Calibrating for Light backscatter from fractal aggregates

Slides:



Advertisements
Similar presentations
1 Outline Basic Idea Simple Theory Design Points Calibration of Forces Selected Biological Applications.
Advertisements

Polarization measurements for CLARREO
Ashida lab Toyota yusuke
Physical Pharmacy 21 Particle Size Sizing Technique 3: Laser Diffraction Photon Correlation Spectroscopy Kausar Ahmad Kulliyyah of Pharmacy, IIUM
Size dependence of dipole and quadrupole plasmon resonances of light-induced sodium clusters Anastasiya Derkachova, Krystyna Kolwas Institute of Physics,
Preliminary Results of Laser Ranging to Un-cooperative Targets at Shanghai SLR Station Yang FuMin, Zhang ZhongPing, Chen JuPing, Chen WanZhen, Wu ZhiBo,
Chapter 3 – Energy Balance and Temperature. The Fate of Solar Radiation We owe it all to the sun… 3 things can happen to solar (and all) radiation: 1)
Nanoparticle Optics Lab Part II Light Scattering.
Instructor: Lichuan Gui
HFT 405, nm 405nm 488nm 405nm Only 405 and 488 are reflected All other wavelengths are transmitted 488nm 405nm This is the first beam splitter that.
Optical Diagnostics Hg_jet_meeting, Thomas Tsang tight environment high radiation area non-serviceable area passive components optics only, no.
Optical Alignment with Computer Generated Holograms
Work Package 2 – Overview of instrumentation, data gathering and calibration issues Lidar Calibration Ewan O’Connor, Anthony Illingworth and Robin Hogan.
Vijay Natraj Ge152 February 9, 2007 Light Scattering.
LASERS - PARTICLE SIZE ANALYSIS
1 Laser Remote Sensing Optical Receiver & Detection System Laser Probe Gas R = Velocity  time R There can be: absorption, scatter and/ or fluorescence.
Optical Diagnostics Thomas Tsang tight environment high radiation area non-serviceable area passive components optics only, no active electronics back.
Climate Change Graphs. Activity You and your partner will receive a graph from the IPCC (Intergovernmental Panel on Climate Change). You will analyze.
Status of IPBSM Improvement N. Terunuma, KEK 2012/July/13 ATF2 Weekly Meeting.
Rayleigh Scattering & Mie Scattering
Single-Scattering Stuff + petty chap 12 intro April 27-29, 2015.
Lidar remote sensing for the characterization of the atmospheric aerosol on local and large spatial scale.
Project Overview Laser Spectroscopy Group A. A. Ruth Department of Physics, University College Cork, Cork, Ireland.
Rayleigh and Mie Scattering
Particle Scattering Single Dipole scattering (‘tiny’ particles)
Wenbo Sun, Bruce Wielicki, David Young, and Constantine Lukashin 1.Introduction 2.Objective 3.Effect of anisotropic air molecules on radiation polarization.
Sea Ice Yearly Minimums in the Arctic from
MT Workshop October 2005 JUNE 2004 DECEMBER 2004 End of OCTOBER 2005 ? MAY 2002 ? Capabilities of multi-angle polarization cloud measurements from.
Dispersive spectrometers measure transmission as a function of frequency (wavelength) - sequentially--same as typical CD Interferometric spectrometers.
Climate Change 101. What Is Climate? What Is the Greenhouse Effect?
SCM 330 Ocean Discovery through Technology Area F GE.
Turbidity Measurement By Douglas Rittmann, Ph.D., P.E. Water/Wastewater Consultant To UTEP Laboratory Course On February 21, 2006.
Optical methods for in-situ particle sizing
1 Atmospheric Radiation – Lecture 18 PHY Lecture 18 Radiation and Climate.
Second Harmonic (SH) Radiation from Twined ZnO Single Nanorods (NR) in Transmission Geometry. Presented by: Aaron Ricca Dr. S. W. Liu.
When light passes from vacuum (index of refraction n = 1) into water (n = 1.333), Q the wavelength increases and the frequency is unchanged 2. the.
Congresso del Dipartimento di Fisica Highlights in Physics –14 October 2005, Dipartimento di Fisica, Università di Milano An application of the.
Aerosol Limits for Target Tracking Ronald Petzoldt ARIES IFE Meeting, Madison, WI April 22-23, 2002.
Rain Detection & Attenuation for Remote sensing; & auxiliary sensors
MICROSCOPE DESIGN. beam expander and objective Why do we need a beam expander? What facts about the laser do we need to know? How much expansion do we.
1 Objective Finish with PM measurements Discuss Friday’s filed measurements 1.
Ceilometer absolute calibration to calculate aerosol extensive properties Giovanni Martucci Alexander Marc de Huu Martin Tschannen.
Optical Diagnostics Thomas Tsang tight environment high radiation area non-serviceable area passive components optics only, no active electronics transmit.
METR Advanced Atmospheric Radiation Dave Turner Lecture 4.
Summer '07 at CLS Small Angle X-Ray Scattering Peter ChenChithra Karunakaran & Konstantine Kaznatcheev.
ce/features/earth/climate/en/challenge/index. htm?width=835&height=680&popup=true.
Date of download: 6/1/2016 Copyright © 2016 SPIE. All rights reserved. (a) Vision of the Brillouin lidar operated from a helicopter. The center ray represents.
WEEK #2 Physics-II (Ph-1002) Dispersion Polarization
Nuclear Chemistry/Solar Neutrino Group
Good Luck! Final Exam Review Phys 222 – Supplemental Instruction
Suspended Nanomaterials
The Multisensor Camera
SFB 641 The SFB Laboratory contributes 2 different techniques for the measurements of ice nuclei to VI Aerosol-Cloud Interaction: 1. in situ-measurements.
Date of download: 1/9/2018 Copyright © ASME. All rights reserved.
Volume 126, Issue 4, Pages (April 2004)
transmitted radiation
Measurements from Viktor Mechanics from Richard Model from Fabian
L 32 Light and Optics [2] Measurements of the speed of light 
عنوان: روش پراکندگی نور دینامیکی برای مطالعه اندازه نانوذرات
Gel time of different volume fractions of polystyrene particles
Optical measurement.
Complex Nanophotonics
24-8 Interference by Thin Films
Temperature and CO2 Trends.
q q A B R O F f Refractive spherical surface Index n q/n b b = q - q/n
L 32 Light and Optics [2] Measurements of the speed of light 
CALIPSO First-Light Observations – All 3 Lidar Channels
Polarizing Beamsplitter
Volume 126, Issue 4, Pages (April 2004)
Meteorological Instrumentation and Observations
Presentation transcript:

Calibrating for Light backscatter from fractal aggregates

Why? [1]

Spherical Liquid Water Droplet Aerosol (m=1.33) The source Spherical Liquid Water Droplet Aerosol (m=1.33)

Backscatter Setup CCD Detector Laser (λ= 633nm) Aerosol Target Beam splitter Beam Dump

Results Intensity (arbitrary units) Angle (˚)

Sizing: forward scattering Mie ripples, but polydispersity wipes them out Guinier regime: θ~λ/(πd) CCD Detector Laser (λ= 633nm) Mirror Aerosol Target Lens Polarizers Iris

Results

Final Results Backscatter suggests smaller size: ~1.5µm Forward scattering suggests bigger size: ~6µm DLS suggests mid-range size: ~2.5-4µm Very likely polydisperse. Backscatter apparatus likely works, but needs more testing.

Reference [1]"Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, 2007." IPCC - Intergovernmental Panel on Climate Change. Ed. S. Soloman, D. Qin, M.Manning, and Z. Chen. Internation Panel on Climate Change. Web. 09 Nov. 2011.