Estimating ocean surface currents accurately is crucial for a wide range of applications,
including marine navigation, environmental monitoring, and coastal management. Traditional
methods for measuring surface currents face challenges such as limited spatial coverage
and sensitivity to environmental noise, making the development of more accurate and robust
techniques a pressing need in oceanography. This thesis focuses on improving the accuracy
and robustness of ocean surface current estimation using X-band radar image sequences by
introducing two novel algorithms.
In the first part of this thesis, a Symmetry of Doppler Shifts (SDS) method is introduced
for retrieving surface current information from radar images. The method focuses
on extracting the wave angular frequencies and corresponding wavenumbers from the radar
image sequences. Then, Doppler shifts are calculated based on wavevectors that exhibit
symmetry with respect to the origin in the wavenumber plane. These Doppler shifts are
used to estimate both the speed and direction of surface currents. Simulations with synthetic
data show that the SDS method achieves a root mean square error (RMSE) of 0.13
m/s for current speed and 1.4° for direction. The results indicate that the method performs
with accuracy comparable to existing techniques under simulated conditions.
The second part of this research builds on the SDS method by integrating it with an
enhanced Polar Current Shell (PCS) algorithm. The improvements include the application of
Kernel Density Estimation (KDE) for noise filtering, interquartile range filtering to remove
outliers, and symmetry-based noise reduction. The modified PCS method also employs
a single curve-fitting process, analyzing all wavenumbers in the PCS domain collectively
rather than individually. The improved algorithm was validated with both simulated data
and real-world radar data from a Decca radar (2008) and a Koden radar (2017). Results
show that the modified PCS method reduces the RMSE for speed by 0.06 m/s and direction
by 3.8° for the Decca radar, and by 0.02 m/s for speed and 4.6° for direction for the Koden
radar, compared to the original PCS method
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