
Microwave Radar and Radiometric Remote Sensing
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Content
- Microwave Radar and Radiometric Remote Sensing
- Preface
- Photo Credits
- Computer Codes
- Contents
- Chapter 1 Introduction
- 1-1 Why Microwaves for Remote Sensing?
- 1-2 A Brief Overview of Microwave Sensors
- 1-3 A Short History of Microwave Remote Sensing
- 1-3.1 Radar
- 1-3.2 Radiometers
- 1-4 The Electromagnetic Spectrum
- 1-5 Basic Operation and Applications of Radar
- 1-5.1 Operation of Remote-Sensing Radars
- 1-6 Basic Operation and Applications of Radiometers
- 1-6.1 Radiometer Operation
- 1-6.2 Applications of Microwave Radiometry
- 1-7 Image Examples
- Chapter 2 Electromagnetic Wave Propagation and Reflection
- 2-1 EM Plane Waves
- 2-1.1 Constitutive Parameter
- 2-1.2 Maxwell's Equations
- 2-1.3 Complex Permittivity
- 2-1.4 Wave Equations
- 2-2 Plane-Wave Propagation in Lossless Media
- 2-3 Wave Polarization in a Lossless Medium
- 2-3.1 Linear Polarization
- 2-3.2 Circular Polarization
- 2-3.3 Elliptical Polarization
- 2-4 Plane-Wave Propagation in Lossy Media
- 2-4.1 Low-Loss Dielectric
- 2-4.2 Good Conductor
- 2-5 Electromagnetic Power Density
- 2-5.1 PlaneWave in a Lossless Medium
- 2-5.2 PlaneWave in a Lossy Medium
- 2-5.3 Decibel Scale for Power Ratios
- 2-6 Wave Reflection and Transmission at Normal Incidence
- 2-6.1 Boundary between Lossless Media
- 2-6.2 Boundary between Lossy Media
- 2-7 Wave Reflection and Transmission at Oblique Incidence
- 2-7.1 Horizontal Polarization-Lossless Media
- 2-7.2 Vertical Polarization
- 2-8 Reflectivity and Transmissivity
- 2-9 Oblique Incidence onto a Lossy Medium
- 2-10 Oblique Incidence onto a Two-Layer Composite
- 2-10.1 Input Parameters
- 2-10.2 Propagation Matrix Method
- 2-10.3 Multiple Reflection Method
- PROBLEMS
- Chapter 3 Remote-Sensing Antennas
- 3-1 The Hertzian Dipole
- 3-2 Antenna Radiation Characteristics
- 3-2.1 Antenna Pattern
- 3-2.2 Beam Dimensions
- 3-2.3 Antenna Directivity
- 3-2.4 Antenna Gain
- 3-2.5 Radiation Efficiency
- 3-2.6 Effective Area of a Receiving Antenna
- 3-3 Friis Transmission Formula
- 3-4 Radiation by Large-Aperture Antennas
- 3-5 Rectangular Aperture with Uniform Field Distribution
- 3-5.1 Antenna Pattern in x-y Plane
- 3-5.2 Beamwidth
- 3-5.3 Directivity and Effective Area
- 3-6 Circular Aperture with Uniform Field Illumination
- 3-7 Nonuniform-Amplitude Illumination
- 3-8 Beam Efficiency
- 3-9 Antenna Arrays
- 3-10 N-Element Array with Uniform Phase Distribution
- 3-10.1 Uniform Amplitude Distribution
- 3-10.2 Grating Lobes
- 3-10.3 Binomial Distribution
- 3-11 Electronic Scanning of Arrays
- 3-12 Antenna Types
- 3-12.1 Horn Antennas
- 3-12.2 Slot Antennas
- 3-12.3 Microstrip Antennas
- 3-13 Active Antennas
- 3-13.1 Advantages of Active Antennas
- 3-13.2 Digital Beamforming with Active Antennas
- PROBLEMS
- Chapter 4 Microwave Dielectric Properties of Natural Earth Materials
- 4-1 Pure-Water Single-Debye Dielectric Model ( f = 50 GHz)
- 4-2 Saline-Water Double-Debye Dielectric Model ( f = 1000 GHz)
- 4-3 Dielectric Constant of Pure Ice
- 4-4 Dielectric Mixing Models for Heterogeneous Materials
- 4-4.1 Randomly Oriented Ellipsoidal Inclusions
- 4-4.2 Polder-van Santen/de Loor Formulas
- 4-4.3 Tinga-Voss-Blossey (TVB) Formulas
- 4-4.4 Other Dielectric Mixing Formulas
- 4-5 Sea Ice
- 4-5.1 Dielectric Constant of Brine
- 4-5.2 Brine Volume Fraction
- 4-5.3 Dielectric Properties
- 4-6 Dielectric Constant of Snow
- 4-6.1 Dry Snow
- 4-6.2 Wet Snow
- 4-7 Dielectric Constant of Dry Rocks
- 4-7.1 Powdered Rocks
- 4-7.2 Solid Rocks
- 4-8 Dielectric Constant of Soils
- 4-8.1 Dry Soil
- 4-8.2 Wet Soil
- 4-8.3 esoil in 0.3-1.5 GHz Band
- 4-9 Dielectric Constant of Vegetation
- 4-9.1 Dielectric Constant of Canopy Constituents
- 4-9.2 Dielectric Model
- PROBLEMS
- Chapter 5 Radar Scattering
- 5-1 Wave Polarization in a Spherical Coordinate System
- 5-2 Scattering Coordinate Systems
- 5-2.1 Forward Scattering Alignment (FSA) Convention
- 5-2.2 Backscatter Alignment (BSA)Convention
- 5-3 Scattering Matrix
- 5-3.1 FSA Convention
- 5-3.2 BSA Convention
- 5-4 Radar Equation
- 5-5 Scattering from Distributed Targets
- 5-5.1 Narrow-Beam Scatterometer
- 5-5.2 Imaging Radar
- 5-5.3 Specific Intensities for Distributed Target
- 5-6 RCS Statistics
- 5-7 Rayleigh Fading Model
- 5-7.1 Underlying Assumptions
- 5-7.2 Linear Detection
- 5-7.3 Square-Law Detection
- 5-7.4 Interpretation
- 5-8 Multiple Independent Samples
- 5-8.1 N-Look Amplitude Image
- 5-8.2 N-Look Intensity Image
- 5-8.3 N-Look Square-Root Intensity Image
- 5-8.4 Spatial Resolution vs. Radiometric Resolution
- 5-8.5 Applicability of the Rayleigh FadingModel
- 5-9 Image Texture and DespeckleFiltering
- 5-9.1 Image Texture
- 5-9.2 Despeckling Filters
- 5-10 Coherent and Noncoherent Scattering
- 5-10.1 Surface Roughness
- 5-10.2 Bistatic Scattering
- 5-10.3 Specular Reflectivity
- 5-10.4 Bistatic-Scattering Coefficient
- 5-10.5 Backscattering Response of a Smooth
- 5-11 Polarization Synthesis
- 5-11.1 RCS Polarization Response
- 5-11.2 Distributed Targets
- 5-11.3 Mueller Matrix Approach
- 5-12 Polarimetric Scattering Statistics
- 5-13 Polarimetric Analysis Tools
- 5-13.1 Scattering Covariance Matrix
- 5-13.2 Eigenvector Decomposition
- 5-13.3 Useful Polarimetric Parameters
- 5-13.4 Image Examples
- 5-13.5 Freeman-Durden Decomposition
- Chapter 6 Microwave Radiometry and Radiative Transfer
- 6-1 Radiometric Quantities
- 6-2 Thermal Radiation
- 6-2.1 Quantum Theory of Radiation
- 6-2.2 Planck's Blackbody Radiation Law
- 6-2.3 The Rayleigh-Jeans Law
- 6-3 Power-Temperature
- 6-4 Radiation by Natural Materials
- 6-4.1 Brightness Temperature
- 6-4.2 Brightness Temperature Distribution
- 6-4.3 Antenna Temperature
- 6-5 Antenna Efficiency
- 6-5.1 Beam Efficiency
- 6-5.2 Radiation Efficiency
- 6-5.3 Radiometer Measurement Ambiguity
- 6-6 Theory of Radiative Transfer
- 6-6.1 Equation of Radiative Transfer
- 6-6.2 Brightness-Temperature Equation 6-6.3 Brightness Temperature of a Stratified
- 6-6.4 Brightness Temperature of a Scatter-Free Medium
- 6-6.5 Upwelling and Downwelling
- 6-7 Terrain Brightness Temperature
- 6-7.1 Brightness Transmission Across a
- 6-7.2 Emission by a Specular Surface
- 6-7.3 Emissivity of a Rough Surface
- 6-7.4 Extreme Surface Conditions
- 6-7.5 Emissivity of a Two-Layer Composite
- 6-8 Downward-Looking Satellite
- 6-9 Polarimetric Radiometry
- 6-10 Stokes Parameters and Periodic
- Chapter 7 Microwave Radiometric Systems
- 7-1 Equivalent Noise Temperature
- 7-2 Characterization of Noise
- 7-2.1 Noise Figure
- 7-2.2 Equivalent Input Noise Temperature
- 7-2.3 Noise Temperature of a Cascaded
- 7-2.4 Noise Temperature of a Lossy Two-Port
- 7-3 Receiver and System Noise
- 7-3.1 Receiver Alone
- 7-3.2 Total System Including Antenna
- 7-4 Radiometer Operation
- 7-4.1 Measurement Accuracy
- 7-4.2 Total-Power Radiometer
- 7-4.3 Radiometric Resolution
- 7-5 Effects of Receiver Gain
- 7-6 Dicke Radiometer
- 7-7 Balancing Techniques
- 7-7.1 Reference-Channel Control Method
- 7-7.2 Antenna-Channel Noise-Injection
- 7-7.3 Pulsed Noise-Injection Method
- 7-7.4 Gain-Modulation Method
- 7-8 Automatic-Gain-Control (AGC)
- 7-9 Noise-Adding Radiometer
- 7-10 Summary of Radiometer
- 7-11 Radiometer Calibration
- 7-11.1 Receiver Calibration
- 7-11.2 Calibration Sources
- 7-11.3 Effects of Impedance Mismatches
- 7-11.4 Antenna Calibration
- 7-11.5 Cryoload Technique
- 7-11.6 Bucket Technique
- 7-12 Imaging Considerations
- 7-12.1 Scanning Configurations
- 7-12.2 Radiometer Uncertainty Principle
- 7-13 Interferometric Aperture Synthesis
- 7-13.1 Image Reconstruction
- 7-13.2 MIR Radiometric Sensitivity
- 7-14 Polarimetric Radiometer 7-14.2 Incoherent Detection
- 7-14.1 Coherent Detection
- 7-15 Calibration of Polarimetric
- 7-15.1 Forward Model for a Fully
- 7-15.2 Forward Model for the Polarimetric
- 7-15.3 Calibration by Inversion of the
- 7-16 Digital Radiometers
- Chapter 8 Microwave Interaction with Atmospheric Constituents
- 8-1 Standard Atmosphere
- 8-1.1 Atmospheric Composition
- 8-1.2 Temperature Profile
- 8-1.3 Density Profile 8-1.5 Water-Vapor Density Profile
- 8-1.4 Pressure Profile
- 8-2 Absorption and Emission by
- 8-2.1 Electromagnetic Interaction with Individual Molecules
- 8-2.2 The Shape of a Spectral Line
- 8-2.3 Absorption Spectrum
- 8-2.4 Oxygen Spectrum
- 8-2.5 Water-Vapor Spectrum
- 8-2.6 Total Gaseous Spectrum
- 8-3 Opacity of the Clear Atmosphere
- 8-4 Emission by the Clear
- 8-5 Extinction by Hydrometeors
- 8-5.1 Electromagnetic Interaction with
- 8-5.2 Mie Scattering
- 8-5.3 Rayleigh Approximation
- 8-5.4 Frequency Response
- 8-6 Dielectric Properties of
- 8-6.1 Water Particles
- 8-6.2 Ice Particles
- 8-6.3 Snowflakes
- 8-7 Extinction and Backscattering by Clouds, Fog, or Haze
- 8-7.1 Drop-Size Distribution
- 8-7.2 Mie versus Rayleigh
- 8-7.3 The Rayleigh Volume Extinction Coefficient
- 8-7.4 Cloud Attenuation Above 50 GHz
- 8-7.5 Volume Backscattering Coefficient
- 8-8 Extinction and Backscattering by Rain
- 8-8.1 Drop-Size Distribution
- 8-8.2 Volume Extinction Coefficient
- 8-8.3 Volume Backscattering Coefficient
- 8-9 Radar Equation for Meteorology
- 8-10 Emission by Clouds and Rain
- 8-11 Error Sources and Estimation
- 8-11.1 Error Sources and Estimation Statistics
- 8-11.2 Model Validation
- 8-11.3 The Curse of Remote Sensing
- Chapter 9 Radiometric Sounding of the Atmosphere
- 9-1 Atmospheric Weighting Function
- 9-1.1 Upward-Looking Temperature Weighting Function
- 9-1.2 Downward-Looking Temperature Weighting Function
- 9-2 Data Representation
- 9-2.1 Analysis of the Information Content of Atmospheric Sounding Data
- 9-2.2 Principal Components Analysis (PCA)
- 9-3 Inversion Techniques
- 9-3.1 General Formulation
- 9-3.2 Least-Squares Solution of the Ill-Posed Problem
- 9-3.3 Constrained Linear Inversion Method
- 9-3.4 Optimal Estimation Method
- 9-3.5 Statistical Inversion Method
- 9-3.6 Backus-Gilbert Synthetic-Averaging Inversion Method
- 9-3.7 Retrievals Based on Neural Networks
- 9-4 Temperature-Profile Retrieval from Ground-Based Observations
- 9-4.1 Single-Frequency Multiangle Observations
- 9-4.2 Multifrequency Single-Angle Observations
- 9-4.3 Pressure Height
- 9-5 Water-Vapor Profile Retrieval from Ground-Based Observations
- 9-6 Retrieval of Integrated Precipitable Water Vapor (IPWV) from Ground-Based Observations
- 9-7 Retrieval of Cloud Liquid-Water Path (LWP) from Ground-Based Observations
- 9-7.1 Physical Basis
- 9-7.2 Statistical Inversion
- 9-8 Estimation of Propagation Delay
- 9-9 Space-Based Atmospheric Sounding Radiometers
- 9-9.1 Vertical Shifting of the Weighting Functions
- 9-9.2 Swath Width
- 9-9.3 Cloud Sensitivity
- 9-9.4 Calibration
- 9-9.5 Modeling and Retrieval Algorithm Complexity
- 9-9.6 Compatibility with Other Sensors
- 9-10 Atmospheric Sounding by Downward-Looking Radiometers
- 9-10.1 Brightness Temperature
- 9-10.2 Examples of Retrieved Parameters
- 9-11 Atmospheric Limb Sounding
- 9-11.1 Fundamental Considerations
- 9-11.2 The NASA Aura Microwave Limb Sounder
- 9-12 Global Precipitation Mapping Using Atmospheric Sounding Observations
- 9-12.1 Physical Foundation: Attenuation and Scattering
- 9-12.2 Example: Precipitation Retrieval Using ATMS
- 9-13 GPS Radio Occultation
- Chapter 10 Surface-Scattering Models and Land Observations
- 10-1 The Role of Scattering Models
- 10-2 Surface Parameters
- 10-2.1 rms Height
- 10-2.2 Surface Correlation Length
- 10-2.3 rms Slope
- 10-2.4 Fresnel Reflection Coefficient
- 10-2.5 Smooth-Surface Criteria
- 10-3 Surface-Scattering Models
- 10-3.1 I2EM Parameters
- 10-3.2 Multiscale Surfaces
- 10-3.3 Role of Correlation Function
- 10-3.4 Role of rms Height
- 10-3.5 Role of Correlation Length
- 10-3.6 Role of Dielectric Constant
- 10-3.7 Role of Polarization Ratios
- 10-3.8 Comparison with Experimental Backscattering Measurements
- 10-3.9 Comparison with Experimental Bistatic Measurements
- 10-3.10 Applicability of Surface Scattering Models
- 10-4 Scattering by Random and Periodic Surfaces
- 10-4.1 Backscattering by Nonperiodic Random Surfaces
- 10-4.2 Backscattering by Periodic Surfaces
- 10-5 PRISM (Polarimetric Radar Inversion for Soil Moisture)
- 10-5.1 Co-Pol and Cross-Pol Ratios
- 10-5.2 PRISM-1
- 10-5.3 PRISM-2
- 10-6 SMART (Soil Moisture Assessment Radar Technique)
- 10-7 Model Comparisons
- 10-8 Concluding Observations
- Chapter 11 Volume-Scattering Models and Land Observations
- 11-1 Heuristic Single-Scattering Model for Vegetation
- 11-1.1 Direct Ground Contribution
- 11-1.2 Direct Volume Contribution-The Cloud Model
- 11-1.3 Canopy-Ground Contributions
- 11-1.4 Ground-Canopy-Ground Contribution
- 11-1.5 Single-Scattering Radiative Transfer Model
- 11-2 Isotropic and Rayleigh Scatterers
- 11-2.1 Canopy Elements as Isotropic Scatterers
- 11-2.2 Canopy Elements as Rayleigh Scatterers
- 11-3 Heuristic Single-Scattering Model for Snow-Covered Ground
- 11-4 Penetration Depth
- 11-5 Radiative Transfer Theory
- 11-5.1 Extinction Matrix
- 11-5.2 Phase Matrix
- 11-5.3 Scattering and Absorption Cross
- 11-5.4 Applicability Conditions
- 11-5.5 Phase Matrix of Simple Objects
- 11-5.6 Boundary Conditions for a Planar Interface
- 11-6 Iterative Solution of the Radiative Transfer Equation
- 11-6.1 Iterative-Solution Method
- 11-6.2 Upward- and Downward-Propagating Intensities
- 11-6.3 Zeroth-Order Solution
- 11-6.4 First-Order Solution
- 11-6.5 Rayleigh Scatterers
- 11-6.6 Distinct Upper Boundary
- 11-7 Approximate Form of S2RT/R Model
- 11-7.1 Applicability of the Single-Scattering Model
- 11-7.2 Comparison with Experimental Observations
- 11-8 Radar Observations of Vegetation Canopies
- 11-8.1 Penetration Depth in Soil
- 11-8.2 Propagation Properties of Cultural Vegetation
- 11-8.3 Extinction by a Canopy Containing Stalks
- 11-8.4 Role of Soil Surface Contribution
- 11-8.5 Relationship to Leaf-Area Index
- 11-8.6 Relationship to Canopy Water Content
- 11-9 Soil-Moisture Inversion Example
- 11-9.1 The Direct Model
- 11-9.2 The Inverse Model
- 11-10 Look-Direction Dependence
- 11-11 Effects of Dew, Wind, and Other Environmental Factors
- 11-12 Radar Backscattering from Tree Canopies
- 11-12.1 Propagation Properties of Forest Canopies
- 11-12.2 Angular and Frequency Response
- 11-12.3 MIMICS
- 11-12.4 Canopy Biophysical Parameters
- 11-12.5 Backscatter Response to Forest Parameters
- 11-12.6 Response at VHF-Band
- 11-12.7 Response at P- and L-Bands
- 11-13 SIR-C/X-SAR Case Study
- 11-13.1 Raco Supersite Description
- 11-13.2 Land-Cover Classification
- 11-13.3 Estimation of Forest Biophysical Parameters
- 11-14 Propagation Properties of Snow
- 11-14.1 Dry Snow
- 11-14.2 Wet Snow
- 11-15 Backscattering Behavior of Dry Snow
- 11-15.1 Radiative Transfer Model
- 11-15.2 Role of Snow-Ground Interface
- 11-15.3 Measuring Snow Thickness Over Sea Ice
- 11-16 Backscattering Behavior of Wet Snow
- 11-16.1 Angular Dependence
- 11-16.2 Frequency Dependence
- 11-16.3 Wetness Dependence
- 11-16.4 Diurnal Variations
- 11-16.5 Seasonal Variations
- 11-16.6 Millimeter-Wave Observations
- Chapter 12 Emission Models and Land Observations
- 12-1 Emissivity and Reflectivity
- 12-2 Emission by a Specular Surface
- 12-3 Rough-Surface Emissivity
- 12-3.1 I2EM
- 12-3.2 Semiempirical Models
- 12-3.3 Model Parameters at L-Band
- 12-3.4 Model Parameters at Other Frequencies
- 12-4 Emission by a Periodic Surface
- 12-5 Radiative Transfer Equation for Vegetation-Covered Ground
- 12-5.1 Scalar Radiative Transfer Equation
- 12-5.2 Boundary Conditions
- 12-5.3 Weakly Scattering Medium
- 12-6 ZRT Model for Layer with Distinct Upper Boundary
- 12-7 Applicability of the ZRT Vegetation Model
- 12-7.1 Model Behavior for Specular Soil Soil Surface
- 12-7.2 Model Behavior for Moderately Rough Soil Surface
- 12-7.3 Experimental Observations
- 12-7.4 Single-Scattering Albedo
- 12-7.5 Vegetation Optical Thickness
- 12-8 Estimation of Soil Moisture and Vegetation Water Content
- 12-8.1 Single-Channel Soil Moisture Retrieval
- 12-8.2 Multichannel Soil Moisture Retrieval
- 12-8.3 Change Detection
- 12-9 Operational Satellite Missions
- 12-9.1 Soil Moisture and Ocean Salinity (SMOS) Mission
- 12-9.2 Soil Moisture Active Passive (SMAP) Mission
- 12-10 Optical Depth and Emissivity of Forest Canopies
- 12-11 Emission by Snow-Covered Terrain
- 12-11.1 Radiative Transfer Models
- 12-11.2 Response of Dry Snow to Water Equivalent
- 12-11.3 Snow Classes
- 12-11.4 Snow Wetness
- 12-11.5 Diurnal Variations
- 12-11.6 Satellite Observations
- 12-12 Coherent and Incoherent Emissivities
- 12-12.1 Coherent Emissivity
- 12-12.2 Incoherent Emissivity
- 12-13 Microwave Emission by Lake Ice
- Chapter 13 Radar Measurements and Scatterometers
- 13-1 CW Radar
- 13-1.1 Target Stationary Relative to Radar
- 13-1.2 Signal Scintillation
- 13-1.3 Target Moving Relative to Radar
- 13-2 Pulsed Radar
- 13-3 Range and Doppler Resolution
- 13-4 Frequency-Modulated Radar
- 13-5 Matched Filtering
- 13-6 Pulsed-FM Radar
- 13-7 Pulsed Radar, General Modulation
- 13-8 Measurement Precision
- 13-8.1 Effective Number of Samples
- 13-8.2 Radiometric Precision
- 13-9 Ambiguities in Radar
- 13-9.1 Range Ambiguity
- 13-9.2 Speed Ambiguity
- 13-9.3 Radar Ambiguity Function
- 13-10 Radar Calibration
- 13-10.1 Internal Calibration
- 13-10.2 External Calibration
- 13-10.3 Measurement Precision
- 13-11 Passive Calibration Targets
- 13-11.1 Flat Rectangular Plate
- 13-11.2 Flat Circular Plate
- 13-11.3 Sphere
- 13-11.4 Corner Reflector
- 13-11.5 Luneburg-Lens Reflector
- 13-11.6 Comparison of Calibration Targets
- 13-12 Active Radar Calibrators (ARCs)
- 13-13 Polarimetric Active Radar Calibrator
- 13-14 Polarimetric Scatterometers
- 13-14.1 Network Analyzer Principles of Operation
- 13-14.2 Network Analyzer Operation as a Scatterometer
- 13-14.3 Microwave Polarimetric Scatterometers
- 13-15 Calibration of Polarimetric Radars
- 13-15.1 System Distortion Matrices
- 13-15.2 Distortionless Antennas
- 13-15.3 Reciprocal Distortion Matrices
- 13-15.4 Matrix Inversion
- 13-15.5 Antennas with Diagonal Distortion Matrices
- 13-15.6 Nonreciprocal Systems with Full Distortion Matrices
- 13-16 GNSS-R Bistatic Radar
- 13-16.1 The Delay Doppler Map
- 13-16.2 The Cyclone Global Navigation Satellite System (CYGNSS)
- Chapter 14 Real- and Synthetic-Aperture Side-Looking Airborne Radar
- 14-1 Introduction
- 14-2 Real-Aperture SLAR
- 14-2.1 SLAR Resolution
- 14-2.2 The SLAR Radar Equation
- 14-2.3 SLAR Systems
- 14-3 Synthetic-Aperture Radar (SAR)
- 14-3.1 Ways to Consider SAR
- 14-3.2 Synthesized Aperture
- 14-3.3 Doppler Beam-Sharpening Approach
- 14-3.4 Correlation or Matched Filtering with Reference Point-Target Response
- 14-3.5 Dechirping Comparable with Range Pulse-Compression Dechirping
- 14-3.6 Optical-Focusing Equivalent of SAR
- 14-4 SAR Resolution
- 14-4.1 Synthesized-Aperture Point of View
- 14-4.2 Unfocused SAR
- 14-4.3 Doppler Point of View
- 14-4.4 Comparison of Real-Aperture and Synthetic-Aperture Resolution
- 14-5 Ambiguity Considerations in SAR
- 14-5.1 Scanning Synthetic-Aperture Radar
- 14-5.2 Other SAR Observation Geometries
- 14-6 SAR Power Considerations
- 14-6.1 SAR SNR Equation
- 14-6.2 Radiometric Resolution
- 14-7 SAR System Configurations
- 14-8 Speckle in Radar Images
- 14-8.1 Speckle in SLAR Images
- 14-8.2 Speckle in SAR Images
- 14-9 Introduction to SAR Processing
- 14-9.1 SAR Signal Spectra
- 14-9.2 Range Migration
- 14-9.3 Depth of Focus
- 14-9.4 SAR Image Processing: The Range-Doppler Algorithm
- 14-9.5 SAR Image Processing: the Backprojection Algorithm
- 14-10 Geometric Distortion in Radar Images
- 14-10.1 Elevation Distortion
- 14-10.2 Range Distortion
- 14-10.3 SLAR Motion Distortion
- 14-10.4 SAR Motion Errors
- 14-10.5 SAR Attitude Errors
- 14-11 Elevations from SLAR and SAR
- 14-11.1 Shadows
- 14-11.2 Stereo with Radar
- 14-11.3 Squint Stereo
- 14-11.4 Mountains and Buildings
- 14-12 Ionospheric Effects
- 14-12.1 Rotation Angle
- 14-12.2 Impact on SAR Data
- 14-12.3 Impact on Radiometric Data
- Chapter 15 Interferometric Synthetic-Aperture Radar
- 15-1 Brief History of Radar
- 15-2 2-D versus 3-D Measurements
- 15-2.1 Interferometric Phase
- 15-2.2 Height Measurement Precision
- 15-2.3 The Role of SNR
- 15-3 Cartographic Corrections
- 15-4 Forming the Radar Interferogram
- 15-4.1 Displacement versus Range
- 15-4.2 Offset Determination
- 15-4.3 Multilooking
- 15-4.4 Correlation
- 15-5 Decorrelation
- 15-5.1 Speckle
- 15-5.2 Decorrelation Model
- 15-5.3 Calculation of Spatial Baseline Decorrelation
- 15-5.4 Rotational Decorrelation
- 15-5.5 Temporal Decorrelation
- 15-6 Measurement of Topography
- 15-6.1 Inferring Topography from Interferometric Phase
- 15-6.2 Phase Unwrapping
- 15-6.3 Curved-Earth Phase Pattern
- 15-7 Mapping Earth's Topography: The SRTM Mission
- 15-8 Along-Track Interferometry
- 15-8.1 Temporal Baseline
- 15-8.2 Ocean Currents
- 15-9 Measuring Surface Deformation
- 15-10 Worldwide Dual Satellite InSAR Coverage: The TanDEM-X Mission
- 15-11 Time-Series InSAR Applications
- 15-11.1 Stacking
- 15-11.2 Small Baseline Subset Analysis (SBAS)
- 15-11.3 Persistent Scattering (PS)
- Chapter 16 Radar Remote Sensing of the Ocean
- 16-1 Wind-Vector Scatterometry
- 16-2 Wind and Wave Modeling
- 16-2.1 Wind
- 16-2.2 Waves
- 16-3 Radar Scattering
- 16-3.1 Ocean Surface Statistics
- 16-3.2 IEM Scattering Model
- 16-3.3 Comparison with Measurements
- 16-3.4 Empirical Fits for IEM Parameters
- 16-3.5 The Wind Geophysical Model Function
- 16-4 Rain
- 16-4.1 Modeling the Surface Effects of Rain
- 16-4.2 Perturbation Model Regimes
- 16-5 Wind Scatterometers
- 16-5.1 Scatterometer Viewing Geometry
- 16-5.2 Fan-Beam Wind Scatterometers
- 16-6 Measurement Precision
- 16-6.1 Doppler-Filtering Scatterometers
- 16-6.2 Range-ResolutionWind Scatterometers
- 16-7 Scanning Pencil-Beam Wind Scatterometers
- 16-7.1 Scanning Loss
- 16-7.2 Measurement Precision
- 16-7.3 Dealing with Rain
- 16-8 Wind-Vector Retrieval
- 16-8.1 Noise-Free Retrieval Algorithm
- 16-8.2 Retrieval in the Presence of Noise
- 16-9 SAR Imaging of OceanWinds
- 16-10 Properties of Sea Ice
- 16-10.1 The Nature of Sea Ice
- 16-10.2 Physical Properties
- 16-10.3 Penetration Depth in Sea Ice
- 16-11 Sea-Ice Radar Scattering
- 16-11.1 Ocean versus Sea-Ice Discrimination
- 16-11.2 Discriminating between Different Ice Types
- 16-11.3 Measuring Ice Thickness
- 16-11.4 Snow on Sea Ice
- 16-11.5 Scatterometer Mapping of Sea-Ice Extent
- 16-11.6 Scatterometer Mapping of Sea-Ice Type
- 16-12 Radar Imaging of Sea Ice
- 16-13 Iceberg Tracking
- 16-14 Radar Detection of Oil Spills
- 16-14.1 SAR Observation of Oil Slicks
- 16-14.2 Scatterometer Observation of Oil Slicks
- Chapter 17 Spaceborne Altimetry
- 17-1 Introduction
- 17-2 Signal Modeling
- 17-2.1 Ocean Surface Signal Model
- 17-2.2 Land-Surface Signal Modeling
- 17-3 Height Estimation Errors and Corrections
- 17-3.1 Precision Orbit Determination
- 17-3.2 Atmospheric Effects
- 17-3.3 Sea-State and EM Bias
- 17-3.4 Significant Wave Height
- 17-3.5 Wind Speed
- 17-3.6 Topography
- 17-3.7 Bathymetry
- 17-4 Practical Sensor Considerations
- 17-4.1 Range Compression and Deramping
- 17-4.2 Range Tracking
- 17-4.3 Orbit Considerations
- 17-5 Synthetic-Aperture Altimetry
- 17-6 Wide-Swath or Imaging Altimetry
- 17-7 CryoSat-2 Mission
- Chapter 18 Radiometric Remote Sensing of the Ocean
- 18-1 Brightness Temperature of the Sea Surface
- 18-1.1 Spectral Sensitivity
- 18-1.2 Brightness Temperature of a Smooth Surface
- 18-1.3 Penetration Depth in Sea Water
- 18-2 Measurement of Sea-Surface Temperature and Salinity
- 18-2.1 Sensitivity Analysis for Salinity
- 18-2.2 Sensitivity Analysis for Sea-Surface Temperature
- 18-2.3 Satellite Measurement of SST
- 18-2.4 Satellite Measurement of SSS
- 18-3 Measurement of Near-Surface Wind Vector
- 18-3.1 Azimuth Variation
- 18-3.2 Wind-Speed Dependence
- 18-3.3 WindSat Retrieval Algorithm
- 18-4 Mapping Sea-Ice Type and Concentration
- 18-4.1 Coherent versus Incoherent Emissivity
- 18-4.2 Aircraft Observations
- 18-4.3 Models for the Emissivity of Sea Ice
- 18-4.4 Satellite Observations
- 18-4.5 Sea-Ice Algorithms
- 18-5 Oil-Slick Detection
- 18-5.1 Emissivity of an Oil-CoveredWater Surface
- 18-5.2 Airborne Observations
- Appendix A
- Appendix B
- Appendix C
- Appendix D
- Bibliography
- Index
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