=
d
e
p
t
h
s
=
G
e
o
E
l
e
v
a
t
i
o
n
D
a
t
a
[
G
e
o
P
o
s
i
t
i
o
n
[
T
a
b
l
e
[
{
l
a
t
,
1
8
0
}
,
{
l
a
t
,
-
8
5
,
6
5
,
0
.
1
}
]
]
,
U
n
i
t
S
y
s
t
e
m
"
M
e
t
r
i
c
"
]
;
Superimpose the elevation profile onto the anomaly plot:
I
n
[
4
]
:
=
d
e
p
t
h
s
P
l
o
t
=
L
i
s
t
P
l
o
t
T
r
a
n
s
p
o
s
e
[
{
R
a
n
g
e
[
-
8
5
,
6
5
,
0
.
1
]
,
d
e
p
t
h
s
}
]
,
;
S
h
o
w
[
a
n
o
m
a
l
y
P
l
o
t
,
d
e
p
t
h
s
P
l
o
t
]
O
u
t
[
4
]
=
Related Symbols
StandardOceanData
GeoElevationData
Quantity
Entity
GeoPosition
Publisher Information
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Wolfram Staff