'Mie scattering' diaporamas de présentation

Upcoming Deadlines

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Interaction Between Radiation and the Material

Interaction Between Radiation and the Material. Prof. Arnon Karnieli The Remote Sensing Laboratory Jacob Blaustein Institute for Desert Research Ben-Gurion University of the Negev Sede-Boker Campus 84990, ISRAEL. Radiation Interaction with a Matter. Transmission.

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Radiation Laws Scattering Absorption Radiation Windows Reflectance Terrain-Energy Interactions For Monday: Read Chapter

Radiation Laws Scattering Absorption Radiation Windows Reflectance Terrain-Energy Interactions For Monday: Read Chapter 3. Electromagnetic Radiation II. http://www.crh.noaa.gov/news/display_cmsstory.php?wfo=mqt&storyid=99827&source=0. Stephan Boltzmann Law.

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Techniques for Determining PSD of PM: Laser Diffraction vs . Electrical Sensing Zone

Techniques for Determining PSD of PM: Laser Diffraction vs . Electrical Sensing Zone. A 242 nd ACS National Meeting Presentation: Paper ID18440. Z. Cao 1 , M. Buser 2 , D. Whitelock 3 , L. Wang-Li* 1 , Y. Zhang 4 , C.B. Parnell 5 1 NCSU, 2 OSU, 3 USDA-ARS, 4 UIUC, 5 TAMU. Introduction:.

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Geant4 Milagro Simulation

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Scattering

Scattering. Types of Scattering in the Atmosphere. Rayleigh Mie Geometric. Rayleigh Scattering in Visible Spectrum. Blue sky Red Sunset Blue water (from underwater). Rayleigh Scattering. Wavelength of light is much larger than scattering particles

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Remote Sensing Part 2

Remote Sensing Part 2. Atmospheric Interactions & Pre-processing. Review : Color Theory. red(255) + green (255) + blue (255) = white red(0) + green (95) + blue (0) = dark green red(255) + green (0) + blue (255) = purple red(0) + green (255) + blue (255) = cyan

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Inelastic Scattering

Inelastic Scattering. Raman. Compton. Acoustic Mode Scattering. Bragg and Brillouin. Why the sky is blue?. Rayleigh Scattering.

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Visualizing the Traversal of Charged Particles in a Diffusion Cloud Chamber

Visualizing the Traversal of Charged Particles in a Diffusion Cloud Chamber . Liquid Vs. Gases Intermolecular Forces Vapor Pressure. The Basics. Ionization Energy Temperature Condensation Ideal Gas Law. The Cloud Chamber?.

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Remote sensing/digital image processing

Remote sensing/digital image processing. Color Arithmetic. red + green = yellow green + blue = cyan red + blue = magenta. Image Display. Example color combinations red(255) + green (255) + blue (255) = white red(0) + green (95) + blue (0) = dark green

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Remote sensing/digital image processing

Remote sensing/digital image processing. Color Arithmetic. red + green = yellow green + blue = cyan red + blue = magenta. Image Display. Example color combinations red(255) + green (255) + blue (255) = white red(0) + green (95) + blue (0) = dark green

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Cloud Radar in Space: CloudSat

Cloud Radar in Space: CloudSat While TRMM has been a successful precipitation radar, its 17-18 dBZ minimum detectable signal does not allow views of light precipitation and/or clouds (except some anvils) due to wavelength and sensitivity

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EE 230: Optical Fiber Communication Lecture 5

EE 230: Optical Fiber Communication Lecture 5. Attenuation in Optical Fibers. From the movie Warriors of the Net. Attenuation/Loss In Optical Fibers. Mechanisms: Bending loss Absorption Scattering loss dBm refers to a ratio with respect to a signal of 1 mW. Bending Loss.

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Electromagnetic radiation : Interaction with matter and atmosphere

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Signal Degradation in Optical Fibers

Signal Degradation in Optical Fibers. Signal Attenuation & Distortion in Optical Fibers . Signal attenuation (fiber loss) largely determines the maximum repeaterless separation between optical transmitter & receiver.

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Acceptance and Counting Rates of EUSO

Acceptance and Counting Rates of EUSO. Detecting UHECR from space The EUSO detector : Who does what. Some characteristics of UHECR A statistical view of clouds A first approach of the acceptance The influence of clouds on the signal The different Atmosphere Sounding Devices

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Cloud liquid water and ice content by multi-wavelength radar Nicolas Gaussiat Henri Sauvageot

Cloud liquid water and ice content by multi-wavelength radar Nicolas Gaussiat Henri Sauvageot Anthony J. Illingworth. Dual-Wavelength measurements. For a dual-wavelength pair ( Long, Short) :. DWR is due to (1) differential attenuation , (2) Mie scattering :.

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Light Scattering

Light Scattering. Rayleigh Scattering & Mie Scattering. What is Scattering?. Process by which particles suspended in a medium of a different index of refraction diffuse a portion of the incident radiation in all directions

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Scattering and reflection

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