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OverviewFull Product DetailsAuthor: V.E. Zuev , Yu.F. Arshinov , A.A. Zemlyanov , Yu.D. KopytinPublisher: Springer Imprint: Kluwer Academic Publishers Edition: 1985 ed. Volume: 4 Dimensions: Width: 15.50cm , Height: 1.90cm , Length: 23.50cm Weight: 1.360kg ISBN: 9789027717368ISBN 10: 9027717362 Pages: 292 Publication Date: 30 June 1985 Audience: College/higher education , Professional and scholarly , Postgraduate, Research & Scholarly , Professional & Vocational Format: Hardback Publisher's Status: Active Availability: In Print This item will be ordered in for you from one of our suppliers. Upon receipt, we will promptly dispatch it out to you. For in store availability, please contact us. Table of Contents1: Microphysical and Optical Characteristics of Atmospheric Aerosols.- 1.1. Introduction.- 1.2. Preliminary Discussion.- 1.3. Light Scattering by Clouds and Fogs.- 1.4. Light Scattering by Hazes.- 1.5. Microphysical and Optical Characteristics of Precipitation.- 1.6. Scattering Phase Functions of Polydispersed Aerosols.- References: Chapter 1.- 2: Low-Energy (Subexplosive) Effects of Radiation on Individual Particles.- 2.1. Regular Regimes of Droplet Vaporization in the Radiation Field.- 2.2. Vaporization of Haze Particles Consisting of a Solid Nucleus and a Shell of Salt in Solution.- 2.3. Some Peculiarities in the Vaporization of Solid Aerosol Particles by High-Power Radiation.- 2.4. Burning of Carbon Aerosol Particles in a Laser Beam.- 2.5. Initiation of Droplet Surface Vibrations by Laser Radiation.- References: Chapter 2.- 3: The Formation of Clear Zones in Clouds and Fogs Due to the Vaporization of Droplets under Regular Regimes.- 3.1. Basic Characteristics of the Process of Clearing a ‘Frozen’ Cloud.- 3.2. Stationary Cleared Channels in Moving Clouds.- 3.3. The Unstable Regime of Moving Cloud Clearance.- 3.4. The Determination of the Parameters of the Cleared Zone Taking into Account the Angular Beam Width and Wind Speed.- 3.5. The Generalized Formula Describing the Beam Intensity in the Process of Beam-Induced Clearing.- 3.6. The Cleared Channel under Conditions of Turbulent Aerosol Transport.- 3.7. Nonlinear Extinction Coefficient of Aerosols.- 3.8. The Investigation of Beam-Induced Clearing of Natural Fogs.- References: Chapter 3.- 4: Self-Action of a Wave Beam in a Water Aerosol under Conditions of Regular Droplet Vaporization.- 4.1. Basic Equations of Wave Beam Self-action in a Discrete Scattering Medium.- 4.2. The Field of the Effective ComplexDielectric Constant of the Aerosol (within the Beam).- 4.3. Description of the Mean Intensity of a Beam.- 4.4. The Influence of Thermal Distortions of Wave Beams and Fluctuations of the Medium on the Beam-Induced Dissipation of Water Aerosols.- References: Chapter 4.- 5: Laser Beam Propagation through an Explosively Evaporating Water-Droplet Aerosol.- 5.1. Droplet Explosion Initiated by High-Power Laser Radiation.- 5.2. Droplet Explosion Regimes.- 5.3. Attenuation of Light by an Exploding Droplet.- References: Chapter 5.- 6: Propagation of High-Power Laser Radiation through Hazes.- 6.1. Nonlinear Optical Effects in Hazes: Classification and Features.- 6.2. Nonlinear Scattering of Light by Thermal Aureoles around Light-Absorbing Particles.- 6.3. Thermal Self-Action of a High-Power Laser Pulse Propagating through Dusty Hazes.- 6.4. Laser Radiation Transfer in Combustible Aerosols.- 6.5. Thermal Blooming of the cw and Quasi-cw Laser Beams due to Light Absorption by Atmospheric Aerosols and Gases.- References: Chapter 6.- 7: Ionization and Optical Breakdown in Aerosol Media.- 7.1. Physical and Mathematical Formulations of the Problem.- 7.2. Theoretical Analysis of Pulsed Optical Breakdown on Solid Aerosol Particles.- 7.3. The Influence of Atmospheric Turbulence on the Concentration of Optical Breakdown Centers.- 7.4. Laboratory Experiments on Laser Sparking.- 7.5. Optical Breakdown of Water Aerosols.- 7.6. Field Experiments on the Nonlinear Energetic Attenuation of Pulsed CO2-Laser Radiation during the Optical Breakdown of the Atmosphere.- References: Chapter 7.- 8: Laser Monitoring of a Turbid Atmosphere Using Nonlinear Effects.- 8.1. Brief Description of the Problem.- 8.2. Distortions of Lidar Returns caused by the Nonlinear Effects of the Interaction of High-Power LaserRadiation with Aerosols.- 8.3. An Analysis of the Criteria for Detecting a High-Power Laser Beam in Fog when the Beam Power is Sufficient to Dissipate the Fog.- 8.4. Remote Spectrochemical Analysis of Aerosol Composition using the Emission and Luminescent Spectra Induced by High-Power Laser Beams.- 8.5. An Analysis of the Possibilities of Sensing the High-Power Laser Beam Channel using Opto-Acoustic Techniques.- References: Chapter 8.- Index of Subjects.ReviewsAuthor InformationTab Content 6Author Website:Countries AvailableAll regions |