Zakfulrchuk: Internal Waves in the Laptev Sea
45
0.000 00:;6 1l~'ON
26..00
26.45
TOC
S
0
p
3.0
330.
a
·,0
2.5
32.5
, . N
·20
2.0
32.0
,
,
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1.5
315
0
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'500
2400
1J(XXl
0
600
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,BOO
2.000
3000
.00'
oen 0.03
,
' N TO C
S
250 260 270
0
0,5
3' 6
·'0
315
00
31.4
·20
, . N 03
3' ,3
.31)
02
3'2
.4)
0.1
3'.1
0
500
1200 1BOO 2400 3000 3600
0
600
'200 '600 2.000 3000 3600
000
002
004
,
,
' N
24
25 26 Z1
rc
S
0
P
2.5
29'
C
·'0
N
2,0.
·20
28.8
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285
'0
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0
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000
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,
, N
26 V
28 29
TOC
S
0
P
05
345
d
·200
0.0
34,0
..:00
, . .0.5
33,5
-600
N
. ,' .0
33.0
·'000
H.m
32.5
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2400
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4600
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Seconds
Seconds
Figure 2: Vertical profiles of density (p, c,u,), Brunt-Viiisiilii frequency (N, sec!) and smal-scale fluctuations of
temperature (TOC) and salinity (S) in the seasonal pycnocline at depths a) 25 m (stations \1), b) IS m (station
14), c) 25 m (station 16 and d) 23 m (station 80) in different points of the Laptev Sea,