Propagation of acoustic signals along a range-dependent track in the A
rctic Basin is considered. The form of a model pulse is compared with
the wave form obtained in acoustic monitoring in the Arctic Basin. Cal
culations were carried out with a program based on the coupled mode me
thod. This program takes into account the hydroacoustic waveguide para
meters affecting the amplitude-time signal structure. This allowance y
ielded a satisfactory agreement between calculations and the experimen
t. The effect of hydrological factors on the sound held structure and
characteristics of separate modes are considered. This consideration a
llows us to determine the trend of temperature changes of the Atlantic
waters intruding in the Arctic Basin and temperature changes in the u
pper water layer.