-
I/)
Q)
.2 32.830
(ij
E
.(3
Q)
~
Q)
"0
::J
...
~ 32.81
....J
-
I
\ 9 ~
I/)
1 0
. 68
0
0.590
Q)
::J
0
O'.te_OJ>8
0.585 (J)
Ql
0.580
:r
0.575~
.(3
Q)
"0
"0
0.570 ~
- Q)
........
"0
0.565
::J
-
0.560
:.=
......--....
0.555
Longitude (decimal values)
Longitude (decimal values)
Fig. S. Areal distributions of salinity (in practical salinity units) near the Fuliya saline spring off the western shore of Lake
Kinneret. Data from a water depth of 1.5 m was collected by the D-TDMS operated along several transects parallel to the
shoreline 50 to 100 m apart from each other. Variations in salinity, given as practical salinity units (PSU,) are shown on a
gradual gray scale for the studied area, whereas the lake cost line
is presented by a contour line. The location of the Fuliya
Spring is shown bv a circle
-.)
+>
~
CIl
"
~
=
~
~
~
I/)
Q)
.2 32.830
(ij
E
.(3
Q)
~
Q)
"0
::J
...
~ 32.81
....J
-
I
\ 9 ~
I/)
1 0
. 68
0
0.590
Q)
::J
0
O'.te_OJ>8
0.585 (J)
Ql
0.580
:r
0.575~
.(3
Q)
"0
"0
0.570 ~
- Q)
........
"0
0.565
::J
-
0.560
:.=
......--....
0.555
Longitude (decimal values)
Longitude (decimal values)
Fig. S. Areal distributions of salinity (in practical salinity units) near the Fuliya saline spring off the western shore of Lake
Kinneret. Data from a water depth of 1.5 m was collected by the D-TDMS operated along several transects parallel to the
shoreline 50 to 100 m apart from each other. Variations in salinity, given as practical salinity units (PSU,) are shown on a
gradual gray scale for the studied area, whereas the lake cost line
is presented by a contour line. The location of the Fuliya
Spring is shown bv a circle
-.)
+>
~
CIl
"
~
=
~
~
~