This paper presents the results illustrating temporal fluctuations in the noise power spectrum level of shallow water ambient noise in the bandwidth of 100 Hz to 4 kHz by analyzing its statistical properties. Experiment was conducted to measure the shallow water ambient noise at 25 m depth for a period of 15 hours with an omni-directional hydrophone deployed at 5 m from the sea surface. The data were collected every hour for a period of 1 minute. Wind speed was also measured during the data collection and the variation in wind speed was between 1.5 to 2.5 m/s. The analysis result shows the variation in the average noise spectrum level was found to be higher in the lower (100 Hz to 1 kHz) and higher frequencies (3 kHz to 4 kHz) of the band and found to be almost constant in between.
[1]
G. M. Wenz.
Acoustic Ambient Noise in the Ocean: Spectra and Sources
,
1962
.
[2]
C. L. Piggott.
Ambient Sea Noise at Low Frequencies in Shallow Water of the Scotian Shelf
,
1964
.
[3]
Robert J. Urick,et al.
Principles of underwater sound
,
1975
.
[4]
Robert H. Mellen,et al.
The Thermal‐Noise Limit in the Detection of Underwater Acoustic Signals
,
1952
.
[5]
W. Richardson.
Marine Mammals and Noise
,
1995
.
[6]
Rex K. Andrew,et al.
Underwater Ambient Noise
,
2007
.
[7]
R A Wagstaff.
RANDI: Research Ambient Noise Directionality Model
,
1973
.