Compared to radio waves, acoustic waves have become the most effective way in underwater wireless communication [1] . It is because radio waves are highly attenuated and spreading occurs due to high frequency. Hence they can propagate only over very short distances. On the other hand if acoustic waves are used, long distance communication can be established. However underwater wireless communication is still challenging due to frequency band limitation and underwater channel disturbances in the form of ambient noise. The disturbance is generated by both natural (seismic, wind marine animals, rain, breaking waves etc.) and manmade sources (shipping, other machineries etc.). We will discuss ambient noise properties in details and reducing algorithm afterwards [2] - [4] .

Oceans are filled with various types of sound which may be generated by natural or man-made sources. Breaking waves, rain, marine, shrimp, volcanoes, earthquakes can be god examples of natural sources. Ships, military sonars exemplify man made sources.

This background noise present in the ocean is called ambient noise. All types of noise is not present everywhere all the time.

Ambient noise sources can be categorized by frequency. The typical frequency range of various types of ambient noise is shown by Wenz in the Wenz curve [5] . In the range of 20 Hz to 500 Hz, the noise is primarily due to distant shipping. In this range frequency content can be detected even after eliminating other types of shipping noise at the receiver. Moreover it is easy to understand that the noise level expressed in terms of signal power level (SPL) will be greater where shipping traffic is heavier. For example, low frequency ambient noise level is lower in the southern hemisphere as shipping traffic is very low. In the frequency range 0.5 KHz to 100 KHz the noise is mainly due to spray and bubbles associated with breaking waves. In this range noise is proportional to wind speed that is noise level increases with increasing wind speed. Above 100 KHz thermal noise dominates which arises due to random motion of water molecules. Thermal noise determines the ultimate minimum level of sound that can be used for communication purpose in a particular time and location [6] .

Wavelets are mathematical functions which break up the data into different frequency components and hence each frequency component can be studied at different resolution. Wavelet analysis is superior to Fourier analysis in the sense that Fourier analysis is well suited for frequency analysis but if we require time frequency analysis then Fourier analysis becomes useless. That is wavelet analysis provides us with time frequency data of the signal. That is we can determine through wavelet analysis where and at what frequency noise spikes or discontinuities occur. In fine wavelets are specially designed for non-stationary signals which are transient in behavior [7] [8] .

For many signals, the low-frequency content is the most important part as because it contains the information. The high-frequency content, on the other hand, imparts flavor or nuance. Considering the human voice, If we remove the high-frequency components, the voice sounds different, but we can still tell what's being said. However, if we remove enough of the low-frequency components, we hear gibberish. In wavelet analysis, we often speak of approximations and details. The approximations are the high-scale, low-frequency components of the signal. The details are the low-scale, high-frequency components. The thresholding process of wavelet coefficients can be divided into two steps.

The new thresholding method consists of thresholding value estimation and thresholding function design both for detail and approximation coefficients at each level of wavelet decomposition. Detail coefficients carry the original information signal between 8 to 12 KHz range and approximation coefficients carry the noise component. The ambient noise component is dominating in between 1 to 4 KHz range [5] [11] .

As the first step in our proposed thresholding method we offer the new threshold value for detail and approximation coefficients as follows

where,

Threshold value for detail coefficients;

Threshold value for approximation coefficients;

Highest level of decomposition;

Current level of decomposition;

;

Number of approximation coefficients at current level;

Number of detail coefficients at current level.

When data size is large the general thresholding estimation gives under fitted results [7] [8] .

Proposed detail coefficient thresholding function,

Proposed approximation coefficient thresholding function,

where Approximation coefficients at level; Threshold value for approximation coefficients.

In our proposed method we assume a reference signal of 10 KHz frequency. The noise data is provided by MREG, Swansea University, UK. The data was recorded in high tidal current over the board 11/05/2013 at 07.06 am on the West coast of Wales.

The noise reduction algorithm can be described on a step by step basis as follows:

Step1: 10 KHz reference signal is used to produce the noisy signal (noisy signal = Ref. Signal + Noise).

Step 2: A level 8 wavelet Decomposition is performed using discrete wavelet transform (dwt) function.

Step 3: Detail coefficients at level 1 to 8 are modified using proposed thresholding method.

Step 4: Approximation coefficients are at each level are modified using proposed method.

Step 5: Inverse Wavelet Transform is performed to reconstruct the denoised signal.

The algorithm is applied on two sets of noise data to ensure algorithm efficiency.

To proof the efficiency of the proposed thresholding value estimation method and thresholding function, we calculate the SNR, RMSE and PSD of the denoised signal. Table 1 and Table 2 show the result of simulation.

In Table 1 and Table 2 we calculate SNR, RMSE and PSD respectively for wavelet filter types “db2”, “Haar”, “coif1” and “sym4” using hard, soft and proposed thresholding function. For each type of function we have calculated the statistical parameter values using universal and proposed threshold estimation method.

From the above data it is clear that the devised method has produced improved SNR, PSD and lower RMSE for all noise data sets compared with global soft or hard thresholding methods. The PSD of noise signal being almost similar in frequency contents is showing that the noise spectrum have a peak in the lower frequency region as expected with the information signal at higher frequency region showed in Figures 1-5. The soft thresholding function with proposed estimation method has produced improved SNR with lower RMSE specially when noise signal strength is strong. The devised method seems to be efficient for all wavelet filter types applied to this experiment.

The authors would like to thank Mr Merin Broudic, Research Assistant Marine Renewables, Low Carbon Research Institute (LCRI Marine), School of Engineering, Swansea University, UK, for his perpetual support.