http://www.loc.gov/mods/v3 http://www.loc.gov/standards/mods/v3/mods-3-2.xsd
Nonlinear Ocean Dynamics: Synthetic Aperture Radar delivers the critical tools needed to understand the latest technology surrounding the radar imaging of nonlinear waves, particularly microwave radar, as a main source to understand, analyze and apply concepts in the field of ocean dynamic surface.
Intro -- Nonlinear Ocean Dynamics: Synthetic Aperture Radar -- Copyright -- Dedication -- Contents -- Preface -- Chapter 1: Nonlinear ocean motion equations: Introduction and overview -- 1.1. Introduction -- 1.2. What is meant by ocean dynamics? -- 1.3. What is meant by nonlinear? -- 1.4. Classification of ocean dynamic flows -- 1.4.1. Steady flow -- 1.4.2. Incompressible flow -- 1.4.3. Irrotational flow -- 1.4.4. Vorticity -- 1.5. Ocean dynamic circulation -- 1.6. What is the difference between circulation and vorticity? -- 1.7. Primitive equation of ocean dynamics -- 1.7.1. Continuity equations -- 1.7.2. Stream function based on continuity equations -- 1.7.3. Equation of continuity by the Lagrangian and Eulerian descriptions -- 1.8. Navier-Stokes equations -- 1.8.1. What are the Navier-Stokes equations? -- 1.8.2. The Navier-Stokes equations -- 1.8.3. Conservation of energy -- 1.8.4. Time domain -- 1.8.5. Compressibility -- 1.8.6. Low and high Reynolds numbers -- 1.9. Turbulence -- 1.10. Equations of motion in a rotating frame -- 1.11. Conservation equation of ocean waves -- 1.12. Water level exchange and water flow -- 1.12.1. The alternating direction implicit (ADI) method -- 1.13. Dispersion relation for water waves -- 1.14. Nonlinear water flow and wave propagation -- 1.15. Energy equation of fluid flow -- References -- Chapter 2: Quantization of ocean dynamics -- 2.1. Seawater quantum molecules -- 2.2. Ocean dynamics mimic quantum mechanics -- 2.3. Similarities and differences between quantum field theory and ocean dynamics -- 2.4. Quantum spin of seawater -- 2.5. Kitaev spin seawaters -- 2.6. Hamiltonian mechanics for ocean dynamics -- 2.7. Incompressible flow with Schrödinger equations -- 2.8. Quantum mechanics of Coriolis force -- 2.9. Quantization of barotropic flow -- 2.10. Quantization of vorticity flow -- 2.11. Quantum turbulence.
2.12. Particle theory of ocean waves -- 2.13. Schrödinger equation for description of nonlinear Sea-state -- 2.14. Hamiltonian formulation for water wave equation -- References -- Chapter 3: Quantization of synthetic aperture microwave radar -- 3.1. Quantize concept of aperture -- 3.2. Aperture antenna -- 3.3. Quantization of electromagnetic wave and Maxwell's equations -- 3.4. Microwave radar photons -- 3.5. Microwave cavity main concept -- 3.6. Microwave photon generation by Josephson junctions -- 3.7. Radar systems -- 3.8. What is meant by echolocation detecting and ranging? -- 3.9. Why quantum synthetic aperture radar is necessary -- 3.10. What is meant by quantum SAR? -- 3.11. What are the classifications of quantum SAR? -- 3.12. Classical and quantum radar equations -- 3.13. Quantum SAR illumination -- 3.14. Quantum theory of SAR system -- 3.14.1. Transmitter -- 3.14.2. Receiver -- References -- Chapter 4: Quantum mechanism of nonlinear ocean surface backscattering -- 4.1. What is meant by scattering? -- 4.2. Comparison between coherent and incoherent multiple scattering -- 4.3. What is the role of spin in understanding scattering? -- 4.4. Spin of scattering of particles -- 4.5. Scattering of identical particles -- 4.6. Schrödinger equation for scattering particles -- 4.7. How do the Lippmann-Schwinger equation and the scattering amplitude generalize when spin is included? -- 4.8. Seawater atom-photon scattering -- 4.9. Scattering from roughness surface -- 4.10. Mathematical depiction of SAR backscattering cross-section -- 4.11. Wave function of SAR backscattering cross-section -- 4.12. Quantization of Bragg scattering -- References -- Chapter 5: Relativistic quantum mechanics of ocean surface dynamic in synthetic aperture radar -- 5.1. What is meant by relativity? -- 5.2. Relativistic quantum mechanics versus ordinary quantum mechanics.
5.3. SAR backscatter in relativistic quantum mechanics -- 5.4. Duality of wave packages in relativistic quantum mechanics -- 5.5. Relativities of SAR time pulse range traveling -- 5.6. SAR space-time invariance interval -- 5.7. How is quantum entanglement consistent with the time relativity? -- 5.8. SAR time dilation -- 5.9. SAR length contraction in polarized data -- References -- Chapter 6: Novel relativistic theories of ocean wave nonlinearity imagine mechanismin synthetic aperture radar -- 6.1. What is meant by waves and flows? -- 6.2. Description of ocean waves -- 6.3. How sea waves are formed based on Spooky Action at a Distance -- 6.4. What is doing the waving? -- 6.5. Hamiltonian formula for nonlinear wave description -- 6.6. SAR image mechanism for ocean wave -- 6.6.1. SAR range processing -- 6.6.2. SAR azimuth distribution processing -- 6.6.3. SAR ocean wave imaging theory -- 6.6.4. Differences between linear and nonlinear backscatters -- 6.6.5. Velocity bunching modulation -- 6.7. Relativistic theory of SAR velocity bunching -- 6.8. Relativistic theory of the ocean wavelength in SAR images -- 6.9. Relativistic theory of incidence angle in SAR wave images -- 6.10. Relativistic theory of range bunching -- References -- Chapter 7: Quantum nonlinear techniques for retrieving ocean wave spectral parameters from synthetic aperture radar -- 7.1. Simplification of the magic concept of SAR Doppler shift frequency -- 7.2. SAR sensors for ocean wave simulation -- 7.3. Sea surface backscatter based on the Kirchhoff approximation -- 7.4. Imaging Ocean wave parameters in single polarization SAR data -- 7.5. How to relate wave fields to SAR images -- 7.6. SAR wave retrieval algorithms -- 7.7. Quantum spectra estimation using quantum Fourier transform -- 7.8. Multilooking and cross-spectral analysis -- 7.9. Quantum Monte Carlo wave spectral simulation.
7.10. SAR wave spectra simulated using diffusion quantum Monte Carlo -- References -- Chapter 8: Polarimetric synthetic aperture radar for wave spectra refraction using inversion SAR wave spectra model -- 8.1. What is meant by polarimetric synthetic aperture radar? -- 8.2. Polarimetric matrix formulations and SAR data representation -- 8.3. The coherency matrix THV (for single-look or multilook) -- 8.4. Circular polarization-based covariance matrix CRL -- 8.5. Estimation of azimuth slopes using orientation angle -- 8.6. Alpha parameter sensitivity to the range of traveling waves -- 8.7. Examined POLSAR and AIRSAR data -- 8.8. Wave spectra model -- 8.9. Two-dimensional quantum Fourier transform for retrieving SAR wave spectra -- 8.10. Quasilinear transform -- 8.11. Modeling significant wave height using azimuth cutoff model -- 8.12. AIRSAR/POLSAR cross-spectrum inversion -- 8.13. Differences between deep and shallow water waves -- 8.14. Quantum of wave refraction -- 8.15. Wave refraction graphical method -- References -- Chapter 9: Wavelet transform and particle swarm optimization algorithms for automatic detection of internal wave from syn ... -- 9.1. Introduction -- 9.2. What is meant by internal wave? -- 9.3. Simplification of internal wave generation mechanisms -- 9.4. Mathematical description of internal waves -- 9.5. Kelvin-Helmholtz instability -- 9.6. Internal wave imaging in SAR -- 9.7. Internal wave radar backscatter cross-section -- 9.8. Internal wave detection using two-dimensional wavelet transform -- 9.9. Particle swarm optimization (PSO) algorithm -- 9.10. Tested SAR data -- 9.11. Backscatter distribution along with internal wave in SAR data -- 9.12. Automatic detection of internal wave using two-dimensional wavelet transform -- 9.13. Internal wave packet detection by PSO -- 9.14. Why do internal waves occur in the Andaman Sea?.