Abstract
This chapter delivers a new concept of retrieving sea surface wave spectra from radar images. Quantum nonlinear techniques are discussed and implemented in radar satellite images. In this chapter, diffusion quantum Monte Carlo (DMC) is a technique that makes use of a Green's function characteristic to resolve the Schrödinger equation. DMC can construct the fluctuations of ocean wave surface as a function of the variations image spectral densities owing to the interaction between radar signal energy and sea surface dynamic energy. The greatest common operation of DMC diffusion is matchless controls a renewed experimental function which is also considered as the original state in simulating ocean wave spectral patterns. Finally, for a large projection time, the wave function converges to the lowest state that has an overlap with the trail function. The rapid acceleration of the random walk of DMC, the precise determination of the spectrum peak direction as based on an enhancement phase of the cross-spectrum.
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