Zakharchuk: Internal Waves in the Laptev Sea
27
north·east
200
400
600
800
1000
1"C
1200
1400
1600
1800
a
2000
H,m
S t a t i o n s
32 31 30 29 29a 25 26
27
north·east
200 ~~~~~~~~~::~~~~~~~::====--~
400
600
800
1000
1200
1400
1600
1800
2000
H, m
Figure 4: Vertical profiles of temperature (a) and salinity (b) on stations of section E.
Summary
49
This study describes an observations of high-frequency internal gravity waves in the seasonal
pycnocline in the Laptev Sea. The principal conclusions are as follows:
High-frequency internal waves having frequensies close to the Brunt-Viiisiilii frequency are
observed in the different regions of the Laptev Sea.
27
north·east
200
400
600
800
1000
1"C
1200
1400
1600
1800
a
2000
H,m
S t a t i o n s
32 31 30 29 29a 25 26
27
north·east
200 ~~~~~~~~~::~~~~~~~::====--~
400
600
800
1000
1200
1400
1600
1800
2000
H, m
Figure 4: Vertical profiles of temperature (a) and salinity (b) on stations of section E.
Summary
49
This study describes an observations of high-frequency internal gravity waves in the seasonal
pycnocline in the Laptev Sea. The principal conclusions are as follows:
High-frequency internal waves having frequensies close to the Brunt-Viiisiilii frequency are
observed in the different regions of the Laptev Sea.
