Q)
"C
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:.0:;
co
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Turbidity (NTU)
3.9
3.3
2.7
2.1
1.5
i
32.87
32.n
32.75
32.75
32.73
A
32 . . 73
B
32.73
c
32.71-1
1
1
1
i"-;= 1 1
32.71 -1,
,
,
-r---r 1 1
32.71-1,
,
i
r---r , ,
35.52 35.54 35.56 35.58 35.6 35.62 35.64
35.52 35.54 35.56 35.58 35.6 35.62 35.64
35.52 35.54 35.56 35.58 35.6 35.62 35.64
Longitude
Fig. 4 a-c. Horizontal distribution of water turbidity in a depth layer of 2 m in Lake Kinneret, A During the stratification period of
the lake, June 26, 2000. B During the de stratification event, January 16, 2001. C During the restratification process as stable
thermocline established, March 27, 2001. Data were collected by the U-TUMS operated along several west to east transects, 1.5 3 km
apart from each other. Variations in turbidity, given as nephelometric turbidity units (NTU,) are shown on a gradual gray scale for
the studied area, whereas the lake cost line is presented by a contour line
.....
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N
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[/J
c
~
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~
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!=-
"C
::::J
.......
:.0:;
co
.....J
Turbidity (NTU)
3.9
3.3
2.7
2.1
1.5
i
32.87
32.n
32.75
32.75
32.73
A
32 . . 73
B
32.73
c
32.71-1
1
1
1
i"-;= 1 1
32.71 -1,
,
,
-r---r 1 1
32.71-1,
,
i
r---r , ,
35.52 35.54 35.56 35.58 35.6 35.62 35.64
35.52 35.54 35.56 35.58 35.6 35.62 35.64
35.52 35.54 35.56 35.58 35.6 35.62 35.64
Longitude
Fig. 4 a-c. Horizontal distribution of water turbidity in a depth layer of 2 m in Lake Kinneret, A During the stratification period of
the lake, June 26, 2000. B During the de stratification event, January 16, 2001. C During the restratification process as stable
thermocline established, March 27, 2001. Data were collected by the U-TUMS operated along several west to east transects, 1.5 3 km
apart from each other. Variations in turbidity, given as nephelometric turbidity units (NTU,) are shown on a gradual gray scale for
the studied area, whereas the lake cost line is presented by a contour line
.....
-..l
N
?>
[/J
c
~
' "
~
~
!=-
